The thickness of the lithospheric plate can vary, but on average it ranges from 100 to 250 kilometers in thickness. The thickness can change depending on factors such as tectonic activity and location.
The lithospheric plates vary in thickness but generally range from 5 to 200 kilometers (3 to 124 miles). Thicker plates are found beneath continents, while thinner plates are located beneath oceans.
The study of lithospheric plates is called plate tectonics. It focuses on the movement and interactions of the Earth's lithospheric plates, which form the outer shell of the Earth. Plate tectonics help explain processes like earthquakes, volcanoes, and mountain building.
Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
The thickness of the Earth's crust can vary, but on average it is about 40 km thick beneath continents and about 8 km thick beneath oceans. This difference in thickness is due to the continuous process of plate tectonics, where oceanic crust is constantly being created and destroyed at mid-ocean ridges and subduction zones.
The lithospheric plates vary in thickness but generally range from 5 to 200 kilometers (3 to 124 miles). Thicker plates are found beneath continents, while thinner plates are located beneath oceans.
The last person to answer was a complete and total idiot. The correct answer is the Pacific Plate.
annually
plate tectonics
Tectonic plate consist of lithospheric mantle overlain by crustal
The study of lithospheric plates is called plate tectonics. It focuses on the movement and interactions of the Earth's lithospheric plates, which form the outer shell of the Earth. Plate tectonics help explain processes like earthquakes, volcanoes, and mountain building.
Continental plates are generally thicker than oceanic plates. Continental plates can range from 20-200 km thick, while oceanic plates are typically around 5-10 km thick.
A thick accumulation of sediments and small tectonic blocks formed from material scraped off a descending lithospheric plate is known as an accretionary wedge. This geological feature typically forms at convergent plate boundaries, where one tectonic plate is subducting beneath another. The process involves the accumulation of sediments and crustal material that is scraped off the subducting plate and piled up at the trench. Over time, this can lead to significant geological formations, often associated with mountain ranges and volcanic activity.
Tectonic plate consist of lithospheric mantle overlain by crustal
Part of California are on the North American Plate and parts are on the Pacific Plate.
Subduction.
crust: average of 32 km thick mantle: 2900 km thick outer core: 2200 km thick inner core 1250 km thick