U.S.S.R.-IRAN BOUNDARY
Document Type:
Collection:
Document Number (FOIA) /ESDN (CREST):
CIA-RDP79-00976A000200010003-4
Release Decision:
RIPPUB
Original Classification:
S
Document Page Count:
60
Document Creation Date:
November 16, 2016
Document Release Date:
November 15, 1999
Sequence Number:
3
Case Number:
Publication Date:
February 1, 1951
Content Type:
REPORT
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Published February 1951,
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CENTRAL INTELLIGENCE AGENCY
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WARNING
This document contains information affecting the national
defense of the United States, within the meaning of Title
18, Sections 793 and 794, of the U. S. Code, as amended.
Its. transmission or revelation of its contents to or
receipt by an unauthorized person is prohibited by law.
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M-15
USSR-IRAN BOUNDARY
February 1951
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USSR-IRAN BOUNDARY
TABLE OF CONTENTS
Page
I. Introduction . . . . . . . . . . . . . . . . . . . . . . . 1
II. History of the Boundary . . . . . . . . . . . . . . . . . . . 4
A. West of the Caspian Sea . . . . . . . . . . . . . 4
B. East of the Caspian Sea . . . . . . . . . . . . . . 5
III. Description of the Boundary Area . . . . . . . . . . . . . . 10
A. West of the Caspian Sea . . . . . . . . . . . . . . 10
B. East of the Caspian Sea . . . . . . . . . . . . . . 13
IV. Boundary Disputes and Potential Disputes . . . . . . . . . . 18
A. Soviet Encroachment West of the Caspian Sea . . . . 18
1. Status of the Boundary . . . . . . . . . . . . 18
2. Maps Illustrating the Boundary Problem . . . . 20
B. Disputes and Potential Disputes East of the
Caspian Sea . . . . . . . . . . . . . . . . . . . . 23
1. Lower Atrek River Area . . . . . . . . . . . . 23
a. Boundary Problem . . . . . . . . . . . . . 23
b. Maps Showing Changes in the Lower Atrek
River Area . . . . . . . . . . . . . . . . 34
2. Firuze and Areas to the East . . . . . . . . . 39
V. Relevant Map Coverage of the Boundary . . . . . . . . . . . .. 45
A. USSR Compilations . . . . . . . . . . . . . . . . . 45
B. British Compilations . . . . . . . . . . . . . . . . 46
C. Iranian Compilations . . . . . . . . . . . . . . . . 47
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The current USSR-Iran boundary emerged as a result of the advance of
Russia into the Caucasus and Central Asia during the 18th and 19th centuries.
For a short time in the early 18th century this advance carried Russia south
of the Caspian Sea, but the foothold could not be maintained. Rivalries
between Russia and the other great powers have enabled Iran to maintain
the boundary in approximately the same position since the 1890's. Iran,
alone, has not been a powerful deterring force to Russian expansion south-
ward since the death of the powerful Iranian ruler, Nadir Shah, in 171+7.
The USSR-Iran boundary west of the Caspian Sea was defined in 1828
and amended in 1893. The boundary east of the Caspian Sea was defined in
1881 and in 1893. Ambiguities in these definitions and disagreements
that arose when the time came to demarcate the boundary on the ground
led to at least one serious dispute concerning the location of the line.
Other potential disputes have also been noted as a result of the failure
on the part of the Soviet Union to adhere to the 1921 Treaty of Friendship
with Iran.
In the 1921 Treaty the Soviet Union professed to embark upon a more
"enlightened" policy toward Iran. Although the treaty purported to restore
certain areas to Iran, its vague terms and the failure of the Soviet
r r
Government to implement it have led to further confusion and misunderstanding.
Note: This report has not been coordinated with the intelligence organiza-
tions of the Departments of State, the Army, the Navy, and the Air
Force.
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Since the end of World War II and even well after the termination of
Soviet postwar occupation of parts of Iran, there have been a number of
skirmishes between Soviet and Iranian border forces. In some areas Soviet
forces have followed a consistent policy of moving their posts forward into
Iranian territory, thus, in effect, advancing the boundary also. A joint
Iranian-Soviet commission for the settlement of boundary disputes was estab-
lished and held its first meeting in November 1950. No agreements had
been reported by the end of 1950.
The most important area in active dispute is along the lower Atrek
River, immediately east of the Caspian Sea. West of the Caspian Sea,
principally on the Moghan Steppe, are areas in which the Soviets have
actually advanced their frontier posts into Iran across a boundary that
had been agreed upon and demarcated. In addition, there are areas of
potential dispute east of the Caspian Sea, in the central mountainous
section of the USSR-Iran boundary and along the Hari Rud.
US officials have been hampered in making a proper evaluation of
conflicting claims by lack of firsthand knowledge of the areas in question.
Accounts of incidents along the Atrek River immediately east of Gasan-
Kuli Bay, in particular, have been based on out-of-date mapE.. At the time
the incidents occurred, Iranian border forces in this area may have lacked
adequate knowledge of: (1) the location of the boundaryl and (2) the
relative positions of places.
1. Reference is made here to the boundary shown on Soviet ziaps. Throughout
the report and on the accompanying maps the terms "internat'_onal boundary"
and "boundary" mean the boundary according to the Soviet version, since it
is the actual operating boundary in most areas. Where alluuiion is made to
the boundary claimed by the Iranians, this fact is indicated.
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In this report the agreements that form the legal basis for the boundary
are discussed from the point of view of boundary history, and factors to be
considered in evaluating the more important conflicting claims are presented.
All available primary source maps relevant to the USSR-Iran boundary are
analyzed on the basis of accuracy of portrayal of boundary data, with
special emphasis on disputed areas. The present report incorporates the
results of this research analysis. Questions of sovereignty and fishing
rights in the Caspian Sea and water rights on rivers flowing along or
across the boundary are not considered.
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II. HISTORY OF THE BOUNDARY
A. West of the Caspian Sea
The present USSR-Iran boundary west of the Caspian Sea had its in-
ception in the Treaty of Gulistan in 1813. By the terms of the treaty
Russia expanded across the Caucasus Mountains. Iran ceased to be a major
power in the Caucasus area. The complete definition of the boundary line,
however, came with the next Russian advance southward and is embodied in
the Treaty of Turkmanchai of 1828.1 This treaty gave the 113ussians the
provinces of Erivan (Yerevan) and Nakhichevan and described the frontier
from Turkey (the Ottoman States) eastward to Iranian Astara on the Caspian
Sea. The boundary established has remained in effect since 1828, except
in the Abbasabad district.
The boundary was demarcated shortly after the Treaty of Turkmanchai
was negotiated. An Englishman on the boundary commission, Lieutenant-
Colonel W. Montieth, described his field maps so completely that the des-
criptions serve to a great degree in lieu of the demarcation maps, which
are unavailable.2
In 1893 a convention between Russia and Iran dealing mainly with the
area east of the Caspian also restored to Iran the land along the right
1. Treaty of Peace between Russia and Persia signed at Turkmanchai
10 February 1828. British and Foreign State Papers, 1827-1828, Vol. RV,
London, 1829, pp. 669-675.
2. W. Montieth, Notes on Georgia and the New Russian Conquests beyond the
Caucasus, Part II, "Description of the frontier of Russia and Persia as
settled by the Commissioners in the years 1828 and 1829," Fp. 29-10 (no
place or date of publication given).
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bank of the Aras River opposite the former fortifications of'Abbasabad;l
this land had been ceded to Russia by Article IV of the Treaty of
Turkmanchai.
B. East of the Caspian Sea
The USSR-Iran boundary from the Caspian Sea eastward to the Afghan
frontier is the result of three basic agreements between Russia and Iran
during the period from 1869 to 1893?
In 1869 the Russians recognized Iranian sovereignty up to the banks
of the Atrek River.2 The boundary along the lower course of the Atrek
just east of Gasan-Kuli Bay, however, has never been demarcated to the
satisfaction of both parties.
The Akhal-Khorassan Convention in 1881 described the boundary east of
the Caspian Sea from Gasan-Kuli Bay to the "oasis at the road from Gavers
(Gyaurs) to Lutfabad, leaving the fortress of Baba Durmaz to the east."3
1. Convention between Russia and Persia for Territorial interchange,
signed at Teheran 27 May-8 June 1893. British and Foreign State Papers,
1893-1894, Vol. LXXXVI, London, 1899, pp. 1246-1249. Article III, p. 1247-,
described the new frontier in the Abbasabad district, west of the Caspian
Sea.
2. Agreement between Russia and Persia, recognizing the Atrek River as the
boundary, 13 December 1869. Treaties &c. concluded between Great Britian
and Persia, and between Persia and Other Foreign Powers, wholly or artiall
in force on the 1st April 1891, London, 17-91, pp. 133-134. This boundary
agreement covered an area extending inland to the end of the Gurgan district
only, a distance of approximately 30 miles.
