3000

3000

3000

2900

2900

2800

2800

3100

3100

3100

3000

2900

2900

2800

2800

2600

2500

2600

2700

2500

2600

2700

2800

2800

2900

2400

2400

2400

2500

2500

2600

2700

2700

2300

2300

2300

2200

2200

3200

3200

3200

3200

3100

3000

3300

3400

3300

3000

3200

2900

3100

3100

2800

2900

3100

3200

3100

3000

2900

2800

3000

3000

3100

3100

3200

3200

3300

3000

2800

2700

2600

2600

2600

2700

2800

2600

2500

2900

2900

2900

2800

2800

2700

3000

3000

3000

3000

3000

3100

3100

3200

3000

2900

2900

2900

2900

2900

2900

3000

2900

2800

2900

2900

2800

2800

2800

2800

2800

2800

2700

2700

2700

2700

2700

2600

2600

2600

2600

2500

2500

2500

2500

2400

2400

2400

2400

2400

2400

2400

2500

2500

2500

2500

2400

2400

2500

2500

2500

2500

2500

2600

2600

2700

2800

2300

2300

2300

2300

2200

3100

3100

2700

2600

2600

2700

2700

2700

2700

2600

2500

2500

2500

2600

2400

2500

2500

2700

2800

2800

2800

2800

2800

2900

2900

3000

3000

3100

3100

3200

3200

3300

3000

3100

3200

3300

2900

3000

3100

2900

2900

2800

Dar-e Kata

Dar-e

Parandaz

Dar-e Jangalzarak

Dar-e Ahankashan

Dar-e Nawe Gala

Dar-e Churghori

Dar-e

Darrahe

Aevo

Dar-e Haftadchashma

Dar-e Langar

Dar-e Khusk

Keshnal

Rakhna

Garmaw

Dar-e

Deh-e Sorkh

Dar-e Khusk

Dar-e Jangalzarak

Keshnal Rakhna

 Dar-e Nawe Gala

Dar-e Ahankashan

Dar-e HaftadchashmaDar-e Haftadchashma

Sheta - i - Kohmardi

15.0

1.5

55.0

1.2

50.0

1.3

15.0

1.5

70.0

1.25

10.0

2.5

69.0

1.3

60.0

1.3

174.5

0.3

46.0

1.07

49.0

2.5

180.0

0.9

10.0

1.2

30.0

1.2

45.0

1.5

63.0

20.0 0.8

1.2

60.0

0.6

65.0

0.4

20.0

0.7

8.0

0.8

3.5

1.0

5.0

5.2

11.2

1.4

15.0

1.0

35.0

1.3

25.0

1.2

12

6

8

947

1764

1512

1778

982

559

554

548

9

10

16hg

15

16

5

2 1

1hg

3

22

24

14

12

13

20

25

7hg

4

1764

554

Rakhna

Bahre Yar

Asyabed

Cheshmiak

Cambar

Katalok

Dewalak

Dahana

Darrahe Asya

Kuatkhana

Jare Deh Surkh

Qal’a-i-Afdzal

Qish Arbab-shirin

BADGHIS

GHOR

HERAT

30

70

55

15

30

10

20

10

10

10

15

5

25

25

15

10

20

10

20

15

15

5

25

30

20

20

30

40

25 35

10

10

10

10

30

20

60

65

45

5

5

5

5

5

5

5

70

68

68

68

68

75

70

70

70

65

70

70

80

87

80

70

80

70

85

65

60

70

70

70 60 70

80

80

70

85

75

80

67

70

75

80

80

60

40

30

5

5

5

5

5

35 25

5

5

10

15

20

5

10

60

10

75

15

60

20

15

10

20

18

70

20

60

80

80

5

5

75

70

70

60

METERS METERS

B B’

3500

3000

2500

2000

1500

3500

3000

2500

2000

1500

METERS METERS

A A’

B

A

A’

B’

