is formed by the shore of the Caspian until it touches the Bay of Hassan Kul north of As arabad. East of the Caspian Sea and beginning at Has an Kuli Bay the river Atrek serves as the frontier as far as Chat. It then extends east and south-east to Serrakhs on the Tejen River in 36° 40′ N. and 61° 20′ E. The distance from Mt Ararat to Serrakhs in a straight line is about 930 m. The frontier from Mt Ararat to Astara was defined by the treaty of Turkmanchai (Feb. 22, 1828), and a convention of the 8th of July 1893. The frontier east of the Caspian was defined by the Akhal-Khorasan Boundary Convention of the 21st of December 1881 and the frontier convention of the 8th of July 1893.
The eastern frontier extends from Serrakhs to near Gwetter
on the Arabian Sea in 25° N. and 61° 30′ E., a distance of about
800 m. From Serrakhs to near Kuhsan the boundary
is formed by the Tejen River (called Hari Rud, or
river of Herat, in its upper course); it then runs
Eastern
Frontier.almost due south to the border of Seistan in 31° N., and then
through Seistan follows the line fixed by Sir Frederick Goldsmid’s
and Sir Henry McMahon’s commissions in 1872 and
1903–1905 to Kuh i Malik Siah. From this point to the sea the
frontier separates Persian territory from British Baluchistan
and runs south-east to Kuhak and then south-west to Gwetter.
This last section was determined by Sir Frederick Goldsm1d’s
commission in 1871.
The southern boundary is the coast line of the Arabian Sea
and the Persian Gulf from Gwetter to the mouth of the Shatt
el Arab, a distance of about 870 m., comprised
between 48° 40′ E. and 61° 30′ E. The islands situated
close to the northern
shore of the Persian Gulf areSouthern
Frontier.
Persian territory, they are, from east to west, Hormuz (Ormus),
Larak, Kishm, Hengam, Furur, Kish (Kais), Hindarabi,
Shaikh-Shu’aib, Jebrin, Kharak, Kharaku (Khorgu).
Physical Geography.—Modern Persia occupies the western and larger half of the great Iranian plateau which, rising to a height of from 4000 to 8000 ft. between the valleys of the Indus and Tigris, covers more than a million square miles. Taking the Kuren Dagh or Kopet Dagh to form the northern scarp of this plateau east of the Caspian, we find a prolongation of it in the highlands north of the political frontier on the Aras, and even in the Caucasus itself. On the north-west Persia is united by the highlands of Armenia to the mountains of Asia Minor; on the north-west the Paropamisus and Hindu Kush connect it with the Himalayas. The lines of boundary on the western and eastern faces are to be traced amid high ranges of mountains broken here and there by deserts and valleys. These ranges lie for the most part north-east and south-east, as do those in the interior, with a marked exception between Teherān and Bujnurd, and in Baluchistan, where they lie rather north-east and south-west, or, in the latter case, sometimes east and west. The real lowlands are the tracts near the sea-coast belonging to the forest-clad provinces of the Caspian in the north and the shores of the Persian Gulf below Basra and elsewhere. The Persians have no special names for the great ranges. Mountains and valleys are known only by local names which frequently cover but a few miles. Even the name Elburz, which European geographers apply to the chains and ranges that extend for a length of over 500 m. from Azerbaijan in the west to Khorasan in the east, stands with the Persians Only for the 60 or 70 m. of mountains north and north-east of Teherān, including the cone of Demavend. The great central range, which extends, almost unbroken, for nearly 800 m. from Azerbaijan in the north-west to Baluchistan in the south-east, may aptly be called the Central Range. It has many peaks 9000 to 10,000 ft. in height, and some of its summits rise to an elevation of 11,000 ft. and near Kermān of nearly 13,000 ft. (Kuh i Jupar). The valleys and plains west of the Central Range, as for instance those of Mahallat, Joshekan, Isfahan, Sirjan, have an elevation of 5000 to 6500 ft.; those within the range, as Jasp, Ardahal, So, Pariz, are about 1000 ft. higher; and those east of it slope from an elevation of 5000 to 6000 ft. down to the depressions of the central plateau which, east of Kum, are not more than 2600 ft. and east of Kermān 1500 to 1700 ft. above the sea-level. Some of the ranges west of the Central Range, which form the highlands of Kurdistan, Luristan, Bakhtiari and Fars, and are parallel to it, end near the Persian Gulf; others follow the Central Range, and take a direction to the east at some point between Kermān and the sea on the western frontier of Baluchistan. Some of these western ranges rise to considerable elevations; those forming the Turko-Persian frontier west of the lake of Urmia have peaks 11,000 ft. in height, while the Sahand, east of the lake and south of Tabriz, has an elevation of 12,000 ft. Farther south, the Takht-i-Bilkis, in the Afshar district, rises to 11,200 ft., the Elvend (ancient Orontes), near Hamadan, to ll,600. The Shuturun Kuh, south of Burujird, is over 11,000 ft. in height, the Shahan Kuh, Kuh-i-Gerra, Zardeh Kuh and Kuh-i-Karan (by some writers called Kuh-i-Rang), all in the Bakhtiari country west of Isfahan, are 12,800 to 13,000 ft. in height; and the Kuh-i-Dina (by some writers wrongly called Kuh-i-Dinar) has an elevation of over 14,000 ft. Still farther south, towards Kermān, there are several peaks (Bid-Khan, Lalehzar, Shah-Kuh, Jamal Bariz, &c.) which rise to an elevation of 13,000 ft. or more, and the Kuh-i-Hazar, south of Kerman, is 14,700 ft. in height. Beginning near Ardebil in Azerbaqan, where the cone of Savelan rises to an elevation of 15,792 ft. (Russian trigonometrical survey), and ending in Khorasan, the great Elburz range presents on its southern, or inward, face a more or less abrupt scarp rising above immense gravel slopes, and reaches in some of its summits a height of nearly 13,000 ft.; and the peak of Demavend, north-west of Teherān, has a height of at least 18,000 ft. There are several important ranges in Khorasan, and one of them, the Binalud, west of Meshed and north of Nishapur, has several peaks of 11,000 to 12,000 ft. in height. In south-eastern Persia the Kuh-i-Basman, a dormant volcano, 11,000 to 12,000 ft. in height, in the Basman district, and the Kuh-i-Taftan, i.e. the hot or burning mountain (also called Kuh-i-Nushadar from the “sal ammoniac,” nushadar, found on its slopes), an active triple-peaked volcano in the Sarhad district and 12,681 ft. in height (Captain Jennings), are notable features.
