List
| World | Rift/Valley | Length |
|---|
| Earth | Great Rift Valley | 6,000 km (3,700 mi) |
| Canadian Arctic Rift System | 4,800 km (3,000 mi) |
| West Antarctic Rift System | |
| Midcontinent Rift System | 2,000 km (1,200 mi) |
The system of rift valleys that characterizes the African continent represents a perfect environment to understand the evolution of mankind; for the important paleoanthropological discoveries in Ethiopia, Kenya, Tanzania, Uganda and Zaire, the African rift valleys are indeed considered the "cradle of mankind", that is
The Rift Valley consists of a group of independent interior basins, extending from Djibouti in the north to Tanzania in the south, nearly half being located in Ethiopia.
| Name of basin | Total area of basin | Area in the country |
|---|
| Kenya | | 102 452 |
| Southern lakes: | 178 800 | |
| Kenya | | 25 000 |
| Tanzania | | 153 800 |
An estimated 1,000 to 1,500 Hadza live in the central Great Rift Valley and the surrounding plains in north-central Tanzania, where they subsist almost entirely off the land: hunting animals, foraging for roots and fruit, gathering honey.
In Kenya, Uganda and the fringes of South Sudan, the Great Rift runs along two separate branches that are joined to each other only at their southern end, in Southern Tanzania along its border with Zambia. The two branches are called the Western Rift Valley and the Eastern Rift Valley.
The Great Rift Valley is a series of contiguous geographic trenches, approximately 7,000 kilometres (4,300 mi) in total length, that runs from the Beqaa Valley in Lebanon which is in Asia to Mozambique in Southeast Africa.
These include the 3 largest lakes in Africa - Victoria, Tanganyika and Malawi - as well as lakes Turkana, Albert, Edward, Kivu and several others. The lakes are important habitats for a number of fish and amphibian species, abundant birdlife and numerous crocodiles.
Lake Nkugute found in Rubirizi district is shaped like an African map. Most people refer to it as Lake Africa.
Lake Tanganyika, second largest of the lakes of eastern Africa. It is the longest freshwater lake in the world (410 miles [660 km]) and the second deepest (4,710 feet [1,436 metres]) after Lake Baikal in Russia.
Lake Kyoga is also known as a rift valley lake which is an extension of the Victoria Nile that flows through the lake and also its way from Lake Victoria to lake Albert, the major inlet from Lake Victoria is controlled by the Nalubaale power station in Eastern Jinja.
Lake Baikal (5,315 feet [1,620 meters])
Lake Baikal, in Siberia, holds the distinction of being both the deepest lake in the world and the largest freshwater lake, holding more than 20% of the unfrozen fresh water on the surface of Earth.Typically, water levels begin to rise in the spring when rain falls on the lakes or trickles in from the land and when snowmelt floods the tributaries that empty into the lakes. Over the summer, those levels peak. Come autumn, the weather is typically cool and dry, and lake water evaporates.
The system of rift valleys that characterizes the African continent represents a perfect environment to understand the evolution of mankind; for the important paleoanthropological discoveries in Ethiopia, Kenya, Tanzania, Uganda and Zaire, the African rift valleys are indeed considered the "cradle of mankind", that is
c) Rift valleys have steep sides because they are formed when the earth crust is divided, they are not like those valley which are formed by soil erosion.
The most well-known rift valley on Earth is probably the so-called "Great Rift Valley System" which stretches from the Middle East in the north to Mozambique in the south. The area is geologically active, and features volcanoes, hot springs, geysers, and frequent earthquakes.
The lake has an area of 50 square miles (129 square km), is 11 miles (18 km) long and 5 miles (8 km) wide, and has an average depth of 17 feet (5 m). A freshwater lake with no visible outlet, its waters seep into lavas at its northern end, where a rocky shore contrasts with the alluvial flat on its southern border.
A rift valley is a linear shaped lowland between several highlands or mountain ranges created by the action of a geologic rift.
Narmada flows westwards through a rift valley between the Vindhyan Range on the north and the Satpura Range on the south. The Narmada, also called the Rewa, is a river in central India and the sixth longest river in the Indian subcontinent.
Ethiopia is home to over 20 lakes, most of which are a result of the Great African Rift Valley which extends from Jordan all the way down to Mozambique in Southern Africa. The rift has spawned some of the largest, deepest and oldest lakes in the world, with Ethiopia hosting a few.
If these two rift zones continue they will break apart the crustal plates they are located on and will create new plates. Sea water will flood the rift valleys and they will eventually become seas like the Red Sea.
Lake Albert, the northernmost of the chain of lakes in the Great Rift Valley, is visible in the top left. With a length of about 160 km, a width of 30 km and a maximum depth of 51 m, it is Africa's seventh largest lake.
Very few active rift valleys are found on continental lithosphere. The East African Rift, the Baikal Rift Valley, the West Antarctic Rift, and the Rio Grande Rift are Earth's major active continental rift valleys. The East African Rift is part of the “Great Rift Valley” system discussed below.
The most extensive of the continental rift valleys are those of the East African Rift System, which extend northward to the Red Sea and eastward into the Indian Ocean. Other notable examples include the Baikal Rift Valley (Russia) and the Rhine Rift Valley (Germany).
Answer: The common among the pictures is the formation of divergent plate boundary, where it forms the rift valleys and oceanic ridges.
Rift ValleysA rift valley is also known as a graben. Rift valleys are thought to have been developed either from the action of tensional forces in the crust or from the action of compressional forces.
Thank you! is a valley with steep slides that is formed when sections of the crust extend along fault lines. Central block of land subsides between two parallel faults due to tensional force, Sections left standing beside rift valleys are block mountains.
Block Mountains
They are formed when large areas of land are broken and displaced vertically. The uplifted terms are known as horsts and the lowered ones are called graben. The Rhine valley and the Vosges mountains are examples of block mountains.Note: There are three rivers in India which flow through a rift valley. The two other rivers which flow through a rift valley are Damodar and Narmada.
