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Geological Formation

Sivalik Hills

Sedimentary and Stratigraphic Formations

The Sivalik Hills, also called the Churia Hills, are a mountain range of the outer Himalayas extending roughly 2,400 kilometers from the Indus River eastward to near the Brahmaputra River, across parts of India, Pakistan and Nepal, with widths of 10 to 50 kilometers and average elevations of 1,500 to 2,000 meters. The range is built from sandstone and conglomerate, poorly consolidated sedimentary deposits eroded from the higher Himalayas and laid down 16 to 5.2 million years ago during the Tertiary period, making the Sivaliks geologically young compared to the main Himalayan range. The hills are bounded on their southern edge by the Main Frontal Thrust fault system, which produces steep southern slopes and marks the transition to the Indo-Gangetic plains below. The name Sivalik means tresses of Shiva in Sanskrit.

Connections

Caused By

Orogeny, Processes

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: Sivalik Hills

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: Sivalik Hills
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Sivalik Hills

Also in Geography Atlas: where this subject is found.

Source Wikidata: Sivalik Hills

Also in Geography Atlas: where this subject is found.

Source Wikidata: Sivalik Hills
Sources
Wikidata: Sivalik Hills
Wikidata Q613624, class allow-list match (w-wdresolver-0926)View the Source
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