15,000-year-old viruses found in Tibetan glacier

A team of researchers from The Ohio State University and Lawrence Berkeley National Laboratory has found a host of ancient virus groups in ice cores taken from a Tibetan glacier. They have written a paper about their discovery ...

River people: Life along Asia's key waterways

From the flood-ravaged banks of the Brahmaputra to the disappearing wetlands of the Mekong, Asia's main waterways—and the people that live along them—are fighting for survival.

The growing Tibetan Plateau shaped modern biodiversity

Holding particular biological resources, the Tibetan Plateau is a unique geologic-geographic-biotic interactive unit and hence plays an important role in the global biodiversity domain. The Tibetan Plateau has undergone vigorous ...

China aims to build its own Yellowstone on Tibetan plateau

There's a building boom on the Tibetan plateau, one of the world's last remote places. Mountains long crowned by garlands of fluttering prayer flags—a traditional landscape blessing—are newly topped with sprawling steel ...

Integrated solutions for the Indus Basin

A new integrated modeling framework could help the Indus Basin region find solutions to water resource challenges and interconnected sustainable development goals. The new framework, described in a perspective article published ...

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Plateau

In geology and earth science, a plateau ( /pləˈtoʊ/ or /ˈplætoʊ/; plural plateaus or rarely plateaux), also called a high plain or tableland, is an area of highland, usually consisting of relatively flat terrain. A highly eroded plateau is called a dissected plateau. A volcanic plateau is a plateau produced by volcanic activity.

Plateaus can be formed by a number of processes, including, upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Magma rises from the mantle causing the ground to swell upward, in this way large, flat areas of rock are uplifted. Plateaus can also be built up by lava spreading outwards from cracks and weak areas in the crust, an example of such a plateau is the Columbia Plateau in the northwestern United States of America. Plateaus can also be formed due to the erosional processes of glaciers on mountain ranges, in this case the plateaus are left sitting between the mountain ranges. Water can also erode mountains and other landforms down into plateaus.

Plateaus are classified according to their surrounding environment, common categories are: intermontane, piedmont, and continental plateaus.

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