Distribution of Gold and 

Some ·Base Metals in the 

Slana Area, Eastern 

Alaska Range, Alaska 

.};\'(if!:)fif.' :~::::..';·;;)(:;:;:{·) Work done in cooperation with the State of Alaska, Division of Mines and Minerals 

~\~ 1 n r:::::::: :.~:~: f ~ ~ =. =.:.:. ~-::·.~::::::::· ~:~~:~:~ 

Distribution of Gold and 

Some Base Metals in the 

Slana Area, Eastern 

Alaska Range, Alaska 

By Donald H. Richter and Neal A. Matson, Jr. 

GEOLOGICAL SURVEY CIRCULAR 593 

Work done in cooperation with 

the State of Alaska, Division 

of Mines and Minerals 

Washington 1968 
United States Department of the Interior 

STEWART l. UDALL, Secretary 

Geological Survey 

William T. Pecora, Director 

Free on application to the U.S. Geological Survey, Washington, D.C. 20242 
Abstract- - - - - -

Introduction - - - -

CONTENTS 

Geologic setting- - - - - - - - - - - - - - - - - - - - - - - - - - -

Economic geology- - - - - - - - - - - - - - - - - - - - - - - - - - - - - -

Geochemistry- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -

Sampling and analytical procedures - - - - - - - - - - - - - - - - - - -

Background and anomalous concentrations of metals - - - - - - - - - -

Distribution of metals in stream sediments - - - - - - - - - - - - - - -

Distribution of gold in rocks - - - - - - - - - - - - - - - - - - - - - - -

Economic potential - - - - - - - - - - - - - - - - - - - - - - - - - - - - -

References cited - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -

ILLUSTRATIONS 

Figure 1. Index map of part of south-central Alaska showing 

Page 

1 

1 

1 

2 

2 

2 

2 

3 

3 

4 

4 

Page 

Slana area- - - - - - - - - - - - - - - - - - - - - - - - - - 13 

2. Sample-location map, Slana area- - - - - - - - - - - - - - - 14 

3. Explanation for geologic maps showing distribution 

of gold and base metals (figs. 4 -8)- - - - - - - - - - - - - 15 

4-8. Maps showing distribution of gold and base metals in the 

Slana area: 

4. Gold - - - - - - - - - - - - - - - - - - - - - - - - - - 16 

5. Copper- - - - - - - - - - - - - - - - - - - - - - - - - - 17 

6. Lead - - - - - - - - - - - - - - - - - - - - - - - - - - - 18 

7. Zinc - - - - - - - - - - - - - - - - - - - - - - - - - - - 19 

8. Molybdenum- - - - - - - - - - - - - - - - - - - - - - - 20 

TABLES 

Table 1. Gold and base-metal content of stream sediments- - - - - - - -

2. Gold content of rocks- - - - - - - - - - - - - - - - - - - - - - -

3. Concentration of gold and base metals- - - - - - - - - - - - - -

III 

Page 

5 

11 

12 

Distribution of Gold aRd Some Base Metals in the Slana Area, 

Eastern Alaska Range, Alaska 

By Donald H. Richter and Neal A. Matson, Jr. 

Abstract 

In the Slana area of the eastern Alaska Range, Paleozoic and 

Mesozoic sedimentary and volcanic rocks have been extensively 

intruded by two suites of igneous rocks, one dioritic and one quartz 

monzoniJ:ic. Anomalous concentrations of gold and copper are associated with diorite-quartz diorite intrusives, as indicated by 

stream-sediment and bedrock samples, and anomalous concentrations of lead-zinc and lead-molybdenum are associated with the 

zoned Ahtell Creek quartz monzonite-granodiorite pluton. Metal 

concentrations as high as 7 ppm (parts per million) gold, 365 ppm 

zinc, 250 ppm lead, aQd 25 ppm molybdenum have been found in 

the stream sediments. The distribution of gold in bedrock follows 

very closely the pattern shown by the stream-sedimentdata. Random samples of dioritic rocks and their hypabyssal equivalents, 

from areas drained by streams anomalously high in gold, contain 

as much as 0.3 ppm gold. The data suggest that (1) placer gold deposits may be present in streams draining the p r inc i p a I area 

anomalous in gold and (2) bedrock sources of the anomaly should 

be evaluated as possible low-grade disseminated gold deposits. 

INTRODUCTION 

The Alaska Division of Mines and Minerals made 

geologic and geochemical studies of the Slana area of 

the eastern Alaska Range from 1963 to 1966. The s e 

studies resulted in a geologic report (Richter, 1966) 

and in the identification of two base-metal anomalies 

(Richter, 1 ~65). The investigations were continued and 

extended by the U.S. Geological Survey in 1967 as part 

of its Heavy Metals program particularly to determine 

the relationship of gold to the geologic setting. Gold 

analyses made on all the stream-sediment samples 

and many rock samples collected during the Statesponsored studies disclosed sev~eral gold anomalies 

and the fact that the geologic associations of gold are 

markedly different from those of the base metals. This 

report presents all the newly available data on gold 

distribution as related to geology of the Slana are a 

together with a review of the published data on the 

base metals. 

The Slana area, as informally r e fer r e d to here, 

covers approximately 240 square miles on the south 

flank of the eastern Alaska Range, mostly between 

the Chistochina and Slana Rivers (fig. 1). It includes 

parts of the Gu1kana C-1 and D-1 and the Nabesna 

C-6 and D-6 quadrangle maps (scale 1:63,360). The 

Tok Cutoff of the Glenn Highway runs about 26 miles 

through the area and affords relatively easy access 

to most of the back country. 

1 

GEOLOGIC SETTING 

The Slana area lies south of the Den a 1 i fault, a 

major trans-Alaska strike-slip lineament, in aregion 

of upper Paleozoic and Mesozoic sedimentary and volcanic rocks that have been intruded by two compositionally and texturally distinct groups of igneous rocks. 

A genera'Iized stratigraphic column and brief description of the bedded rocks are given below. 

Cretaceous and Jurassic 

Angular unconformity. 

Permian - - - - - - - -

Unconformity. 

Description 

A r g i 11 i t e containing 

i n t e r b e d d e d siltstone, g r a y w a c k e, 

and conglomerate. 

Amygdaloidal b a sa 1 t 

containing interbedded limestone, 

bas a 1 t, and limestone conglomerate. 

Permian - - - - - - - - - - - - Limestone, argillite, 

and minor coarser 

grained clastic 

r o c k s (Manko men? 

Formation). 

Permian - - - - - - - - - - - - Volcaniclastic r o c k s 

c on t a i n i n g minor 

imp u r e limestone. 

