DEPARTMENT OF THE INTERIOR

UNITED STATES GEOLOGICAL SURVEY

GEORGE OTIS SMITH, DIRECTOR

1 BULLETIN 523

NITRATE DEPOSITS

BY

HOYT S. GALE

WASHINGTON

GOVERNMENT PRINTING OFFICE 

1912

CONTENTS.

Page.

Introduction............................................................... 5

Chilean nitrate deposits................................................. 5

Imports of nitrates..................................................... 6

Mineralogy of the nitrates............................................... 6

Uses of sodium and potassium nitrates................................... 8

Deposits of nitrate salljs...................................................... 9

General nature........................................................ 9

Cave niter............................................................ 9

Source of data.......................................................... 9

Review of occurrences................................................. 10

Eastern United States.............................................. 10

Wyoming......................................................... 12

Colorado........................................................... 14

Idaho............................................................ 15

Utah............................................................. 16

Miscellaneous occurrences....................................... 16

Greenwich Canyon, Grass Valley............................... 16

Oregon............................................................ 19

Nevada........................................................... 19

Nitrate salts near Lovelock...................................... 19

Potassium nitrate north of Gerlach............................... 23

Niter salts near Railroad Valley................................ 25

California........................................................ 25

. Arizona........................................................... 27

New Mexico....................................................... 28

Texas............................................................ 28

British Columbia. ................................................... 29

Nitrate specimens in the National Museum.................................. 29

Origin of nitrate salts....................................................... 29

Primary source........................................................ 29

Occurrence in soils..........................................".......... 30

Hypotheses of origin................................................... 30

The process of nitrification............................................. 31

Summary.............................................................. 35

Value of the deposits....................................................... 35

ILLUSTRATIONS.

Page. 

PLATE I. Map showing distribution of niter claims near Lovelock, Nev..... 20

II. Niter claims north of Gerlach, in the northern Granite Range, Washoe

County, Nev.: A, Upper claims; B, Lower claims............... 24

FIGURE 1. Map showing location of niter deposits and prospects in Greenwich

Canyon, near Grass Valley, Piute County, Utah................ 17

2. Map showing location of upper and lower groups of niter claims near

Gerlach, Washoe County, Nev.................................. 23

3

NITRATE DEPOSITS.

By HOYT S. GALE.

INTRODUCTION.

CHILEAN NITRATE DEPOSITS.

Dana says, ;< The nitrates, being largely soluble in water, play but 

an unimportant r61e in mineralogy." However, some immense deposits, said to be the largest in the world, occur in northern Chile, 

in the deserts of Atacama and Tarapaca. No attempt will be made 

here to describe or review these, as the literature contains many 

accounts of them, some of which are listed below:

Forbes, D., On the geology of Bolivia and southern Peru: Quart. Jour. Geol. Soc. 

1 London, vol. 17, 1861, pp. 7-62. 

L'Olivier, V., Le nitrate de soude dans l'Am6rique du sud: Annales chim. phys.,

5th ser., vol. 7, 1876, p. 289.

Flagg, J. W., Nitrate of soda, its locality, mode of occurrence, and methods of extraction: Am. Chemist, vol. 4, 1874, pp. 403^08.

Pissis, A., Nitrate and guano deposits in the Desert of Atacama, London, 1878, published by authority of the Chilean Government. 

Muntz, M. A., Recherches sur la formation des gisements de nitrate de soude: Compt.

Bend. Acad. Sci., vol. 101, 1885, p. 1265. 

Ochsenius, C., Einige Angaben iiber die Natronsaltpeter-Lager landeinwarts von

Taltal in der chilenischen Provinz Atacama-: Zeitschr. Deutsch. geol. Gesell., 1888,

pp. 153-165. 

Abercromby, Ralph, Nitrate of soda and the nitrate country: Nature, vol. 40, 1889,

p. 186. 

Buchanah, J., The extraction of nitrate of sodium and iodine in northern Chile:

Jour. Soc. Chem. Ind., vol. 12, 1893, p. 128.

Newton, William, The origin of nitrate in Chile: Geol. Magazine, vol. 3, 1896, p. 339. 

Darapsky,°L., Das Departement Taltal (Chile), Berlin, 1900. 

Semper and Michels, Die Salpeterindustrie Chiles: Zeitschr. f. Berg-, Hiitten-, u.

Salinenwesen preuss. St., 1904, pp. 359-482. 

Simmersbach, B., and Mayr, F., Die chilenische salpeterindustrie: Zeitschr. prakt.

Geologic, 1904, pp. 273-277. 

Penrose, R. A. F., jr., The nitrate deposits of Chile: Jour. Geology, vol. 18, 1910,

pp. 1-32. 

Clarke, F. W., The data of geochemistry, 2d ed.: Bull. U. S. Geol. Survey No. 491,

pp. 242-246, 1911. 

Newsom, J. F., Chilean nitrate deposits: Bull. Min. and Met. Soc. America No. 46,

March 30, 1912, vol. 5, No. 3, pp. 56-61.

5
6 NITEATE DEPOSITS.

IMPORTS OF NITRATES.

The most important of the nitrate salts commercially are sodium 

nitrate (cubic niter) and potassium nitrate (niter or saltpeter). 

These salts are largely utilized in this country, as is shown by the 

statistics of imports. Nearly all the nitrates imported come from 

Chile. The domestic production, if there is any, is insignificant.

The following statement of the imports for the year 1911 is supplied by the Bureau of Statistics, Department of Commerce and 

Labor:

Imports of nitrates, 1911.

Quantity.

7,944,757

7?7.,486

544,532

Value.

§265,061

. 37,739

16,814,268

The foregoing figures include nitrates imported "for consumption/' 

and do not quite agree with the statement contained in the following 

table, which includes all nitrates imported. The difference may 

represent material held over in warehouses from a preceding or to a 

succeeding year.

Imports oj'nitrate of'potash and nitrate of'soda into the United States from foreign countries 

during-the year ending Dec. 81, 1911.

Country.

Canada..... . ...........................................

Chile...................................................

Nitrate of potash or 

crude saltpeter.

Quantity.

Pounds. 

22,046

7,923,701

7,945,747

Value.

8367

264,694

265,061

Nitrate of soda.

Quantity.

Tons. 

101

9,323 

535, 454

544,878

Value.

S4,508 

J 

418,600 

16,391,147

16,814,256

' MINERALOGY OF THE NITRATES.

The nitrates known to occur in nature are as follows: 1

1. Soda niter (nitrate of soda, cubic niter)... .NaN03

2. Niter (nitrate of potash, saltpeter).......... KN03

3. Nitrocalcite............................. .Ca(N03 )2 +nH20

4. Nitromagnesite.............................Mg(N03 )2 +nH20

5. Nitrobarite................................Ba(N03 )2

6. Gerhardtite..............................Cu4 (OH)R(N03 )2

7. Darapskite............................... .NaN03 .Na2S04 +H2O

8. Nitroglauberite........................... 6NaN03 .2Na2S04+3H20

i Dana, E. S., System of mineralogy, 6th ed., 1892, pp. 870-873.
MINEEALOGY. 7

1. Soda niter, or nitrate of soda (cubic niter), in natural form has 

the same crystalline form and cleavage as calcite; that is, it is 

rhombohedral. Composition, NaN03 = nitrogen pentoxide 63.5, soda 

36.5. Peflagrates on charcoal with less violence than niter, causing a 

yellow light. Colors the flame intensely yellow. Is also deliquescent. 

The pure salt forms transparent, colorless, anhydrous rhombohedra, 

whose angles closely approximate to right angles, whence its name 

"cubic niter." It is very soluble in water, and its solubility increases 

much with increase of temperature, 100 .parts of water dissolving 

about 70 parts at 0° C. to about 80 parts at 15° and 125 parts at 

68° C. .

2. Niter, or potassium nitrate (saltpeter), in crystalline form is 

orthorhombic. Composition, KN03 = nitrogen pentoxide 53.5, potash 

46.5 = 100. Occurs naturally as thin white granular crusts or masses 

or in minute needle-form crystals, and as a thin coating on earth, walls, 

arid rocks. Is a transparent crystalline salt with a cooling, rather 

sharp, saline taste. Deflagrates strongly when thrown on burning 

coals. Imparts a strong violet color to the flame when color is not 

masked by the presence of much sodium. Dissolves readily in water 

and is not altered by exposure.

3. Nitrocalcite, or nitrate of lime (calcium nitrate), occurs in nature in efflorescent silken white or gray tufts and masses and has 

a sharp and bitter taste. Composition (hydrous calcium nitrate), 

Ca(NOg ) 2 + nH20. On burning coals it slowly fuses with a slight detonation and dries. It is very deliquescent before but not after being 

desiccated by heat. It occurs in Kentucky in limestone caverns; 

also in Arizona, and doubtless in many other localities.

4. Nitromagnesite, or nitrate of magnesia, is described as a white 

salt occurring in efflorescences and having a bitter taste. Composition (hydrous magnesium nitrate), Mg(N03 ) 2 + nH20. It is reported 

to be found in limestone caverns along with nitrocalcite, but its 

existence as a natural product has not been definitely determined.

5. Nitrobarite, or barium nitrate, occurs hi colorless crystals, in 

part covered with a thin brownish-black coating, resembling wad. 

Composition, Ba(N03 ) 2 = nitrogen pentoxide 41.4, baryta 58.6 = 100. 

It is reported from Chile.

6. Gerhardtite is a basic cupric nitrate, with the composition 

Cu(N03 ) 2 .3Cu(OH) 2 = nitrogen pentoxide 22.5, cupric oxide 66.2, 

water 11.3 = 100. Crystalline, transparent, with a highly perfect 

cleavage, yielding thin flexible laminae of a deep emerald-green 

color and brilliant vitreous luster. Easily fused, coloring the flame 

green, and, with soda on charcoal, is easily reduced to metallic 

copper, with deflagration. Soluble in dilute acids, but insoluble hi 

water. It was first reported from a few specimens found with 

acicular crystals of malachite in cavities in cuprite at the United
8 NITRATE DEPOSITS.

Verde copper mines at Jerome, Ariz. Another occurrence in the 

Clifton-Morenci district, in the same State, is described by Lindgren, 1 

specimens having been determined by Hillebrand.

7. Darapskite is a double salt composed of the nitrate and sulphate 

of sodium. Composition, NaN03 .Na2S04 + H2 0 = nitrogen pentoxide 

22.0, sulphur trioxide 32.7, soda 38.0, water 7.3 = 100; or sodium 

nitrate 34.7, sodium sulphate 58.0, water 7.3 = 100. Tetragonal, 

occurring in square tabular crystals, colorless and transparent. 

The water is readily expelled by heat, without decrepitation. It is 

reported from the Pampa del Toro in Atacama, Chile, where it is 

said to be intimately associated with blodite and soda niter.

8. Nitroglauberite occurs as a white, homogeneous mass with 

fibrous crystalline structure. Composition, 6NaN03 .2Na2S04 + 3H20 = 

sodium nitrate 60.1, sodium sulphate 33:5, water 6.4 = 10Q. Soluble 

in water. Occurs in the desert of Atacama, Chile.

