Andere Kunden interessierten sich auch für
![Exposed Cross-Sections of the Continental Crust]( "Exposed Cross-Sections of the Continental Crust")
Exposed Cross-Sections of the Continental Crust106,99 €![The Deep Proterozoic Crust in the North Atlantic Provinces]( "The Deep Proterozoic Crust in the North Atlantic Provinces")
The Deep Proterozoic Crust in the North Atlantic Provinces107,99 €![Faults and Subsurface Fluid Flow in the Shallow Crust]( "Faults and Subsurface Fluid Flow in the Shallow Crust")
Faults and Subsurface Fluid Flow in the Shallow Crust59,99 €![Geoelectromagnetic Investigation of the Earth¿s Crust and Mantle]( "Geoelectromagnetic Investigation of the Earth¿s Crust and Mantle")
Geoelectromagnetic Investigation of the Earth¿s Crust and Mantle79,99 €![Observation of the Continental Crust through Drilling I]( "Observation of the Continental Crust through Drilling I")
Observation of the Continental Crust through Drilling I79,99 €![Formation and Evolution of Earth's Crust]( "Formation and Evolution of Earth's Crust")
Formation and Evolution of Earth's Crust135,00 €![Seismic Exploration of the Deep Continental Crust]( "Seismic Exploration of the Deep Continental Crust")
Seismic Exploration of the Deep Continental Crust40,99 €
In geology, a crust is the outermost solid shell of a rocky planet or moon, which is chemically distinct from the underlying mantle. The crusts of Earth, our Moon, Mercury, Venus, Mars, Io, and other planetary bodies have been generated largely by igneous processes, and these crusts are richer in incompatible elements than their respective mantles.