inner core outer core lower mantle upper mantle lithosphere
physical structure is geology and geology is a movement in the earths crust which is also physical structure.
Seismic tomography is a method that tells us about Earth's internal structure. It uses seismic waves generated by earthquakes to create detailed images of the Earth's interior. By analyzing how these waves travel through the Earth's layers, scientists can infer information about the composition, density, and temperature of different regions within the Earth.
Internal forces: tectonic plate movement, volcanic activity, and earthquakes. External forces: weathering, erosion by water/wind/ice, and impact events (e.g. meteorites).
The Earth's layers of rock are classified by their composition and physical properties. The main layers are the crust (continental and oceanic), mantle, and core (outer and inner). These layers are distinguished by differences in chemical composition, density, and temperature.
The physical structure of the Earth's rocks is changed by geological processes such as weathering, erosion, and sedimentation, as well as tectonic activities like folding, faulting, and volcanic eruptions. These processes can alter rock composition, texture, and structure over time, leading to the formation of different rock types, such as sedimentary, metamorphic, and igneous rocks. Additionally, human activities, such as mining and construction, can also impact the physical structure of rocks.
physical structure is geology and geology is a movement in the earths crust which is also physical structure.
Earths Outer Structure.
The study of the Earth's physical structure and history is known as geology. Geologists analyze rocks, minerals, landforms, and layers of the Earth to understand processes like plate tectonics, erosion, and sedimentation that have shaped the planet over millions of years.
Seismic tomography is a method that tells us about Earth's internal structure. It uses seismic waves generated by earthquakes to create detailed images of the Earth's interior. By analyzing how these waves travel through the Earth's layers, scientists can infer information about the composition, density, and temperature of different regions within the Earth.
Internal forces: tectonic plate movement, volcanic activity, and earthquakes. External forces: weathering, erosion by water/wind/ice, and impact events (e.g. meteorites).
The Earth's layers of rock are classified by their composition and physical properties. The main layers are the crust (continental and oceanic), mantle, and core (outer and inner). These layers are distinguished by differences in chemical composition, density, and temperature.
Light, Heat,Electricity, magnitism
it is landform
Tectonic activities, (Earths internal movements).
Techtonic plates
what involves both chemical and physical change on earths surface
geologist study the earths structure.