3. Convention between Persia and Russia of 9-21 December 1881, defining
the boundary between the two countries east of the Caspian Sea (Akhal-
Khorassan Boundary). Treaties &c I. in force on the lot April 1891;
Article I, pp. 137-138. Article II provided for "Special Commissioners"
to trace the boundary defined by Article I. According to Article III,
Persia evacuated the forts of Giamab and Kulkulab, which lay north of the
line described in Article I.
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From this rather indefinite point to the frontier of Afghanistan the
boundary is described by Article V of the Convention of 1893.1 In addition,
by the Convention of 1893 Iran'gave to Russia "the village of Firuze' and
the entire district between the frontier line established in 1881 and the
line extending-from the Kenare Mountains to the summit of the Bir Range."
In return, Iran received confirmation of its possession of the village of
Hisar Qal'eh (Hissar).2 Article V provided for the appointment of com-
missioners to trace the frontier (1) from Baba Durmaz eastward to the
Afghanistan frontier and (2) in the districts of Firuze and Hissar.
Most of the boundary defined in 1881 was demarcated about 1886. A
protocol dealing with the boundary from Baba Durmaz to Gasan-Kuli Bay is
said to have been signed on 10 February 1886, and maps of he border region
at the scale 1:84,000 were prepared. An additional agreement and another
protocol regarding the boundary along the lower Atrek were negotiated, but
the boundary in this area continued to be in dispute. The Convention of
1893 was followed by protocols of 23 January 1894, 8 November 1894, and 9
November 1894,3 which presumably dealt with the demarcation of the boundary
from Baba Durmaz to the Afghan frontier and in the areas west of Baba Durmaz
that were ceded to Russia. Copies of these boundary protocols and maps
are not available in Washington.
1. Convention between Russia and Persia for Territorial interchange,
signed at Teheran 27 May-8 June 1893. British and Foreign State Papers,
1893-1894, Vol. LXXXVI, London, 1899, pp. 1246-1249.
2. The Hissar in question is shown as Hisar Qal'eh on Sheet J40R.
Muhammadabad, of the September 1942 edition of the 1:253,440, British
Geographical Section, General Staff, series (GSGS 3919)-
3. Mohammed Ali Mokhbar, The Frontier of Iran (in Persiar), Teheran,
1945, p. 16.
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In 1921, following the rise of the Soviets, a new treaty was concluded
between Iran and the Socialist Republic.1 In this Treaty the Soviets dis-
avowed the "policy of oppression" toward Iran followed by the former
"imperialistic" Tsarist Government and declared that
...all treaties, agreements and conventions signed between
the Tsarist Government of Russia and Persia, by which the
former impaired the rights of the people of Persia, are
hereby cancelled and declared null and void.2
This declaration of general policy was followed in Article III by ter-
ritorial provisions. The article provided that
The High Contracting Parties agree to recognize and accept
the Russian-Persian frontier according to the decisions of
the Frontier Commission of 1881.... /T_he7 Soviet Government...
abandons its interest in the island of Ashouradeh and other
islands situated along the coast of the Persian province of
Astrabad. It also returns to Persia the village of Firouzeh
fFiruze', together with the lands adjoining it, which were
transferred to Russia in accordance with the Agreement of
May 20, 1893.
The Persian Government, on its part, consents to the
town of Sarakhs, known as Russian Sarakhe or Old Sarakhs
/erakhs7, together with the lands adjoining it, which lie
along the Sarakhs River, remaining in the possession of Russia.3
Before the treaty was ratified by the Iranian Government, an exchange
of notes took place between the Iranian Minister of Foreign Affairs and
the Soviet Diplomatic Representative in Teheran. The Iranian official
1. Treaty of Friendship, 26 February 1921. Soviet Treaty Series, Vol. I,
1917-1928, Washington, D.C., 1950, pp. 92-98?
2. Soviet Treaty Series, Vol. I. p. 93-
3. Soviet Treaty Series, Vol. Z, p. 93_
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requested clarification of certain articles of the treaty which, according
to him, were "worded vaguely" and asked that the "error which has been
made in Article III, in which the word 'Commission' was written instead of
'Treaty,"' should be corrected. According to the Iranian Fo:eign Minister,
the only treaty concluded in 1881 was the frontier delimitation treaty
referred to in Article III. In reply, the Soviet representative referred
to the "small error to which you draw attention in Article III with re-
ference to the Convention of 1881" and gave some general assurances that
he personally would be willing to promote negotiations for a total or
partial revision of all the articles in question "as far as the interests
of Russia permit."1 The treaty, according to its own provisions, was toy
become effective upon being signed at Moscow, 26 February 1921, but ratifi-
cation was delayed. The two governments did not actually exchange ratifi-
cations until 26 February 1922.
Apparently the questionable articles were never revised. Firuze and
its adjacent area were not ceded to Iran, nor did the Soviet Union con-
sent to make any other boundary adjustments in favor of Iran... The Soviets,
however, retained control of Russian Sarakhs. (See map CIA 11657.)
The Treaty of 1921 made provision for a mixed commission of Russians
and Iranians to decide on territorial questions in dispute. In 1922 a
mixed commission was set up to 'study the boundary question. Soviet
1. Exchange of Notes Relative to Articles III, V, VI, XIII and XX of the
Treaty of Friendship Signed. at Moscow, February 26, 1921. The Iranian
/ersian7 note dated Teheran, 12 December 1921 was signed by "Mocharos-
Saltaneh, Persian Minister for Foreign Affairs." The Soviet note dated
Teheran, 12 December 1921 was signed by "Rotstein fTothsteir.7, Diplomatic
Representative of R.S.F.S.R.", Soviet Treaty Series, Vol. I, p. 150.
- 8 -
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objections regarding matters which were considered indisputable by the
Iranians were so numerous that the Iranian mission returned to Teheran
after 11 months in the field without reaching any agreements.1
1. Mokhbar, The Fron;-ier of Iran, p. 17.
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III. DESCRIPTION OF THE BOUNDARY AREA
A. West of the Caspian Sea
The topography along the boundary west of the Caspian Sea is shown on
the accompanying map (CIA 11686). With the exception of the boundary in the
northeastern part of the Moghan Steppe area, the line follows river courses
and divides between drainage basins, usually through mountainous country,
throughout most of its length.
In the northwest the USSR-Iran boundary begins at the meeting of the
strewn Ninji Kara Su with the Aras River. Eastward from this point the
boundary follows the roughly parabola-shaped course of the Aras River to the
vicinity of Tazakend on the Moghan Steppe. In general, the demarcation gave
islands in the Aras River to the nation to which the islands were the closer.
On available maps, however, there is no positive evidence that indicates
sovereignty over islands in the river, though it was established at the time
of demarcation.
The valley of the Aras River varies in width where it separates the
mountain systems of the Nakhichevan, Armenian, the Azerbaijan SSR's from
the Iranian Province of Azerbaijan. The northwestern sector of the
basin is wider than the central part. Approximately 15 miles west of
Julfa the valley narrows sharply and becomas entrenched between the
mountains for a distance of over 10 miles. Between Julfa and the vicinity
of Khuda Afarin the valley is generally narrow. In this section the valley
is dominated by the Qara Ddgh massif on the Iranian side and the Zangezurskiy
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Khrebet and associated ranges on the Soviet side. In the 30-mile stretch
between Khuda Afarin and the point where the Qara Su joins the Aras the
basin gradually widens. Beyond the junction the river cuts northeastward
through the widening Moghan Steppe to the vicinity of Tazakend.
From a point slightly northeast of Tazakend the boundary follows a
straight southeasterly line for approximately 31 miles across the Moghan
Steppe to a point just west of the Azerbaijan SSR town of Belyasuvar on
the stream Bolgar Chai. This is the area in which the Soviet forces have
made the largest continuous incursion across the Iranian frontier. (See
map CIA 11686.)
Beyond Belyasuvar the boundary extends in a generally southward
direction up the S-shaped curve of the Bolgar Chai to its headwaters.
From here it follows the crest of the Reshteh-E-Talesh hills, continues
southwestward, then turns southeastward along the divide between the
basin of the Qara Su and small streams flowing into the Caspian until
it reaches the Astara River, which it follows to the Caspian Sea.
Some Kurdish groups are found in the extreme northwestern part of
the boundary area. The people of the rest of the Aras Basin, however,
are primarily Azeri-speaking Turks, who are concentrated in scattered
villages or groups of villages. Julfa, Maku, Khoi, and Marand, in
reality, are large aggregations of several villages surrounded by fields.
With the exception of Julfa, these settlements are market towns for the
crops of neighboring oases, which produce opium, tobacco, cereals, dried
fruit, and cotton. East of the Aras Basin are the nomadic tribes of the
Moghan Steppe and scattered hill people of the Reshteh-E-Talesh area.
