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The largest in the last one million years is the 14-kilometre (8.7 mi) Zhamanshin crater in Kazakhstan and has been described as being capable of producing a nuclear-like winter. [11] The source of the enormous Australasian strewnfield (c. 780 ka) is a currently undiscovered crater probably located in Southeast Asia. [12] [13]
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).
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.
Our world is a pretty special place, full of breathtaking sights, awesome people, vibrant plants, and majestic wildlife. However, we tend to take it for granted, forgetting how incredible it is.
A well-known crater lake, which bears the same name as the geological feature, is Crater Lake in Oregon. It is located in the caldera of Mount Mazama . It is the deepest lake in the United States with a depth of 594 m (1,949 ft).
Family returns to their Lebanese city to find a crater where their 50-year-old home once stood By LUJAIN JO Associated Press BAALBEK, Lebanon (AP) — In eastern Lebanon's city of Baalbek, the Jawhari family gathered around a gaping crater where their home once stood, tears streaming as they tried to make sense of the destruction.
The Vredefort impact structure is the largest verified impact structure on Earth. [1] The crater, which has since been eroded away, has been estimated at 170–300 kilometres (110–190 mi) across when it was formed.
The Chesapeake Bay impact crater is a buried impact crater, located beneath the mouth of Chesapeake Bay, United States. It was formed by a bolide that struck the eastern shore of North America about 35.5 ± 0.3 million years ago, in the late Eocene epoch. It is one of the best-preserved "wet-target" impact craters in the world. [3]