USES OF SODIUM AND POTASSIUM NITRATES.

Sodium nitrate is used for many of the purposes for which the 

potassium salt is employed, but its hygroscopic nature makes it 

unavailable for the manufacture of gunpowder or fireworks. For 

making nitric acid, for supplying that acid in sulphuric-acid manufacture, and for use as a fertilizer, it has, however, entirely replaced 

potassium nitrate. It is also the principal source of the potassium 

salt, which is obtained from it by double decomposition with the 

potassium chloride of Stassfurt.

Potassium nitrate (niter or saltpeter) is used chiefly in the manufacture of gunpowder or other explosives, but is also used for fireworks,, for lucifer matches, for curing meat, for manufacture of

certain kinds of glass, for flux in metallurgical assays, for some 

dyeing, and in medicine.

Munroe 2 has summarized the consumption of nitrate of soda in 

the United States for 1905 for the manufacture of various commodities as follows:

Consumption of nitrate of soda in 1905.

Short tons. 

Explosives................................................ 133,034

Fertilizers................................................. 42, 213

Chemicals.................................................. 38,048

Sulphuric, nitric, and other acids............................ 29,301

Glass...................................................... 11,915

Dyestuffs .................................................. 261

254,772

1 Lindgren, Waldemar, Copper deposits of the Clifton-Morenci district, Arizona: Prof. Paper U. S. Qeol. 

Survey No. 43,1905, p. 121. 

a Munroe, C. £., The nitrogen question: Proc. U. S. Naval Institute, vol. 35, No. 3,1910, p. 715.
NITBATE DEPOSITS. 9

DEPOSITS OF NITRATE SALTS.

GENERAL NATURE.

Nitrate salts, although not generally found in large amounts, are 

widely distributed in natural deposits and occur in several forms. 

They are found in all fertile soils, though usually rather sparingly, 

but are not generally supposed to be recoverable from these for commercial use as nitrate salts except possibly under some rather unusual 

conditions. (See pp. 14, 26.) They are also found in more or less 

concentrated deposits the so-called cave niter deposits which are 

generally small but are widely distributed in this and in other 

countries.

CAVE NITER.

Cave niter deposits include potassium, sodium, calcium, and other

nitrates found in protected portions of fractured or cavernous ledges 

or in shallow caves, notably in arid or desert regions. Some such 

deposits have from time to time become more or less well known 

through attempts to exploit them as sources of commercial nitrate 

salts. A number have been brought to special notice by the field 

work done in connection with the fertilizer investigations made by the 

United States Geological Survey during the latter half of the year 

1911, especially investigations relating to potash salts.

The term "cave deposits" is applied to certain accumulations of 

niter salts but does not imply that the material necessarily originated 

in a cave. Potassium or sodium nitrate is frequently found in crevices or under overhanging ledges or in caves in cliffs of many kinds of 

rock, especially in situations where the rock affords a good protection 

from the solvent action of rain or snow waters, and particularly where 

precipitation is small and ground water too low to dissolve and carry 

off these very soluble salts. In such places clear white crystalline 

salts are found in veins several inches thick in the fractures of the 

rocks and also in protected portions of the loose material that have 

fallen to the base of the cliffs. These nitrate salts also form coatings 

or even stalactites on the walls or roofs of overhanging ledges. Such 

deposits, though occurring in widely scattered localities, exhibit 

much.similarity and many of them have doubtless a common origin.

SOURCE OF DATA.

Published accounts of deposits of nitrate salts occurring at many 

localities throughout the United States, and in fact throughout the 

world, are numerous. Some of these accounts have been collated and 

are republished in the following pages. The original accounts are 

scattered, and many of them were found rather by chance than by 

bibliographic search, being included as minor or accessory notes under
10 NTTBATE DEPOSITS.

titles covering entirely extraneous subjects. The following compilation is therefore not supposed to be complete, and it is hoped that 

it can be augmented and republished later, when additional data shall 

have been accumulated. Together the references furnish an interesting commentary on these deposits considered as a type. Their 

description as "cave" deposits and the frequent suggestion that they 

are derived from guano or animal remains comes from many independent sources. Such testimony can not, however, be accepted as 

conclusive or as covering all deposits, for there seems to be little 

doubt that some nitrates or nitrogen compounds may have originated 

in other ways.

To the reported occurrences of such nitrate salts, as described in 

the literature, are added several short descriptions and some chemical 

analyses personally obtained by the author from several localities. 

In a number of the following quotations the term niter is doubtless 

used loosely as referring to any of the natural nitrate salts.

Among many earlier references to the subject the following quotation is taken from a mineralogy by Phillips:*

Niter, nitrate of potash. Niter or saltpeter occurs in crusts, and in capillary crystals 

of which the forms are not discernible; it is whitish or of a yellowish-white; is translucent or transparent; brittle, saline, and cooling to the taste; it deflagrates when placed 

on a hot coal.

It occurs on or near the surface of the earth, and on old walls, etc.

It is found on many of the plains of Spain; and on the chalk near Evreux, in France, 

from which it is gathered seven or eight times every year; and in the deep grottoes of 

Mont Homburg, in Germany. In Italy it is afforded by the calcareous soil of Molfetta. 

Hungary, the Ukraine, and Podolia furnish Europe with abundance of niter. In 

Arabia it occurs in a valley between Mount Sinai and Suez. Persia affords it, and it 

is very common in India, especially on a large plain about "0 miles from Agra in 

Bengal, which is said to have been formerly well peopled. It is found at the Cape of 

Good Hope. The mountainous regions of Kentucky, which are calcareous and full 

of caverns, afford it to the inhabitants of North America. In South America the plains 

bordering the sea near Lima are covered with it.

REVIEW OF OCCURRENCES. 

EASTERN UNITED STATES.

That nitrates occur in the caverns of Alabama, Georgia, Tennessee, 

Virginia, Kentucky, Indiana, and other States is generally and even 

popularly recognized, in part through tales that relate the use of niter 

derived from such sources for the manufacture of gunpowder during 

war times. These deposits have also been described and their 

manner of origin has been discussed. 2

1 Phillips, William, An elementary introduction to the knowledge of mineralogy, 3d ed., 1823, p. 189.

2 Hess, W. H., The origin of nitrates in cavern earths: Jour. Geology, vol. 8,1900, pp. 129-134. Nichols, 

H. W., Nicrates in cave earths: Jour. Geology, vol. 9,1901, pp. 236-243. Merrill, G. P., Rocks, rock weathl 

ering, and soils, 1897, pp. 372-373; also, The nonmetallic minerals, their occurrence and uses, 2d ed., 1910, 

pp. 315-321.
EASTEBN UNITED STATES. 11

The following footnotes are contained in the first edition of a 

mineralogy by Phillips/ with citations of the original sources quoted 

therein:

Nitrate of potash. A native earth, is said to exist on one of the southern branches of 

the river Potomac, in Maryland, bordering on Virginia, from which saltpeter is manufactured. The material was rusty or reddish brown and soft enough to be scraped by 

the finger nail. The base seemed to be a bolar or argillaceous earth. On powdering 

some of it and adding sulphuric acid I was saluted by the fumes of the nitrous acid. 

(Law, in Med. Repos., vol. 12, p. 296.)

Native saltpeter exists in Kentucky associated with particles of quartz and sandrock. 

Of this it is reported there are extensive strata, horizontally disposed. In the specimens I have seen the saltpeter seemed to be distributed through the whole rocky mass, 

to cement the siliceous particles together, and to assist their coherence, though in some 

parts the saltpeter filled up fissures between the parallel layers of the sandrock and 

Occupied in like manner veins and cracks across the strata.

The saltpeter caves in Virginia and Kentucky have been mentioned already. The

estimate of their product is highly consoling to our country. Their history as well as 

that of the saltpetrous sandrocks afford curious problems for chemists to solve. (Brown, 

6 Trans. Am. Philos. Soc., 13 Med. Kepos., p. 367.)

The occurrence of niter as crystalline crusts on mica slate on 

Nantahala River, in Cherokee County, N. C., is noted in a list of 

minerals from that State. 2

References to the occurrence of these salts are contained in a 

mineralogical list published in 1888 by the United States Geological 

Survey, 3 and hi a later revision of this list, which was not published. 

Unfortunately, the source of the information does not accompany 

the notes. The following localities are cited:

Alabama: Mter is found in limestone caves and was mined during 

the Civil War.

Arkansas: Niter or saltpeter is found in Marion and Newton counties, in caves of the limestone region.

Illinois: Niter is reported as occurring in caves in Jackson County 

and on Cave Creek.

Indiana: Niter occurs in caves in Harrison and Crawford counties.

Kentucky: Niter occurs in Mammoth Cave, Edmonson County, and 

in small quantities in hundreds of caves in limestones in the southern 

and central parts of the State.

Missouri: Saltpeter has been found in caves in Pulaski, Maries, 

Calloway, and Ozark counties. "It occurs in magnesian limestone. 

It is no longer gathered."

Tennessee: Niter or saltpeter is reported in "many caves in"limestone formation, and especially in the Cumberland table-land; not of 

much account."

1 Phillips, William, An elementary introduction to the knowledge of mineralogy, New York, 1818, p. 137.

2 Qenth, F. A., and Kerr, W. C., The minerals and mineral localities of North Carolina: Geology of North 

Carolina, vol. 2,1885, p. 81.

B Williams, Albert, List of useful minerals of the United States: Mineral Resources U. S. for 1887, U. S. 

Geol. Survey, 1888, pp. 688-810.
12 NTTBATE DEPOSITS.

West Virginia: Saltpeter or'' peter dirt'' is found in caves in Green- ( 

brier, Monroe, and Pocahontas counties, and has been mined there.

More specific reference is made to the occurrence of niter earth in 

Wyandotte Cave, Indiana, "similar to that used for the manufacture 

of saltpeter during the war of 1812."* An analysis of the material is 

quoted which shows an equivalent of 6.55 per cent niter, and another 

analysis, of bat guano from caves, is given, as follows:

Analysis of bat guano from Wyandotte Cave in Indiana.

Loss at red heat..................:............................ 44.10

Organic matter................................................ 4. 90

Ammonia..................................................... 4. 25

Silica......................................................... 6.13

Alumina..................................................... 14. 30

Ferric oxide .................................................. 1. 20

Lime........................................................ 7. 95

Magnesia.................................................... 1.11

Sulphuric acid................................................ 5. 21

Carbonic acid................................................. 3. 77

Phosphoric acid.1............................................ 1. 21

Chloride of alkalies and loss................................... 5. 87

100. 00

The recovery of niter from the caves of Indiana is also mentioned 

in a later report of the State Geological Survey 2 in the descriptions 

given of Saltpetre Cave in Monroe County, Wyandotte Cave in Crawford County, and Saltpetre Cave in Crawford County.

