File:Transantarctic_mountain_hg.jpg · Wikimedia Commons · See Wikimedia Commons
Transantarctic Mountains
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The Transantarctic Mountains are a major mountain range that stretches across Antarctica, dividing the continent into distinct regions. They matter because they are one of Earth's longest mountain ranges and provide important information about Antarctica's geology and climate history.
AI-generated from the Wikipedia summary — may contain errors.
Wikidata facts
- Instance of
- mountain range
- Continent
- Antarctica
- Area
- 584000
- Elevation
- 4528
- Highest point
- Mount Kirkpatrick
- Material used
- igneous rock
- Image
- Transantarctic mountain hg.jpg
- Width
- 300
- Length
- 3500
Show 6 more facts
- native label
- Transantarctic Mountains
- located in/on physical feature
- Antarctica
- Commons category
- Transantarctic Mountains
- topic's main category
- Category:Transantarctic Mountains
- time period
- Cambrian
- on focus list of Wikimedia project
- Wikipedia:Vital articles/Level/4
Sources (2)
via Wikidata · CC0
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Encyclopedic overview
The Transantarctic Mountains (abbreviated TAM) comprise a mountain range of uplifted rock (primarily sedimentary) in Antarctica which extends, with some interruptions, across the continent from Cape Adare in northern Victoria Land to Coats Land. These mountains divide East Antarctica and West Antarctica. They include a number of separately named mountain groups, which are often again subdivided into smaller ranges.
The range was first sighted by James Clark Ross in 1841 at what was later named the Ross Ice Shelf in his honour. It was first crossed during the British National Antarctic Expedition of 1901-1904.
Excerpted from Wikipedia’s “Transantarctic Mountains” article, available under the CC BY-SA 4.0 licence.
Gallery (9)
On the map
2 mapped locations
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