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Three important motor routes cross the USSR-Iran boundary west of the
Caspian Sea (see maps CIA 11686 and 11692) -- at Astara, Jul.fa, and Pul
Dasht.
On the Iranian side of the boundary the Astara crossing leads to
(1) The Fulfa - Tabriz - Teheran road via either (a) the
Astara - Ardebil - Bustanabad route or (b) the Ardebil -
Ahar ?- Tabriz route;
(2) The capital, Teheran, via (a) the Astara - Reisht - Qazvin
route or (b) the Astara - Resht - Chalus route;
(3) Roads leading southward to the Persian Gulf, Damascus, and
Baghdad via (a) Teheran or (b) Qazvin.
On the Soviet side the Astara crossing leads to Baku, at wh_ch point primary
routes radiate out into the Caucasus (see map CIA 11692).
The crossing at Iranian Julfa ranks with the Astara crossing in
importance. Julfa connects by one primary route to Teheran via Tabriz, and
by another primary route to Khoi, from which point a primary route leads to
the Turkish frontier. On the Soviet side, Dzhul'fa is connected with the
Soviet road network leading to Tiflis and the Black Sea (see map CIA 11692).
Pul Dasht is the motor crossing closest to the Turkish frontier. The
route from Pul Dasht connects with the primary route that intersects the
Maki-Khoi primary route approximately 8 miles southeast of ]4aku, from which
point another primary route leads into Turkey.
On the USSR side of the boundary the broad-gauge (5-foot) Transcaucasus
railway roughly parallels the Aras River. This part of the railway connects
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with (1) Tiflis via Yerevan (Erivan) and (2) Baku, all of which connect
with the Ukrainian rail net. A branch also leads southward from Baku,
ending approximately 3 miles north of the Soviet town of Astara.
Although a twin-arched steel railroad bridge at Julfa crosses the
Aras River into Iran, there is at present no exchange of railroad cars
between countries. The bridge is approximately 500 meters upstream
from the motor bridge and is the only rail crossing along the entire
USSR-Iran frontier either east or west of the Caspian Sea.
The railway on the Iranian side of the boundary extends from Julfa
southward 92 miles to Tabriz. This section of the line is broad-gauge
(5-foot), like the Soviet Transcaucasus line. The Julfa-Tabriz line is
reportedly being considered for conversion to standard gauge (1+ feet
82 inches), in conjunction with the program for linking Tabriz to Mianeh,
which is the present railhead for the standard-gauge line running west
from Teheran. From Teheran the line runs southward to the Persian Gulf
at Khurramshahr and Bandar-e-Shahpur.
B. East of the Caspian Sea
The USSR-Iran boundary area east of the Caspian Sea includes a
mountainous area in the middle, with lowland valleys at either end --
that of the Atrek near the Caspian on the west and that of the Hari Rud
(Tedzhen) an the east. The Soviet Union is in possession of nearly all of
the great Central Asian lowland, and the principal Central Asian route from
Krasnovodsk via Ashkhabad and Mary (Merv) to the east lies entirely within
Soviet territory (see map CIA 11692).
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The boundary begins on the Caspian Sea and proceeds across a partially
reclaimed lowland to a point near longitude 54?10'E. At this point the line
dips southeasterly along the approximate axis of the old channel of Gasan-
Kuli Bay to approximately latitude 37?17'N. Thence the boundary runs
northeasterly to the approximate position of latitude 37?21+'N longitude
54?30'E, where it joins a channel called the sukhoye ruslo Atrek (dry
river bed Atrek) by the Soviets and the Musa Khcn by the Iranians (see
map CIA 11674).
The dry river bed Atrek continues to form the boundary until it
reaches the relatively permanent channel of the Atrek slightly north of
the Iranian town of Inchaburun. Beyond this the boundary fcllows the
Atrek, which winds northward and northeastward through the lowland to
Chat-i-Atrek (see map CIA 11657).
Most of the central section of the frontier area lies within the
Kopet Dag mountain system and associated ranges. At Chat-i-Atrek the
boundary turns northeasterly, and, between the neck of land separating
the Atrek and Sumbar Rivers, follows the ridges of the Songt Dag and
Syagirim Dag eastward to approximately 38?05'N - longitude F6?19'E.
From this point the boundary runs northward to the Chandir River,
thence turns northeast across the mountains and east across the ridge
separating the Chandir and Sumbar Rivers to the SLmmbar River. Beyond
this point it follows the Sumbar approximately to the intersection of the
river with the meridian of 57?E. There the boundary begins a northward
curve to a point a few minutes north of latitude 38?15'N, ircluding a
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part of the extreme upper watershed of the Sumbar River within Iran. At
approximately longitude 57?15'E the boundary begins a southeasterly course
and continues along a ridge of the Kopet Dag system, the Tapparov, to a point
a few minutes south of latitude 38?N and a few minutes east of longitude
57?15'E. Here the boundary begins a more easterly and southerly course
along another crest of the Kopet Dag system, the Masinev. The boundary
*then continues to the southeast, crosses the stream Firuzanin Su, and
turns more sharply southeast at approximately longitude 37?45'E - latitude
58?10'N. From this point the boundary continues south to approximately
latitude 37?)40'N - longitude 58?l2'E, where the line again swings in an
irregular eastward course, emerging from the mountains west of Lutfabad.
The boundary skirts Lutfabad on the north before turning south again.
The line passes to the east of Hisar Qal'eh (Hissar in the 1893 convention)
and continues south to the stream Zangenanli Chai, where it turns south-
eastward through the mountains to the Chechehen River. From this point
the boundary runs due east to the Hari Rud (Tedzhen River) north of Iranian
Sarakhs and follows the Hari Rud to the Afghan frontier just north of
Zulfigar.
The people of the immediate boundary area are neither ethnically nor
linguistically unified. In general, the Turkoman people of the lower Atrek
River area and the western part of the highlands along the border speak
a form of Azeri sometimes called Jaghatai. Racially and linguistically,
they are more akin to groups in Central Asia than to the Turkic elements
in Persian Azerbaijan. Eastward the highlands border area has Turkoman,
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Iranian, and a few Kurdish and Hazara ethnic groups. In thy; lower mountain
border areas that merge with the Harf Rud Valley, Persian in the chief language
spoken in an area containing Afghan Hazara, Turkoman, and Iranian groups.
The route crossings between the USSR and Iran east of he Caspian
Sea, classified on the basis of importance, are shown on thy: accompanying
map (CIA 11692). Motorable routes cross or connect with th.3 frontier at
four places -- west of Inchaburun,1 and at Ba,jgiran, Lutfabid, and Sarakhs.
Of these four, the one on the sukhoye ruslo Atrek (dry river bed Atrek)
immediately north of Tengeli provides the shortest approach to Gurgan and
Teheran. In the USSR this route continues to Kizyl-Arvat oa the Turk-
Sib railway.
Farther eastward there is an entrance from the USSR into Iran at the
Bajgiran frontier post. This route connects the Soviet town of Ashkhabad
with the Iranian town of Quchan and forms a principal link oetween the
Krasnovodsk Ashkhabad-Mary (Merv) route in the USSR and the Teheran-Quchan-
Meshed route in Iran. The route through Lutfabad extends wastward to the
intersection with the Ashkhabad-Bajgiran-Quchan road north of Quchan.
Farther eastward a route from Iranian Sarakhs on the Hari-Rud
extends into the interior to Meshed, the key road center of extreme north-
eastern Iran. Routes from Meshed lead ultimately to both the Afghanistan
1. A wooden bridge across the lower Atrek south of Lake Beum-Bash is
sometimes mentioned in connection with the boundary dispute. It is on a
track leading southeastward from near Chikishlyar, but this route seems to
be of little importance at present.
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and Pakistan frontiers. From Russian Sarakhs there is a road connection
with Tedzhen on the Ashkhabad-Mary route to Samarkand.
No rail lines crosses the USSR-Iran frontier east of the Caspian
Sea. The nearest rail line to the boundary is the Soviet Turk-Sib
railroad, a broad-gauge (5-foot) line. At Lutfabad, this line passes very
close to the boundary. An Iranian rail line extends from Teheran to
Shahrud and is projected eastward to Meshed.
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IV. BOUNDARY DISPUTES AND POTENTIAL DISPUTES
A. Soviet Encroachment West of the Caspian Sea
The USSR-Iran boundary west of the Caspian Sea was define(, in 1828 and
p4rtially modified in 1893. The boundary has been officially demarcated
except for a small area around Shandan rock where it is merely defined.
During the period from 1948 to 1950 the Soviets have been noticeably
violating the demarcated boundary. The accompaning map, entitled U.S.S.R.-
Iran Frontier Area West of the Caspian (CIA 11686), shows the extent of
Soviet encroachment.