The records concerning Wyandotte Cave go back only to 1812. During the war with 

England the demand for gunpowder became so great that much of the nitrous earth in 

the caves of Indiana and Kentucky was utilized in the manufacture of potassium 

nitrate, or saltpeter, one of the principal ingredients of gunpowder. What is now called 

the " Old Cave," was the only portion of Wyandotte then known to the whites, and to 

it the name of " Indiana Saltpetre Cave'' was given by a Dr. Adams, who first preempted 

the land on which the cave was located, for the purpose of manufacturing saltpeter. 

He carried on the business on an extensive scale from 1812 to 1817, and remains of 

leaching hoppers, troughs, etc., can yet be seen near the mouth of the cave, and at 

"Saltpetre Cave," about a third of a mile distant. The close of the war made the 

"petei1 " business unprofitable, and Dr. Adams relinquished his claim.

WYOMING.

Cross s describes an occurrence of potash niter in the Leucite 

Hills, Wyo., on North Table Butte, the summit of which he reached 

through a cleft on the northern side. He says:

On the eastern side of the gap through which the top is gained a cavity or recess 

with overhanging roof, of irregular shape, several feet in length and depth, was found

1 Cox, E. T., Eighth, Ninth, and Tenth Ann. Repts., Geol. Survey Indiana, 1870, p. 163.

2 Blatchley, W. S., Indiana caves and their fauna; Twenty-first Ann. Eept., Geol. Survey Indiana, 1896, 

pp. 136,149-151,173.

* Cross, Whitman, Igneous rocks of the Leucite Hills and Pilot Butte, Wyo.: Am. Jour. Sci., 4th ser., 

vol. 4, August, 1897, pp. US-141.
WYOMING. 18

in nearly massive rock. It was fully exposed to the prevalent northwesterly breeze, 

and rain could penetrate to the inner wall only when driven by very strong winds. 

In this sheltered space was found a very unusual mineral in a rather coarse, granular 

aggregate, and of sufficient mass to allow collection of specimens several inches in 

diameter. It seemed to occur as a partial crust to the cavity and as a fil ling for irregular 

fissures which extended downward and backward into the body of the rock. A 

columnar mass several inches in diameter connected roof and floor of the recess at one 

point where they were no less than 1 foot apart. Fragments of rock were attached to 

the column, and its stalactitic shape is probably an accident. This white granular 

substance was analyzed by L. G. Eakins and found to be essentially nitrate of potash. 

The exact result is given below:

Analysis ofnitef, etc.

K,0. ........................

«N205 - ......................

CaO........................

so...........................

H20.........................

Na

Cl. ..'........ ................

...................... 44.91]

..................... 51.49

..................... 1.09

....... ............. 1.59

..................... .63

..................... .07]

..................... .09

96.40 niter.

3.31 gypsum,

.16 halite.

99.87

It is regretted that the nature of this substance was not recognized in the field, in 

order that close observations of its occurrence might have been made. As far aa 

known there is nothing to indicate the derivation of this niter from organic substances 

of any kind, yet such an origin is either evident or assumed as probable for all other 

occurrences of natural nitrates of which I find mention in manuals of mineralogy. 

This occurrence is, however, entirely different from all others of which notice has 

been found in literature. While extended discussion of the genesis of this deposit of 

niter is at present useless, it may well be pointed out that ammonia gas is a common 

exhalation product of volcanoes in their fumarolic stage, and that ammonium chloride, 

sal ammoniac, is deposited in clefts, fissures, or tubular cavities of lavas at Vesuvius, 

JStna, Solfatara, Hecla, and other volcanoes. The lavas of the Leucite Hills contained 

fluorine, chlorine, and sulphurous compounds, as will be shown by the rock analyses, 

and it is certainly a noteworthy coincidence, if nothing more, that one of the bestknown occurrences of sal ammoniac is in the leucitic lavas of Vesuvius, rich in potash.

As regards the occurrence of North Table Butte, there is no special reason to assume 

a volcanic conduit at this point, yet this occurrence would seem to suggest such a 

channel at no great distance.

Other minerals were not seen in this cavity, the niter being deposited directly on 

the rocks. The presence of soda niter at the Boars Tusk, described below, renders 

this occurrence all the more interesting. Although the nature of the niter was not 

definitely recognized at the time of its discovery, the peculiar astringent taste was 

noted then and the true character as a nitrate was speedily established. Specimens 

of this 

*******

niter may be seen in the National Museum.

In several places where the breccia (which composes the mass of the column known 

as the Boars Tusk) was open and cavernous a scanty white coating was observed on 

protected rock faces. Unfortunately the character of this substance was not suspected, 

and only a single small specimen was with difficulty procured for analysis. It proves 

to be a soda niter containing a little potash, as shown by the following analysis made 

by L. G. Eakins.

« NaOo calculated for ZjO.
14 ' ITCTBATE DEPOSITS.

Analysis of soda niter. 

Na20............................................. 32.09

10.66 KNOa.

.71 gypsum. 

.54 water.

.......................................... 4.97

N205 ............................................. 61.58

Cap............................................. .24]

S03 ............................................. .33

H20............................................ .68,

01.............................................. Trace.

99.89

The discovery of soda niter in anything resembling this occurrence has not been 

announced before, as far as I can ascertain. The similarity in the conditions of 

occurrence of the two nitrates described above adds to the strength of the hypothesis 

that both are intimately related in origin to the peculiar magma of this region. Yet 

it is possible that organic matter from clefts above inhabited by birds or small animals 

might have furnished the nitrogen for this niter.

COLOEADO.

The occurrence of nitrate salts in unusual amounts in soils, forming 

a type distinct from that of the "cave deposits," has been discussed 

by Headden,1 who calls attention to a condition existing in Colorado 

which may be analogous to that in the much-exploited "niter fields" 

of southern California (p. 26). He states that remarkable quantities 

of nitrates have already accumulated over large areas in widely 

separated portions of Colorado. These areas are all characterized 

by a brown color on the surface arid appear oily or wet, sometimes 

glistening. The spots have been generally supposed to owe their 

appearance to "black alkali." On testing, however, "black alkali" 

or sodium carbonate was rarely found to be present in excess 

and examination revealed comparatively large quantities of nitrates.

Such spots are invariably barren, and experiment has shown that an 

excess of nitrates is injurious or fatal to plant growth and might 

produce the effects observed. The soil of these areas, especially in 

the less advanced stages of nitrification, has a soft, velvety feel 

under the foot and in later stages becomes mealy on the surface. 

Some of the soil, especially that of a clayey nature, is defiocculated, 

becomes muddy, and retains water with great tenacity. 

In summary, Headden says:

We have found large areas in the eastern and likewise in the western portions of 

the State, sections about 380 miles apart. Also in the southern portion near the New 

Mexican boundary and within 40 miles of the northern boundary, localities about 270 

miles apart. It is not to be inferred that these niter areas are continuous, but they 

are in fact quite extensive, in places being continuous for miles. I have stated the 

conditions in Colorado, but neither these nor the occurrences are confined to this

i Headden, W. P., The occurrence and origin of nitrates in Colorado soils, some of their effects, and what 

they suggest: Pnxx Colo. Sci. Soc., vol. 10,1911, pp. 99-122.
IDAHO. 15

\

State. The amounts of nitrates found are also sufficiently large to entitle the suggestion to consideration. Analyses of surface samples have shown that 6.5 per cent of 

the air-dried soil consisted of nitrates. The area involved in this case was not less than 

10 acres, and as the sample was taken to a depth of 2 inches we would have 210 tons 

on the 10 acres of this land taken to this depth. In another sample taken to a depth 

of 5 inches we found 2.6 per cent of nitrates. This was from a large piece of land, 

40 acres in all, but, assuming that only 8 acres of it was as rich as this, we would have 

172 tons in the top 5 inches of the land. There °are hundreds of acres of land in this 

State which carry from 1 to 5 tons of nitrates in the top 2 inches of the soil. These 

conditions are met with at altitudes of from 3,300 to 7,500 feet.

The rate of fixation obtained by experiment, 5,616 pounds of nitrogen for each 

4,000,000 pounds of soil per annum, is sufficiently large to further entitle the suggestion to consideration. The nitrification obtained by experiment is also significant; 

that is, corresponding to the formation of 5 tons per acre-foot of soil per annum.

After explaining the nitrifying action of bacteria in the soil and 

describing experiments to prove that this action does take place in

such soil spots, Headden concludes:

The nitrates accumulated in these areas do not owe their origin to the ordinary white 

alkali of the country, nor have they been washed off of adjoining lands, nor yet have 

they been brought into these areas from adjoining lands by ground waters, unless these 

ground waters flow from other nitrated areas, such as a mesa rich in nitrate spots.

These nitrated areas are not in any way dependent upon the geological formations 

of the country.

The irrigating waters, whether river or reservoir waters, do not contain unusual 

quantities of nitrates, the range being from a trace to 0.5 part per million.

Fixation takes place rapidly in these soils, the maximum result obtained in 27 days 

corresponded to the fixation of 5,616 pounds of nitrogen per acre-foot per annum, or 

17.5 tons of proteids.

Nitrification also takes place. The maximum increase obtained in 48 days was 138 

per cent of the nitric nitrogen present at the beginning of the experiment, which corresponded to the formation of 5 tons of sodic nitrate per acre-foot, or 4,000,000 pounds 

of soil 

*******

per annum.

The areas involved, their wide distribution throughout this State, and their probable 

presence in other portions of the semiarid West, together with the rates of fixation and 

nitrification obtained by direct experiment, suggest the probability that the nitrates 

of Nevada, Chile, and Peru owe their origin ,to the fixation and nitrification of atmospheric nitrogen by bacteria, azoto- and nitro-bacter.

IDAHO.

Niter salts have been reported from several localities in Idaho, notably in Bannock County, near Soda Springs 1 and Pocatello; in 

Blame County; in the southwestern part of the State, near the 

Utah-Nevada line; and in Wayne County, in the central part of the 

State. These are believed to be deposits of the cave type and are 

reported as of very small extent and probably of little economic 

value. The following analyses are reported by Stewart as reprei Stfiwart, Robert, The occurrence of potassium nitrate in western America: Jour. Am. Chem. Soc., vol. 

33,1911, pp. 1952-1954.
16 NITBATE DEPOSITS.

senting the deposit in a cave of red sandstone at the locality 35 miles 

northeast of Soda Springs:

Composition of crude nitrate.

1.

4.22

11.12

2.91

0.11

30.89

1.54

TVnpfl

2.

2.73

11.48

2.12

0.17

31.55

1.58

T*POPO

UTAH.

Miscellaneous occurrences. Nitrate salts are reported by George T. 

Henry, of Marysvale, to have been found'by chemical test in specimens of a pure white salt taken from rock ledges in Hobble Canyon, 

which is the next canyon south of Provo, Utah. Hobble CJeek is 

described by Mr. Henry as running through the town of Springville, 

Utah.

Mineral Resources for 1887 contains a reference * to saltpeter or 

nitrate of potash occurring near Fillmore, Millard County, and to 

"several small beds near Parawan, etc., Iron County."

