The Zagros Mountains are a major fold and thrust mountain belt stretching roughly one thousand five hundred kilometers from northwestern Iran through southeastern Iraq toward the Strait of Hormuz. The range formed, and continues to form, through the ongoing collision of the Arabian and Eurasian tectonic plates, which has folded and thrust thick layers of sedimentary rock into long, parallel ridges. The foothills of the Zagros hold some of the largest oil and gas reserves in the Middle East, trapped within the range's folded rock structures.
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Source Zagros Mountains (Wikipedia)
Source Zagros Mountains (Wikipedia)
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Source Zagros Mountains (Wikipedia)
Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Zagros Mountains
In Discipline
Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Zagros Mountains
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Also in Geography Atlas: where this subject is found.
Source Wikidata: Zagros Mountains
Also in Geography Atlas: where this subject is found.
Source Wikidata: Zagros Mountains
Also in Geography Atlas: where this subject is found.
Source Wikidata: Zagros Mountains
Sources
Wikidata: Zagros Mountains
Wikidata Q167021, class allow-list match (w-wdresolver-0926)View the Source Zagros Mountains (Wikipedia)
Associated With: Miocene, Article text, age Miocene
This collision mainly happened during the Miocene (about 25-5 mya) and folded the entirety of the rocks that had been deposited from the Paleozoic (541-242 mya) to the Cenozoic (66 mya, present) in the passive continental margin on the Arabian Plate.
Associated With: Limestone, Article text, rock Limestone
The mountains are completely of sedimentary origin and are made primarily of limestone.
Associated With: Gypsum, Article text, rock Gypsum
There is also much water-soluble gypsum in the region.
Caused By: Folding, Article text, process Folding
Stresses induced in the Earth's crust by the collision caused extensive folding of the preexisting layered sedimentary rocks.
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