1. Status of the Boundary
The most continuous incursion has taken place on the ]4oghan Steppe
between Tazakend and Belyasuvar. In this area the Soviet3 have in-
timidated the nomadic Shahsaven families, who consequently camp several
miles back from the border.1 When these families migrate southward to
summer quarters in the latter part of April, the Soviets hove into the
semipermanent evacuated encampments and often construct dugouts. A new
frontier is then marked out by the Soviets by plowing a new border fur-
row. When the Shahsaven families return in the winter, they again settle
several miles back from the boundary to avoid contact with the Soviets.
Upon a new seasonal migration, this process is-repeated, and Soviet pene-
tration progressively obliterates the old frontiers. The Soviets are also
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contributing to the obliteration of the established boundary at Tazakend
by opposing any Iranian attempt to construct a weir on the Aras River to
retard the river from eroding away the site. Since Tazakend serves as an
anchor site for the boundary in the area, its disappearance would be of
material assistance to the Soviets in a further advance into Iranian ter-
ritory.
Smaller areas of Soviet encroachment are located south of the Moghan
Steppe near the Soviet sites of Dyman and Mistan and the Iranian sites of
Minavar and Baghcheh Sarai (see map CIA 11686).
Research on the problem of the location of the legal boundary has
brought to light what appears to be an earlier Russian violation of the
boundary. The description of the boundary by Commissioner Montieth has
clarified the position of the boundary on Shandan Height. He states that
The commissioners having disputed regarding which branch
of the Astara River was mentioned in the Treaty as forming the
Frontier. It was agreed that the lesser range on which stands
the rock of Shindan fshandan7, and divides the middle from the
Northern branch of the Astara River should constitute the
boundary. Thus rendering unavailable for either party the
strong position of Shindan.l
The 1941 edition of the 1:200,000 and the 1939 edition of the 1:100,000
Astara sheets of the General'nyy Shtab Kraenoy Armii (General Staff Red
Army) map series however follow the earlier Russian precedent of including
Shandan within what is now the USSR. All sheets of the maps of the British
Geographical Section, General Staff, of the same area at 1:210,000 and
1:253,440 also follow earlier official Russian sources in depicting the
boundary. All subsequent compilations have continued to show only the
1. Montieth, Notes on Georgia..., Part II, footnote p. 40.
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Russian boundary claim in the Shandan area.l The explanation to the Shandan
encroachment may have its basis in the terrain of the area, which over-
whelmed the boundary commissioners. Montieth states:
The last part of the Frontier can hardly be said tc be
defined nor was it practicable on.account of the thick 'ungle,
and rocky ridge on which the Shindan stands, to follow the
ridge to the junction with the Astara ravine which then marks
the frontier to the Sea.2
The Shandan area is the only place in which the boundary coamiissioners
divided the dominating height between the two countries but c.id not
demarcate the boundary on account of rugged terrain. Here the Russians
have merely proceeded to attach the territory to their country (see map
CIA 11686).
2. Maps Illustrating the Boundary Problem
The demarcation on the Moghan Steppe followed the broad provisions
of Article IV of the Treaty of 1828. A pyramid was built near the
point of boundary departure from the Aras River; the line then ran
...in a right line through the plain of Magan in a dire-3tion
of S322E to another pyramid erected near Billasewar, on the
Balarood river, a distance of 45 versts; the intermedia-;,e
space being traced by a line of pyramids (or stone circles)
of six feet high3 /ic7.
2. Montieth, Notes on Georgia..., Part II, p. 4+0.
3. Montieth, Notes on Georgia..., Part II, p. 38.
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Unfortunately, no dermarcation maps are available. One Russian map appears
to be the basis of most boundary representations on the Moghan Steppe
between Tazakend and Belyasuvar -- the 1910 revision of the 1898 edition
of Sheet Z9 of the 1:210,000, or 5-verst, series. The map agrees with the
treaty and the subsequent demarcation of the boundary on the Moghan Steppe.
All British 1:253,440 (Quarter-Inch Series) sheets entitled Prishibinskoe
use this official Russian source
An incorrect representation of the boundary on the Moghan Steppe is
shown on Sheet J-39-13, Bel.yasuvar, of the 1:100,000 General'nyy Shtab
Rabotche Krestyanskaya Krasnaya Armiya (General Staff Red Army of Workers
and Peasants) map, 1938 edition. This map does not agree with either the
treaty definition or the demarcation of the boundary. Soviet border forces
using the map would be unable to identify in its entirety the accepted
boundary on the Moghan Steppe.
The situation with respect to boundary information for the Moghan
Steppe is equally
the USSR and Iran
maps covering the
adequately define
following Iranian
serious for Iranian border forces. No boundary between
is shown on either the Iranian 1:50,000 or the 1:253,440
Moghan Steppe. Iranian forces, consequently, cannot
the extent of Soviet encroachment from these maps. The
sheets cover the Moghan Steppe:
Scale
Sheet No.
Title
1:50,000
8
yank
1:50,000
5
Moghan
1:50,000
9
Moghan
1:50,000
10
Moghan
1:253,440
8A
Moghan
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The Soviet encroachment is especially serious because it crosses a
demarcated border. An analysis of available material discloses no basis
for such advance. Regardless of the depth of the encroachment upon Iranian
territory, the fact remains that the boundary is poorly demarcated at pre-
Sent. Stone pyramids 6 feet high, erected well over 100 years ago, can
hardly constitute good demarcation points today. Fixed points, based on a
mutually accepted datum, should be determined for the stretch of boundary
between Tazakend and Belyasuvar.
A recently received mapl with accompanying notes provides some in-
formation hitherto unknown and reveals some Iranian misconcertions con-
cerning the boundary on the Moghan Steppe and Reshteh-E-Taleeh.
The map contributes the following: (1) information on the extent and
location of Soviet penetration of Iran, (2) information on border land-
marks and Iranian methods of measuring distances between thetI, (3) fairly
detailed marginal notes outlining the Iranian claim, (4+) eviLence of Iranian
awareness of specific conditions in the Astara River, and (5; verification
of Iranian claims to Shandan Height.
Misconceptions on the map and its marginal notes include; (1) the
precise angle of the boundary over the Moghan Steppe; (2) th() attribution
to the Turkman Chad Treaty of 1828 of terrain features that are not con-
tained in that treaty; and (3) a treatment unfavorable to Ir3.n of some
features of the boundary demarcation that were actually favorable.
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B. Disputes and Potential Disputes East of the Caspian Sea
1. Lower Atrek River Area
a. Boundary Problem -- According to the Convention of 1881, the
westernmost portion of the USSR-Iran boundary line near the Caspian was
fixed as follows: "Beginning at the Hasan Kuli fGasan-Kuli7 Gulf, the
course of the river Atrek serves as the frontier as far as Chat /hat-i-
Atrek7."1 This portion of the boundary has been in dispute ever since the
signing of the 1881 Convention because the lower Atrek River proved to be
inadequate as a boundary reference line.
The Atrek, rising in the Kopet Dag, flows westward througn the plateau
and then across the trans-Caspian plain to a point north of the Iranian
town of Inchaburun, some 50 to 60 miles below Chat-i-Atrek. The stretch of
the river between Chat and Inchaburun serves fairly well as a boundary be-
cause the Atrek flows in a single channel through an entrenched valley.
From the general vicinity of Inchaburun to the Caspian, a distance of a-
bout 40 miles, the waters of the Atrek divide into a number of channels
(see map CIA 1167+). The northern, or principal, channel extends almost
directly west from the neighborhood of Inchaburun. It is bordered on
either side by marshy land, and in places the banks of the stream merge
imperceptibly with the surrounding marsh.
During the course of time the main channel of the lower Atrek has
changed its position considerably. At one time it reportedly flowed into
the.Caspian Sea or Gasan-Kuli Bay north of its present course. At a later
1. British and Foreign State Papers, 1881-1882, Vol. LXXIII, London,
1889, p. 98.
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ill , PET
date it seems to have run south of the present course, emptying into what
was then the southern part of the Gasan-Kuli Bay. From the 1370's to the
present, however, the river bed has apparently remained in approximately
the same position. Practically all Russian and British maps published
during this period are in agreement in placing the principal channel in
about the position it now occupies.
The main channel forms the northern side of a roughly triangular area
having its apex at Inchaburun and its base along the Caspian, The other
aide of the triangle is formed by the boundary between Iran and the USSR.
The boundary extends along a channel of the Atrek that diverges from the
main channel near Inchaburun and trends southweatwardly, ending somewhat
less than halfway between Inchaburun and the coast. The channel is re-
ferred to on some Russian maps as the sukhoye ruslo Atrek or "dry river
bed Atrek" and appears to be identical with the channel calla3d the Musa
Than by the Iranian. From the point where this dry or inte:^mittent channel
ends the boundary continues southwestwardly over dry land, time sharply
northward, and finally westward to the Caspian (see map CIA 1167+). The
Musa Than channel probably carried more water at one time than it does at
present and probably ran into the southern part of Gasan-Kuli Bay along or
near the line of the present boundary. Another channel or series of inter-
connecting channels, and midway between the main Atrek and the boundary
extending from near the Musa Than westward toward the Caspian, is identi-
fied on the British Quarter-Inch Map as the "Old bed of Atrek River."