G. B. Loring, of Monroe, Utah, reports beds of nitrate salts, proved 

by tests or analysis made by Prof. Talmadge, from a locality 2£ miles 

above the Rob Roy mine in Wildcat Canyon, about 8 or 9 miles northeast of the town of Beaver. The salt is said to occur disseminated in 

limestone and lava, where exposed in cliffs.

Greenwich Canyon, Grass Valley. An essentially pure potassium

nitrate has been found in Greenwich Canyon, Piute County, on the 

east margin of the Sevier Plateau, 5 miles south, 70° E. from Marysvale Peak, near the north boundary of Piute County, Utah. The 

located claims are situated in the upper portion of the canyon, which 

is tributary to Otter Creek in Grass Valley, joining that stream at a 

point 4 miles south of the town of Koosharem and a short distance 

north of Greenwich. Two groups have been located, the lower near 

the fork of the main creek about 1£ or 2 miles above (northwest of) 

the Grass Valley road and the upper at least 5 miles from the Grass 

Valley road. These localities are represented on the map (fig. 1).

The deposit is of essentially the same type as those at Gerlach, 

Nev. (p. 23), and elsewhere, but the amount of salts to be seen is less. 

The salts are found in caves or brecciated cliffs and ledges that border the canyon valley. Evidences of habitation by bats or other nestbuilding animals are seen in the same cliffs. x

i Williams, Albert, op. cit., p. 796.
UTAH. 17

The foothills or interstream ridges that range from the Marysvale 

Plateau eastward down to Grass Valley are capped by a basaltic lava 

flow, vesicular at the top, which is apparently of comparatively 

recent date, but which preceded the last or present canyon-cutting

Fratras 1. Map showing location of niter deposits and prospects In Greenwich Canyon, near Grass

Valley, Plute Co., Utah.

stage of the existing stream valleys. Modern stream valleys are 

somewhat uniformly intrenched below these basaltic flows, which 

were spread on a tilted plain sloping eastward at about the same grade 

as the streams. The rocks over which the basalt flowed are acidic 

52096° Bull. 523 12 2
18 NITEATE DEPOSITS.

volcanics, rhyolite or a related rock, including interbedded flows and 

tuffs, which are exposed at intervals all along Greenwich Canyon, 

especially on the north and northeast sides. These ledge exposures 

are considerably brecciated and weather in cavernous types, forming 

brown or reddish stained bluffs, possibly iron stained by leaching 

from the overlying basalt. The upper portions of the rhyolite flows 

are apparently waterlaid tuffs, evenly bedded, showing distinctly the 

contact with the overlying basalt.

At the niter claims in upper Greenwich Canyon some ledges of the 

rhyolite lava, cavity filled and fractured, make prominent bluffs high 

on the north slope of the canyon. Near the base of the bluffs small 

excavations have revealed seams or vein material of a very soluble 

pure white crystalline salt, having a pungent taste. From this place 

specimen No. 1 of the subjoined analyses was obtained.

Samples collected from the Greenwich Canyon localities and 

analyzed by J. G. Fairchild in the laboratory of the Geological Survey, 

gave the following results:

Tests of supposed niter salts from Greenwich Canyon, near Grass Valley, Utah.

-

Soluble in water: 

N03 ..~ ....................................................

Nn

K..................... .....................................

, CL. ........................................................

SO3 .... ....... ............. .... . ...... ..............

CaO... .....................................................

CO8 . .......................................................

1

46.04

28.53

.18

19.18

0.20

Small.

Small.

2

None....

3 4

0.82

3 to 4

2.65

No. 1 represents the clearest portion of saline material available in

the talus at the base of the cliff on the upper claims in Greenwich 

Canyon.

No. 2 is an alkali salt found on the surface of the ground in the forks 

of the main canyon near the lower claims. This salt appears to be 

leaching from a decomposing rhyolitic soil in the creek wash. Its 

taste suggests sodium carbonate or sulphate.

No. 3 is from a cave in a brecciated rhyolite bluff on the lower claims 

at the north side of Greenwich Canyon, just below the creek forks. 

There was no evidence of bat nests at this place.

No. 4 was a limy white lenticular vug in the brecciated rhyolite or 

tuff at same locality as No. 3. This material is said to have been used 

locally for whitewash. The report by Mr. Fairchild shows it to be an 

impure bauxite, with a small amount of soluble -nitrates, probably of 

potassium.

Only the sample from the upper claim proved to contain much 

niter and it is apparent that the quantity of such material available 

is very limited. It perhaps would not be warranted to attempt a
OEEGON. 19

judgment of the ground as a whole from the small number of samples 

taken for test. The niter is apparently more abundant where bat 

nests are numerous and less abundant where the nests do not 

appear. It is not certain that the nests are those of bats.

OREGON.

Stafford reports on the presence of niter in Oregon as follows: 1

Saltpeter is reported in marsh deposits of southeastern Oregon, and, it has been 

claimed, in quantities sufficient to justify extraction. A very interesting occurrence 

is noted near Mount June, southern Lane County, where a ledge of earthy material 

carrying large quantities of niter is exposed. Claims have been staked by Elmer 

Doolittle and associates, of Cottage Grove.

A recent press notice 2 announces prospective developments of 

nitrate of soda deposits on the west side of Wagontire Mountain, 

about 60 miles southwest of Burns, almost on the line betweenHarney and Lake counties. Prospectors from Vale, Oreg., are said 

to be taking active interest in this ground.

NEVADA.

Nitrate salts near Lovelock. The existence of nitrate salts in ledges 

and caves on the south side of Humboldt Lake, southwest of Lovelock, Humboldt County, Nev., is said to have been known since 

1868. The writer is indebted to Mr. J. R. Hunter, of Lovelock, 

who accompanied him on a trip to the property and who, by his 

familiarity with the ground and the work that has been done, was 

able to point out the more salient features of the deposits. He is 

also indebted to Mr. John T. Reid, of Lovelock, for the greater part of 

the following history of these deposits and of the work that has been 

done on them.

Reports state that the salts were first used by the Indians, who had 

long known the projecting point of rock in sees. 13 and 14, T. 25 N., 

R. 31 E., as Medicine Rock, and who had been accustomed to visiting 

the place and licking the rock, believing that thereby they derived 

some medicinal benefit. The first discovery of niter is said to have 

been made on a site between sees. 13 and 14, T. 25 N., R. 31 E., by 

William Silverwood, still a resident of Lovelock, who claims to have 

located claims there in 1868. From time to time others have located 

or relocated this and other ground in the vicinity. The matter was 

taken up more actively in 1887, when a small pit was dug to determine 

the depth of the material, after which interest in the matter was 

again allowed to lapse. About 1902 or 1903 the claims passed into 

control of the American Nitrate & Potash Co., of San Francisco, 

which for a time seemed about to undertake active development, but 

which has done no work on the property.

1 Stafford, 0. F., Mineral resources and mineral industry of Oregon for 1903: Bull. Univ. Oregon, No. 4, 

new ser., vol. 1,1904, p. 105.

2 Portland Oregonian, Aug. 5,1912.
20 NITRATE DEPOSITS.

In sec. 36, T. 24 N., R. 29 E., some disconnected exploratory work 

has been done by several individuals. The discoveries at this point 

are also reported to date back as far as 1868. James Say, proprietor 

since the early fifties of a station on the old emigrant road passing by 

this route, is said to have called attention to salts of a peculiar acrid 

taste which he found in neighboring ledges, but he was probably 

unaware of their nature. About 1902 or 1903 some preliminary 

experimental development work was done under the supervision of 

W. M. Courtis, of Detroit, but was later allowed to lapse.

The deposits occur on the west slope of the Humboldt Range. 

(See PL I.) The "Niter Buttes" are also noted by I. C. RusseU * who 

describes the rocks and gravels that compose them and discusses the 

terraces and bars that record former more-elevated lake shores along 

them, and who locates them on the maps at the extreme southern 

end of the Humboldt Range near the mouth of the Humboldt River, 

where that stream joins the waters of the Carson Sink.

The Lovelock niter beds have been staked as mineral locations, as 

shown by the shaded areas on the map (PI. I), the extent of location 

given being based on data furnished by Mr. Reid.

This.depbsit was described by Van Wagenen in a brief note published in 1902.2

The locality was visited by the writer on August 8, 1911, when a 

somewhat hurried review of the northern group of claims was made and 

a number of samples were collected for analysis from the under side of 

projecting or o v^erhanging ledges, which are here composed of an 

aciolic (probably rhyolitic) lava, at places a coarse volcanic breccia. 

The following analyses of the material were made in the laboratory 

of the Geological Survey:

Analyses of supposed niter salts collected near Lovelock, Nev. 

[J. G. Fairchild, analyst.]

Insoluble in water. . 

Soluble in water: 

N08 ............

"NTft

K. .............

Cl. .............

S03 ..........

CaO. ...........

1

94.25

0.1

Trace.

2

92.81

0.05

3

95.37

Trace.

little.

4

95.18

Trace.

5

34.32 

0.61

23.74

Trfl/»A

29.60

7.98

Not

over 2.

6

30.89 

35.65

20.20

rTrnr>P

10.90

Trace.

little.

7

4.00 

53.12

26.26

Trsc6

8.83

1.33

0.53

8

92.86

0.19

9

78.06

S

fU.

2 CM

8.05

Not

over 2.

little.

10

10.58

O

flO

34.59

XTrtTlP

52.00

1 nn

little.

Nos. 1 to 4, inclusive, were from reported niter ground in approximately the southwest corner of sec. 5, T, 24 N., R. 31 E. (PI. I). The 

material has a rather strong saline taste, but contains no niter. The

i Russell. I. C., Geological history of Lake Lahontan, a Quaternary lake of nortnwest Nevada: Mon. 

TI. S. Geol. Survey, vol. 2,1885, pp. 109-110 and map, p. 106. 

* Van Wagenen, T. H., Nitrate deposits, Humboldt Co., Nov.: Min. and Soi. Press, vol. 84,1902, p. 63.
U. S. GEOLOGICAL SURVEY BULLETIN 523 PLATE

R. 29 E . R. 30 E. R.3IEA.^'^v 3fffify f * v 

" ^T'' * li/f' /11 < * ./ i

**"r ' > V

3 /[" 2 / I' L-A^i

NOEX MAP OF NEVADA

3MOW.INO LOCATION 

OF AREAS DISCUSSED IN THIS 

REPORT

R.29E.

Contour intervals 25 and 100 feet

Datum is mean sea level

Full line contours from maps by U. S. Reclamation ServiceBroken contours from U. S Geological Survey atlas sheetR.30E.

MAP SHOWING DISTRIBUTION OF NITER CLAIMS NEAR LOVELOCK, NEV.
ifrEVADA. 21

general situation of the ground from which these four samples were 

collected, though reported as niter-bearing, is, however, different in 

character from that where the remaining samples were taken, and no 

apparent relation to the overhanging cliffs or cave formations was 

observed. Therefore the negative character of these tests bears no 

significant relation to the rest of the analyses.

