Mount Adam, Falkland Islands
Encyclopedia
Mount Adam is a mountain on West Falkland
West Falkland
West Falkland is the second largest of the Falkland Islands in the South Atlantic. It is a hilly island, separated from East Falkland by Falkland Sound. Its area is and its coastline is long. Including the adjacent small islands the land area is .-Population:The island has fewer than 200...

, part of the Hill Cove Mountains range. It is the highest mountain on West Falkland and is one of the highest in the islands. It has the remains of glacial cirque
Cirque
Cirque may refer to:* Cirque, a geological formation* Makhtesh, an erosional landform found in the Negev desert of Israel and Sinai of Egypt*Cirque , an album by Biosphere* Cirque Corporation, a company that makes touchpads...

s on it, and is of similar height to Mount Usborne
Mount Usborne
Mount Usborne is a mountain on East Falkland. At above sea level, it is the highest point in the Falkland Islands.The mountain is referenced by Charles Darwin in Chapter 9 of the Zoology of the Voyage of the Beagle and is named after , Master's Assistant on HMS Beagle, the ship that took Darwin...

 on East Falkland
East Falkland
East Falkland the largest of the Falkland Islands in the South Atlantic, has an area of and a coastline long. Most of the population of the Falklands live in East Falkland, almost all of them living in the northern half of the island...

. Its summit is at 700 metres (2,296.6 ft)

As one of the highest mountains of the Falklands, it experienced some glaciation. The handful of mountains over 2,000 feet (610 m) have:
"pronounced corries with small glacial lake
Glacial lake
A glacial lake is a lake with origins in a melted glacier. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create...

s at the their bases, morainic
Moraine
A moraine is any glacially formed accumulation of unconsolidated glacial debris which can occur in currently glaciated and formerly glaciated regions, such as those areas acted upon by a past glacial maximum. This debris may have been plucked off a valley floor as a glacier advanced or it may have...

 ridges deposited below the corries suggest that the glaciers and ice domes were confined to areas of maximum elevation with other parts of the islands experiencing a periglacial climate
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