3500

3000

2500

2000

1500

3500

3000

2500

2000

1500

Miocene Intrusive Complex

Dikes of diorite porphyry, granodiorite porphyry, monzonite 

porphyry, and syenite porphyry, undifferentiated

Second phase

Granite porphyry, quartz porphyry, and plagiogranite 

porphyry, undifferentiated

First phase

Diorite porphyry, granodiorite porphyry, monzonite porphyry, 

and syenite porphyry, undifferentiated

INTRUSIVE ROCKS

DESCRIPTION OF MAP UNITS

STRATIFIED ROCKS

Fluvial deposits (Recent)—Deposits of flood plain and low 

terraces. Coarse, well-rounded gravel; sand, sandy loam, and 

loam

Fluvial deposits (Recent? to upper Quaternary)—Deposits of 

flood plain and low terraces. Coarse, well-rounded gravel;

rounded cobbles; sand, and loam

Fluvial deposits, undivided (Quaternary)—Deposits of flood plain 

and low terraces. Coarse, well-rounded gravel; clay, sandy loam, 

and loam

Conglomerate and other rocks (lower Quaternary to upper

Neogene)—Conglomerate and lesser amounts of coarse, 

siliceous sandstone; coarse, well-rounded gravel; rounded cobbles; 

and obliquely laminated sand and clay

Disconformity

Limestone and other rocks (lower Paleogene to Upper 

Cretaceous)—Limestone and lesser amounts of marl, quartz 

sandstone, and conglomerate

Disconformity

Sandstone and other rocks (Middle to Lower Triassic)—Sandstone 

and lesser amounts of coarse-grained siliceous sandstone; 

siltstone, limestone, volcanogenic rock, and tuffaceous sandstone

EXPLANATION OF MAP SYMBOLS

Contact—In cross sections, shown dotted where inferred

Contact—Disconformable

Fault—Dashed where inferred; dotted where concealed

Intense schistosity

Intense brecciation—Crushed intrusive rocks

Orebody boundary—Inferred

Strike and dip of bedding—Dip values shown where known

Strike and dip of dike contact—Dip values shown where known

Strike and dip of schistosity—Dip values shown where known

Fossil location—Brachiopods, pelecypods, amminoids

Trench and number—hg indicates trench dug by Herat group in 

1971 (see Dronov and others, 1972)

Sample transect and number

Sample location and number

Sample data—Top number, thickness of mineralized zone in 

meters; bottom number, average gold concentration in grams 

per ton (g/t)

Site of photograph—Tip of arrow indicates direction of view; 

number keyed to figure

Ephemeral stream

Province boundary

Road or trail

Village

Hornfels

Silicification, pyritization, limonitization, and (or) kaolinization

Skarns

Magnetite

Magnetite-hematite

Epidote, epidote-hematite, garnet, epidote-garnet

Gold-bearing zone

ZONES OF ALTERATION

Chirico, P.G., and Moran, T.W., 2011, Topographic and hydrographic GIS 

dataset for the Afghanistan Geological Survey and U.S. Geological Survey 

2010 minerals project: U.S. Geological Survey Data Series 624, available 

only at http://pubs.usgs.gov/ds/624/.

Doebrich, J.L., and Wahl, R.R., comps., 2006, Geologic and mineral 

resource map of Afghanistan, version 2: U.S. Geological Survey 

Open-File Report 2006–1038, 1 sheet, scale 1:850,000; also available 

at http://pubs.usgs.gov/of/2006/1038/.

Dronov, V.I., Kalimulin, S.M., and Sborshchikov, I.M., 1972, Geological 

structure and minerals of northern Afghanistan: Unpublished data on file 

at the Ministry of Mines and Industries, Kabul, Afghanistan.

Peters, S.G., King, T.V.V., Mack, T.J., Chornack, M.P., eds., and the U.S. 

Geological Survey Afghanistan Mineral Assessment Team, 2011, 

Summaries of important areas for mineral investment and production 

opportunities of nonfuel minerals in Afghanistan: U.S. Geological Survey 

Open-File Report 2011–1204, 2 vols., 1,810 p. plus appendixes on 

DVD, also available at http://pubs.usgs.gov/of/2011/1204/.

