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Geological Formation

Ural Mountains

Structural and Tectonic Formations

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.

Connections

Associated With

Carboniferous, Eras
Source Ural Mountains (Wikipedia)
Limestone, Materials
Source Ural Mountains (Wikipedia)
Sandstone, Materials
Source Ural Mountains (Wikipedia)
Triassic, Eras
Source Ural Mountains (Wikipedia)

Caused By

Faulting, Processes
Source Ural Mountains (Wikipedia)
Folding, Processes
Source Ural Mountains (Wikipedia)
Source Ural Mountains (Wikipedia)
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: 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
In the Other Atlases

Found In

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
Wikidata Q35600, class allow-list match (w-wdresolver-0926)View the Source
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.
View the Source
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