Geography of Karachi

Map of Karachi

Karachi is Pakistan's largest city and is the capital of Sindh; it lies on Pakistan's southern coast, on the Arabian Sea just northwest of the Indus River Delta. City geographic coordinates are 24°51′ N 67°02′ E. Most of the land consisted largely of flat or rolling plains, with hills on the western and Manora Island and the Oyster Rocks. The Arabian Sea beach lines the southern coastline of Karachi. Mangroves and creeks of the Indus delta can be found toward the southeast side of the city. Toward the west and the north is Cape Monze, locally known as Ras Muari, an area marked by projecting sea cliffs and rocky sandstone promontories. Some excellent beaches can be found in this area. Khasa Hills and Mulri Hills lie in the northwest and form the border between North Nazimabad Town[1] and Orangi Town. The Manghopir Hills lies northwest of Karachi, between Hub River and Manghopir. The hills in Karachi are the offshoots of the Kirthar Range. The highest point of these hills in Karachi is about 528m in the extreme north. All these hills are devoid of vegetation and have wide intervening plains, dry river beds and water channels.[2] The rivers in Karachi are Malir River and Lyari River. The Indus River flood plain is near Karachi. The city is located on the Arabian Sea coastline.

Originally a tiny fishing village, Karachi became a trading center in the 18th century. The British, after gaining control of the region in the 19th century, developed the city into an important port. Rapid growth came after Pakistan became independent in 1947, largely, because of the city having been historically the largest urban centre during British rule in regions forming modern Pakistan. Karachi was the national capital from 1947 until 1959. Over the next several decades it became one of the fastest growing cities in the world, doubling its population from 1981 to 1999.[3]

The hills in Karachi are the off-shoots of the Kirthar Range. The highest point of these hills in Karachi is about 528m in the extreme north. All these hills are devoid of vegetation and have wide intervening plains, dry river beds and water channels.[4]

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