Permian and 

Pennsylvanian(?) - - - - - - - Andesitic v o 1 can i c 

rocks, including 

flows, tuffs and 

breccias, mud-avalanche deposits, and 

volcaniclastic rocks. 

T hi s sedimentary and volcanic sequence, except 

for some of the younger Mesozoic rocks, was intruded by a large heterogeneous diorite-quartz diorite complex and a number of satellitic( ?) bod i e s 

whose composition was similar but also inc 1 u de d 

granodiorite, gabbro, and anorthosite. A more alkalic, 

zoned pluton of quartz monzonite and granodiorite, 
termed the Ahtell Creek pluton in previous reports, 

intruded the Permian volcanic and volcaniclastic rocks 

in the western part of the area. Both groups of intrusive igneous rocks are younger than Permian and 

probably older that Late Jurassic, although neither 

their absolute nor relative age is well known. 

The structural grain of the area, revealed by faults, 

fold axes, bedding, and orientation of some of the 

dioritic intrusives, parallels the northwestward trend 

of the Alaska Range and its tectonic elements. Only 

the Ahtell Creek pluton, which trends northward, appears to be discordant with the regional structure. 

Bedding and flow layering in most of the rocks dip at 

moderate angles to the northeast toward the Denali 

fault. 

ECONOMIC GEOLOGY 

Prospecting has been carried out in the Slana area 

since before the turn of the century, and between then 

and the early 1930's a number of argentiferous basemetal quartz veins were discovered. Placer gold was 

also discovered during the early prospecting. Figures 

4-8 show the distribution of gold and base metals in 

the area. The letters and numbers used with references to figures in subsequent sections are map coordinates. 

It was not until 1934 that a placer deposit on Grubstake Creek (fig. 4, D-3) was exploited commercially 

(Moffit, 1938, p. 48-50). This placer deposit and another on Slope Creek (fig. 4, D-4), which drains the 

same general area, have been worked intermittently 

since then. Total gold production from these two deposits probably has been less than $30,000, and at 

present ( 1968) both properties are inactive. There is 

no recorded production from any of the veins in the 

area; however, two prospects, the Silver Creek (figs. 

4-8, F -3) and the Silver Shield (figs. 4-8, E-4), are 

currently being explored. 

The veins and the lead, zinc, and m o I y b den u m 

anomalies are spatially and apparently genetically 

r e 1 ate d to the Ahtell Creek quartz monzonitegranodiorite pluton. These veins and anomalies indicative of possible mineral deposits occur chiefly 

in the fine-grained border zone around the southern 

1 o be of the pluton and in adjacent hornfels country 

rock. Most of the veins are thin simple hydrothermal 

fissure fillings which are dominantly massive white 

quartz and locally minor barite and carbonate minerals and scattered crystals or segregations of galena, 

chalcopyrite, sphalerite, andargentiferous tetrahedrite. In the strongly altered area south of Long 

Lake (figs. 4-8, C-2), small scattered flakes of molybdenite are associated with quartz, pyrite, and 

sericite. 

The placer gold in Grubstake and Slope Creeks is 

fine grained and wiry and shows no evidence of lengthy 

transport. Earlier it had been thought that the gold 

was also derived from lode deposits within the border 

zone of the Ahtell Creek pluton (Richter, 1965 ); how2 

ever, the data presented here suggest that the gold is 

not associated with this pluton but rather with the 

more mafic diorite-quartz diorite intrusives. 

GEOCHEMISTRY 

The geochemical data presented in this report are 

based on the chemical and spectrographic analyses 

of 258 samples of stream sediments and 105 samples 

of rock collected between 1963 and 1967. These data 

show anomalous concentrations of gold and base metals 

in many stream sediments throughout the Slana area 

and define a number of anomalies which may be significant. Emphasis is directed toward the gold anomalies and the distribution of gold in the country rock; 

the base-metal an om a 1 i e s have been discussed in 

earlier reports (Richter, 1965, 1966), and only a brief 

review of their salient features is presented here. 

Sample locations for both stream sediments and 

rocks are shown in figure 2. Analytical results are 

given in tables 1 and 2 and are shown on the metaldistribution maps (figs. 4-8). 

Sampling and Analytical Procedures 

Stream-sediment samples were collected from active streams at sites yielding as much fine material 

as possible. Copper, lead, zinc, and molybdenum analyses were made on the -80-mesh fraction of all samples by a number of laboratories using colorimetric, 

atomic-absorption, or spectrographic techniques (see 

headnote, table 1 ). Gold analyses were also made on 

the -80-mesh material by Geological Survey laboratories using a hydrobromic acid extraction and atomicabsorption spectrophotometry. For samples weighing 

10 grams or more the lower limit of determination 

for gold was 0.02 ppm (parts per million). However, 

many samples weighed less than 10 grams, and for 

these, 5-, 2-, or even 1-gram amounts were used; 

these small samples raised the lower limit of determination to 0.04, 0.1, and 0.2 ppm gold, respectively. 

Hence, not all gold values are directly comparable, 

and it is very probable that many of the small samples 

contain gold in concentrations exceeding 0.02 ppm. 

The 105 rock samples analyzed for gold were selected from available specimens in an attempt to insure a representative suite of the various rock types 

and to give as much geographic coverage as possible. 

The samples were crushed, ground to -150 mesh, and 

analyzed by the same method used for the stream sediments. Ten grams of material was available for all 

the rock analyses. 

Background and Anomalous Concentrations ofMetals 

Data on the concentration of gold, copper, lead, zinc, 

and molybdenum in the rocks and stream sediments 

of the Slana area are summarized in table 3 and compared with average crustal abundances of these elements. 

These data indicate that the Slana area as a whole 

is not anomalous with respect to any of the analyzed 

elements. All the elements-with the possible excep-
tion of gold, for which data below a concentration of 

0.02 ppm are not available-generally occur in concen- · 

trations of the same order of magnitude as their estimated abundance in the earth's continental crust. 

Moreover, both the mode (most frequent concentration) calculated from stream-sediment samples and 

the mean and mode calculated from rock samples for 

the four base metals are virtually the same. The apparent low mode for copper in rocks may be due to 

limited rock-sample data. 

In this report, concentrations of copper, lead, zinc, 

and molybdenum approximately t h r e e times mean 

background or more are considered anomalous; these 

concentrations are for copper, 150 ppm; lead, 30ppm; 

zinc, 180 ppm; and molybdenum, 6 ppm. These values 

correspond rough 1 y to the break point on the lognormal frequency distribution curves of the met a 1 s 

in stream sediments of the Slana area (Richter, 1966 ). 

For gold the lower limit of detection, or 0.02 ppm, is 

considered anomalous. 

