An impact basin on the Moon is a large, circular depression formed by the collision of a celestial body, such as an asteroid or a comet, with the lunar surface. These basins often feature a raised rim and may contain a central peak or ring structure. They are significant geological features that provide insights into the Moon's history and the processes that shaped its surface. Renowned examples include the Imbrium and Serenitatis basins.
The South Pole-Aitken Basin is the oldest, largest, and deepest impact feature on the moon, dating back around 4 billion years. It is a massive basin located on the far side of the moon and is approximately 2,500 kilometers in diameter.
The largest impact basin in the solar system is the South Pole-Aitken Basin located on the Moon. It is over 2,500 kilometers (1,553 miles) in diameter and is one of the oldest and largest basins known in the solar system.
A crater is a depression that is caused when an object hits a heavenly body, such as the moon. Since the moon has almost no atmosphere - and therefore no wind - the craters that have formed aren't erased over time from erosion (which has occurred here on Earth). The largest crater on the moon, the Aitken basin, is 2,500 km across and 13 km deep.
The largest feature on the moon is the South Pole-Aitken Basin, which is an impact crater that spans approximately 2,500 kilometers (1,550 miles) in diameter.
The South Pole-Aitken basin on the Moon is the largest and oldest impact crater in the solar system. It measures about 2,500 kilometers (1,550 miles) in diameter and is over 13 kilometers (8 miles) deep. This massive basin is of significant interest to scientists because it may provide insights into the Moon's geological history and the early solar system.
A Impact Basin
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The South Pole-Aitken Basin is the oldest, largest, and deepest impact feature on the moon, dating back around 4 billion years. It is a massive basin located on the far side of the moon and is approximately 2,500 kilometers in diameter.
The South Pole-Aitken basin.
The largest impact basin in the solar system is the South Pole-Aitken Basin located on the Moon. It is over 2,500 kilometers (1,553 miles) in diameter and is one of the oldest and largest basins known in the solar system.
A crater is a depression that is caused when an object hits a heavenly body, such as the moon. Since the moon has almost no atmosphere - and therefore no wind - the craters that have formed aren't erased over time from erosion (which has occurred here on Earth). The largest crater on the moon, the Aitken basin, is 2,500 km across and 13 km deep.
The largest feature on the moon is the South Pole-Aitken Basin, which is an impact crater that spans approximately 2,500 kilometers (1,550 miles) in diameter.
Impact crater is now more prevalently used for the term impact basin.
The South Pole-Aitken basin on the Moon is the largest and oldest impact crater in the solar system. It measures about 2,500 kilometers (1,550 miles) in diameter and is over 13 kilometers (8 miles) deep. This massive basin is of significant interest to scientists because it may provide insights into the Moon's geological history and the early solar system.
when meteorites and other objects strike the moon, they leave behind depressions in the moons surface. The depression left behind by an object striking the moon is known as an imoact basin, or impact crater.
when meteorites and other objects strike the moon, they leave behind depressions in the moons surface. The depression left behind by an object striking the moon is known as an imoact basin, or impact crater.
When meteorites or other objects strike the Moon, they create impact craters. These craters vary in size and shape depending on the size and velocity of the impacting object. Over time, the continuous bombardment has formed the cratered surface we see on the Moon today.