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Satellite image of the Tibetan Plateau between the Himalayan mountains to the south and the Taklamakan Desert to the north. In geology and physical geography, a plateau (/ p l ə ˈ t oʊ, p l æ ˈ t oʊ, ˈ p l æ t oʊ /; French:; pl.: plateaus or plateaux), [1] [2] also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the ...
Dieng temple complex. Dieng Plateau (Javanese: ꦣꦶꦲꦾꦁ; Javanese pronunciation:) is a plateau in Central Java, Indonesia that forms the floor of the caldera complex on the Dieng Volcanic Complex.
The Lembang Fault is an active geological fault with a slip rate of 2 millimeters per year that crosses Lembang city and runs 22 kilometers north of the Bandung basin, ranging from Mount Palasari to Cisarua. 700 years ago, earthquakes occurred at several points along the fault line and could potentially trigger up to a magnitude 7 quake.
Minangkabau mosque circa 1892–1905 photographed by Christiaan Benjamin Nieuwenhuis The Minangkabau Highlands is a mountainous area in the province of West Sumatra, located around three mountains— Mount Marapi, Mount Singgalang, and Mount Sago —in west-central Sumatra, Indonesia. The highlands are part of the Barisan Mountains, the largest mountain range in Sumatra. They are home to the ...
The 125 most topographically prominent summits on Earth; No. Peak Range (or island) Location Coordinates [1]Prominence (m) Height (m) Col (m) Encirclement parent Prominence parent
Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level.
Landsat Image over SRTM Elevation by NASA, showing the Cape Peninsula and Cape of Good Hope, South Africa in the foreground.. GIS or geographic information system is a computer system that allows for visualizing, manipulating, capturing, and storage of data with associated attributes.
Amazon River near Manaus, Brazil, an example of a lowland river habitat. The generally more turbid, warm, slow-flowing waters and fine sediment beds of lowland rivers encourage fish species with broad temperature tolerances and greater tolerances to low oxygen levels, and life history and breeding strategies adapted to these and other traits of lowland rivers.