Queen Alexandra Range Explained
The Queen Alexandra Range (-84°N 168°W) is a major mountain range about long, bordering the entire western side of Beardmore Glacier from the Polar Plateau to the Ross Ice Shelf.The range is in the Transantarctic Mountains System, and is located in the Ross Dependency region of Antarctica.
Discovery
The Queen Alexandra Range was discovered on the journey toward the South Pole by the British Antarctic Expedition, 1907–09 (BrAE), and was named by Ernest Shackleton for Queen Alexandra, Queen of the United Kingdom, 1901-10.Shackleton and his men, and a later expedition headed by Robert Falcon Scott, both collected rock samples from the range that contained fossils. The discovery that multicellular life forms had lived so close to the South Pole was an additional piece of evidence that accompanied the publication (in 1910 and independently in 1912) of the theory of continental drift.
Location
The Queen Alexandra Range is bounded by the Beardmore Glacier along its southeast edge, which divides it from the Commonwealth Range of the Queen Maud Mountains to the east. The west of the range is bounded by the Antarctic Plateau in the south.Further north it is bounded by the Walcott Névé to the east, which separates the range from the Colbert Hills. The Walcott Névé joins the Law Glacier in the Bowden Névé which feeds the Lennox-King Glacier.This glacier bounds the northwest part of the range, and separates it from the Holland Range to the north.The northern tip of the range extends to the Ross Ice Shelf between the Lennox King Glaciers and Beardmore Glacier.
Major glaciers
- Beardmore Glacier (-83.75°N 171°W) is of the largest known valley glaciers, over long, descending the polar plateau and flowing north between the Queen Alexandra Range and Commonwealth Range, to enter the Ross Ice Shelf.
- Law Glacier (-84.0833°N 161°W) is a glacier about wide between the south end of the Queen Elizabeth Range and the MacAlpine Hills, gradually descending east-northeast from the polar plateau to Bowden Névé.
- Bowden Névé -83.5°N 165°W is a névé about wide, lying southward of Mount Miller between Queen Elizabeth Range and Queen Alexandra Range.
- Walcott Névé -84.3833°N 202°W is a névé, about in area, bounded by the Marshall Mountains, Lewis Cliff and Mount Sirius.
- Lennox-King Glacier (-83.4167°N 168°W) is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and Queen Alexandra Ranges to enter Richards Inlet, Ross Ice Shelf.
Mountains and peaks
Mountains and peaks over high include:
Features
Major features that are the focus of a named or unnamed group of lesser features, include:
- Morris Heights (-83.4667°N 211°W), a relatively smooth ice-covered heights, forming a peninsula-like divide between Beaver Glacier and King Glacier at the north end of the Queen Alexandra Range.
- Mount Elizabeth (-83.9°N 191°W), a massive ice-free mountain, high, standing south of Mount Anne.
- Mount Mackellar (-83.9833°N 205°W), a massive mountain, high, standing at the head of Mackellar Glacier, south of Pagoda Peak.
- Grindley Plateau (-84.15°N 171°W), a high icecapped plateau in the central Queen Alexandra Range, bordered by the peaks of Mount Mackellar, Mount Bell and Mount Kirkpatrick.
- The Cloudmaker, a massive mountain, high, standing at the west side of Beardmore Glacier, just south of Hewson Glacier. It is easily identifiable by its high, ice-free slope facing Beardmore Glacier.
- Mount Kirkpatrick (-84.3333°N 191°W), a lofty, generally ice-free mountain in Queen Alexandra Range west of Mount Dickerson. At it is the highest point in the Queen Alexandra Range.
- Adams Mountains, a small but well defined group of mountains bounded by the Beardmore Glacier, Berwick Glacier, Moody Glacier and Bingley Glacier.
- Mount Falla (-84.3667°N 219°W), a prominent conical mountain, high, standing northeast of Mount Stonehouse, between Berwick Glacier and Prebble Glacier.
- Marshall Mountains (-84.6167°N 194°W), a group of mountains overlooking Beardmore Glacier. They are bounded on the north by Berwick Glacier, and on the south by Swinford Glacier.
