How does the size of an impact crater compare to the size of the object that creates it?
The faster the incoming impactor, the larger the crater. Such a high-speed impact produces a crater that is approximately 20 times larger in diameter than the impacting object. Smaller planets have less gravitational "pull" than large planets; impactors will strike at lower speeds.
Accordingly, how large is an impact crater compared to the impactor?
How large is an impact crater compared to the size of the impactor? 10 times larger. Regarding this, how do you measure the depth of an impact crater? A classic image analysis technique is to use shadow lengths to determine vertical dimensions. In planetary science, shadow lengths are often used to determine the depths of impact craters (on the Moon, Mars, and elsewhere) and the heights of their rims.
What is the diameter of impact crater?
Meteor Crater Meteor Crater, also known as Barringer Crater Impact crater/structure Confidence Confirmed Diameter 0.737 miles (1.186 km) Depth 560 feet (170 m) 19 more rows And another question, how deep are the craters on the moon? Well-preserved large craters like Tycho (about 53 miles [85 kilometers] across), Copernicus (58 miles [93km] wide), and Aristarchus (25 miles [41km] in diameter) have rim-to-floor depths of about 15,700 feet (4,800 meters), 12,500 feet (3,800m), and 9,800 (3,000m), respectively.
Also, what is the deepest crater on earth?
The largest impact crater on Earth, the Vredefort crater in South Africa, is 99 miles (160 km) wide and was likely created about 2 billion years ago, according to NASA's Earth Observatory. How did the size of the Pebble affect the size of the crater formed? When dropped from a given height, the greater the mass, the larger the crater. When dropped from a given height, the greater the volume, the larger the crater.
Moreover, why are the craters on the moon the same depth?
Gravity limits the height of crater rims and the depth of their interior just as it limits the height of mountains and the depth of canyons by limiting the angle of repose on slopes. The result is that large impact craters appear quite shallow. This is true of all the planets and moons.
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