Distribution of Metals in Stream Sediments 

The two conspicuous base-metal anomalies in the 

area, mentioned and described previously (Richter, 

1965, 1966), are obvious from inspection of the metal 

distribution maps. The 1 a r g est of these is a leadmolybdenum anomaly in the vicinity of Long La k e 

(figs. 6 and 8, C-1, -2, andD-1, -2). Slightly anomalous zinc con cent r at ion s were detected in a few 

streams, but with the exception of one stream, copper 

was not present in amounts much above background. 

The other anomaly, high in lead and zinc, is south of 

Flat Creek (figs. 6 and 7, E-2 and F -2). Both anomalies are largely within the border zone of the Ahtell 

Creek pluton. Conspicuous quartz-pyrite alteration 

zones, some as large as 5 acres in extent, and a few 

thin quartz-sulfide veins are exposed near Long Lake. 

The Flat Creek anomaly, which is currently being explored by private industry, is in an area of low relief 

and extensive tundra cover, and no mineralized outcrops were found. 

West of Ahtell Creek a number of streams draining 

the border zone of the Ahtell Creek pluton contain 

slightly anomalous amount s of one or more base 

metals. The relatively high concentration of lead in 

E-4 (fig. 6) is on a small stream draining the Silver 

Shield silver-lead prospect. 

Copper is rather widely distributed throughout the 

area and shows a closer spatial association with the 

diorite-quartz diorite intrusives than with the Ahtell 

Creek pluton. Anomalous concentrations of copper 

occur sporadically along the entire southwest flank of 

the large diorite-quartz diorite mass and 1 o c a 11 y 

around a number of the smaller dioritic intrusives 

(fig. 5). The strongest anomaly, which shows concentrations as high as 400 ppm, is southwest of Indian 

Pass Lake (fig. 5, C-4, -5 and D-4) in an area of 

numerous small hornblende-diorite intrusives. Another small hornblende-diorite intrusive in B -2 and 

C-3 is also the apparent source of a smaller anomaly. 

3 

The hornblende diorites in both these anomalous areas 

are locally pyritized and conspicuously limonite 

stained. The single copper anomaly in the northeast 

part of the area (fig. 5, A-9) is on a stream draining 

cupriferous amygdaloidal basalts and is the only anomaly not known to be related to intrusive rocks. 

The distribution of gold in the Slana area, as defined by the analyses of stream sediments, shows, 

like cop p e r, a marked association with the diorite 

intrusives and with a few exceptions does not correspond to the distribution of the other base met a l s. 

Of more than 30 streams with detectable gold, only 

five drain the quartz-vein-rich border zone of the 

Ahtell Creek pluton and its peripheral hornfels zone. 

Three of these, including one with the strongest 

stream-sediment anomaly detected (7 .1 ppm gold), 

are in an area where dioritic rocks also occur (fig. 4, 

F-2). 

The strongest and most conspicuous gold anomaly 

is southwest of Indian Pass Lake (fig. 4, C-4, -5 and 

D-4) in an irregular area underlain by a number of 

small hornblende diorite intrusives and is coincident 

with the strong copper anomaly. Sediments in 13 

streams draining the area contain more than 0.02 

ppm gold, and sediments in three of these contain 2 

ppm gold. The local placer go 1 d in Grubstake and 

Slope Creeks apparently also has its source in this 

area and not in the nearby border zone of the Ahtell 

Creek pluton, as previously thought. Surprisingly, the 

sediments in Grubstake Creek, the larger of the two 

placer deposits, are only moderately enriched in gold 

(0.04 ppm, sample 94), and this fact suggests that some 

other streams, which show much higher gold concentrations, could also contain gold placer deposits. 

Elsewhere in the area anomalous concentrations of 

gold occur principally along the southwest border of 

the large diorite-quartz diorite complex (fig. 4, B-5 

and C-6), southeast of the Slana River around an arcuate quartz diorite intrusive (fig. 4, D-8, -9 and 

E-8), and west of Ahtell Creek near a small diorite 

intrusive (fig. 4, B -3 ). These t h r e e anomalies are 

defined by only a few stream-sediment samples with 

gold concentrations generally well below 2 ppm and 

are not nearly as promising as the an om a 1 y near 

Indian Pass Lake. 

Distribution of Gold in Rocks 

Gold analyses on 105 rocks collected throughout 

the area as representative geologic samples-not as 

ore mineral samples-show a golddistributionpattern 

similar to that shown by the stream-sediment data. 

Gold analyses of rocks are 1 i s ted in tab 1 e 2 and 

plotted on the gold distribution map (fig. 4 ). 

Only 11 of the rocks analyzed contain detectable 

gold (0.02 ppm or more), and all these are diorites, 

quartz diorites, or hornblende-feldspar porphyries 

believed to be hypabyssal equivalents of the dioritic 

rocks. Moreover, none of the rocks containing detectable gold is from an area outside the anomalies 
defined by the stream sediments. In particular, the 

anomaly southwest of Indian Pass Lake includes the 

most rock samples (seven) showing enrichment in 

gold 2:.nd also the sample with the highest gold content (0.3 ppm, sample R60). Two diorite sa mp 1 e s 

from the anomalous area in B-5 (fig. 4) are enriched 

in gold, as are two quartz diorite samples from the 

anomalous area southeast of the Slana River. Many 

of the rocks containing detectable gold also con t a in 

disseminated pyrite, but pyrite is common in intrusive 

rocks in the area and probably is equally or m or e 

abundant in some of the analyzed quartz monzonitegranodiorite rocks and hornfels. 

ECONOMIC POTENTIAL 

The gold geochemical anomaly in the central part 

of the Slana area appears to warrant further exploration. Sediments in at least three streams draining the 

anomalous area contain in excess of 2 ppm gold, a 

fact suggesting the presence of local placer deposits. 

However, it is probable that the original lode gold 

(possibly in quartz veins) was coarse enough to supply material for workable placer deposits only in the 

restricted area in the border zone of the Ahtell Creek 

pluton at the head of Grubstake and Slope Creeks. lf, 

as seems likely, the gold is disseminated throughout 

the diorites, gold particles in the other streams draining the anomalous area may be extremely fine grained 

and not recoverable by conventional placer mining. 

The possibility of a large low-grade lode deposit 

within the apparent dioritic source rocks of the anomaly should not be discounted. Detailed sampling of the 

dioritic intrusives, especially the more pyrite-rich 

4 

areas, rm y reveal gold concentrations higher than the 

0.3 ppm found in this reconnaissance sampling of the 

bedrock. 

