WebSUMMARY. Both the Moon and Mercury are airless, virtually unchanging worlds that experience extremes in temperature. Mercury has no permanent atmosphere, although it does have a thin envelope of gas temporarily trapped from the solar wind. The main surface features on the Moon are the dark maria and the lighter-colored highlands. The lunar maria are large, dark, basaltic plains on Earth's Moon, formed by ancient asteroid impacts on the far side on the Moon that triggered volcanic activity on the opposite (near) side. They were dubbed maria, Latin for 'seas', by early astronomers who mistook them for actual seas. They are less reflective than the "highlands" as a result of their iron-rich composition, and hence appear da…
Lunar Maria: Volcanic Basins on the Moon - Earth How
WebThe Moon is Earth's only natural satellite.It is the fifth largest satellite in the Solar System and the largest and most massive relative to its parent planet, with a diameter about one-quarter that of Earth (comparable to the width of Australia). The Moon is a planetary-mass object with a differentiated rocky body, making it a satellite planet under the geophysical … WebJan 11, 2024 · The maria formed about 3.0 to 4.0 billion years ago, when the Moon was continually bombarded by meteoroids ( Figure below). Large meteorites broke through the Moon’s newly formed surface. This eventually caused magma to flow out and fill the craters. Scientists estimate volcanic activity on the Moon ended about 1.2 billion years ago. china honey packing bottle
How Was the Moon Formed? Space
WebFeb 25, 2016 · Maria Were formed on the moon from molten rock but the moon hasn't had volcano's for billions of years. What is a moons maria? Maria is a bunch of Basaltic material (which is igneous... WebSep 9, 2016 · The maria distribution on the lunar surface shows an asymmetry with most of them located in the nearside. A possible explanation is that the crust is significantly … http://www.actforlibraries.org/comparing-lunar-highlands-and-maria/ china honey mandarin