At one time this channel probably connected with the Musa 1U.an near the
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nomad camp named Musa Than (see map CIA 11671+, Inset B). In naming this
channel "Old bed of Atrek River," British cartographers probably meant to
represent the stream termed "Old Atrek"on earlier Russian maps. More re-
cent and more detailed Russian maps show an intricate network of small
waterways in the space between the main Atrek and the boundary and do not
identify any of them as the "Old Atrek". It is significant that the so-
called "Old Atrek" is not represented by the British as the channel that
carries the boundary; the boundary channel, the Musa Khan, diverges from
the Old Atrek in the vicinity of Kara-Degish and continues to the south-
west.
In the 1870's and 1880s, Gasan-Kuli Bay was a shallow, lagoon-like
expanse of water 18 miles long, more or less, that extended in a north-
south direction roughly parallel to the main body of the Caspian and con-
nected with it by a narrow strait. The bay was narrower in the middle
than at either end and was thus divided into a northern and a southern
basin. The main channel of the Atrek flowed into the northern basin.
The Old Atrek and the Musa Khan, assuming that there were identifiable
channels by those names, flowed into or toward the southern basin (see map
CIA 11674, inset A). Since the 1880's, Gasan-Kuli Bay has gradually con-
tracted in area because of the lowering of the water level of the Caspian
and probably siltation from the Atrek. The southern basin had definitely
disappeared by 1921, as shown on map CIA 11671-, inset B. In the late 1920's,
or early 1930's a vestige of the northern basin still remained, its north-
eastern limit being approximately latitude 37?26'N and longitude 51?02'E.
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At present the bay has disappeared entirely except for a small indentation
in the Caspian coast line -- the place where the effective boundary ends.
Salt flats or salt marsh cover much of the area formerly occupied by the
bay. Most of the channels of the Atrek seem to end at about the position
of the eastern shore line of Gasan-Kull Bay of the 1870's. according to
recent Soviet maps, the main channel appears to be connected with the sea
by a canal (not shown on the accompanying map because of insufficient data).
ca the other hand, claims that the main channel enters
the Caspian north of the vestigial ('asap-Kuli Bay and the village of the
same name.
The flow of the Atrek varies conElderably from season to season.
During the wet seasor of spring and early summer the waterways are flooded,
and the main channel widens to a corridor of about three and one-half miles.
At this season, surface water probably reaches the Caspian from the dif-
ferent channels, even though the ce"tnable channels themselves do not ex-
tend to the sea. During the dry season, Atrek water that is not diverted
for irrigation upstream is dissipated in the marshes, and very little, if
any, reaches the Caspian as surface irainage. Probably the main channel
is no larger at this season than many of the other interlacing channels.
Even in 1880 the dry season flow of water into Gasan-Kuli Bey was small.
A British traveler about that time had difficulty in findin*; a main channel
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25X1A
of the Atrek, but he was told that in the wet season the Atrek carried a
large volume of water to the bay.l
The area of the lower Atrek is inhabited by Turkomans. Its agri-
cultural resources appear to be negligible. Near Chikishlyar, immediately
northwest of the area, is a potential oil field. Surface indications of
oil have been mentioned in field reports as occurring at Naft-i-Ja (Place
of Oil), but it is not absolutely certain whether the oil indications are
at Naft-i-Jah Post on the boundary or at Naft-i-Jah Hill south of the
boundary.
Article II of the Convention of 1881 stipulated that commissioners
were to be appointed by Iran and Russia to trace the boundary on the ground
and erect boundary markers. the following
events took place after the signing of the 1881 Convention. A canal from
Banda Tepe, west of Inchaburun, to Senger Tepe was dug either by the
Russians or by the native Turkomans under Russian direction. Water di-
verted into this canal formed the channel of Musa Khan, named after a nomad
camp on its banks. About 188+, boundary commissioners were sent to the
field by each country to demarcate the line in the region of the lower Atrek.
1. Edmond O'Donovan, The Merv Oasis: Travels and Adventures East of
the Caspian During the Years 1879-80-81, 2 Vols., London, 1882, Vol. 1,
pp. 116-121. The map accompanying the work shows the main Atrek as
emptying into the northern part of Gasan-Kuli Bay. An evaluation of
O'Donovan's accounts of his journeys along the lower Atrek River in 1879
has revealed his mistaken notion that he crossed the main channel of the
Atrek River. Actually, in his crossing he mistook the southern part of
Gasan-Kuli Bay for the Atrek.
2. Mokhbar, The Frontier of Iran, pp. 13-14+;
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The Iranian representative, Soleiman Khan, proposed that befcre the de-
marcation took place, the courses of the Atrek and the Mnsa Ehan should be
examined and that the boundary should be placed along the main channel of
the Atrek. The Russian representative, Colonel Karpoff, stated that he had
been instructed by his government to designate the Musa Khan as the "Atrek"
and to place the boundary along it. He admitted that the real Atrek was
the one so designated by the Iranians. The work of the commissioners was
suspended because of this failure to agree.
On 28 November 1885 a new agreement was signed fixing the boundary a-
long the Musa Khan rather than the main channel of the Atrek,: This agree-
ment was signed by the Iranian Foreign Minister and the Russ-.an Ambassador
in Teheran. It was negotiated under Russian pressure and apparently was
not approved or ratified by the Iranian Government. The Iranian Govern-
ment now claims that the Foreign Minister had no authority to sign the
agreement. Nevertheless, demarcation commissioners were sen-c into the
field and placed boundary markers along the Musa Khan. A protocol of de-
marcation was signed by representatives of the two countries on 6 March 1886
establishing the boundary along the course of the Musa Khan from Banda
Tepe to Gasan-Kuli Bay.
It is fairly certain that the diversion of water into tae Musa Khan
did not cause any major shift in the main and secondary chanaels of the
lower Atrek. The Tearist Government may have been serious in the claim
advanced through Colonel Karpoff that the Musa Khan should be termed the
"Atrek," but if so, mamy Russian cartographers, official and unofficial,
remained unaware of this fact. Russian maps, with two exceptions, continued
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to show the northern main channel as the true Atrek.. The chief exception
was Sheet 18 of the 1:1,680,000 Map of the Southern Bordering Strip of
Asiatic Russia, an official map published in 1892, which represented the
Atrek as flowing into the southern end of Gasan-Kuli Bay. The 1921
edition of this map, however, indicated that the southern end of the bay
had disappeared and that the "River Atrek" had become the "dry river bed
Atrek." Soviet maps continue to indicate the Musa Khan channel as the
"dry river bed Atrek," and they show the main northern channel as the
Atrek.
The Treaty of 1921 made no specific mention of the.lower Atrek area
in its territorial provisions. It did provide, however, that the two
countries would have equal rights in the use of the waters of the Atrek and
other frontier rivers. A convention providing for the use of frontier
waters and rivers was signed by Iran and the Soviet Union on 20 February
1926. Among other provisions the convention stated that the waters of the
Atrek River should be used in equal amounts by the two countries, but no
mention was made of the location of the boundary.1
In the period between the two World Wars the boundary remained along
the line of the Musa Khan, although a few encroachments were made from the
Soviet side. As the shore line of Gasan-Kuli Bay continued to recede, the
1. Soviet Treaty Series, Vol. 1, Article XVI, p. 315.
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question undoubtedly arose as to the apportionment of the nev land between
the two countries. Judging from the cartographic evidence, the Soviets
made certain small adjustments in the boundary in order to settle the
question in their own favor. The 1938 edition of the Kizyl-Atrek (J-4o-X
sheet of the Red Army 1:200,000 map series represents the boundary as end-
ing near the northern end of the bay, at approximately latitude 37?26'N-
longitude 54?02'E. The 1942 edition of the same sheet does not show
Gasan-Kuli Bay. The boundary on this sheet turns westward at about longi-
tude 54?05'E-latitude 37?23'15"N, extending thence to the Caspian in a
slightly curved line, as shown on map CIA 11674. The Soviet3 had thus taken
a bite off the northern extension of Iranian territory near the Caspian.