Peters, S.G., Ludington, S.D., Orris, G.J., Sutphin, D.M., Bliss, J.D., and 

Rytuba, J.J., eds., and the U.S. Geological Survey–Afghanistan Ministry 

of Mines Joint Mineral Resource Assessment Team, 2007, Preliminary 

non-fuel mineral resource assessment of Afghanistan: U.S. Geological 

Survey Open-File Report 2007–1214, 810 p., available at 

http://pubs.usgs.gov/of/2007/1214/.

Shcherbina, Y.I., Tarasenko, V.I., and Palvanov, G., 1974, Report on the 

results of prospecting and evaluation implemented by the Adreskan crew 

in 1972 within the copper-gold-bearing occurrence of Afghanistan: 

Geological map of the Ahankashan area with data on mineral resources, 

scale 1:12,000, graphic supplement 1, and Geological map of the area 

of the Ahankashan-Rakhna basin, scale 1:50,000, graphic supplement 2 

(Appendix 2): Kabul, Ministry of Mines and Industries of the Royal 

Government of Afghanistan, report no. 0822 [prepared by V/O 

Technoexport U.S.S.R. for the Ministry of Mines and Industries of the 

Royal Government of Afghanistan under contract no. 50728]. 

Unpublished data on file at Department of Geological and Mineral 

Survey, Kabul, Afghanistan.

REFERENCES

These maps are a redrafted and modified version of the Geological map 

of the area of the Ahankashan-Rakhna basin, scale 1:50,000 and 

Geological map of the Ahankashan area with data on mineral 

resources, scale 1:12,000 (Shcherbina and others, 1974). The original 

maps and cross sections are contained in an unpublished Soviet report (no. 

0822), prepared in cooperation with the Ministry of Mines and Industries of 

the Republic of Afghanistan in Kabul during 1974. The redrafted maps 

and cross sections illustrate the geology of the Ahankashan and Rakhna 

basins, located within Badghis, Ghor, and Herat Provinces.

The Ahankashan and Rakhna prospect area is one of several gold and 

copper deposits within west-central Afghanistan. Here, various felsic to 

intermediate igneous porphyries intrude Lower Triassic to lower Paleogene 

sedimentary rocks, producing mineral and ore-bearing zones related to 

hydrothermal alteration, skarns, silicification, and crushing (brecciation). 

Mineralized skarns contain assemblages such as magnetite, magnetitehematite, epidote-hematite, and epidote-garnet, as well as disseminations 

of chalcopyrite, covellite, chalcocite, cuprite, malachite, and azurite. Gold 

mineralization is mainly associated with zones of crushing along faults, and 

with small silicified igneous veins within granite and quartz porphyry of the 

so-called “second phase” Miocene intrusive rocks, primarily located in the 

southern part of the Ahankashan pluton (maps A and B). Ores associated 

with the Miocene “first phase” porphyries, mainly in the northern lobe of 

the Ahankashan pluton, are less common than those associated with the 

“second phase” porphyries (map B). Gold and copper mineralization, of 

“second phase” porphyries, is spatially associated with zones of 

hydrothermal alteration and intense crushing, where rocks have been 

silicified, pyritized, limonitized, and kaolinitized. Gold-bearing zones of the 

Ahankashan pluton are mainly in the northeastern and southwestern 

portions of the intrusion and are up to 1.5 kilometers in length and 800 

meters in width (Shcherbina and others, 1974). Gold concentrations 

determined from skarn samples commonly range from 0.2 to 5.0 grams 

per ton (g/t), with some samples as high as 32.2 g/t (Shcherbina and 

others, 1974). Also, from skarn samples, copper concentrations were 

determined to be as high as 3.6 weight percent, but more commonly less 

than 1.0 weight percent. All skarn samples also contained lead, zinc, and 

molybdenum, although lead and zinc concentrations were generally less 

than 0.4 weight percent, and molybdenum less than 0.05 weight percent 

(Shcherbina and others, 1974). 

