| Mount Morning | |
|---|---|
 Aerial view of Mount Morning from the northeast. | |
| Highest point | |
| Elevation | 2,725 m (8,940 ft)[1] |
| Prominence | 1,515 m (4,970 ft)[1] |
| Listing | Ultra |
| Coordinates | 78°30′S 163°30′E / 78.5°S 163.5°E[2] |
| Geography | |
  Mount Morning | |
| Geology | |
| Mountain type | Shield volcano |
| Volcanic belt | McMurdo Volcanic Group |
| Last eruption | Unknown[3] |
Mount Morning is a shield volcano at the foot of the Transantarctic Mountains in Victoria Land, Antarctica. It lies 100 kilometres (62 mi) from Ross Island. Mount Morning rises to an elevation of 2,723 metres (8,934 ft) and is almost entirely mantled with snow and ice. A 4.1 by 4.9 kilometres (2.5 mi × 3.0 mi) wide summit caldera lies at the top of the volcano and several ice-free ridges such as Hurricane Ridge and Riviera Ridge emanate from the summit. A number of parasitic vents mainly in the form of cinder cones dot the mountain.
The volcano was initially active during the Miocene and erupted in two separate stages with a hiatus in between. The older stage has a different chemical composition than the recent one and is heavily eroded by glaciers. The most recent parasitic vents were active about 20,000 years ago and the volcano could erupt again.
- ^ a b "Antarctica Ultra-Prominences" Peaklist.org. Retrieved 2012-08-01.
- ^ Martin, Cooper & Dunlap 2010, p. 359.
- ^ "Morning". Global Volcanism Program. Smithsonian Institution. Retrieved 2020-03-19.