A comparison of the two editions of this sheet also reveals a minor
change in the boundary in favor of the Soviet Un'on south of the nomad
camp Chalayuk. This change is so small that it may or may not be a carto-
graphic inadvertence. Iranians also refer to Soviet occupation in 1934
of some territory at Chetli, on the Atrek a short distance E.bove the point
where the main Atrek and the Musa Khan diverge.1
An Iranian general made a survey of the main Atrek below Beum-Bash
Lake in 1922 and claimed to have found that the channe.i entered the sea
north of Gasan-Kuli Bay.2 It is doubtful if other Iranian troops or of-
ficials have been allowed to enter the disputed triangle be';ween the Musa
Khan and the main channel of the Atrek at any time since 1831. The Soviet
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forces withdrew from northern Iran following World War II to the Musa an
line. About eight frontier guard posts were established by Soviet forces
within the disputed triangle. Iranian frontier guard posts were established
opposite several of the Soviet posts, and a namt3r of skirmishes took place
between the forces of the two countries in the latter part of 1948 and in
1949.- In one of these, 11 Iranian soldiers were taken prisoners. Incidents
took place at Sanger Tepe; at Tazehabad post, near the point where the
boundary meets the Caspian coast; and at the Iranian guard post of Naft-i.-
Ja, which is located just south of the southernmost point of the boundary.
The last should not 'be confused with Naft-i-Ja Hill, which is some 5 miles
south of the border.1 In the spring of 1950 Soviet border troops still
occupied the posts in the disputed triangle. Near Naft-i-Ja post Soviets
were reported to have run oil tests. Although the Soviets are reported to
have laid barbed wire entanglements along most of the Iranian-Soviet frontier
east of the Caspian, they did not place any along the boundary south of the
disputed triangle.
Since nc boundary has been agreed upon by the two countries, the
stationing of Soviet troops south of the main channel of the lower Atrek
and the frontier incidents cannot technically be described as violations
of Iranian territory unless Soviet troops advanced south of the boundary
1. Incidents also occurred to the northeast, outside of the area in dispute.
On 4 August 1945, Lieutenant Colonel Kurajin, Commissioner on the Soviet
frontier, stationed at Dashburun, entered Maraveh and forced the Persian
officer.commanding the police to destroy the dams on the Atrek River. By
this action more water was diverted to Soviet territory, with a resulti
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claimed by the USSR. US intelligence reports at the time of the incidents
did not state the precise locations of the incursions. From the general
descriptions and the sketch maps supplied, it appears that most of the
incidents occurred along or very near the boundary claimed by the Soviet
Union. At Tazehabad and along the Caspian coast, however, Soviet forces
advanced considerably southwest of the boundary claimed by t:ae?USSR (see
map CIA 11674). At least one of these reports was based on a sketch map
supplied by an Iranian official, which places the line of th3 Soviet claim
too far to the north, thus giving the impression that Soviet forces had
advanced much farther south of their claimed line than was actually the
case.1 This mistake in location of the Soviet-claimed line or the boundary
in effect in 1950, results from the use of the British Quarter-Inch Series
(1:253,440). The Iranian sketch is based on this series, which is inade-
quate for purposes of boundary location in the disputed area..
Although it is not the purpose of this report to venture a definitive
opinion regarding the merits of the respective Iranian and Soviet claims
on the 'Lower Atrek, some tentative conclusions based on the above discus-
sion are justified.
Iranians claim that the Convention of 1881 is bindingtn respect to the
lower Atrek because (1) the Agreement of 1885 and the demarcation protocol
of 1886 which fixed the boundary along the Musa Khan were not ratified by
Iran, and (2) the Soviet-Iranian Treaty of 1921 provided that the 1881
Convention should be the definitive instrument for settling the boundary
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on the lower Atrek. If the transactions of 1885 and 1886 were repudiated
by Iran, as claimed, the Convention of 1881 would appear to be the only in.
strument having validity. However, the claim that the Soviet Government in
the Treaty of 1921 accepted the provisions of the Convention of 1881 as
applicable to the lower Atrek may be open to question. The Treaty of
1921 did not state that the Soviet Government would return territory on
the lower Atrek to Iran, although it did name the Firuze area to the east,
which Soviet Russia undertook to return. The Soviet Union could claim
that the willingness expressed in Article III of the Treaty to "recognize
and accept" the boundary defined by the "Frontier Commission of 1881" was
intended to cover only the area specifically named later in the same article
but not the Atrek area.
There seems to be no legal basis for the present boundary across the
area formerly occupied by Gasan-Kuli Bay. The Russians probably moved the
boundary around to suit their own purposes. From the old shore line of
the bay eastward along the old course of the Musa Than the Russians may have
advanced the boundary slightly to the south of the line defined by the 1886
protocol.
If and when it is possible to negotiate a settlement of this dispute,
the definitions of the boundary in the lower Atrek region given in the
Convention of 1881 and the Protocol of 1886 (regardless of which one of
these documents is selected as definitive) should be replaced by an en-
tirely new definition. Even at the time it was written, the Convention of
1881 was unsatisfactory in its provisions regarding the lower Atrek because
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of the difficulty in determining with precision of the main channel of the
river.. At present the 1881 and the 1886 instruments are inapplicable, since
both made provision for a boundary only as far west as Gasan-Kuli Bay. An
agreed boundary will have to be defined across the area of the former bay.
If the boundary is related to the Musa Khan, account will have to be taken
of the fact that all or most of this channel is now dry. If the boundary
continues to cross the lower Atrek area, it would be well to define the.
boundary in terms of fixed points and straight segments between the points
rather than in terms of water courses.
An understanding of the dispute on the part of US officials has been
hampered by a lack of direct knowledge derived from field investigation of
the area. Intelligence reports have relied upon inaccurate and out-of-date
British and Iranian maps, whereas the only reasonably accurate maps are the
1942 editions of the 1:200,000 Red Army series.
The preceding discussion has been based in part upon an examination
of Tsarist, Soviet, British, and Iranian maps. The most useful and re-
levant maps are discussed and evaluated from the point of view of boundary
data.in the following section.
b. Maps Showing Changes in the Lower Atrek River Area
A shift in the channel of the Atrek River in the delta area occurred
prior to 1881. In point of time the best available primary source that
por-crays this channel shift is the Russian one-inch to 20-yrerst (1:81+,000)
Map of the Transcaspian Kray published by the Military Topographic Depart-
ment of the Caucasus, dated 1875 but authorized for publication 1882. One
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channel was labeled "new Atrek," and a more southerly branch "old Atrek"
(see map CIA 11674, inset A).
The channel labeled "new Atrek" on the one-inch to 20-verst Map of
the Transcaspian Kray is shown as entering the northern. part of Gaean-Kuli
Bay on the following Russian maps:.
(1) Sheet IX of the one-inch to 40-verat (1:680,000) series en-
titled, Turkestan Military Circuit, prepared by the Turkestan Military-
Topographic Section in 1877 from current data.
(2) The 1:4,200,000 Map of Asiatic Russia and Adjoining Countries,
compiled by the Military-Topographical Division in 1884. This map gives
the northernmost channel of the Atrek as the boundary between the USSR and
Persia.
(3) Sheet V of the 1:4,200,000 set entitled Map of Asiatic Russia
and Adjoining Countries, which was compiled and published by the Military-
Topographical Division in 1884 and reprinted in 1920. This map portrays
the northernmost distributary as the main channel.
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(4) The 1:4,200,000 Map of the Basins of the Oceans, Seas, Rivers
and Lakes of Asiatic Russia and the Neighbouring States, conHtructed by
A. de Tillo, a member of the Academie Imperials des Sciences (St. Petersbourg)
and of the A.cademie des Sciences (Paris), published in 1905. Charnels of
the Atrek River were represented as entering the northern part of Gasan-
Kuli Bay.
(5) Sheet %PIII, Ashkhabad', Gerat', Astrabad', and Meshkhed',
1921 edition from the 1892 printing of a map at 1:1,680,000 entitled Map of
the Southern Bordering Strip of Asiatic Russia. The southern part of
Gasan-Kuli is shown as completely filled in, with the boundary following
the line of the old channel through the southern part of the bay. The
line continues inland on a course labeled "dry bed of the Atrek," which in
reality is the Musa Khan. This 1:1,680,000 map shows the main channel of
the Atrek to the north of the so-called "dry bed", but within the disputed
area it does not name the main channel. The importance of the 1921 edition
lies in its corrections to the 1892 edition. The 1892 edition showed
Gasan-Kuli Bay possessing both northern and southern parts, frith the Atrek
flowing into the southern part. By 19xl the southern part of the bay is
represented as being filled in, leaving 'only the northern pa:-t as the bay.
The same representation continued through the 1937 and 1938 editions of
the 1:200,000 Kizyl-Atrek sheet of the General Staff Red Army series. In
1935 the northern part of the bay was 10 feet deep 4-1/2 mils away from
the shore, according to the U.S. Navy translation of Piloting of the Caspian
Sea (in Russian), published by the Hydrographic Division of the Main Office
of the Naval Forces of the Workers and Peasants Red Army, Leningrad, 1935,
p. 641.