Nos. 5 to 10, inclusive, were collected in the group of claims extending from sec. 33 to sees. 13 and 14, T. 25 N., R. 31 E.

No. 5 consisted of a sample of salts, shown by the tests to be mainly 

sodium chloride, which occurred as a crusted coating under a projecting ledge of red brecciated rhyolite.

No. 6 was collected at the discovery monument of the Queen placer 

claim, 160 acres, located April 5, 1911, in the "Lake mining district,

Churchill County, Nev., about 5 miles south of the Big Five Reservoir, 

at the big bluff in the foothills where it juts against the valley." The 

salts were incrusted under a ledge projecting in cave form. In the 

sample collected approximately 70 percent of the water-soluble portion 

proved to be sodium nitrate.

No. 7 was collected in the same locality as No. 6, but from a somewhat different position. Both represent the selected portion of the 

white incrusted salts chipped from the ledge face or from seam fillings. 

The analysis shows that about 75 per cent of the water-soluble portion 

of this sample is composed of sodium nitrate. The rock is evidently 

a red brecciated lava, probably rhyolite, carrying large included 

bowlders, rounded and subangular blocks of shale, and other country 

rock. The point is a prominent rock headland on the margin of the 

valley, topped by one of the rock-cut terraces of a lower important 

stage of Lake Lahontan levels. At least four other distinct shoreline terraces show at higher levels. The rock is seamed and coated 

by marked incrustations of white salts in more protected parts. One 

much-fissured zone shows a foot or two of quite strongly charged 

material. A carload of about 20 tons is reported to have been taken 

at this place and shipped for experimental treatment. The only salts 

visible, however, are those occurring in weather-protected portions of 

the ledges, especially where decomposed or much jointed. So far as 

can be judged from the surficial aspect of the deposit the quantity of 

such material available is probably not great.

Nos. 8 and 9 gave negative tests for nitrates. No. 8 was collected 

from decomposed rhyolite in talus form at the foot of the main ledge, 

detrital from the overhanging ledge, but probably weather leached; 

No. 9 was taken from the thoroughly decomposed soil sliding down 

over the outcrop of this lava rock in place.

No. 10 was collected in a cave one-fourth to one-half mile east of 

the section stone marking the corner between sees. 14, 15, 22, and 23, 

T. 25 N.., R. 31 E. The stone which stands about 3 miles north of the
22 NITRATE DEPOSITS.

Queen placer claim close to the remains of an old stone house that stood 

on the immigrant trail of the pioneer days, is distinctly marked with the 

customary notches and is probably an original corner. Tests showed 

the sample to consist mainly of sodium chloride with a little niter, but 

the type of occurrence is essentiaUy similar to that at the Queen 

placer. Excavations in the cave have revealed human bones supposed 

to be Indian remains purposely buried. Some sacks of the ore taken 

from the cave contained material consisting of incrusted salts coating 

the face of the ledge at the back of the cave and represented the purest 

white salt in evidence.

Samples similar to those -described were collected by L. J. Pepperberg from cliffs in the NE. £ sec. 14, T. 25 N., R. 31 E., and were 

analyzed by F. F. Fitzgearld, with the following results, which have 

not before been published:

Analyses of supposed niter-bearing material from near Lovelock, Nev.

A12O3 ... ............................................................

Fe2O3 ............................................................... 

Ca... ................ :..............................................

K.... ..............................................................

Na.... .............................................................

^O.......... ......................................................

CI.... ..............................................................

804..:....................-.........................................

N08 .. ..............................................................

Supposed 

niter salts.

1.56

} 0.57

0.78

3.88

33.31

0.52

50.10

9.90

Trace.

100. 62

Adjacent 

rock.

5.09

2.59

2.50

Leached 

rock top 

of cliff.

0.42

The water-soluble portion of these samples proved to be essentially sodium chloride.

It is to be noted that the only'consider able showing of niter salts 

contained in the present series of samples is represented by the two 

specimens of the best material from the crevices in the rock on the 

Queen placer claim. Furthermore, the water-soluble portion of this 

is shown to be essentially sodium and not potassium nitrate, with 

some sodium chloride. It is possible that the composition of the 

salts at this place has been influenced by the saline constituents of 

Lake Lahontan waters, which have undoubtedly covered the ground.

In explanation of the origin of the niter it is suggested, although 

admittedly far from conclusively proved, that the prominent headland that these ledges must have formed in Lake Lahontan at or 

succeeding the period in which the rock bench was cut by wave action 

along the lake shore was probably inhabited by ducks, sea gulls, or 

other birds, possibly in large numbers, even as similar rocks are thus 

inhabited in Great Salt Lake to-day. Decomposition of organic 

matter in contact with alkaline material might account for the pro-
NEVADA. 23

duction and dissemination of nitrate salts, which may nave penetrated widely the fissures and crevices of the much-fractured rhyolite. 

The subject is further discussed on page 30 in a more general review 

of the origin of nitrate deposits.

Potassium nitrate north of Gerlach. An occurrence of almost pure 

potassium nitrate in natural form has been found in the northern part 

of the Granite Range, Washoe* County, Nev. (See index map, PI. 

I.) The claims were visited in October, 1911, by George Otis Smith, 

Alfred H. Brooks, and the author. The locality is in T. 37 K, R. 22 

E., and is reached by road and trail from Gerlach, a station on the 

Western Pacific Railway. The route from Gerlach lies north along 

the western margin of the Blackrock Desert for about 12 miles, thence 

northwest across a large alkali flat at the east base of the Granite

R.22E.

12

MAGNETIC 

DECLINATION

***«?!*

13 .4$

UPPEff^NITER

FIGUKE 2. Map showing location of upper and lower groups of niter claims near Gerlach, 

Washoe County, Nev.

Range, and thence, following tributary drainage, to Leadville, a mining camp near the northern end of that range. From Leadville the 

route followed was by trail across the divide and down the western 

flank of the range to the prospected ground, which is about 3 miles 

distant and 1,400 feet lower than the place where the trail crosses the 

crest of the range. Figure 2 shows the location of the claims.

The niter salts occur under ledges and in cavelike cliff formations 

in a canyon on the upper waters of Grass Valley Creek, an upper 

tributary to Little Highrock Canyon. (See PL II.) A small amount 

of exploratory prospecting has failed to reveal much more of the 

character of the deposit than shows at the surface. It is, however, 

essentially similar to that at Lovelock and elsewhere. The niter is 

found as a white crystalline salt in crevices and concentrated in veins
IHTBATE DEPOSITS.

in the slide rock at the base of the cliffs, partly or wholly in positions 

protected from leaching by rain, snow, or surface waters. A collection of samples representing the salts, or supposedly saline-bearing 

material, was made at points indicated by crosses on the map (fig. 2). 

Analyses follow:

Analyses of niter samples from deposits north of Gerlach, Nev. 

[J. G. Fairchild, analyst.]

Water-soluble portion: 

N03 .....................

SO^.... .................

K. ....... ...............

Na......................

Cl. ........... ...........

CaO.....................

 PtOi.... ....................

I

98.88

0.3±

2o

34.10

5.45

0.67

63.18

0.64

3

10.04

52.40

33.61

1.07

4

91.83

3.07

0.80

0.50

0.30

5

14.58

50.42

31.42

1.28

Small.

6

98.36

0.72

0.42

0.04

Trace.

7

76.75

9.96

4.97

0.58

0.30

cO. 5

8

88.09

5.44

Tr&cs

1.40

0.96

O A\

9

QR 50

0.32

0.26

0.04

a No. 2 is a guano with abont 49 per cent loss on ignition. 6 Nonvolatile chlorine, c Approximate.

Nos. 1 and 2 come from the upper nitrate claims; No. 1 is from a 

sugary siliceous-like seam in rhyolite lava exposed in a cliff on the 

north side of upper Grass Valley Creek (W. \ sec. 13, T. 37 N., R. 

22 E., Nev.); and No. 2 is supposed bat guano from upper corner 

under cave near seam from which No. 1 was taken.

Nos. 3 to 9 are from the lower claims. No. 3 is a white crystalline 

salt from a seam about 3 inches thick, occurring in soil and slide rock 

at base of an overhanging cliff of rhyolite lava in the lower canyon of 

Grass Valley Creek (near middle of north side sec. 15, T. 37 N., R. 

22 E.). No. 4 is a blackened coating staining the cliff face near the 

locality of No. 3, supposed to be a leaching from bat guano. No. 5 is 

a white Crystalline salt dug from a fissure in the face of the cliff about 

50 feet west of the locality of No. 3. No. 6 is a specimen of shattered 

rhyolite rock collected from a prospect pit near a blast hole in the same 

locality as Nos. 3 and 4. No. 7 is a brownish or blackened earthy 

deposit from a fissure in the face of the cliff, -containing many rock 

fragments, near the locality of Nos. 3 and 4. No. 8 is an iron-stained 

rhyolite rock, containing salt in seams and cracks, taken from a 

brecciated cliff in the forks of Grass Valley Creek about 200 feet east 

of the locality of No. 3. No. 9 is from a prospect pit on the south side 

of Grass Valley Creek, just above the forks of the creek and about 600 

feet east and a little south of the quarter section corner on the north 

side of sec. 15, T. 37 N., R. 22 E. It consists mainly of rock fragments with no evident coating of salts.

In considering these analyses from a commercial standpoint it 

should be borne in mind that the samples containing the richer salts 

are all selected samples, representing only what appeared to be the 

very best material that was available in the prospects, and that there
U. S. GEOLOGICAL SURVEY 

A. UPPER CLAIMS. 

NITER CLAIMS NORTH OF GERLACH, IN THE NORTHERN GR
25

.is as yet no really sufficient evidence that the quantity now in evidence 

can be much increased by further development.

These analyses show that the water-soluble portions of the purer 

salt samples (3 and 5) are essentially pure potassium nitrate in natural 

form, the insoluble impurities being chiefly earth or rock fragments 

accidentally included in scraping up the samples. Such a salt in 

merchantable quantities would be worth about $65 a ton in eastern 

markets. As the potassium oxide of a pure potash niter constitutes 

38.7 per cent of the salt and the nitrate radicle the remainirg 61.3 

per cent, it appears that the water-soluble portions of samples 3, 5, 

6, 7, 8, and 9 consist chiefly of potassium nitrate with a relatively 

small proportion of sodium nitrate.

The sample of guano shows a potassium content, but has little 

nitrogen in nitrate form. It contains soluble nitrogen in the form of

ammonia, and probably also in the albumenoid form, but the latter 

was not chemically determined.

The country rock in the vicinity of the Gerlach niter prospects 

consists almost entirely of acidic volcanic lavas showing vesicular, 

ropey, and flow structures exposed in many places in cliffs and 

ledges. Glassy obsidian is found throughout the area as fragments in 

soil that covers the hill slopes, as well as in layers intercalated with 

other forms of the flow rock. The. country rock is probably rhyolite.