Diorite and quartz diorite intrusives are not restricted to the Slana area of the eastern Alaska Range 

but are known to occur throughout the range from western Alaska through Canada to southeast Alaska. In many 

areas these dioritic rocks are conspicuously altered 

and (or) contain abundant disseminated sulfides. However, little is known concerning the gold content of 

these rocks. One area in which gold deposits seem to 

be genetically related to diorite is in the Chulitna district of the central Alaska Range, where Ross (1933) 

reported that some of the lodes are disseminated iron 

sulfide deposits in diorite porphyry. 

REFERENCES CITED 

Moffit, F. H., 1938, Geology of the Slana-Tokdistrict, 

Alaska: U.S. Geol. Survey Bull. 904, 54 p. 

Richter, D. H., 1965, Geochemical investigation ofthe 

Slana district, south-central Alaska, 1963 and 1964: 

Alaska Div. Mines and Minerals Geochem. Rept. 

2, 14 p. 

1966, Geology of the Slana district, south-

__ c_e_n-tral Alaska: Alaska Div. Mines and Minerals 

Geol. Rept. 21, 51 p. 

Ross, C. P., 1933, Mineral deposits near the West 

Fork of the Chulitna River, Alaska: U.S. Geol. Survey Bull. 849-E, p. 289-333. 

Taylor, S. R., 1964, Abundance of chemical ele~ents 

in the continental crust-A new table: Geoch1m. et 

Cosmochim. Acta, v. 28, no. 8, p. 1273-1285. 
Table 1.--Gold and base-metal content of stream sediments 

[N, not detected (below value shown in parentheses). Ins., insufficient 

sample for analysis. Analysts: Gold, all samples (atomic absorption), 

W. L. Campbell, R. L. Miller, M. s. Rickard, and T. A. Roemer; base metals, 

samples (map No.) 210, 211, 232-234, 239, 244-247 (semiquantitative spectrographic), K. J. Curry and R. T. Hopkins; base metals, all other samples 

(colorimetric and atomic absorption), various (see Richter, 1965, 1966)] 