Taking the area of Persia at 628,000 sq. m. the drainage may thus be distributed: (1) into the Arabian Sea and Persian Gulf, 135,000 sq. m.; (2) into the Caspian, 100,000; (3) into the Seistan depression, 43,000; (4) into the Urmia Lake, 20,000; (5) into the interior of Persia, 330,000. The first Rivers. district comprises most of the south-western provinces and the whole of the coast region as far east as Gwetter; the second relates to the tracts west, south and east of the southern part of the Caspian Sea. The tracts south of the Caspian are not more than 20 to 50 m. wide; those on the west widen out to a depth of 250 m., meeting the watershed of the Tigris on the one side and that of the Euphrates and Lake Van on the other, and embracing between the two the basin of Lake Urmia. On the east the watershed of the Caspian gradually increases in breadth, the foot of the scarp extending considerably to the north of the south-eastern angle of that sea, three degrees east of which it turns to the south-east, parallel to the axis of the Kopet Dagh. The third drainage area comprises Persian Seistan with part of the Helmund (Hilmend) basin and a considerable tract adjoining it on the west. The fourth is a comparatively small area on the western frontier containing the basin of Lake Urmia, shut off from the rest of the inland drainage, and the fifth area takes in a part of Baluchistan, most of Kermān, a part of Fars, all Yezd, Isfahan, Kashan, Kum, Irak, Khamseh, Kazvin, Teherān, Samnan, Damghan, Shahrud, Khorasan and the central desert regions.
Four rivers belonging essentially to Persia, in reference to the Caspian watershed, are the Seafid Rud or Kizil Uzain on the south-west, the Herhaz on the south and the Gurgan and Atrek at the south-eastern corner of that inland sea. The Seafid Rud rises in Persian Kurdistan in about 35° 50′ N. and 46° 45′ E., a few miles from Senendij. It has a very tortuous course of nearly 500 m., for the distance from its source to the Caspian, 57 m. east of Resht, is only 210 m. in a straight line. The Kizil Uzain takes up some important affluents and is called Seafid Rud from the point where it breaks through the Elburz to the sea, a distance of 70 m. It drains 25,000 to 30,000 sq; m. of the country. The Herhaz, though not important in length of course or drainage, also, like the Seafid Rud, breaks through the Elburz range from the inner southern scarp to the north. It rises on the slopes of the Kasil Kuh, a peak 12,000 ft. in height within the Elburz, and about 25 m. north of Teherān, flows easterly through the Lar plateau, where it is known as the Lar River, and takes up several affluents; turns to the north-east at the foot of Demavend, leaving that mountain to the left, and flows due north past Amol to the Caspian. Its length is about 120 m. The Gurgan rises on the Armutlu plateau in Khorasan east of Astarabad, and enters the Caspian in 37° 4′ N., north-west of Astarabad, after a course of about 200 m. The Atrek rises a few miles from Kuchan and enters the Caspian at the Bay of Hassan Kuli in 37° 21′ N., after a course of about 300 m. From the sea to the Russian frontier post of Chat the river forms the frontier between Persia and the Russian Transcaspian region.
The drainage of the rivers which have no outlet to the sea and form inland lakes and swamps (kavir) may be estimated at 350,000 sq. m., including the drainage of Lake Urmia, which is about 20,000 sq. m. Fourteen rivers flow into the lake: the Aji Chai, Safi Chai, Murdi Chai and Jaghatu from the east, the Tatau (Tatava) from the south, and nine smaller rivers from the west. During heavy rains and when the snows on the hills melt, thousands of streams flow from all directions into the innumerable depressions of inner Persia, or help to swell the perennial rivers which have no outlet to the sea. These latter are few in number, and some of them barely suffice for purposes of agricultural irrigation, and in summer dwindle down to small rills. The perennial streams which help to form the kavirs (salt swamps) east of Kum and Kashan are the Hableh-rud, rising east of Demavend, the Jajrud,
