These basins are generally flat and low-lying.
The basins that filled up with water became lakes.
Lesser divides enclose basins in Hejaz, Najd, and Jordan.
The glaciers dug thousands of basins in the weaker areas of rock.
…basins, the Carpentaria Basin, the Eyre Basin, and the Murray Basin.
The basins of northern Brazil have carbonate deposits mixed with clastics.
New chambers and basins were built to control the water flowing from Gatún Lake.
There are more than 2,000 coal-bearing sedimentary basins distributed around the world.
The Eyre and Murray basins are entirely terrestrial, but the Carpentaria is partly inundated by the sea.
In general, however, the basins with the highest drainage density are also those with the steepest slope.
Those rifted basins largely followed the previous Paleozoic sutures along the western side of the continent.
After the last glaciation the melting waters collected in shallow lakes in the intermediate elevated basins.
These basins and their adjacent slopes, which are intensively cultivated, contain roughly half of Ecuador’s population.
Such basins are typically found along the western margin of the Pacific Ocean near the convergence of two tectonic plates.
Examples of basins of the early Paleozoic age are the Beni basin in Bolivia and the Alhuampa and Las Breñas basins in northern Argentina
Examples of basins of the early Paleozoic age are the Beni basin in Bolivia and the Alhuampa and Las Breñas basins in northern Argentina.
The basins are generally 4,000 to 5,000 feet (1,200 to 1,500 meters) above sea level, and the mountain ranges rise 3,000 to 5,000 feet (900 to 1,500 meters) above the level of the basins.
From roughly north to south they include the Arabian, Somali, Mascarene, Madagascar, Mozambique, Agulhas, and Crozet basins in the west and the Central Indian (the largest), Wharton, and South Australia basins in the east.
Lakes may occupy basins that have been caused by the removal in solution of some of the more-soluble constituents in the underlying strata; occasionally lake basins have been formed directly by crustal movements or by collapse of volcanic cones.
The yearly average numbers of tropical storms occurring in the various ocean basins are as follows: North Atlantic 13, northeastern Pacific 16, northwestern Pacific 27, northern Indian 5, southwestern Indian 10, and Australian (that is, the southwestern Pacific and southeast Indian basins) 16.
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