Map No. Samele No. Sample Concentration ~eem~ (fig. 2) weight 

Laboratory Field (g) Au Cu Pb Zn Mo 

1 355 SD-91 10 N(0.02) 135 15 95 2 

2 356 92 5 N ( .04) so 15 90 2 

3 357 93 10 N( .02) 55 15 65 1 

4 358 94 10 N( .02) 45 10 60 1 

5 359 95 10 N ( .02) so 15 60 1 

6 354 88 5 N( .04) 60 20 90 1 

7 361 98 10 N( .02) 40 10 70 1 

8 362 99 10 N( .02) 20 10 65 1 

9 565 DR-64-451 10 N( .02) 40 10 40 

10 564 450 5 N( .04) 55 15 60 

11 648 454 .1 2.0 250 15 80 

12 649 455 1 N( .2) 175 20 80 

13 650 456 2 N( .1) 450 30 100 

14 637 395 1 N( .2) 250 5 105 2 

15 563 448 2 N( .1) 75 20 80 1 

16 562 442 5 N( .04) so 30 65 

17 555 430 2 N( .1) 110 70 115 

18 646 440 2 N( .1) 100 75 120 1 

19 561 441 2 N( .1) 175 90 150 4 

20 560 439 10 .02 75 100 85 3 

21 559 438 10 N( .02) 50 30 60 

22 558 437 5 N( .04) 45 20 55 

23 644 433 1 N( .2) 150 180 60 4 

24 360 50-96 10 N( .02) 25 10 65 2 

25 581 DR-64-4770 5 N( .04) 185 100 140 10 

26 582 478 5 N( .04) 125 50 75 

27 580 476 2 N( .1) 140 35 55 2 

28 579 475 10 N( .02) 75 30 60 

29 578 474 5 N( .04) 140 40 60 1 

30 643 427 10 N( .02) 135 200 140 

31 554 428 2 N( .1) 85 150 95 4 

32 568 459 10 N( .02) 55 55 190 

33 569 461 10 N( .02) 70 200 ,us 

34 577 472 5 N( .04) 70 65 120 

35 570 462 5 N( .04) 55 220 140 1 

36 572 464 5 N( .04) 30 35 120 

37 573 465 5 N( .04) 55 100 300 1 

38 575 468 5 N( .04) 40 10 90 

39 574 467 10 N( .02) 40 180 180 

40 647 445 1 N( .2) 125 250 75 6 

41 645 436 5 N( .04) 45 100 110 

42 557 435 2 .3 85 35 300 25 

43 556 434 2 N( .1) 100 80 185 4 

44 566 457 10 N( .02) 55 65 115 

45 567 458 5 N( .04) 40 10 60 

5 
Table 1.--Gold and base-metal content of stream sediments--Continued 

Map No. Sam2le No. Sample Concentration ~22m~ (fig. 2) weight 

Laboratory Field (g) Au Cu Pb Zn Mo 

46 588 DR-64-497 2 N(O.l) 40 45 70 3 

47 551 411 10 N( .02) 40 50 140 

48 550 410 10 N( .02} 35 30 60 

49 549 409 2 N( .1) 40 45 110 

50 542 374 5 N( .04) 70 15 135 2 

51 541 373 5 N( .04) 45 80 340 2 

52 540 372 10 N( .02} 30 10 60 1 

53 539 367 2 N( .1) 45 30 110 2 

54 538 364 2 N( .1) 45 30 100 2 

55 636 370 Ins. 75 20 110 2 

56 535 361 10 N( .02) 75 45 235 2 

57 584 482 2 N( .1) 75 30 105 2 

58 585 484 2 N( .1) 75 65 160 4 

59 518 318 2 N( .1) 100 55 300 6 

60 651 488 1 7.1 45 45 205 2 

61 652 489 2 N( .1) 70 50 365 3 

62 536 362 5 N( .04) 45 40 160 2 

63 534 360 2 N( .1) 70 50 210 2 

64 495 Ins. 60 215 300 4 

65 654 494 2 N( .1) 45 90 190 4 

66 530 351 2 N( .1) 80 65 145 5 

67 529 350 2 .7 90 55 140 4 

68 635 352 1 N( .2) 160 140 205 4 

69 537 363 1 N( .2) 40 100 110 3 

70 528 348 2 N( .1) 50 45 125 3 

71 532 355 10 N( .02) 40 20 60 4 

72 533 357 2 N( .1) 185 25 175 3 

73 531 354 2 N( .1) 55 25 210 2 

74 653 492 1 N( .2) 55 55 150 4 

75 513 308 10 .2 75 70 175 4 

76 512 307 10 N( .02) 35 5 65 2 

77 527 346 2 N( .1) 50 15 110 2 

78 526 345 10 N( .02) 45 10 60 

79 525 344 10 N( .02) 30 55 5 2 

80 511 304 10 N( .02) 20 5 65 2 

81 522 336 5 N( .04) 30 5 70 1 

82 514 311 5 N( .04) 20 5 35 2 

83 5r9 325 5 N( .04) 40 15 55 

84 521 333 2 N( .1) 40 5 90 

85 520 331 2 N( .1) 30 5 60 2 

86 593 520 2 N( .1) 55 15 95 

87 307 5D-1 10 N( .02) 45 80 205 3 

88 548 DR-64-404 5 .6 35 40 95 

89 638 402 10 N( .02) 35 35 60 

90 547 401 Ins. 60 50 240 

91 639 405 5 N( .04) 50 45 190 

92 546 398 2 N( .1) 80 45 105 

93 543 380 2 N( -.1) 45 20 105 

94 363 5D-100 10 .04 215 30 90 4 

95 544 DR-64-390 2 N( .1) 35 5 55 

6 
Table 1.--Gold and base-metal content of stream sediments--Continued 

Map No. Sam:ele No. Sample Concentration ~:e:em2 (fig. 2) weight 

Laboratory Field {g) Au Cu Pb Zn Mo 

96 63-A-62 Ins. 70 25 80 

97 545 DR-64-392 2 N(O.l) 45 30 60 5 

98 552 413 5 N( .04) 45 15 145 

99 640 417 5 .08 40 25 150 

100 641 419 5 N( .04) 40 40 200 3 

101 642 420 1 N( .2) 100 5 110 

102 553 421 2 .1 80 10 100 

103 353 5D-65 5 N( .04) 100 5 85 7 

104 349 60 5 N( .04) 95 10 85 5 

105 348 59 5 N( .04) 150 15 80 7 

106 347 58 10 .02 200 10 85 7 

107 346 57 5 N( .04) 160 5 65 5 

108 345 56 10 N( .02) 145 10 75 4 

109 350 62 5 N( .04) 115 10 90 5 

110 344 53 10 N( .02) 50 5 60 3 

111 340 48 10 N( .02) 195 5 80 4 

112 342 50 5 N( .04) so 5 85 3 

113 163 Ins. 205 5 45 2 

114 164 Ins. 175 10 40 2 

115 351 63 2 N( .1) 30 -5 75 3 

116 341 49 5 N( .04) 25 5 60 2 

117 343 51 10 N( .02) 40 5 60 2 

118 337 42 5 N( .04) 50 10 80 4 

119 352 64 5 N( .04) 65 5 130 4 

120 338 43 5 N( .04) 20 5 35 2 

121 336 41 5 N( .04) 140 10 115 4 

122 335 40 10 N( .02) 100 5 80 5 

123 339 45 2 N( .01) 40 5 85 4 

124 334 39 5 N( .04) 90 5 60 3 

125 333 38 5 N( .04) 50 10 60 3 

126 332 36 5 N( .04) 65 5 80 3 

127 617 DR-64-570 5 .04 150 5 50 

128 667 571 1 N( .2) 300 15 60 

129 666 567 5 .2 180 140 

130 618 573 10 .02 150 20 95 

131 613 563 10 .4 100 5 115 

132 614 564 2 .7 140 5 85 

133 619 575 5 N( .04) 100 10 50 

134 615 566 2 N( .1) 90 10 70 

135 624 580 2 N( .1) 170 45 100 

136 623 579 5 N( .04) 110 10 75 

137 622 578 5 .08 170 20 70 

138 621 577 2 N( .1) 80 15 80 

139 620 576 5 .06 170 25 90 

140 612 561 2 2.0 180 25 120 

141 609 553 10 .08 200 5 125 

142 628 584 10 N( .02) 100 5 70 

143 629 585 2 N( .1) 90 10 70 

144 630 586 2 N( .1) 80 5 75 

145 665 556 1 N( .2) 140 15 115 

7 
Table 1.--Gold and base-metal content of stream sediments--Continued 

Map No. SamJ:!le No. Sample Concentration (J:!J:!m) 

