Political
Situation
Daghestan is a republic of Russian Federation. Being
a member of Russian Federative Soviet Socialist Republics, Daghestan Autonomous Soviet
Socialist Republic was established on 20th January 1921. After dissolving of USSR, it has
become a republic dependant to Russian Federation.
Being in the south of European part of Russian
Federation, Daghestan covers 50,300 km2 on the north side of Caucasian Mountains. It is
surrounded by the high summits of Caucasian mountains in the south and west by Guton
summit, 3646 meters high, and Bazardyuzu (Pazardüzü) summit, 4480 meters high. There is
Caspian Sea on the east, Khalmukh Autonomous Republic on the north, Chechen and North
Caucasia on west and northwest, Georgia on southwest and Azerbaijan on its south. Its
capital is Mohackale. Some other big cities are Derbent, Kizlar, Izlerbas and Buynak.
Daghestan is a compount word; including the word
“Dag” meaning mountain in Turkish” and suffix “-istan” meaning land in Persian.
So it has a geographical meaning not a nationalistic aspect. In Russian, it is called
Strana Gor meaning “Land of Mountains. It has five geographical regions. Sulak, Samur
and Kurak rivers formed deep valleys on their route to Caspian Sea. It has very limited
rain on the south sides of Caucasian Mountains. So some parts has no vegetable existence.
Second region is the second mountain range of 920
meters high on the north of this first region. This is a very rainy region because of
north and northwest waves, and it is covered with forests. Narrow coast line between the
mountains and the Caspian Ssea is the third region. There are spreading rivers coming from
narrow valleys. This region has rich ail and gas resources. The fourth region starts with
the large plain and involves low and marsh areas including Terek river delta. Just after
this delta starts the long and sandy Agragan Peninsula. Lastly, it is the fifth reigon
which includes Noghay Plain covered by sandy areas just on the north of Terek river. This
region has a hot and dry climate and shows sahara characteristics.
Most important rivers of Daghestan are Sulak
river, reaching Caspian Sea in Mohackale after joining the Ghazi Kumukh, Kara, Avar and
Andi brooks; Terek on the north, coming from Chechen; and Samur, reaching Caspian Sea
through southeast. Running generally in parallel with mountains, these rivers had an
important role in forming Daghestan’s geographical formation by making 1000 meters deep
valleys.
Daghestan's climate is generally hot and dry. On
low places temperature is around -3, 6 ºC in January and 23 ºC in June. Sulak, Terek and
Samur plain on the north of Daghestan is a plain area without water, of which
highest point 26 meters, and lowering through the sea. Not much population live
here. Some coast line is also below sea level. Between Kuma and Terek there are many marsh
and salt lakes. Between Terek and Sulak, the brooks, Aktas, Yarıksu, Yamansu ve Aksay are
used for agriculture today. Except the higher places in northwest, this area are quite
dry. Being plain without water and forest, not rainy and having north waves, in the places
in north the temperature is 40 ºC in summer and –40 ºC during winter.
Agriculture can only be done near Terek river and southwest by artificial watering
systems. In other places, various Turk tribes live a nomadic life and raising livestock.
On coast line, settlers are occupied with fishery.
Daghestan has many natural resources. Forests on
mountainous area and in valleys and canyons have leafed trees, where there are pine and
birch trees on high hills. Above these tree line, there is an Alpin meadows. On hillsides
there are Sahara type plants which often loose leaves. On lower sides, there are
black-brown fruitful soil. On Caspian sea there are salty marsh places.
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