It has been generally assumed by those interested in the development of these deposits that the nitrate salts are formed by leaching 

from the country rock and that they accumulate or are preserved in 

places protected from the weather. On the basis of this assumption 

it has been supposed that some portions of the bedrock may be 

sufficiently rich in niter to be mined or quarried and treated directly 

for recovery of the salts. However, the fact that the salts are nearly 

always observed in ledges and cliffs which have been and now show 

evidence of being inhabited by bats or other nest-building animals 

leads to the very strong suggestion that the origin of the niter is to 

be found in comparatively recent organic agencies. If the niter salts 

have originated through decomposition of bat or other guano at the 

surface of the ledges alone, the deposit 'can scarcely be of sufficient 

extent to be of much commercial value. (As to origin see also p. 30.)

Niter salts near Railroad Valley. Niter salts have been prospected, 

it is said, in some of the canyons bordering the west side of Railroad 

Valley, which is situated nearly in the center of the State. (See 

index map, PI. I.)

CALIFORNIA.

Williams * reports that fine samples of soda niter were taken from 

a deposit near Calico, San Bernardino County, Cal., and were said to 

have been sent to San Francisco for examination.

i Williams, Albert, Nitrate of soda: Mineral Resources U. S. for 1882, U. S. Geol. Survey, 1883, p. 599.
26 NITEATE DEPOSITS.

Gilbert Bailey 1 notes potash niter found in the desert northeast of 

Salton, Riverside County, Cal., and also mentions soda niter as 

crystals lining a cave in the Calico district.

Other deposits which appear to belong to a class differing somewhat from the common or cave type have been recorded as containing nitrate salts of possible economic value. Gilbert Bailey 2 gives a 

rather full account of some extensive deposits of low-grade niter beds 

situated principally in Inyo County, Cal., along the lower valley of 

Amargosa River above its junction with the southern end of Death 

Valley. These nitrate beds have long been known, but continued 

prospecting seems to have failed to reveal material of sufficient 

richness or quantity to justify serious attempt at development.

A considerable number of analyses of these niter-bearing earths are 

quoted, some of which show high percentages of nitrate salts. It is 

understood, however, that average samples of these earths usually 

run low in. their nitrate content, generally less than 1 or 2 per 

cent, the higher values being obtained from occurrences of comparatively local extent. These soils are presumed to have received their 

nitrate salts as the result of bacterial action on organic matter contained in the soils. In the dry desert climates the salts are supposed 

to have been brought in solution by capillarity to the surface, where 

by evaporation they are commonly deposited in rich nitrate-bearing 

saline crusts, their preservation there being chiefly dependent on the 

unusual dryness of the climate. The average content of the soil for 

any considerable depth would probably run very low. The localities 

of such deposits are listed by Bailey 3 as follows: "In Inyo County in 

the Confidence, Tecopah, and Upper Canyon beds; and in San 

Bernardino County in the , Valley, Round Mountain, Saratoga, 

Lower Canyon, Salt Springs, and Owl Spring beds."

Other deposits of apparently similar occurrence are reported along 

lower Colorado River 4 about 30 miles south of Needles, Cal., and at 

places between that locality and Yuma.

Hilgard 5 describes some places in California where nitrates occur 

in the soil in exceptional abundance. Such, for instance, is an alkali 

tract lying in the bottom of Merced River in a local basin of impervious limestone surrounded by a low ridge which is only exceptionally 

overflowed by the river; so that even the salts that have bloomed 

out on the surface are not usually washed away. An analysis of this 

soil follows.

1 Bull. Cal. State Mining Bureau No. 24, 1902, p. 109 and map.

2 The saline deposits of California: Bull. California State Min. Bur., No. 24, 1902, pp. 154-180.

s Op. cit., pp. 170-180.

* Turner, H. W., The sodium nitrate deposits of the Colorado: Min. and Sci. Press, vol. 94,1907, pp. 634- 

635. Graeff, F. W., Nitrate deposits of southern California: Eng. and Min. Jour., vol. 90. 1910, p. 173.

6 Hilgard, E. W., Alkali lands, irrigation, and drainage in their mutual relations: Rept. University California, College Agr., appendix, for 1890,1892, pp. 25-26.
ABIZONA. 27

^

Composition of alkali salt from Merced bottom, Merced County, Cal.

' Soluble salts in 100 parts of soil crust........................... 1.00

v Sodium sulphate (Glauber's salt).. .............................. 3.88

Sodium nitrate............................................... 10.72

Sodium carbonate (sal soda).. .................................. 63.00

Sodium chloride (common salt)................................ 1. 21

-* Sodium phosphate............................................ 4.10

The following composition is quoted from Hilgard as representing 

the soluble salts in an alkali crust at the San Joaquin Valley Agricultural Experiment Station, near Tulare City, Cal.:

Composition of alkali salt in San Joaquin Valley, near Tulare City, Cal,

Potassium sulphate. .......................................... 3. 25

Sodium nitrate.............................................. 16.40

Sodium sulphate. ............................- 20. 91

Sodium chloride.............................................. 12. 21

Sodium carbonate........................................... 27.02

Sodium phosphate........................................... 1. 87

Organic matter......'........................................ 17.07

\ Ammonium carbonate........................................ 1.27

100.00

Bailey records * the occurrence of niter at several other localities, as 

follows:

Pilot. The Pilot niter district, located on the old beach line east of Searles-Lake, 

at the south end of the Slate Range. It takes its name from Pilot Peak, a famous 

landmark of the desert that is about 20 miles south of this district.

Danby. The existence of niter has been reported * * * in the playa deposits 

near the salt beds at Danby Lake, and locations were filed upon the land in 1901.

Volcano. Locations covering 4,800 acres have been made along the old beach lines 

[of Lake Le Conte, the former high level of the Salton Sea] east of the Mud Volcanoes, 

in T. 10 S., B. 14 E. in this [San Diego] County. The few specimens brought in gave 

from 3 to 5 per cent of niter.

ARIZONA.

Lindgren notes the occurrence of gerhardtite, a nitrate of copper, 

in the Clifton-Morenci district, Arizona,2 where this mineral is found 

in the cliffs of granite porphyry in the deeply eroded .Chase Creek 

Canyon at Metcalf. He describes the mineral as formed by the 

trickling of atmospheric waters over and through rocks containing a 

small percentage of copper.

Dana also notes that gerhardtite has been found in the copper 

mines at Jerome, Ariz.

Potassium, sodium, and calcium nitrate are reported by Guild 3 

from several localities in Arizona, as follows:

This well-known compound (niter, KN03 ) is frequently formed on old walls, in 

caves, and on the sides of mine shafts, usually, however, in such small quantities as

i Bailey, G. E., The saline deposits of California: Bull. California State Min. Bur. No. 24,1902, pp. 178,180. 

a Lindgren, Waldemar, Copper deposits of the Clifton-Morenci district, Arizona: Prof. Paper IT. S. Geol. 

Survey No. 43,1905, p. 121. 

» Guild, F. N., The mineralogy of Arizona, Chemical Pub. Co., Easton, Pa., 1910, p. 81.
28 JTITBATE DEPOSITS.

to escape observation. It is even said to develop in old mortars to the extent of 

5 per cent (Dana, System of Mineralogy). The writer has observed it associated with 

sodium carbonate as a thin white covering on the surfaces of the overhanging limestone shelves in the ancient cliff dwellings of Walnut Canyon, about 12 miles from 

Flagstaff. The walls of the canyon here are made up of layers of soft and hard limestone, or more appropriately calcareous sandstone, which has disintegrated, yielding 

a series of shelves that have been very conveniently utilized as dwellings by the 

ancient inhabitants of Arizona.

Nitrocalcite "is a hydrous nitrate of calcium sometimes met with in limestone 

caves, where doubtless an interaction has taken place between the calcium carbonate 

and bat guano or other organic compounds. A bacteriological action may also be 

concerned in its formation more or less direct from the atmosphere. It has been 

reported as occurring in the Mammoth Cave in Kentucky. A sample of this mineral 

mixed with a large quantity of earth was received at the University of Arizona during 

the summer of 1907 and identified as calcium nitrate by Dr. A. E. Vinson of the 

Agricultural Experimental Station. Correspondence with the sender of the sample 

brought the following interesting information:

"The calcium nitrate occurs in vents in the lower Carboniferous limestone, fissures 

that cut across the bedding planes and are therefore perpendicular. There are several of these vents grouped close together exposed to full view in the railroad cut 

facing the Gila River about 2 miles above Winkelman. The face at this spot is sheer 

wall about 100 feet high and the vents filled with the nitrate are visible from top to 

bottom. None of them are more than 6 to 8 inches wide, and the nitrocalcite seems 

to be mixed with red iron."

Cameron * quotes reports of nitrate deposits at Briggs, Yavapai 

County, Ariz.

NEW MEXICO.

/

Nitrate salts are quoted by Cameron 1 as reported at Pena Blanca, 

near Mesquite, Dona Ana County, and at Queen, Eddy County, N.

Williams 2 states that nitrate of soda had been reported as occurring 

in the extreme southeastern portion of New Mexico in considerable 

quantity. " It is deposited here by a few springs, the greater number 

being in [the State of] Chihuahua, Mexico, just across the boundary 

line. No disposition is made of the product, beyond the shipment 

of a limited quantity to Chihuahua by Mexicans."

TEXAS.

W. B. Phillips has reported nitrate of soda in Candelaria, Presidio 

County, Tex., the type of deposit possibly being similar to that of 

the deposits in adjacent parts of Mexico, especially in the State of 

Chihuahua.

Potassium niter in Texas 3 is also noted as occurring in "tufts, 

masses, or incrustations in cave deposits from El Paso County, north

1 Cameron, F. K., A preliminary report on the fertilizer resources of the United States: S. Doc. No. 190, 

62d Cong., 2d sess., 1912.

2 Williams, Albert, Mineral Resources IT. S. for 1882, U. S. Geol. Survey, 1883, p. 599.

8 Simonds, F. W., The minerals and mineral localities of Texas: Bull. University Texas No. 5, 1902. t>. 60.
ORIGIN OF NITRATE SALTS. 29

of Van Horn, specimens of which were collected by E. M. Skeats. It 

is said to occur also in San Saba County."

Williams' quotes niter as occurring in caves in "Burnet, San Saba, 

and other counties to the west of them."

BRITISH COLUMBIA.

Niter is reported in Canada 3 as having been found in cavities in 

calcareous tufa on Nazco Kiver and at Big Bar, Fraser River, British 

Columbia.

NITRATE SPECIMENS IN THE NATIONAL MUSEUM.

Specimens of niter from the Leucite Hills, Wyo., of calcium nitrate 

from Mammoth Cave, Ky., and of the white granular salt from

Gerlach, Nov., are in the collections of the National Museum. Other

than these the collections contain no examples of niter salts from the 

United States, although the German and Chilean localities are well 

represented.

ORIGIN OF NITRATE SALTS.

PRIMARY SOURCE.