(fig. 2) weight 

Laboratory Field (g) Au Cu Pb Zn Mo 

146 664 DR-64-555 1 N(0.2) 300 25 210 

147 610 557 5 1.2 150 5 70 

148 611 558 5 2.4 130 20 120 

149 606 548 10 .04 200 5 240 

150 605 547 2 N( .1) 225 10 135 

151 607 550 5 N( .04) 90 5 110 

152 663 551 2 2.7 150 20 145 1 

153 508 552 2 N( .1) 250 15 125 

154 632 588 10 N( .02) 50 5 60 1 

155 633 589 10 N( .02) 50 5 65 

156 634 591 10 N( .02) 80 5 65 

157 597 532 2 N( .1) 50 5 90 

158 660 529 2 N( .1) 400 5 75 

159 661 530 10 .2 450 10 70 

160 594 526 5 .4 175 10 85 

161 595 527 2 N( .1) 55 20 85 

162 662 531 2 N( .1) 70 15 60 

163 330 5D-34 5 N( .04) 80 10 80 3 

164 329 33 5 N( .04) 85 10 100 3 

165 327 31 5 N( .04) 50 5 120 4 

166 658 DR-64-524 2 .1 135 10 75 

167 331 5D-35 10 .2 250 20 110 7 

168 328 32 5 .04 115 30 125 7 

169 659 DR-64-525 5 N( .04) 35 5 60 

170 657 523 6 .06 85 15 110 

171 656 522 5 N( .04) 40 10 70 

172 655 521 10 N( .02) 20 5 25 

173 592 519 2 N( .1) 55 15 65 

174 598 534 2 N( .1) 60 10 75 

175 590 517 5 N( .04) 55 5 75 

176 589 516 2 N( .1) 50 20 80 

177 599 535 2 N( .1) 70 15 45 

178 604 543 5 N( .04) 40 10 45 2 

179 515 J12 5 N( .04) 40 10 85 2 

180 523 339 10 .02 55 5 60 

181 603 542 2 N( .1) 55 5 60 

182 600 538 10 N( .02) 45 5 25 

183 601 540 10 N( .02) 65 5 60 

184 602 541 5 N( .04) 75 15 55 

185 377 5D-117 2 N( .1) 65 10 85 3 

186 376 115 2 N( .1) 130 10 75 3 

187 364 102 2 N( .1) 205 10 95 5 

188 375 114 2 N( .1) 95 10 75 3 

189 374 113 10 N( .02) 115 10 120 3 

190 373 112 10 N( .02) 60 5 50 2 

191 365 103 5 N( .04) 70 10 80 3 

192 366 104 10 .02 130 10 80 5 

193 367 105 5 N( .04) 115 5 85 4 

194 368 106 10 N( .02) 110 10 80 4 

195 369 107 5 N( .04) 160 20 115 5 

8 
Table 1.--Gold and base-metal content of stream sediments--Continued 

Map No. Sam2le No. Sample Concentration ~2eml (fig. 2) weight 

Laboratory Field (g) Au Cu Pb Zn Mo 

196 372 5D-110 10 N(0.02) 120 10 125 3 

197 371 109 5 N( .04) 100 5 105 3 

198 370 108 10 N( .02) 150 15 115 3 

199 627 DR-64-583 10 N( .02) 110 20 65 

200 626 582 5 N( .04) 180 55 105 

201 625 581 2 .85 250 20 100 

202 407 50-150 10 .02 90 5 80 2 

203 631 DR-64-587 5 N( .04) 80 10 55 

204 524 343 10 N( .02) 135 5 80 2 

205 408 5D-151 2 N( .1) 230 10 165 3 

206 410 153 10 N( .02) 125 10 115 2 

207 409 152 10 N( .02) 105 5 95 3 

208 411 155 Ins. 105 5 115 3 

209 412 157 5 N( ~04) 125 5 95 3 

210 158 ACH-158 10 N( .02) 150 N(lO) N(200) N(2) 

211 157 157 10 N( .02) 200 N(lO) N(200) N(2) 

212 413 50-158 5 N( .04) 75 5 90 2 

213 388 129 5 N( .04) 80 5 140 3 

214 389 130 10 N( .02) 30 5 95 3 

215 390 132 10 N( .02) 110 10 185 4 

216 378 118 5 .04 95 10 65 2 

217 379 119 2 N( .1) 100 5 80 2 

218 381 122 10 N( .02) 115 10 120 2 

219 382 123 5 N( .04) 125 15 100 2 

220 383 124 5 N( .04) 125 10 90 2 

221 380 121 5 N( .04) 185 10 110 2 

222 384 125 10 N( .02) 115 10 95 3 

223 385 126 5 N( .04) 80 5 80 2 

224 386 127 2 N( .1) 120 5 80 2 

225 387 128 10 55 5 65 2 

226 510 60-328 10 N( .02) 190 5 75 2 

227 509 327 5 N( .04) 40 5 55 2 

228 497 315 2 N( .1) 30 5 55 1 

229 501 319 5 N( .04) 35 10 90 2 

230 506 324 2 N( .1) 105 5 65 2 

231 507 325 2 N( .1) 45 5 80 3 

232 186 ACH-186 10 N( .02) 50 N(lO) N(200) N(2) 

233 184 184 10 N( .02) 100 10 N(200) N(2) 

234 185 185 2 N( .1) 150 10 N(200) N(2) 

235 398 50-140 10 N( .02) 85 10 120 3 

236 391 133 .5 N( .04) 70 5 40 2 

237 397 139 2 N( .1) 95 15 150 2 

238 392 134 10 N( .02) 45 5 90 2 

239 187 ACH-187 2 N( .1) 150 N(10) N(200) N(2) 

240 393 5D-135 2 N( .1) 50 5 85 2 

241 396 138 2 N( .1) 210 20 220 5 

242 395 137 10 N( .02) 85 10 140 3 

243 394 136 10 N( .02) 60 10 80 2 

244 188 ACH-188 10 N( .02) 100 N(lO) N(200) N(2) 

245 189 189 10 N( .02) 100 10 N(200) N(2) 

9 
Table 1.--Gold and base-metal content of stream sediments--Continued 

Map No. SamJ2le No. Sample Concentration ~l2l2m~ (fig. 2) weight 

Laboratory Field (g) Au Cu Pb Zn Mo 

246 190 ACH-190 2 N(O.l) 100 20 N(200) N(2) 

247 191 191 10 .04 150 15 N(200) N(2) 

248 325 5D-24 5 N( .04) 40 5 60 3 

249 406 149 10 .1 180 5 50 4 

250 405 148 10 N( .02) 145 5 95 3 

251 403 146 5 .02 175 5 90 4 

Z52 402 145 10 .02 160 5 105 2 

253 404 147 5 N( .04) 285 5 90 4 

254 401 144 5 .2 130 10 85 3 

255 400 143 5 .04 1:35 10 130 3 

256 399 141 10 .04 280 35 200 5 

257 DR-64-429 Ins. 350 250 250 13 

258 313 Ins. 60 20 235 4 

10 
Table 2.--Gold content of rocks 

[Only rocks containing 0.02 ppm or more gold are listed. Analysts (atomic absorption): 

M. s. Rickard, w. L. Campbell, and R. L. Miller] 

Map No. Sa!J!Ele No. Concentration ~:eem2 Description of rocks 

(fig. 2) 

Laboratory Field Au 

R40 ACH-739 SD-32 0.04 Hornblende-feldspar porphyry dike. 

RSO 679 63-A-76A .06 Hornblende-feldspar porphyry dike 

with disseminated pyrite. 

R51 681 77A .02 Porphyritic hornblende diorite with 

disseminated pyrite. 

R53 720 DR-64-320 .02 Hornblende-feldspar porphyry dike, 

highly epidotized. 

R54 721 322 .02 Hornblende-biotite diorite. 

R55 723 324 .02 Hornblende-feldspar porphyry dike. 

R60 685 63-A-606 .3 Hornblende diorite with minor disseminated pyrite. 

R78 727 DR-64-332 .02 Hornblende diorite with disseminated 

pyrite. 

R85 731 336 .02 Hornblende diorite. 

Rl02 763 SD-134 .02 Quartz diorite with .iisseminated 

pyrite. 

Rl04 761 131 .04 Hornblende-quartz diorite with disseminated pyrite. 

11 
Table 3.--Concentration of gold and base metals 

Element 

Gold ---------

Copper--------

Lead----------

Zinc---------

Molybdenum----

Crustal 

Aver agel 

0.004 

55 

12.5 

70 

1.5 

!After Taylor (1964). 

Concentration (ppm) 

Slana area 

Range Mean Mode 

< 0.02-.3 

5-250 47 10-20 

5-35 10 10 

15-140 68 50-60 

1-5 2 3 

Stream sediments3 

Mode 

<0.02 

40-50 

10 

60-70 

2.5 

2Gold based on 105 samples (this report); copper, lead, zinc, and molybdenum 

based on 34 samples (Richter, 1966). 

3sased on 384 samples (Richter, 1966) including the 258 samples for which data 

are presented in this report. 

12 
l.. 

