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Mount Stahlman
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Andes
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier Leverett Glacier in Antarctica is about long and wide, draining northward from the Watson Escarpment, between California Plateau and Stanford Plateau, and then trending west-northwest between the Tapley Mountains and Harold Byrd Mountains to ... * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier * Scott Glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Marie Byrd Land
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roe Glacier
The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east. Geography The Scott Glacier originates on the Antarctic Plateau in the vicinity of D'Angelo Bluff and Mount Howe, and descends between the Nilsen Plateau and the mountains of the Watson Escarpment to enter Ross Ice Shelf just west of the Tapley Mountains. The Tapley Mountains, Watson Escarpment, Mount Blackburn, and the La Gorce Mountains bound the Scott Glacier on its eastern margin, while the Karo Hills, Hays Mountains, Faulkner Escarpment, and Rawson Mountains define the western edge of the Scott's drainage. History Scott Glacier was discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould. The Scott Glacie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pincer Point
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wallace
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Stahlman
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Seebeck
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Herr
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Durham
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Bushnell
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Evans Butte
The Tapley Mountains () is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains. Discovered in December 1929 by the Byrd Antarctic Expedition geological party under Laurence McKinley Gould, and named by Byrd for Harold Tapley of Dunedin, New Zealand, agent for the Byrd AE of 1928–30 and 1933–35. Features Geographical features include: * Albanus Glacier * Bobo Ridge * Durham Point * Evans Butte * Leverett Glacier * Mount Andes * Mount Bushnell * Mount Durham * Mount Herr * Mount Seebeck * Mount Stahlman * Mount Wallace * Pincer Point * Roe Glacier The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, wit ... * Scott Glacier F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
