Kalmuk Steppe, or Kalmyk Steppe is a steppe with a land area of approximately 100,000 km², bordering the northwest Caspian Sea, bounded by the Volga on the northeast, the Manych on the southwest, and the territory of the Don Cossacks on the northwest. The historic home to the Kalmuck or Kalmyks it is in the Federal subject of Astrakhan Oblast in Russia. Before the appearance of the Kalmyks to this region, the area was long known as the Povoletsk steppe by the Russians.
The western Kalmuck Steppe occupied by the Ergeni hills, is deeply trenched by ravines and rises 300 and occasionally 630 ft. above the sea. It is built up of Tertiary deposits, belonging to the Sarmatian division of the Miocene period and covered with bess and black earth, and its escarpments represent the old shore-line of the Caspian. No Caspian deposits are found on or within the Ergeni hills. These hills exhibit the usual black earth flora, and they have a settled population.
The eastern part of the steppe is a plain, lying for the most part 30 to 40 ft. below the level of the sea and sloping gently towards the Volga. Post-Pliocene Aral-Caspian deposits, containing the usual fossils (Hydrobia, Neritina, eight species of Cardium, two of Dreissena, three of Adacna and Lithoglyphus caspius), attain thicknesses varying from 105 ft. to 7 or 10 feet, and disappear in places. Lacustrine and fluviatile mineral deposits occur intermingled with the above. Large areas of moving sands exist near Enotayevsk, where high dunes or barkhans have been formed.
A narrow tract of land along the coast of the Caspian, known as the “hillocks of Baer,” is covered with hillocks elongated from west to east, perpendicularly to the coast-line, the spaces between them being filled with water or overgrown with thickets of reed, Salix, Ulmus campestris, almond trees, &c. An archipelago of little islands is thus formed close to the shore by these mounds, which are backed on the N. and N.W. by strings of salt lakes, partly desiccated. Small streams originate in the Ergenis, but are lost as soon as they reach the lowlands, where water can only be obtained from wells. The scanty vegetation is a mixture of the flora of south-east Russia and that of the deserts of central Asia.
As of 1911, the steppe had an estimated population of 130,000 persons, living in over 27,700 kibitkas, or felt tents. There were many Buddhist monasteries. Part of the Kalmucks were settled (chiefly in the hilly parts), the remainder being nomads. Antony Beevor, in his 1998 book Stalingrad, said that "Russians from the north thought of [Kalmyk Steppe] as 'the end of the world'". In 1943 the people were forcibly deported (see Kalmykia).
- Kalmykia The Kalmyk Steppe was partly occupied by Germans in August-December 1942, the Abwehr until November 1943.
- I. V. Mushketov, Geol. Researches in the Kalmyk Steppe in 1884–1885 (St Petersburg, 1894, in Russian); Kostenkov’s works (1868–1870); and other works quoted in Semenov’s Geogr. Dict. and Russ. Encycl. Dict.
- public domain: Kropotkin, Peter; Bealby, John Thomas (1911). "Kalmuck". In Chisholm, Hugh (ed.). Encyclopædia Britannica. 15 (11th ed.). Cambridge University Press. p. 643. One or more of the preceding sentences incorporates text from a publication now in the
- Guchinova, Elza-Bair (2006). The Kalmyks. Translated by Lewis, David C. London: Routledge. p. 1. ISBN 978-1-138-88225-6.
- Beevor, Antony (1998). Stalingrad. Penguin Books. p. 100. ISBN 0-14-024985-0.