The redrafted maps and cross sections reproduce the topology of rock 

units, contacts, faults, and so forth, of the original Soviet maps and cross 

sections, and they include modifications based on our examination of the 

originals and our observations made during a brief flyover in 2010. Further, 

we have attempted to translate the original Russian terminology and rock 

classifications into modern English geologic usage as literally as possible 

without changing any genetic or process-oriented implications in the 

original descriptions. We also use the age designations from the original 

maps. However, the rock unit colors on the maps and cross sections differ 

from the colors shown on the original version. Colors were selected 

according to the color and pattern scheme of the Commission for the 

Geological Map of the World (CGMW) (http://www.ccgm.org).

Elevations on the cross sections are derived from the original Soviet 

topography and may not match the Global Digital Elevation Model (GDEM) 

topography used on the redrafted maps of this report. Hydrography 

derived from Advanced Spaceborne Thermal Emission and Reflection 

Radiometer (ASTER) may not fit alluvial deposits shown from the 

unmodified original compilations. 

Aerial photographs were taken by R.D. Tucker and W.R. Stettner of the 

U.S. Geological Survey during their flyover in 2010 (figs. 1–11). 

Photograph locations are shown on the maps by symbols keyed to figure 

numbers.

INTRODUCTION

SCALE 1: 50 000

CONTOUR INTERVAL 25 METERS

1 1/ 2 0 1 2 3 MILES

1 .5 0 1 2 3 4 5 6 KILOMETERS

SCALE 1:12 000

1/2 0 1/2 1 MILE

.5 0 .5 1 KILOMETER 

CONTOUR INTERVAL 25 METERS

Modified from original compilation 

of Shcherbina and others (1974); 

see References

Modified from original compilation 

of Shcherbina and others (1974); 

see References

Topography and hydrography derived from Advanced Spaceborne 

Thermal Emission and Reflection Radiometer (ASTER) 30-meter Global 

Digital Elevation Model (GDEM) data, 2009 

Projection and grid: Universal Transverse Mercator (UTM), zone 42 north

World Geodetic System (WGS) 1984 Datum

Topography and hydrography derived from Advanced Spaceborne 

Thermal Emission and Reflection Radiometer (ASTER) 30-meter Global 

Digital Elevation Model (GDEM) data, 2009 

Projection and grid: Universal Transverse Mercator (UTM), zone 42 north

World Geodetic System (WGS) 1984 Datum

A.—Geologic map of the Ahankashan and Rakhna basins and plutons.

B.—Geologic map of the Ahankashan pluton and northern lobe showing gold deposits and trenches. The area is outlined in red on A.

Prepared in cooperation with the 

Afghan Geological Survey

Under the auspices of the U.S. Department of Defense

U.S. DEPARTMENT OF THE INTERIOR

U.S. GEOLOGICAL SURVEY

OPEN-FILE REPORT 2014–1199

USGS Afghanistan Project Product No. 200

Geologic Map of the Ahankashan-Rakhna Basin, Badghis, Ghor, and Herat Provinces, Afghanistan, Modified from the 1974 Original Map Compilation of Y. I. Shcherbina and Others

Compiled by

Robert D. Tucker, Will R. Stettner, Linda M. Masonic, and Anya K. Bogdanow

2014 Printed on recycled paper 

Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement 

by the U.S. Government

For sale by U.S. Geological Survey, Box 25286, Denver Federal Center, Denver, CO 80225; 

http://store.usgs.gov; 1–888–ASK–USGS (1–888–275–8747)

Suggested citation: Tucker, R.D., Stettner, W.R., Masonic, L.M., and Bogdanow, A.K., comps., 2014, 

Geologic map of the Ahankashan-Rakhna basin, Badghis, Ghor, and Herat Provinces, Afghanistan, modified 

from the 1974 original map compilation of Y.I. Shcherbina and others: U.S. Geological Survey Open-File 

Report 2014–1199, 1 sheet, scale 1:50,000 and 1:12,000, http://dx.doi.org/10.3133/ofr20141199.

