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The Nooitgedacht Glacial Pavements comprise a geological feature between Kimberley and Barkly West, South Africa, pertaining to the Palaeozoic-age Dwyka Ice Age, or Karoo Ice Age, (some 300 million years ago) where the glacially scoured (smoothed and striated) ancient bedrock (re-exposed by erosion) was used, substantially more recently, during the Later Stone Age period in the late Holocene ...
Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacial maximum 10,000 to 15,000 years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco.
The geography of Tibet consists of the high mountains, lakes and rivers lying between Central, East and South Asia. Traditionally, Western (European and American) sources have regarded Tibet as being in Central Asia , though today's maps show a trend toward considering all of modern China, including Tibet, to be part of East Asia .
Midui Glacier in Nyingchi. Today, Tibet is an important heating surface of the atmosphere. However, during the Last Glacial Maximum, an approximately 2,400,000 square kilometres (930,000 sq mi) ice sheet covered the plateau. [38] [39] [40] Due to its great extent, this glaciation in the subtropics was an important element of radiative forcing.
This is a list of the extreme points of South Africa, the points that are farther north, south, east or west than any other location in the country. Including the Prince Edward Islands Northernmost Point: Over Vlakte farm, Vhembe District Municipality , Limpopo Province ( 22°7′40″S 29°39′20″E / 22.12778°S 29.65556°E ...
The Rongbuk Glacier (simplified Chinese: 绒布冰川; traditional Chinese: 絨布冰川; pinyin: Róngbù Bīngchuān) is located in the Himalaya of southern Tibet. Two large tributary glaciers, the East Rongbuk Glacier and the West Rongbuk Glacier , flow into the main Rongbuk Glacier.
Sketch map of Kharta and environs. Kharta [note 1] (Chinese: 卡达) is a region in Tibet lying to the east of Mount Everest and centred on the Kharta valley and Kama valley. [note 2] The 40-kilometre (25 mi) Kharta valley starts at the col at Lhakpa La at the head of the Kharta Glacier from which the Kharta Chu (Chinese: 卡达曲) river flows east to join the Phung Chu just beyond Khata village.
Approximate extent of the Karoo Glaciation (in blue), over the Gondwana supercontinent during the Carboniferous and Permian periods. The late Paleozoic icehouse, also known as the Late Paleozoic Ice Age (LPIA) and formerly known as the Karoo ice age, was an ice age that began in the Late Devonian and ended in the Late Permian, [1] occurring from 360 to 255 million years ago (Mya), [2] [3] and ...