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Possibly the information on the 1937 and 1938 maps and in the piloting
directions regarding the extent and depth of Gasan-Kuli Bay was already
out of date at the time it was published. The 1942 editions of the
1:200,000 Kizyl-Atrek, Gurgan, and Ashref sheets of the General Staff Red
Army series, show practically all of the bay as a marshy land (see main
map CIA 11674). Later map evidence from a Soviet air chart also indizates
that most of the area is now land.
The only official post-1881 Russian maps available on which the Atrek
River is shown as entering the southern part of Gasan-Kull Bay are: (1) the
1:4,200,000 Map of Communications of Asiatic Russia, published by the
Ministry of Communications in 1904, and (2) the previously mentioned Sheet
18, Map of the Southern Bordering Strip of Asiatic Russia, 1892 edition.
The most detailed maps, and the latest primary source compilations
covering the delta of the Atrek River, are the 1942 edition of the Ki7.yl-
Atrek, Gurgan, and Ashref sheets of the General Staff Red Army series at
1:200,000. These sheets form the basis for map CIA 11674. All three of
the Russian sheets were compiled and published in 1942. The Kizyl-Atrek
sheet is based on reconnaissance of 1941 and a 1935 map at 1:100,000; the
Gurgan and Ashref sheets are based on 1941 reconnaissance.
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On the Kizyl-Atrek sheet the name "R. Atrek" is reserved for the main
channel of the Atrek River. The same policy has been followed consistently
on other Soviet maps. Surrounding the Atrek are many water courses, among
which is the eukhoye ruslo Atrek (dry river bed Atrek), which forms the
boundary. The main natural channel of the Atrek flows through a long
narrow swamp north of the sukhoye ruslo Atrek.
Recently, in the course of discussion of the lower ;.trek River boundary,
the Iranians presented in detail their version of the situation on a 1:8+,000
map of the disputed area.1 This is the first Iranian map seen in Washington
that shows the modern shore line of Gasan-Kull Bay. The scale is one re-
ported to have been used by the Russians but not hitherto used by the
Iranians for the Lower Atrek area. The map indicated reliance on Russian
sources by the Iranians, as well as a considerable advance in their carto-
graphic knowledge of the area. However, some of the hydrography shown still
seems to be out of date. The map is important because of the specific
textual detail printed on it, which sheds light on some of the more techni-
cal aspects of the dispute. Information on the map, when ccrrelated with
the boundary shown on the 1:200,000 Red Army sheets for the area and with
other evidence, supports the Iranian contention of a Soviet advance from
the vicinity of Naft-i-Ja Post northwestward to. the Caspian Sea (see map
CIA 11674).
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2. Firuze and Areas to the East
The outstanding areas of potential boundary dispute, as distinguished
from areas of actual dispute, are located around Firuze and in the area
stretching east and southeast to the Hari Rud. These are the areas shown
on map CIA 11657 as lying between the "International Boundary" and the
"approximate boundary defined by convention in 1881."
The 1881 boundary created a. salient of Iranian territory extending
northward along both banks of the stream Firuzanin Su, including the village
of Firuze 1 The segment of the boundary somewhat to the east of Firuze is
defined as follows in the Convention of 1881:
...the frontier-line crosses over to the northernmost summit
of the Aselm range, passing along its ridge in a south-easterly
direction, and then skirting round to the north of the village
of Keltechinar LKalateh Chenar7, it runs to the point where
the Ziri Kou and Kizil Dagh Mountains Join, extending thence
south-eastward along the summits of the Ziri Kuh range, until
it issues into the valley of the Baba Durmaz stream. It then
takes a northerly direction, and reaches the oasis at the
road from Gavers to Lutfabad, leaving the fortress of Baba
Durmaz to the east.2
By the terms of the Convention of 27 May/8 June 1893 the Firuze area
was ceded to Russia. The 1893 Convention stated that Iran would cede to
Russia "the village of Firuze and the entire district between the frontier
1. Russian ideas on the alignment of the boundary in 1881 are shown on
the Copy of Map Furnished by Russian Minister in Tehran to Persian Govern-
ment for Negotiation of Akhal-Khorassan Boundary Question, December 1881,
at the scale of 1:1,260,000. This map appears in Treaties &c concluded
between Great Britain and Persia, and between Persia and Other Foreign
Powers, wholly or partially in force on the let April 1891, London, 1891,
to face page 136,
2. British and Foreign State Papers, 1881-1882, Vol. LXXIII, p. 98.
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line established in 1881 and the line extending from the Kenare Mountains
to the summit of the Bir Range."1 In return for this, Russia was pledged
to cede to Iran the Abbasabad district west of the Caspian and the village
of Hisar Qal'eh (Hissar) at the foot of the Kopet Dag near Lutfabad.
Data on these exchanges of territory are incomplete, and their sub-
sequent history is rather obscure. The boundary protocols signed in 1894,
which are not available in Washington, may have dealt in part with the
Firuze and Kalateh Chenar areas. Detailed Russian and British maps indi-
cate that boundary markers were erected along portions of the boundary
in these areas some time before 1897. The Firuze area ceded by Iran can
be determined fairly accurately by consulting the maps.
In the case of the area to the east and west of Kalateh Chenar, on
the other hand, it is difficult to attempt to trace the boundary as des-
cribed in the 1881 convention on currently available maps, and it is even
more difficult to equate the vague wording of the 1893 convention with the
boundary now in effect. The 1881 line shown on the accompanying map
(CIA 11657) appears to be a reasonable interpretation of the convention of
that year. If the interpretation is correct, it is evident that between
1881 and 1893 or 1894 Russia secured territory adjacent to Kalateh Chenar,
in addition to the area around Firuze: Hiser Qal'eh was '_.ncluded in Iran
as provided in the 1893 Convention.
1. British and.Foreign State Papers, 1893-1894., Vol. LXXXII, p. 1246.
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road from Gavers to Lutfabad, leaving the fortress of Baba Durmaz to the
east. The first paragraph of Article V of the 1893 Convention purported
to define the boundary eastward from this point, and the second paragraph
states:
From Bada Durmaz the frontier line follows the crest of
the Ziriku Larin Kuh7Range south-eastwards towards the village
of Khairabad, but before reaching the lattey it runs along the
left side of the Duranghiar /H-uriz7 Valley.
There are three features bearing the name "Baba Durmaz," but only one
corresponds to the fortress designated by that name in the 1881 Convention.
The present boundary passes south of all three of the features bearing
the name "Baba Durmaz." No provisions were made in the 1893 Convention
for carrying the line from the fortress of Baba Durmaz to the crest of
the Zarin Kuh. It is uncertain whether the boundary was ever actually
demarcated northward from the Zarin Kuh to the Baba Durmaz area. Carto-
graphic evidence suggests it was not demarcated.
If the Soviets had implemented the Treaty of Friendship of 1921,
some of the problems described would have been eliminated. The Treaty
states that the Soviet Government
...returns to Persia the village' of Firouzeh /iruzer7, together
with the lands adjoining it, which were transferrid to Russia
in accordance with the Agreement of May 20, 1893.
Firuze and the adjacent lands have, in fact, never been returned to Iran.
The obligation of the Soviet Government regarding this village was ex-
plicit under the 1921 Treaty, whereas the situations regarding obligations
in other boundary areas were only vaguely implied. The Soviet Government
1. British and Foreign State Papers, 1893-1894, Vol. LXXXVI, pp. 1247-1248.
2. Soviet Treaty Series, Vol. 1, p. 93-
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has ignored both the clearly stated promise to return Firuze to Iran and
the more general promise to recognize and accept the frontier according
to the decisions of the "Frontier Commission of 1881."
No specific mention was made in the Treaty of 1921 of the area east
and west of Kalateh Chenar or the Baba Durmaz area. Nevertheless, in
view of the ambiguities of the 1881 and 1893 conventions rEgarding these
areas, the Iranians might claim them under the general promise contained
in Article III of the Treaty of 1921 to "recognize and accE>pt" the boundary
of 1881.
Iranians apparently do not take the potential boundary disputes in
the Kopet Dag area as seriously as they do the active dispute over the
lower Atrek. With the exception of Sheet 22 K of the 1:25_1,440 series
of the Iranian Army Geographical Division, on which part of the boundary
is missing, the most authoritative Iranian maps show only the present
international boundary in the Kopet Dag area, whereas Iran:.an maps are
generally very careful to show the Iranian version of the boundary along
the lower Atrek. The fact that Iranian maps do not show the largest pos-
sible Iranian claims at Firuze'and in areas to the east is in part a result
of Iranian use of Russian map sources for boundary data. :tn view of the
facts that the Soviets have not ceded any of this territory to Iran and
that the Iranian maps are based on Soviet sources, it is not surprising
that possible claims in the Kopet Dag area have not been pressed.