ISSN 2331-1258 (online)

http://dx.doi.org/10.3133/ofr20141199

Index map outlining USGS-Afghanistan 

mineral project areas in green. Area of 

this report shown in red.

64°E

62°E

60°E

66°E 68°E

70°E 72°E

35°N

34°N

74°E 76°E

32°N

33°N

30°N

29°N

31°N

36°N

37°N

38°N

39°N

Figure 7.—Aerial view looking southeast from the northwestern margin of the 

Haftadchashma pluton. Notice the dark-red-brown staining of hematite alteration 

in Triassic rocks on the northern margin of the pluton. 

Figure 8.—Aerial view looking northeast from the center of the Jangalzarak 

pluton. Light-colored rocks in the foreground show the location of the pluton. 

Bedded Triassic and Cretaceous sedimentary rocks dip away from the intrusion.

Figure 9.—Aerial view looking west into the center of the dome-shaped 

Jangalzarak pluton. Notice the dark-red-brown staining of hematite hornfels 

alteration in Triassic rocks on the northern margin of the pluton.

Figure 10.—Aerial view looking southwest along the northeastern margin of the 

Ahankashan pluton, western occurrence. Notice the dark-red-brown hematitic 

alteration where the nearly vertical Cretaceous strata contact the pluton.

Figure 11.—Aerial view looking northwest along the southern margin of the 

Ahankashan pluton, western occurrence. Notice the dark-red-brown hematitic 

alteration along the southwestern margin of the pluton. The plutonic rocks underlie the foreground in the photograph.

Figure 2.—Aerial view of the Ahankashan pluton looking north from the southern 

margin of the pluton. Notice the Soviet trenches in the foreground, which were 

dug perpendicular to the gold- and copper-rich veins and crushed rocks located in 

this part of the pluton. The trench locations are also shown on map (B).

Figure 1.—Aerial view of the Rakhna pluton looking northeast. The dark-red and dark-red-brown 

exposures are identified as Lower to Middle Triassic sedimentary rocks (T1–2

), and the white escarpment 

as Upper Cretaceous to lower Paleogene rocks (K2

–^1).

Figure 3.—Aerial view looking southwest from the Ahankashan igneous pluton 

toward its southwestern margin with overlying Triassic and Cretaceous sedimentary rocks. The Soviet trenches were dug perpendicular to the strike of the goldand copper-rich veins along the pluton. The trench locations are also shown on 

map (B).

Figure 4.—Close-up aerial view of the gold-bearing zones in the Ahankashan 

pluton. View is looking south. The trench locations are also shown on map (B).

Figure 5.—Aerial view looking southwest at the faulted, northern lobe of the 

Ahankashan pluton. The faults mainly crosscut Miocene intrusive rocks. 

Figure 6.—Aerial view of the Haftadchashma pluton looking southwest from the 

northeastern margin of the basin. The plutonic rocks of Miocene age underlie the 

light-colored lower terrane, (d1

N1) on the photograph. Notice the dark-red-brown 

staining of hematite alteration in the Triassic rocks of the foreground. The 

overlying Cretaceous sedimentary rocks are shown in the background.

Q3–4

T1–2

Q

Q4

N2–Q1?

K2

–^1

d1N1

g2N1

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T T 1–2 1–2

T T 1–2 1–2

T1–2

T1–2 T1–2

T1–2

N2–Q1?

K2

–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

g2N1

g2N1

g2N1 Q4

Q4

Q4 Q4

Q4 Q4

Q4

Q4

Q4

Q4

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

N2–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

K2

–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

g2N1

g2N1

g2N1

g2N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1 g2

N1

g2N1

g2N1

Q

Q

Q Q

Q

Q

Q

Q

Q

Q

Q

Q

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q4

Q3–4?

Q3–4

?

Q3–4

?

Q3–4

?

Q3–4

?

