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The Pyramid is on a promontory on the west side of Koettlitz Glacier between Renegar Glacier to the southwest and Walcott Bay to the northeast. Dromedary Glacier is to the northwest. Nearby features include The Almond, Pyramid Trough and The Bulwark. [2] The Alph River flows north through the Pyramid Trough. [3]
Physically, Antarctica is divided in two by the Transantarctic Mountains, close to the neck between the Ross Sea and the Weddell Sea. Western Antarctica and Eastern Antarctica correspond roughly to the western and eastern hemispheres relative to the Greenwich meridian. [note 1] West Antarctica is covered by the West Antarctic Ice Sheet.
A meltwater stream from Koettlitz Glacier on the east side of The Bulwark, a mountain outlier south of Walcott Bay, Scott Coast. The stream flows north and then west, following the perimeter of The Bulwark to enter Trough Lake and the Alph River system. Named by New Zealand Geographic Board (NZGB) (1994) in association with The Bulwark. [11]
The meridian 31° east of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, Europe, Turkey, Africa, the Indian Ocean, the Southern Ocean, and Antarctica to the South Pole. The 31st meridian east forms a great circle with the 149th meridian west.
The scale factor at each pole is adjusted to 0.994 so that the latitude of true scale is 81.11451786859362545° (about 81° 06' 52.3") North and South. The scale factor inside the regions at latitudes higher than this parallel is too small, whereas the regions at latitudes below this line have scale factors that are too large, reaching 1.0016 ...
The antimeridian passes mostly through the open waters of the Pacific Ocean but also runs across land in Russia, Fiji, and Antarctica.An important function of this meridian is its use as the basis for the International Date Line, which snakes around national borders to maintain date consistency within the territories of Russia, the United States, Kiribati, Fiji and New Zealand.
The western side of Prydz Bay features a broad trough crossing from the inner shelf to the shelf edge, Prydz Channel. It is around 100 km wide and is 500 m deep at the shelf break. It is a typical example of a cross-shelf glacial trough that occupy 40.2% of the area of the Antarctic continental shelf [ 3 ] and that are formed by fast-flowing ...
North of Punuk: 41°02′N Iran: North of Qush, West Azerbaijan region: 39°47′N South Korea: North of Daegang-ri, Goseong, Gangwon Province: 38°36′N Afghanistan: South of Qal'Aikhum: 38°22′N Tunisia: Galite Islands Ras ben Sakka ( the northernmost point of mainland Africa) 37°31′N 37°21′N Iraq: North of Sanat: 37°23′N Syria ...