The extreme eastern end of the USSR-Iran boundary mig'it also be sub-
ject to dispute. Within the past year, Soviet guards are :reported to have
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encroached on Iranian territory along the sector of the boundary that fol-
lows the Hari Rud (Tedzhen River).' The Hari Rud is said to have shifted
westward gradually over a period of many years, and the Soviet border posts
on the east bank of the river are reported to have moved westward corre-
spondingly. The location and extent of these changes is not known.
in this area the Convention of 1893 defined the boundary as
...extending eastwards to the bed of the River Tedjen /edzhen7,
which it joins somewhat to the south of the ruins of the Fortress
Koushut Kale. From this point the bed of the River Tedjen will
serve as a b?undary-line to the beginning of the Afghan possessing
at Zulfagar.
There is no record in available sources of any supplementary agreement
to provide for the location of the boundary in case of Hari Rud should
change its course. If this point has not been decided between the two
parties, the Soviet Union would appear to have as much justification for
moving its frontier posts to conform with the shifting river as Iran would
for claiming that its territory had been encroached upon.3
2. British and Foreign State Papers, 1893-189+, Vol. LXXXVI, p. 12+8.
3. The relative merits of the two cases would depend in part upon the
manner in which the stream had changed course. Generally speaking, if a
boundary river suddenly abandons its old course and creates an entirely
new one, the boundary remains along the old channel, whereas, if the stream
changes course by gradual erosion of one bank and deposition on the other,
the boundary changes with the river. There have been exceptions to this,
however. (See Vittorio Adami, National Frontiers in Relation to Inter-
national Law, London, 1927, pp. 22-27).
Despite the merits of claims for either position, it should be re-
called that, in the case of the Amur Island incidents with Japan in the
spring and summer of 1937, the Soviets claimed that a change in the Amur.
River course did not change the frontier.
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In the locality where the boundary meets the Hari Rud, there is a
possibility of confusion garding the location of the boundary. A number
of dry or intermittent channels spread out fanwise from eith,ir side of the
Hari Rud.. The boundary extends from the west to a point within about 3
miles of the Hari Rud, then turns southeastwards and runs along or roughly
parallel to one of the intermittent channels to the point of junction with
the river. The old fortress of Koushut Kale, referred to in the Convention
of 1893, is located on the eastern bank of the Hari Rud almost due east
of the point where the boundary turns southeast. The Sarakhe sheet of the
British Quarter-Inch series indicates that the boundary in this sector has
been demarcated and shows the locations of the markers. This appears to
be the true alignment of the boundary, and it is so represented on most
Russian and Iranian maps. The Sarakhs sheet of the Iranian Army General
Staff map at 1:1,000,000, however, shows the boundary as cortinuing straight
east to the river at a point exactly opposite Koushut Kale. This is pro-
bably an error. Farther south is the Iranian town of Sarakhs, located a
little to the west of the Hari Rud. The Soviet town of the same name is
located some distance east of the river on one of the intermittent tributary
channels. The Treaty of 1921 confirmed Soviet possession of "the town of
Sarakha, known as Russian Sarakhs or Old Sarakhs."
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V. RELEVANT MAP COVERAGE OF THE BOUNDARY1
In the previous sections of this report, maps have been discussed and
evaluated only insofar as they were essential to an understanding of boundary
disputes and violations. Section V is a discussion of all relevant map
coverage available, with emphasis on significant aspects of boundary represen-
tation.
A. USSR Compilations
In general, the best topographic maps of the boundary area are the
19+2 editions of sheets of the 1;200,000 General Staff Red Army series for
northern Iran, both east and west of the Caspian Sea. These sheets also
give the best representation of the present boundary between Iran and
the USSR. The 19+2 editions were compiled from previous editions and from
reconnaissance surveys undertaken by the government of the USSR during its
occupation of northern Iran early in World War II. The detail presented
surpasses that on any previous compilation, but field checks would be
necessary to determine the accuracy of the maps. The sheets were used as
the basis for CIA 11676. One item has been ignored by the Soviets in their
current protests against mapping of areas in Iran adjacent to the USSR
frontier by non-Iranian nationals -- the Soviets themselves have mapped in
depth most of the frontier areas within northern Iran. For this area the
19+2 edition of the 1:200,000 series is the most recent and most authoritative
1. More detailed information about the general content of maps on Iran may
be found in Chapter IX, Section 92, of the National Intelligence Survey,
No. 33, Iran.
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map available.
In the past, sheets of the 1:210,000, or 5-verst Russian series have been
used extensively for boundary data. They show the Russian version of the
boundary in the lower Atrek River area, at Firuze, and in the areas farther
east. The information presented on the topography and transportation in
immediate boundary areas is now out of date.
The available sheets of the 1938-4+1 edition of the 1:100,000 General'nyy
Shtab Rabotche Krestyanskaya Krasnaya Armiya (General Staff Rad Army of
Workers and Peasants) series that cover the boundary on the Moghan Steppe
and Reshteh-E-Talesh show the land on the Soviet side of the `border in fair
detail. Sheet J-39-13 of the 1938 edition, however, is incorrect for the
boundary northwest of Belyasuvar, and the 1939 edition of the Astara sheet
incorporates Shandan within the USSR.
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C. Iranian Compilations
Iran is an outstanding example of a nation that has depended upon
foreign sources for the cartographic representations of its frontiers.
With but few exceptions the Iranians reproduced British maps of the
boundary, which in turn used boundary data given on official Russian
maps. Thus Iran has generally depended directly or indirectly on Russian
sources for maps showing the position of the common frontier. In the case
of the disputed area on the lower Atrek, however, Iranian maps consistently
show the Iranian claim. The Iranian claim is generally shown on the outdated
1:253,41+0 Pahlewidiz sheet. Recently, however, the Iranian claim has been
depicted on a 1:84,000 map, the attributes of which were discussed in a
preceding section of this study.
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Any Iranian maps covering the boundary area must be closely examined
to determine accuracy. If the frontier on an Iranian map of a disputed
area agrees with that on a Russian map, it is often merely the result
of copying and does not necessarily mean that the Iranians accede to
the Soviet claims.
Four Iranian series contain sheets covering the boundary have been
chosen for discussion. These include (1) a 1:50,000 series :?ublished by
the Iranian Army Geographical Division, (2) a 1:253,440 series published
by the same authority, (3) a 1:1,000,000 series by the same authority,
and (4) a 1:1,000,000 series by General Hajeb All Razmara, formerly
chief of the Geographical Section of the Iranian General Staff and
currently Prime Minister of Iran.
The 1:50,000 series for the frontier area west of the Caspian Sea
is not recommended for purposes of boundary location because (1) the
division of the islands in the Aras River does not generally agree with
official demarcation, and (2) no boundary is shown on the Mcghan Steppe
between Tazakend and Belyasuvar, the area of the most continuous Soviet
encroachment across a demarcated section of the boundary.
The Iranian 1:253,1+1+0 series is based on
In same
cases, however, the Iranian. series differs from these sources. Sheet 8A,
Moghan, does not show a boundary on the Moghan Steppe between Tazakend and
E_lyasuvar. Sheet 15 K, Pah].ewidiz, presents the Iranian boundary claim
in the lower Atrek River area, which is reproduced on inset B of map
CIA 11676. All 1:253,1+1.0 maps"of the lower Atrek area, whether British
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or Iranian, are out of date. The best source to use for hydrography and
USSR-Iran boundary claims is the 1942 edition of the General Staff of the
Red Army map, which forms the basis of the accompanying map CIA 11676.
The extent to which the British and Iranian sheets are out of date is
indicated by a comparison of inset B of CIA 11676 with the main map.
Sheet 22 K, Ashkabad (Guchan), of the Iranian 1:253,4+40 series differs
in not showing a boundary west
of the Ashkhabad-Quchin road; the village of Firuze, Claim by Iran, lies
in this boundary area.
The 1:1,000,000 series published by the Iranian Army Geographical
Division is not recommended for use as far as boundary data are concerned.
On Tabriz, Sheet No. 1, the USSR is incorrectly assigned the neck of land
between the Ninji Kara Su and the Aras River in the extreme northwest
near the junction of the Iran, Turkey, and USSR boundaries. Sarakhs,
Sheet No. 17, represents the Iranian-Soviet boundary as extending
eastward to the main stream of the Hari Rid. No basis for this alignment
is known. The alignment of the boundary on the same sheet does not conform
with the accepted line in the Sarakhs area as shown on Sheet 28 of the
1:1,000,000 series published by General Razmara or on any other maps,
including CIA 11657. In view of conflicting reports on USSR action in the
Sarakhs area, the error on Sheet 17 is important, since Iranians using this
sheet might incorrectly interpret Soviet presence in the area as encroachment.
The 1:1,000,000 series by General Razmara, like Sheet 1 of the 1:1,000,000
series of the Iranian Army Geographical Division, incorrectly assigns to the
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the USSR the neck of land between the Ninji Kara Su and the Aras River. In.
the Sarakhs area the position of the boundary is correct. The Iranian
version of the line is given for the lower Atrek River area.
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