A general summary of the natural occurrence and of the chemical 

and geological relations of nitrogen compounds has been published 

by F. W. Clarke,3 and from it the following review is chiefly obtained:

Nitrogen composes about three-fourths of the atmosphere, in which 

it is uncombined and essentially inert. In combined form in the 

earth's surface or in the ocean or other waters it forms an inappreciably small part. It is abundant in organic matter.

All the nitrogen in organic matter came originally from the air. 

Through the agency of microbes or bacteria certain plants withdraw 

nitrogen directly from the air. By decay or combustion of organic 

matter some of this nitrogen is again set free, and some remains in 

combined forms.

Salts of nitrogen occur in most soils, where they are necessary for 

the support of plant growth. They accumulate especially in cave 

earth, if there is an abundance of decomposing organic matter and 

if the soil is protected from the leaching action of surface waters. In 

some arid regions, as in Chile, nitrates exist in enormous quantities.

Oxides of nitrogen are produced by electrical discharges yielding 

with the moisture of the air nitric and nitrous acids. Nitrogen in the 

form of ammonia is also present in the air. Some volcanic waters 

contain nitrogen in the form of ammonium compounds.

i Williams, Albert, List of useful minerals in the United States: Mineral Resources U. S. for 1887, U. S. 

Geol. Survey, 1888, p. 794.

» Hoffman, Q. C., Annotated list of the minerals occurring in Canada: Geol. and Nat. Hist. Survey 

Canada, 1890.

3 The data of geochemistry, 2d ed.: Bull. U. S. Geol. Survey No. 491,1911, pp. 18, 40,49,109, 268-269.
30 NTTBATE DEPOSITS.

OCCURRENCE IN SOILS.

Nitrogen exists in the soil in at least three forms in organic material (albuminoid nitrogen), as ammonia or ammonium salts (amniQniacal nitrogen), and as nitric acid or nitrate salts (nitric nitrogen). 

The average amount of nitrogen present in agricultural soils is given by 

authorities as from 0.1 per cent to 0.3 per cent, though occasionally, 

as in certain soils rich in organic matter, reaching 4 or 5 per cent.3 

Hilgard, as elsewhere quoted (pp. 26-27), describes places at which 

nitrates occur in soil in California in exceptional abundance, and 

Headden has described similar conditions in Colorado (pp. 14-15).

HYPOTHESES OF ORIGIN.

Probably the greater part of the nitrates contained in soils are the 

product of bacterial action. Doubtless some at least of the local 

concentrations of nitrate salts accumulated from this source. Organic 

substances decompose in the presence of certain nitrifying organisms 

which are almost everywhere available in soils and elsewhere, producing ammonia and then nitrous or nitric acid. In contact with the 

free air in a natural soil nitrates are finally produced. The nitrification takes place only in the presence of some base with which the acid 

formed will combine.

Attention may here be 'called to an apparent relation of salt produced to the character of the country rock in which the salt occurs. 

At Gerlach, Nev., and Grass Valley, Utah, the potassium nitrate salts 

are found in a brecciated country rock which is an acidic lava, rich 

in potash-bearing minerals. At Lovelock, Nev., the sodium base may 

have been supplied from residues left by the Lahontan lake waters. 

In the cave deposits of the Eastern States, which are mostly reported 

as occurring in limestone caverns, the common salt is calcium nitrate. 

Thus the nitrate salt is to a certain extent at least a product of 

decomposition or combination with the country rock in which it is 

found.

It is still an unsettled question as to how largely the volcanic 

hypothesis will explain the origin of nitrates either disseminated or in 

the more concentrated deposits. Ammonium salts and nitrides are 

undoubtedly present in volcanic sublimates. The association of 

borates with nitrogen compounds in salines or in solution is suggested 

as indicative of a volcanic origin for the nitrogen, since the volcanic 

origin of many of the borate occurrences seems fairly well established.

No generally accepted or satisfactory explanation for the origin of 

the South American nitrates appears yet to have been found.

Undoubtedly some or perhaps most of the accumulations of nitrate 

salts have been transported in water solution and owe their mime2 Merrill, G. P., Bocks, rock weathering, and soils, 1897, p. 372.
OEIGIF OF NITBATE SALTS. 31

diate position or condition to the manner of crystallization from the 

evaporating waters that contained them. Thus some deposits may 

have been formed by the evaporation of sea, lake, or spring waters, 

in which their ultimate origin is remote, or may have been accumulated through solution from bacterial or other sources near by.

THE PROCESS OF NITRIFICATION.

The following is an extract from a treatise on industrial chemistry, 1 

describing the history of the theories concerning nitrification and a 

summary of the conditions under which the nitrifying bacteria are 

active:

Nitrates are continually being produced in fertile soil; if they are removed by 

washing, they are speedily replaced by a fresh formation. The production is greatest 

in the case of well-manured soils.

The occurrence of potassium nitrate as an efflorescence on soils, TOCks, and old walls, 

especially in hot climates, has long been known. East Indian saltpeter is obtained 

by lixiviating the soil surrounding the house drains in old villages (C. J. 1868,318). 

The enormous deposits of sodium nitrate in the rainless table-land of Peru are of the 

highest technical importance.

The process of nitrification has in former years been artificially conducted on a large 

scale, nearly all the niter employed on the continent of Europe being produced in this 

manner. This manufacture is now superseded, saltpeter being produced more cheaply 

at the present time by the reaction of sodium nitrate with potassium chloride. 'The 

niter-yielding "beds" or "walls" formerly constructed consisted of porous earth, 

enriched with animal manure and wood ashes, watered at first with urine and afterward with water. After two years the niter beds were sufficiently rich in niter to be 

worth extraction; 1,000 pounds of soil might then yield 5 pounds of crude niter. 

General information regarding this manufacture will be found in Dumas's "Traite" de 

chimie." The French mode of operation is described in detail in Boussingault'e 

"Agronomic, chimie agricole et physiologie," 2,1861, 23.

Numerous theories have been held as to the manner in which nitrates are produced 

in soil. It has been assumed that nitrogen gas is oxidized in a moist porous soil by 

ordinary oxygen or by ozone, or that ammonia is oxidized in a similar manner, or by 

the ferric oxide generally present in soil. Nitrogenous organic matter is supposed to 

contribute to the production of niter by acting as a source of ammonia or nitrogen gas. 

An account of most of the theories of this description will be found in a lecture on 

nitrification by Cloez (Lecons de chimie et de physique professe'es en 1861, a la 

Socie'te' chimique de Paris). The theories in question were in fact entirely unsatisfactory, as, although nitrogen, ammonia, and many nitrogenous organic bodies could 

be oxidized by powerful means so as to yield nitric acid, chemists were unable to 

produce this acid under the conditions of a natural soil unless soil itself was present.

The first suggestion that nitrification might possibly be due to the action of a living 

organism came from Pasteur in 1862. A. Muller, in 1873, suggested that the process 

was due to a ferment. Schloesing and Muntz, in 1877, satisfactorily proved that nitrification was the work of a living agent. They showed in this and subsequent communications that the nitrifying agent could be transplanted from one medium to another,

i Thorpe, T. S., Dictionary of applied chemistry, vol. 2,1891, pp. 698-700 (contribution by R. Warington). Abbreviations of the titles of journals and books referred to: A. a., Annales agronomiques? A. Ch., 

Annales de chimio et de physique; C. J., Journal of the Chemical Society of London; C. N., Chemical 

News; C.R.,Comptes rendus hebdomadaires des seances de I'Acad&nie des sciences, Paris; Pr., Proceedings of the Royal Society.
32 NITRATE DEPOSITS.

that its action was strictly limited by the conditions necessary for the life and activity 

of bacteria, and that its function was destroyed by temperatures (55°) and reagents 

(as chloroform), which are fatal to such organisms. The principal papers of Schloesing 

and Mtintz are C. R. 84, 301; 85, 1018; 86, 892: 89, 891, 1074. The main conclusions 

were confirmed by Warington (C. J. 33, 44), and afterward by many other investigators.

The nitrifying organism is one proper to the soil; it occurs also in sewage and in 

river water; it is usually present in air. or rain. The organism does not occur in soil 

beyond a certain depth below the surface. In the heavy soil of Rothamsted, Herts, 

out of 39 samples of soil of about 0.2 gram each, taken at various depths down to 3 feet, 

only one failed to produce nitrification when introduced into a weak urine solution. 

At 5 feet one-half the samples failed to produce nitrification. Below 6 feet the soil had 

apparently no nitrifying power (C. J. 51, 1887, 118).

Schloesing and Miintz attempted to isolate the organism producing nitrification. 

After making many successive cultures in weak sterilized sewage, they found finally 

remaining a small round or oval coccus, which they believe to be the organism in question. No satisfactory proof was, however, given that they had obtained a pure culture. 

Attempts to isolate the organism by cultivation on gelatin have failed.

Lately, P. F. Frankland (Pr. 47, 296), by employing the dilution method of isolation, has apparently succeeded in obtaining the organism in a pure state. When cultivated in an ammoniacal solution containing only mineral salts its form is that of a very 

short bacillus; grown in broth it becomes distinctly a bacillus. It is characteristic of 

the organism that when grown in ammoniacal mineral solutions it refuses to propagate 

on gelatin. From broth cultures a tardy growth on gelatin may be obtained. The 

organism is of very slow growth, and produces little, if any, turbidity in ammoniacal 

mineral solutions.

Still more recently the organism has been isolated by Winogradsky (A. de 1'InstitutPasteur, 1890, 213, 257). By successivevcultivations in mineral solutions he has at last 

only two organisms present. In these he observed the formation of gelatinous clots at 

the bottom of the vessel; these clots possessed the power of nitrifying in a high degree. 

He collected these clots, washed them, and spread them on gelatin. After 10 days he 

seeded fresh ammoniacal solutions from those parts of the gelatin surface on which 

no growth had appeared. He thus obtained the organism pure. When young it is 

nearly round, but is most often ellipsoid; diameter, 0.9-l.Ow; length, l.l-l.Su. The 

longer ones show the strangulation preceding division; the form is occasionally spindleBhaped, With blunt ends. Chains of three of four individuals are rare. There are no 

spores. The organism is generally immobile, and collected at the bottom of the solution in a mass of zooglcea; but for a short period in the course of nitrification a general 

mobility sets in, and the liquid becomes turbid; a day after the organism is again in 

repose. Provisionally, the author designates it a nitromonas.

Little is yet known of the action of the organism when alone, nearly all the experiments on nitrification hitherto made having been confessedly performed with a mixture of organisms.

The substances which are nitrifiable by soil, or in solutions seeded with soil, are 

very numerous; they include ammonia, ethylamine, urea, asparagine, thiocyanates, 

albuminoids, gelatin, etc. In every case apparently in which an organic substance 

is nitrified the formation of ammonia precedes the formation of nitrous or nitric acid, 

ammonia, or rather ammonium carbonate, is thus perhaps the only nitrifiable substance. Whether the nitrifying organism is itself capable of attacking organic matter 

and producing ammonia, or whether the action of other organisms is necessary to 

effect the preliminary formation of ammonia, is yet undetermined.