Glennallen 

..:-

TO ANCHORAGE 

146° 

s 

/ 

W R A 

145° 

10 

I 

N 

0 

I 

G L L 

10 

I 

G 

20 

I 

0 

-, 

I 

I 

I 

-{Slana area 

I 

I ____ j 

U N 

30 MILES 

I 

A 

N 

Figure 1.--Index map of part of south-central Alaska showing the Slana area. 

13 
~ 

,.j;>. 

--~ R69~ I :r 2 , 

~ l l 'ii-4•_•{13 •115 ;rs•I19 1211- I 

}--~- R68 112 ·~· -J ~- 16 120~~1_, ... Rl3 R77 I 

-:-~\ ~ _./ .t.~67 171 ', •!17 )j.ll" :12~1-_ 6 R87 

88 

2 9 

I 

·~:: /' ~~t~~-:7 i', ~~~1;:~- -... __ l" -,, > ~~2 --+-~213 • -- 104 •• 08 I ~I .:126 RT4 I R7~ ---.,E08 ,- I ·-·14 

r-- _,-- ·;_J4'~-- - ~· • • 9 -- ---'. 11 fl0<1 ~1 0 I I 1jl: ••t R7o •1 2 "'20yl _;)>\~' 5 o\207 __ .-" -t , 

\ , , ~1 .-- !f.-;z._- ; :Ri~4 ~ 137' 1 5 o134 __.; 80 ,-, , , ~2~~R9'\ :' - ,1"5k-

'i I I R2 .,. 10 • 13 03 -- ~ I.t 133 '... - / I ... I. •, 206 -----t--------1~ ;'~" r ~ .- --+.------f=-• Rb5 - ---'- ' --- tt--f0-2• - \ Ri2/ ~ - . I 25_,1 6 ~ ~ .. ~ ~\,. j', \ ·~". ,) __ \·~ ... '- 216 

