The Ural Mountains form a roughly 2,500 kilometer long range running north to south through Russia, from the Arctic Ocean coast to the Ural River and northwestern Kazakhstan near the Caspian Sea, and they conventionally mark the boundary between the continents of Europe and Asia. Their highest point, Mount Narodnaya, reaches 1,894 meters, though the range's average elevation is closer to 1,000 to 1,300 meters. The Urals formed during the Uralian orogeny, when the eastern edge of the ancient supercontinent Laurasia collided with the smaller continent of Kazakhstania over roughly 90 million years, from the late Carboniferous into the early Triassic period. That makes the range, at an estimated 250 to 300 million years old, one of the oldest mountain chains still standing on Earth.
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Associated With
Source Ural Mountains (Wikipedia)
Source Ural Mountains (Wikipedia)
Source Ural Mountains (Wikipedia)
Caused By
Source Ural Mountains (Wikipedia)
Source Ural Mountains (Wikipedia)
Source Ural 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: Ural 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: Ural Mountains
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Also in Geography Atlas: where this subject is found.
Also in Geography Atlas: where this subject is found.
Source Wikidata: Ural Mountains
Sources
Wikidata: Ural Mountains
Ural Mountains (Wikipedia)
Associated With: Carboniferous, Article text, age Carboniferous
The collision lasted nearly 90 million years in the late Carboniferous, early Triassic.
Associated With: Triassic, Article text, age Triassic
The collision lasted nearly 90 million years in the late Carboniferous, early Triassic.
Associated With: Sandstone, Article text, rock Sandstone
It is composed of severely eroded sedimentary rocks (sandstones and limestones) that are about 350 million years old.
Associated With: Limestone, Article text, rock Limestone
It is composed of severely eroded sedimentary rocks (sandstones and limestones) that are about 350 million years old.
Caused By: Folding, Article text, process Folding
The sedimentary and volcanic layers are folded and faulted.
Caused By: Faulting, Article text, process Faulting
The sedimentary and volcanic layers are folded and faulted.
Caused By: Karstification, Article text, process Karstification
The western slope of the Ural Mountains has predominantly karst topography, especially in the Sylva basin, which is a tributary of the Chusovaya.
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