Because of weathering and erosion.
Granite, gneiss, and sedimentary rocks like sandstone and limestone are commonly found in the continental crust. These rocks make up the bulk of the Earth's continents and are less dense than those found in the oceanic crust.
The entire ocean floor is recycled in roughly 160 million year cycles through the process of plate tectonics. Because continental plates do not subduct, the rock is much, much older, particularly in the continental interior.
True. Continental crust is primarily composed of lighter rocks such as granite, which are less dense than the basaltic rocks found in oceanic crust. This is why continental crust is thicker and less dense than oceanic crust.
No, fossils are typically found in sedimentary rocks rather than igneous rocks. Sedimentary rocks form from the accumulation and lithification of sediments, making them more likely to preserve fossils due to their layered nature. Igneous rocks, on the other hand, form from the cooling and solidification of molten rock and are less likely to contain fossils.
Rocks near the source of a river tend to be larger, more angular, and have sharper edges due to less erosion. In contrast, rocks found farther downstream are typically smaller, smoother, and more rounded as they have been more weathered and moved by the flowing water.
They're called strata. Strata less than 1cm thick are Laminae.
The oldest rocks are typically found in continental crust regions, particularly in shield areas, which are exposed portions of the ancient crystalline basement rocks. These regions, such as the Canadian Shield or parts of Greenland, contain rocks that have remained relatively undisturbed by tectonic processes. The age of these rocks can often reach over 4 billion years, reflecting the planet's early geological history. Additionally, igneous and metamorphic rocks in these areas are less likely to have been recycled or altered compared to younger sedimentary rocks.
Yes, there are rocks in tundras. Tundras are typically covered with a layer of vegetation, mosses, and lichens, but rocks can still be found in the soil and surface. These rocks may be uncovered during the short summer thaw or exposed in areas where the vegetation is less dense.
The continental crust can be found beneath the land masses or continents on Earth. It is typically thicker and less dense than the oceanic crust, composed of a variety of rock types including granite, sedimentary rocks, and metamorphic rocks.
Crustal rock is normally less dense than mantle rock.
less dense
When you think about it a larger rock has more surface area to be worn away think about it like if you have a large sweet or a small sweet,which will be gone faster if you suck/chew it,the small sweet because there is less of it