' · ,/' ;,: ·"' .. ,, . · \ l,/ -_101-

10,

2 

~~~: b2 ·~~~:r~zt~7 .~,O! Rt :\_ ~~~f,.~:~/~ 7 

~ _ _,__, '> 1':i •, -, / _ _ _,j]_,B .t.Ro R~OAR'JY _ ( ~ 2 199 e.200 ·1 R94 -- -"222 

f 

?:2 30 -:25 & R6& Arj_R;-._19 &R9 ' ~, - -~q lCJO 14b.,--R_ ~14'> _," '!_143 R9b ! • &Rqs 

---- pe-~1 ·•R8 ~-~('- ~ R57"r-•R5~ •14••'148 ~~ p44 • , - 2231 

' ( • 33 I, • R7 --.. >' 22 •'-"'"' ~ 1'• ;r"'. - •"' ~ f . '"• 149 ''•"' •J•,n ,, ~ ~ -- ~ R98 19i1_981I R97 1-q4' -,19,,3- __._ I" 1__.~, '' _ 

, r~O 

1 

~--~- Rti' & *, , 1 -";, ---------r R99 ~~-.; .1 ---_ --~-

/ .. -- - 3~ _, 4~ 1 ... - ,, ' \- -- Ei 153 ; 5~ l5b - •]96 I' 191 

- I ,.?6 43 • • Rl5 ".'--I -9~ ~~ • .;58<52 • 52 ( 1155 Is~_{ ~o -

tR~,1 , . 44 -H5 f I 11 ' k ~ R~o •is9 ~-~~ .}_5? k --ts~ ~ 186 

!-(Ci_ [.A ,.-37 •--39 

; 

./ 

.i 93~ <""A -~ GruJl:_t~ 'g4 R47&&R4b 

48 RlOO 

~ ~ 

l . ~~-- ·-~-~~- ' ------ \ R 4 R45.t. !-t>4 ,1,' 65 166 1~ 6 _.174 , •1 5 ' 

\ 42 7 __ -- -' '_ -~--R-l1~'4~168-i7o;r--- A73_ )- .t.Rol - ~ 'I _ . • _ 

__ · J , , -~~-r=-=-- ---+-l, --_- -~ ~~~~~~3~ "I R41·R·3~~o .::9 ~l'tr:: '~ ~ r-- >-'~ _.-----._\-~-5--~· ~------'.: ·-,-,-1-,:---- ~~-n-- I "£.~, \' """ 1 

""-<.::\::- 'e-\ &Rlb ,·) . :6 p,q \ ._(_ ~83 184 ,./ /-

'---. I 1 R 7 1 -r R36 ..,R3s 

1

!_86 ,~ , 182 ~~~:~~- __ carlson Lake '-.__ I • I ~ .R3-l ' 1 'l .1771 ., - -.-

\ 

I :26, e- ..,R33 85... ' ,'181- 1180 

•- ~~ ~~2 ! .. -~/~ ""---- -.R_2~ II 88 tR-'2 - ~~3 "84 \~-., , /1 ., 

L-_,.?6 63, -,,- ~ "'"", 87 - ' .R31 /t,,_<' I j!l- -: 

~ ~, •• ~ \,55 'f7 _14 68 9 "'?1~-2-5 F~ . ---- -1-- ..,R30 ~ """ ---r~ ---- ~~~ ------ ____ __L___ __ _ 

~. A 

B 

c 

D 

E 

t· .2--

4

- 159 "*~ 2 &R:2 

~51 '-.53 b~~t 6 tR19 'lbl ~ 77 .!c_ 79 t·,_ - ·~-...-~--. , 

-~ ~ -t----1-L -""ee.(-"',~, ~-..179 t _.,iifi1i ~~~ '[c, _.',b, '~·, EXPLANATION ~ J 0 • •R1R I -.: ._R 20 8 

•R

29 

\, ' l, --~~/,{ ,~·--·~,]"--~::-.' - •

45 

Stream-sedimentsample F 

, 11 ~ :2

R3

24 i .1

81 L ~21 {------~- ---- - ,7-=::"'A'-;,~::;,f~~- i~~c~.? ·"c.. ~ ~· _" •R 63 Rock sample 

1 

r 1 p.'i •ij J:---~ ,v/ r~. ~'TIL~O~\ .; tlLl 

""=- ~~-~~ -~=_l~==='- #-=-, ~iti-~ - ~ 'so:-~~~~--}". ~!:1 __ ___JE!'~,o?~ -,.~ ~ s~~/·o,,~~\~~ ~D·-- • 

1 2 3 4 144'00' 5 6 7 8 9 10 

Base from U.S. Geolog1cal Survey, 1:63,360. 

Gulkana C-1, 1949, D-1. 1952; Nabesna 

C-6. 1948, D-6, 1949 

0 4 5 MILES 

Figure 2.--Sample-location map, Slana area. 
...... 

CJl 

UNCONSOLIDATED DEPOSITS 

1---==-t 

~ ) ~ >- f-0: <(<( 

Surficial deposits ~ Z 

Stream, glacial, landslide, and talus deposits 

BEDaDED ROCKS } U ~ 

~0~ <(Z<( 

o:<(IArgillite, siltstone, graywacke, and conglomerate ~ ~ 

u 

EXPLANATION 

GOLD AND BASE-METAL DISTRIBUTION MAPS 

INTRUSIVE ROCKS 

Quartz monzonite and granodiorite 

Includes irregular fine-grained sil-icified border zone 

around Ahtell Creek pluton in west part of area 

~~<~ 

~-~~~ 

Diorite, quartz diorite, gabbro, and anorthosite 

u 

(/) 

(/) 

<( 

0: 

:J 

I 

Limit of bedrock exposure 

Approximate contact 

Fault 

Dashed where inferred 

IIIII I 1111 Ill 

Gold placer workings 

X 

B ~~z Silver and base-metal quartz vein 

...J<(<( 

>- - (f)<:'.~ 

Andesitic volcanic rocks, limestone and argillite, and ~ Z 5 

amygdaloidal basalt with intercalated limestone W ~a.. a..z 

Figure 3.--Explanation for geologic maps showing distribution of gold and base metals 

(figs. 4-8). 
"""" Q\ 

Base from U.S. Geoloaical. Survey. 1:63,360. 

Gulkana C-1, 1949, D-1. 1952; Nabesna 

C-6, 1948, D-6, 1949 

1'~ \ \ 

~{-r, '¥\' 

,.x~, ' 

PPvs 

\--\\1 

'\ ' " 

'0-i 1:0-. /-

-· '" ~/ 

0 2 4 5 "'lLES 

Figure 4.--Map showing distribution of gold in the Slana area. 

I t 

• ~0.2ppm ------w· ··-·· . --

Geology by D. H. Richter, 1963-67 

and N. A. Matson, Jr., 1967 

A 

8 

c 

0 

F 
...... 

-...) 

.,b 

<!".i'J 

+o"-

1, 

J 

Base from U.S. Geological Survey, 1:63,360. 

Gulkana C-1. 1949, D-1, 1952; Nabesna 

C-6, 1948, D-6, 1949 

PIPvs 

G ·~(> 

0 \:>' 

3 

1 0 1 2 3 4 5 MILES 

Figure 5.--Map showing distribution of copper in the Slana area. 

0 

• 

• 

8 

EXPLANATION 

<150 ppm 

150-299 ppm 

?aoo ppm (value shown) 

9 10 

Geology by D. H. Richter, 1963-67, 

and N. A. Matson, Jr., 1967 

c 

62'45' 

F 
~ 

00 

~o"-

1'1<1"'1> 

~'I> 

2 

Base from U.S. Geological Survey, 1:63,360. 

Gulkana C-1, 1949, D-1, 1952; Nabesna 

C-6, 1948, D-6, 1949 

3 

0-.tJ~~"I!i :0,0 ' ' 

4 144°'oo·'', 5 

\ 

\~ 

\~ 

10 

I 

\ \ ~,, ~~ 

\Jd \ \ \ 

\ \ 

o\ ' ' ' ' ' \ 

\ 

() 

PIPvs 

0 00 

0 Gl 

PIPvs 

6 7 

1 0 1 2 3 4 5 MILES 

PF'vs 

0~'' KJa 

o(\ PP~ A 

Q, 

"~" PIPvs 

·,id' ~ 8 

PIPvs 

Jd~ 

Jd,Sll) 

D 

0 

0 

(E 62045' 

d 

EXPLANATION 

0 <30ppm 

• 30-59 ppm 

• ;?so ppm (value shown where ;?140 ppm) 

8 9 10 

Geology by D. H. Richter, 1963-67, 

'- and N. A. Matson, Jr., 1967 

; F 

Figure 6.--Map showing distribution of lead in the Slana area. 
\0 "'""' 

... 0 ... 

._1> 

~.,4'1 

2 

Base from U.S. Geolog1cal Survey, 1:63,360. 

Gulkana C-1, 1949, D-1, 1952; Nabesna 

C-6. 1948, D-6, 1949 

3 5 

0 

'\ \'0! 

\ 

\~ I 

\ \ ~,~·~ \Jd! \ \ : \ \ \ .o\ ', ,, \ 

' \ 

PIPvs 

Q oo 

0 <? 

Pf'vs 

6 

2 

7 

4 MILES 

Figure 7.--Map showing distribution of zinc in the Slana. 

8 

EXPLANATION 

0 <180 ppm 

• 180-359 ppm 

G!~····· · KJa : 

~~p~, .· '. 

b 

w···~" 

~~B ~IPvs 

D 

o· E 

F 

e ~360 ppm (value shown) 

9 10 

Geology by D. H. Richter, 1963-67. 

and N. A. Matson, Jr., 1967 
N 

0 

~o" 

. I 

R"'b 

<f'"~ 

~~\ '-i 

"I 

\.'1~\\"'.;::'' ~,,,,~~...011 ~~.It ~" -. ,"<> II. v • ',· <>~-" ~ 

PIPvs \~~~~~;_u~q~~.!' .:*:; icf:xf_ 

2 

Base from U.S. Geological Survey, 1:63,360, 

Gulkana C-1, 1949, D-1. 1952; Nabesna 

C-6, 1948, D-6, 1949 

3 

1 lndia.n (J/t 1: Pass !c, 'I ~ i( Lake 

(Jd/ li--Jd 

I' 'J ...... 0 t ~I ''-,, /1J 

~~~;,~~:II:~~ 

(}r11~:bH!,'x,q_( \) ~.II b - ,;. '- \\ 

GLENN 

' (l 

l~ 

)//~~ 

-.t~~' 

0'0"' 

4 144°00'. 5 

./ \ 

\ 

\ \ ,, \ 

\ '~ I ' 

I c:P\ ' 

l 

I 0\ \ 0 \ 

\ \ \ <P 

\~ ·' 0~ \Jd \ PIPvs 

\ \ 

\ ' 

\ ' \ 

\ 

\ 

\ 

q 

6 7 

1 0 1 2 3 4 5 MILES 

Qsd 

8 

~KJa 

0~~· 

0 

W_ 

Qsd 

EXPLANATION 

o <6ppm 

• 6-11 ppm 

e ~12 ppm (value shown) 

9 

~~.s <6P1Pvs 

10 

Jd~" 

D 

0 

0 

oE 

62"45' 

d 

F 

Geology by D. H. Richter, 1963-67, 

and N. A. Matson, Jr., 1967 

Figure 8.--Map showing distribution of molybdenum in the Slana area.