impact crater oor Masedonies
impact crater
en
(geology) A crater formed from an impact, typically of a meteorite, as opposed to one formed by other means such as vulcanism.
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ударен кратер
en
circular depression on a celestial object formed by a hypervelocity impact of a smaller body
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The impact crater.
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A 5-mile (8 km)-wide meteorite impact crater is located in Elmore County, just north of Montgomery.
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Another notable geological features is the Dellen lake system, created from flooded meteoric impact craters.
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The planet has few impact craters, demonstrating that the surface is relatively young, approximately 300–600 million years old.
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MESSENGER data has helped identify 51 pyroclastic deposits on the surface, where 90% of them are found within impact craters.
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Among the Uranian satellites, Ariel appears to have the youngest surface with the fewest impact craters and Umbriel's the oldest.
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Venus has some unique surface features in addition to the impact craters, mountains, and valleys commonly found on rocky planets.
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Likewise, the glass in impact craters on Mars could have preserved signs of life if life existed at the site.
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The relative ages of the different surface units on Callisto can be determined from the density of impact craters on them.
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The mare near Pupin is otherwise devoid of significant impact craters, and is nearly featureless except for a faint dusting of ray material.
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Objects with less than a certain kinetic energy are slowed down so much by the atmosphere that they do not create an impact crater.
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A study of the degradation state of the impact craters that host pyroclastic deposits suggests that pyroclastic activity occurred on Mercury over a prolonged interval.
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Ten years later, and after Alvarez's death, evidence of a large impact crater called Chicxulub was found off the coast of Mexico, providing support for the theory.
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A large buried impact crater structure with an estimated age of about 66 million years was later identified under what is now the Yucatán Peninsula (the Chicxulub crater).
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Impact glass, formed by the impact of meteors, which on Earth can preserve signs of life, has been found on the surface of the impact craters on Mars.
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The planet may have had a major global resurfacing event about 500 million years ago, from what scientists can tell from the density of impact craters on the surface.
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The ages of multi-ring structures and impact craters depend on chosen background cratering rates and are estimated by different authors to vary between 1 and 4 billion years.
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Planetary geology includes such topics as determining the internal structure of the terrestrial planets, and also looks at planetary volcanism and surface processes such as impact craters, fluvial and aeolian processes.
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Within Earth's crust, iridium is found at highest concentrations in three types of geologic structure: igneous deposits (crustal intrusions from below), impact craters, and deposits reworked from one of the former structures.
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The study of impact craters indicates that impact frequency has been more or less steady for the past 3.5 billion years, which requires a steady replenishment of the NEO population from the asteroid main belt.
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The frequency of impacts of objects of various sizes is estimated on the basis of orbit simulations of NEO populations, the frequency of impact craters on the Earth and the Moon, and the frequency of close encounters.
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Also, a letter in Sky & Telescope magazine at this time pointed to apparently simultaneous impact craters on Earth (for example, the Clearwater Lakes in Quebec), suggesting that these craters were caused by pairs of gravitationally bound objects.
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When a near-Earth object impacts Earth, objects up to a few tens of metres across ordinarily explode in the upper atmosphere (usually harmlessly), with most or all of the solids vaporized, while larger objects hit the water surface, forming waves, or the solid surface, forming impact craters.
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The largest known primary reserves are in the Bushveld igneous complex in South Africa, (near the largest known impact crater, the Vredefort crater) though the large copper–nickel deposits near Norilsk in Russia, and the Sudbury Basin (also an impact crater) in Canada are also significant sources of iridium.
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Evidence for the impact origin of the crater includes shocked quartz, a gravity anomaly, and tektites in surrounding areas.
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