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- Regolith - Wikipedia
Regolith on Earth originates from weathering and biological processes The uppermost part of the regolith, which typically contains significant organic matter, is more conventionally referred to as soil [15]
- Regolith | Soil Formation, Weathering Erosion | Britannica
regolith, a region of loose unconsolidated rock and dust that sits atop a layer of bedrock On Earth, regolith also includes soil, which is a biologically active medium and a key component in plant growth
- 2. 7: Regolith - Geosciences LibreTexts
The term regolith is used for the layer or mantle of fragmental and unconsolidated rock and mineral material, whether residual or transported, that rests on bedrock
- Regolith - New World Encyclopedia
Regolith is a layer of loose, heterogeneous material covering solid rock It includes dust, soil, broken rock, and other related materials It is found on Earth, the Moon, some asteroids, and other planets On Earth, regolith is an important factor that supports living organisms
- Leveraging Lunar Regolith to Further Space Exploration
Learn about lunar regolith, the layer of dust, rocks, and minerals covering the Moon’s surface, formed by meteoroid impacts over billions of years Discover its significance for space exploration and future lunar missions
- Regolith - (Earth Science) - Vocab, Definition, Explanations | Fiveable
Regolith is a layer of loose, fragmented material covering solid bedrock, which includes soil, dust, and broken rock This term is important for understanding the surface composition of celestial bodies, as it forms the basis for soil development and provides insight into geological processes
- Scientists Say: Regolith - Science News Explores
Regolith is the layer of loose rocks and dust on the surface of moons, asteroids and rocky planets — including Earth This blanket of fine material comes from forces that break down or transform rock
- Regolith | SpringerLink
Based on a combination of two Greek words, regos – a blanket, and lithos – stone, the term regolith was first proposed by Merrill (1897) to describe the unconsolidated particulate matter overlying bedrock on the Earth's surface
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