Q3–4

?

Q3–4?

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2 T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

T1–2

Q

Q

Q

Q

Q

Q

Q4

Q4

Q4

Q4

Q4

Q4

Q4

N2–Q1?

N2

–Q1?

N2

–Q1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

K2–^1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N g 1 2

N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

g2N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1

N2–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2

–Q1?

N2–Q1?

N2–Q1?

N2

–Q1?

N2–Q1?

N2–Q1?

N2

–Q1? N2

–Q1? N2

–Q1?

N2

–Q1?

Haftadchashma

pluton

Jangalzarak

pluton

Ahankashan pluton

Ahankashan pluton

northern lobe

Ahankashan pluton

western occurrence

Rakhna pluton

Ahankashan plutonnorthern lobe

Ahankashan pluton

Jangalzarak pluton

Rakhna pluton

Haftadchashma pluton

Ahankashan pluton

Ahankashan pluton

northern lobe

T1–2

T1–2

T1–2

T Q4 1–2

Q4

N2–Q1?

N2–Q1?

N2–Q1?

N2–Q1?

N2–Q1?

K2–^1

K2–^1

d1N1

Rakhna pluton

Trench 15

Trench 16

Trench 10

Trench 8

Trench 9

Trench 10

Trench 9

Trench 8

Trench 6

T1–2

T1–2

T1–2

K2–^1

K2–^1

K2–^1

K2–^1

d1N1

d1N1

d1N1

d1N1

d1N1

d1N1 d1

N1

d1N1

g2N1

Trench 16

T1–2

T1–2

T1–2

T1–2

K2–^1

K2–^1

K2–^1

d1N1

g2N1

g2N1

g2N1

Trench 10

Trench 8

Trench 9

K2–^1

6

8

9

10

11

2

4

3

5

6

7

5

2

4

3

Outline of Ahankashan gold

deposit and trench map (B)

1

MAGNETIC NORTH

3

APPROXIMATE MEAN

DECLINATION, 2014 TRUE NORTH

°

100 meters = 328 feet NO VERTICAL EXAGGERATION Vertical scale and surface elevations on cross 

sections not modified from the original compilations.

100 meters = 328 feet NO VERTICAL EXAGGERATION Vertical scale and surface elevations on cross 

sections not modified from the original compilations.

64°24'0"E 64°24'30"E

64°23'30"E 64°24'0"E 64°24'30"E 64°25'0"E

64°23'0"E 64°23'30"E

64°22'30"E

64°22'0"E

34°39'0"N 34°39'0"N

34°38'0"N

34°39'30"N 34°39'30"N

34°40'0"N 34°40'0"N

34°40'30"N 34°40'30"N

34°41'0"N

34°42'0"N

34°41'30"N

34°41'0"N

34°41'30"N

34°42'0"N

34°38'0"N

34°37'30"N

34°38'30"N 34°38'30"N

64°27'0"E

64°26'0"E

64°25'0"E

64°24'0"E

64°23'0"E

64°22'0"E

64°21'0"E

64°34'0"E

64°33'0"E

64°32'0"E

64°31'0"E

64°30'0"E

64°29'0"E

64°28'0"E

64°40'0"E

64°39'0"E

64°38'0"E

64°37'0"E

64°36'0"E

64°35'0"E

64°27'0"E

64°26'0"E

64°25'0"E

64°34'0"E

64°33'0"E

64°32'0"E

64°31'0"E

64°30'0"E

64°29'0"E

64°28'0"E

64°40'0"E

64°41'0"E

64°39'0"E

64°38'0"E

64°37'0"E

64°36'0"E

64°35'0"E

34°42'0"N

34°41'0"N

34°40'0"N

34°39'0"N

34°38'0"N

34°37'0"N

34°42'0"N

34°41'0"N

34°44'0"N

34°45'0"N

34°43'0"N

34°40'0"N

34°39'0"N

34°38'0"N

34°36'0"N

34°35'0"N

34°34'0"N

64°25'0"E