Continental plates do not usually shrink or grow in area significantly over short time scales. They can shift, break apart, or collide with each other due to tectonic forces, but their overall size remains relatively consistent. The movement of continents occurs at rates of a few centimeters per year, which is not enough to cause noticeable changes in their size.
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
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.
Oceanic plates are heavier than continental plates because they are denser and thinner. Continental plates are lighter because they are less dense and thicker. The difference in density and composition accounts for the varying weights of the Earth's plates.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
Continental plates do not usually shrink or grow in area significantly over short time scales. They can shift, break apart, or collide with each other due to tectonic forces, but their overall size remains relatively consistent. The movement of continents occurs at rates of a few centimeters per year, which is not enough to cause noticeable changes in their size.
Mountains can both grow and shrink over long periods of time due to tectonic forces such as plate movement and erosion. The process of mountain growth usually occurs over millions of years when tectonic plates push against each other, forcing the Earth's surface to rise. On the other hand, mountains can shrink through erosion caused by weathering and other natural processes that wear down their surfaces.
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
You have to shrink the triangles, grow the block, grow the triangles, grow the octagon.
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.
because you get older not younger there for you grow not shrink .. but sometime as you get old you shrink. depending on who you are and if you take care of yourself
Yes, continental plates are more buoyant than oceanic plates because they are thicker and less dense. Continental plates are made up of less dense material such as granite, while oceanic plates are primarily composed of denser basaltic rock. This difference in density causes continental plates to float higher on the underlying mantle.
Continental plates are thicker and less dense. Continental plates are mainly granitic in composition. Oceanic plates are mainly basaltic in composition. The rock of continental plates is on average, much older than the rock of the oceanic plates. The oceanic plate underlies the oceans, and the continental plate makes up the land masses. Continental plates do not subduct at convergent plate boundaries.
they bang
Continental plates are more buoyant then oceanic plates.
Oceanic plates are heavier than continental plates because they are denser and thinner. Continental plates are lighter because they are less dense and thicker. The difference in density and composition accounts for the varying weights of the Earth's plates.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.