The products of nitrification may be nitrites or nitrates. WTien nitrification takes 

place in a natural porous soil, only nitrates are produced. Nitrites appear in soil only 

as products of reduction when air is excluded by an excess of water. When nitrification is started in a solution by the addition of soil, the oxidation may be purely
OBIGIN OP NITEATE SALTS. 33

nitric in character, or nitrites may be abundantly formed in the earlier stages of the 

process, especially if the solution is strong, alkaline, and at a relatively high temperature; but in the end the nitrites are all converted into nitrates. If, however, successive cultures are made in sterilized ammoniacal solutions, starting with a solution 

nitrified by soil, a point is soon reached at which nitrites only are produced, and 

these nitrites never change into nitrates. An alkaline condition of the solution is 

highly favorable to this change in the character of the process. Some difference is 

thus established in the agent, and it is quite possible by seeding solutions from different 

sources to obtain a purely nitrous and a purely nitric process of oxidation in similar 

solutions and under identical external conditions. That the nitrites are not here a 

product of reduction is shown by their special formation in solutions of ammonium 

carbonate destitute of organic matter (v. also Munro's experiments, C. N. 56, 1887, 62). 

The nitrifying organism separated both by P. F. Frankland and *by Winogradsky is 

found to be only capable of yielding nitrous acid. From these facts we must conclude, 

either that the oxidation of ammonia to nitrites, and of nitrites to nitrates, is a distinct

process performed by different organisms, or that the original organism producing

nitric acid in the soil becomes weakened by continued cultivation in certain soluions and loses its faculty of converting nitrites into nitrates. The true explanation 

is not yet known.

The oxidizing power of the organisms in soil is by no means limited to the oxidation of ammonia or of organic matter. Miintz (A. Ch., May, 1887) has shown that 

iodides may be converted into hypoiodites and iodates, and that bromides undergo a 

similar change. The oxidation of iodides is not apparently a secondary reaction of 

nitrification, for it may take place in the absence of nitrifiable matter. It is interesting to observe in this connection that iodates occur in the deposits of sodium nitrate 

in Peru.

The conditions under which nitrification takes place have been pretty well ascertained. For the nitrifying organism to act with vigor the substances necessary for 

its nutrition must be present. We should suppose, according to the accepted ideas 

respecting the nutrition of such organisms, that a supply of organic carbonaceous matter would be necessary; we have already stated, however, that the nitrifying organism 

has been found to flourish and actively discharge its functions in purely inorganic solutions. Winogradsky has recently established this fact by rigorous experiments, and 

has shown, by determinations of carbon in the solutions, that the nitrifying organism 

is capable of producing organic matter from carbonic acid and ammonia without the 

aid of light. He suggests that, as in the animal body ammonium carbonate is converted into urea, so in this organism an amide may be the first compound produced.

For the nutrition of a living organism the presence of certain ash constituents is 

essential. It has been shown that nitrification can not take place in the absence of 

phosphates (C. J. 45, 641). The necessity for other ash constituents has not yet been 

made the subject of experiment.

The presence of free oxygen is essential to nitrification. Schloesing (C. R. 77, 203, 

353) has determined the rate of nitrification in soil containing different proportions 

of water and maintained in atmospheres containing various proportions of oxygen. 

With soil holding 16 per cent of water a considerable amount of nitrification took place 

: when 1£ per cent of oxygen was present in the atmosphere, but the rate of nitrification increas^i fourfold when 21 per cent of oxygen was present. An increase in the 

proportion of water to 24 per cent raised the rate of nitrification in atmospheres containing a small percentage of oxygen, the quantity of dissolved oxygen being thus 

increased.

For nitrification to take place there must be some base with which the nitrous and 

nitric acid produced may combine. When a solution of ammonium carbonate or 

urea is nitrified, the action proceeds till one-half of the nitrogen is oxidized and then 

52096° Bull. 523 12 3
34 NITRATE DEPOSITS.

stops, ammonium nitrite or nitrate being the final product. The whole of the ammonia 

is nitrified only when an excess of base is present. The substance which acts best 

for this purpose is calcium carbonate; this is also the base usually present in soils. 

If the solution to be nitrified contains a soluble alkali, nitrification is hindered if the 

alkalinity exceeds a very small amount, and does not commence at all when the 

alkalinity is still further increased. The highest degree of alkalinity which has been 

found compatible with nitrification corresponded to 368 parts of nitrogen as ammonium 

carbonate per million of solution. With sodium monocarbonate the limit was nearly 

the same; with disodium carbonate a much smaller degree of alkalinity sufficed to 

prevent nitrification. The same distinction was found to exist between the basic 

and acid carbonates of ammonium.

It follows from what has been just stated that only weak urine solutions can be 

nitrified. In Warington's experiments a 12 per cent solution was the maximum strength 

nitrifiable. This fact must be borne in mind when liquid manure or gas liquor is 

applied to land. If, however, an excess of gypsum is added to urine before the introduction of soil, solutions of far greater strength may be nitrified, the gypsum reacting 

with the ammonium carbonate as soon as it is formed, ammonium sulphate and calcium carbonate being produced (C. J. 45, 653; 47, 758). The favorable influence of 

gypsum on nitrification has been noticed by several investigators.

The activity of nitrification is largely dependent on temperature. The process has 

been shown to occur at temperatures as low as 3°. As the temperature rises the rapidity of the action increases, the optimum temperature being, according to Schloesing 

and Miintz, 37°. Above this point there is, according to the same authorities, a rapid 

decline, very little nitrification taking place at 50°, and beyond 55° there is no action. 

The influence of temperature is a point requiring further study.

In the case of solutions, darkness is far more favorable to nitrification than light. 

When a solution is exposed to a strong light, nitrification ceases altogether.

In a moist, aerated soil, at ordinary temperatures, the nitrification of an ammonium 

salt commences almost immediately after its application. When, on the other hand, 

a few milligrams of soil are introduced into a relatively large bulk of a suitable ammoniacal solution, a period of several weeks may elapse before nitric or nitrous acid appears, 

after which time nitrification will proceed with rapidly increasing speed. This long, 

so-called "incubation period" is probably due to the slow growth of the organism, 

and the difficulty it finds in adapting itself to altered conditions. If, when nitrification is completed, the solution is decanted, and the bottle filled up again with an 

ammoniacal solution similar to the first, nitrification will now commence in a comparatively short time, and by repeating this operation nitrification may be brought to begin 

in a few hours. When two solutions of different degrees of concentration are seeded 

with soil at the same time, nitrification will always commence first in the weaker 

solution.

The process of nitrification is suspended by a high temperature (55°), and by the 

presence of chloroform, carbon disulphide, phenol, mercuric chloride, and other 

bodies which are injurious to the life of bacteria. The drying of a soil, even at a low 

temperature, is fatal to the nitrifying organisms which it contains.

If both organic matter and denitrifying organisms are present, all nitrates present 

may be destroyed; the nitrifying organism is, however, uninjured, and will resume its 

activity as the organic matter disappears. ^

Natural soils and river waters usually contain both nitrifying and denitrifying 

organisms, and the character of the process which occurs is determined by the conditions 

of the moment. The same soil which rapidly nitrifies when in a moist, aerated condition, becomes a vigorous denitrifying medium when waterlogged. The nitrifying 

river water becomes denitrifying when polluted with sewage. The products.of denitrification are various, according to the nature of the organisms present; nitrites, nitric 

oxide, nitrous oxide, or nitrogen gas may be produced. In the case of the three last-
VALUE. 35

named products there is, of course, a loss of nitrogen in the form of gas. For the literature of the subject v. C. J. 53, 1888, 742. Miintz has shown that chlorates, bromates, 

and iodates are reduced equally as nitrates.

The following references may be of use:

The conditions of nitrification, Schloesing (C. R. 77, 203, 353), Warington (C. J. 35, 

429; 45, 637), Munro, (C. J. 49, 632); The nitric acid in soils, Lawes, Gilbert, and Warington (J. R. A. S. 1883, 331), Lawes and Gilbert (C. J. 47, 380), Deherain (A. a. 1888, 

287); The nitrification of manures, Deherain (A. a. 1887, 241), Schloesing (C. R. 109, 

423, 883); The nitric acid in drainage and well waters, Lawes, Gilbert, and Warington 

(J. R. A. S. 1881, 241, 311; 1882, 1; C. J. 51, 500).

SUMMARY.

As explained in the foregoing pages, nitrogen exists chiefly as the 

uncombined gas that forms the greater part of the atmosphere. 

In relatively much smaller proportion; however, it occurs combined 

in three forms, namely, in organic matter, as ammonia and ammonium 

salts, and nitric acid, and nitric acid salts or nitrates. The agencies 

which are known to accomplish the conversion of the inert gaseous 

nitrogen into the combined forms are the assimilating action of growing organisms (plants and animals); the action of microbes or bacteria ; and fixation by the discharge of electricity through the air. The 

occurrence of ammonium salts in volcanic waters is noted without an 

attempt to explain the origin of the salts.

The present paper is intended to deal chiefly with the nitrogen salts 

known to occur in nature in the nitric acid or nitrate form.

The extreme solubility of nitrate salts renders it unlikely that concentrated deposits will remain anywhere except in places not subject 

to or protected from the solvent action of rain, surface, or moving 

ground waters. Thus nitrate salts are found chiefly in caverns, 

caves, or under overhanging ledges, or, as in the Chilean and other 

South American occurrences, in a region of most exceptional aridity.

The frequently reported deposits of nitrate salts in caves or overhanging ledges in this country as well as elsewhere probably constitute a well-defined type. Field observations have led the writer 

to the belief that a considerable number, probably a majority, of 

such deposits are derived from the decomposition of bat or similar 

guano. It happens that these nest-building animals select for their 

habitation sites favorable to the accumulation and preservation of 

the soluble nitrate salts.

VALUE OF THE DEPOSITS.

By fd^iihe greater part of the nitrate salts formed are probably 

carried off in solution by water and distributed or lost sooner or later, 

and only in the few most favored localities are the crystalline salts 

themselves retained. Hence it seems fair to assume that most of 

the reported occurrences of these salts are of little or no economic 

value. This opinion appears to be to a certain extent confirmed by
36 FITEATE DEPOSITS.

the history of nearly every attempt to develop such deposits. Many 

fine specimens or samples showing high percentages of nitrate salts 

are obtained, but the deposits do not continue into the mass of the 

rock, and only rarely can sufncient material for a single shipment be 

collected.

Nevertheless an assertion that none of the nitrates of this or similar 

types of deposits will prove commercially workable is probably not 

warranted.. Such deposits have proved to be of value under exceptional conditions, as when they were utilized for, the manufacture 

of gunpowder, during war times, in the Eastern States; and it is entirely possible that changing conditions may render some of the west- 

'ern deposits valuable. It must be recognized, however, that so far as 

may be judged from present evidence, few, if any, of the known 

deposits at present warrant much outlay for development as a source 

of commercial nitrate salts.

o