THE GEOMORPHOLOGIC CHARACTERISTICS ON THE ORUMIE LAKE AND THAT EFFECT IN HIS REGION ECOSYSTEM

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NADERSEFAT MOHAMMAD HUSSEIN

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Journal: DANESHNAMEH Year:2011 | Volume:- | Issue:82 Page(s): 23-32

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Title

THE GEOMORPHOLOGIC CHARACTERISTICS ON THE ORUMIE LAKE AND THAT EFFECT IN HIS REGION ECOSYSTEM

Author(s)

NADERSEFAT MOHAMMAD HUSSEIN | Issue Writer Certificate

Keywords

TECTONICQ2

ECOSYSTEMQ2

ARTEMIAQ2

ARAGONITEQ2

ENVIRONMENTQ2

GYPSUMQ2

SITUATIONQ2

FECAL PILLS SEDIMENTQ2

HOLOCENEQ2

PERIODQ2

Abstract

The Orumie TECTONIC lack is located in the north western Iran and between of east and west Azerbaijan states and extended more than 5000 scours meters in trend of north to south. This lack is extended large but very less depth in the world. The water of lack is very saturated by salt. The view point of variety of sediments, Geomorphology characters, compound chemistry, saline waters and another specialty is compared with another lacks.The view point of topography, the lack are surrounded all sides by mountains that extended in deferent directs and elevation. The all networks, drainage waters and rivers from every side entered to lack.The thickness sediments are 35 by 40 meters and located on the lover Cretaceous s basement rocks (Aptien) and Miocene Limestone (Miocene formation). Thus present tense the stage and formation time Orumie lack limit 30 by 40 thousand years, but to studies of around this lack, terraces are estimated those are limit 400 or 500 thousand years stage.Also show that studies in about of lack sediment logy and that sides, the climate in the HOLOCENE PERIOD were is arid.The Orumie lack, very sediments formed from chemical elements and very saturated from salt.Also are destructive sediments that related to fresh waters those are formed in effect of climatic changing in the glacier PERIODs.The important sediments of this lack are more ARAGONITE (Fecal pills) those are bio chemistry sediments that is formed from association and accumulation of sediments on around of ARTEMIA Salina. The pure GYPSUM are formed in intern of mud’s.This lack is located in a SITUATION in the Azerbaijan that its distance from the seas and waters is very far. Thus this lack effect in around of its ENVIRONMENT is very important.In the round of lack are located cities and villages. Thus it climatically an influence is very more. Also a numerous of immigration and local birds and animals are lives in the islands of lack and are dependent this ECOSYSTEM.In addition a numbers of insects (Artemia) are lives in the lack. Thus destruction it is greatest injury for this region ECOSYSTEM.

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APA: Copy

NADERSEFAT, MOHAMMAD HUSSEIN. (2011). THE GEOMORPHOLOGIC CHARACTERISTICS ON THE ORUMIE LAKE AND THAT EFFECT IN HIS REGION ECOSYSTEM. DANESHNAMEH, -(82), 23-32. SID. https://sid.ir/paper/91295/en

Vancouver: Copy

NADERSEFAT MOHAMMAD HUSSEIN. THE GEOMORPHOLOGIC CHARACTERISTICS ON THE ORUMIE LAKE AND THAT EFFECT IN HIS REGION ECOSYSTEM. DANESHNAMEH[Internet]. 2011;-(82):23-32. Available from: https://sid.ir/paper/91295/en

IEEE: Copy

MOHAMMAD HUSSEIN NADERSEFAT, “THE GEOMORPHOLOGIC CHARACTERISTICS ON THE ORUMIE LAKE AND THAT EFFECT IN HIS REGION ECOSYSTEM,” DANESHNAMEH, vol. -, no. 82, pp. 23–32, 2011, [Online]. Available: https://sid.ir/paper/91295/en

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