maria
The moon surface features that probably formed when lava flows filled large basins are called maria, which are large, dark plains visible from Earth. These maria were created by ancient volcanic activity that filled the low-lying basin areas with basaltic lava flows.
Maria, also known as lunar seas, are the dark relatively flat regions of the moon's surface that were formed when interior lava filled large basins.
The dark-colored, relatively flat regions of the Moon's surface are called lunar maria. These maria were formed when basins on the Moon were filled with basaltic lava following impact events in the past.
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Ocean basins are large depressions on the Earth's surface that are filled with seawater. They play a crucial role in shaping the Earth's geography by covering about 70 of the planet's surface. Ocean basins also influence the climate, weather patterns, and biodiversity of the planet, making them essential components of the Earth's ecosystem.
Mercury's surface resembles that of Earth's Moon due to its heavily cratered appearance and lack of a significant atmosphere. Both bodies have experienced intense impacts, resulting in a landscape filled with craters of varying sizes. Additionally, Mercury's surface features, such as scarps and basins, can also be compared to those found on the Moon.
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The dark-colored, relatively flat regions of the moon's surface that were formed when interior lava filled large basins are called lunar maria. These areas appear darker than the surrounding highlands due to their lower reflectivity and lack of craters. The lunar maria are thought to have formed from ancient volcanic activity on the moon.
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When lava flowed over the Moon's surface, it formed vast plains known as maria. These are flat, dark areas that were created by ancient volcanic activity on the Moon. The lava flows filled in large impact basins, creating the smooth, dark patches we see on the lunar surface.
Yes, many large basins contain smooth plains that are likely to be filled with lava.
The lowlands that were eroded by glaciers and transformed into wide, deep basins are known as glacial troughs or fjords. As glaciers advanced and retreated, they carved out U-shaped valleys, which later filled with water or sediment, creating these basins. Examples include the Great Lakes in North America and many fjords in Scandinavia. These features are characterized by their steep sides and flat bottoms, a result of the intense erosive power of the moving ice.