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The Nabuyatom crater is a caldera that was formed after a volcano collapsed. [1] The Nabuyatom crater is a circular crater which is found on the south of Lake Turkana, an alkaline lake in the Kenyan Rift Valley [2] and it is one of the tourist sites in Kenya. [1] The closest town, Lodvar, is over 70 kilometers away from the lake and crater. [3]
Lake Turkana (/ t ɜːr ˈ k ɑː n ə,-ˈ k æ n-/) is a saline lake in the Kenyan Rift Valley, in northern Kenya, with its far northern end crossing into Ethiopia. [2] It is the world's largest permanent desert lake and the world's largest alkaline lake.
An E-W-trending chain of small explosion craters cuts the eastern side of the 3-km-wide island. Several small islands to the SE represent partially submerged crater rims, and other cones and lava plugs lie beneath the lake surface near the island. The youngest Central Islands tuffs and lavas may be as young as Holocene (Karson and Curtis, 1992).
The crater lake of Mount Rinjani, Indonesia Lake Yeak Laom, Cambodia Baengnokdam crater lake of Hanla Mountain in winter, South Korea A volcanic crater lake is a lake in a crater that was formed by explosive activity or a collapse during a volcanic eruption .
The following structures are officially considered "unconfirmed" because they are not listed in the Earth Impact Database. Due to stringent requirements regarding evidence and peer-reviewed publication, newly discovered craters or those with difficulty collecting evidence generally are known for some time before becoming listed.
Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. [1] Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley ...
Marsabit is a 6300 km 2 basaltic shield volcano in Kenya, located 170 km east of the center of the East African Rift, in Marsabit County near the town of Marsabit. This was primarily built during the Miocene, but some lava flows and explosive maar-forming eruptions have occurred more recently. At least two of the maars host crater lakes.
The oldest volcano on the island, Kohala, is more than a million years old, [17] while Kīlauea, the youngest, is between 300,000 and 600,000 years of age. [16] Kamaʻehuakanaloa (the ruddy, reddish child of Kanaloa, [ 18 ] formerly Lōʻihi), on the island's flank, is younger and has yet to breach the surface. [ 19 ]