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  • Geology of the Moon - Wikipedia
    The geology of the Moon (sometimes called selenology, although the latter term can refer more generally to "lunar science") is the structure and composition of the Moon, which is quite different from that of Earth
  • Moon Composition - NASA Science
    According to leading theories about how the Moon formed, much of the stuff that makes up the Moon was once part of Earth And like Earth, the Moon consists of three main layers: a crust, a mantle, and a core
  • Its Official: Scientists Finally Confirmed Whats Inside The Moon
    A thorough investigation published in May 2023 found that the inner core of the Moon is, in fact, a solid ball with a density similar to that of iron
  • Internal Structure of the Moon: Crust, Mantle and Core - Geology. com
    These seismographs collected data and enabled researchers to determine that the moon's structure consisted of a thin crust of about 65 kilometers, a mantle about 100 kilometers thick and a core with a radius of about 500 kilometers
  • Moon - Core, Crust, Surface | Britannica
    Combining all available data, scientists have created a picture of the Moon as a layered body comprising a low-density crust, which ranges from 60 to 100 km (40 to 60 miles) in thickness, overlying a denser mantle, which constitutes the great majority of the Moon’s volume
  • Geology of the Moon - New Space Economy
    The geology of the Moon is a testament to the dynamic processes that occur in celestial bodies Its craters, maria, and highlands tell a story of impacts, volcanic eruptions, and ancient tectonic activity
  • The Interior Structure of the Moon: What Does Geophysics Have to Say?
    Figure 2 shows the topography of the Moon (upper left) obtained by the Clementine mission (Smith et al 1997; USGS 2002), as well as the best estimate of the radial gravitational acceleration at the surface (upper right), derived primarily from the Lunar Prospector mission (Konopliv et al 2001)
  • Interior and Geological Activity - University of Rochester
    Our present picture of the Moon's interior is that it has a crust about 65 km thick, a mantle about 1000 km thick, and a core that is about 500 km in radius A limited amount of seismic data suggests that the outer core may be molten
  • Chemical Composition, Mineralogy, and Physical Properties of the Moon’s . . .
    The paper describes the principles of the approach to modeling the internal structure of a planetary body, based on the joint inversion of an integrated set of selenophysical, seismic, and geochemical parameters combined with calculations of phase equilibria and physical properties
  • Astronomy and Astrophysics | Research Starters - EBSCO
    The lunar interior is a fascinating subject that encompasses the Moon's composition, structure, and geological history Unlike Earth, which has a well-defined crust, mantle, and core due to processes like density separation, the Moon's interior exhibits a simpler and less differentiated structure





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