The Earth's crust is the outermost layer of the Earth and is made up of two types: continental crust and oceanic crust. Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the continents and the areas of shallow seabed close to their shores.
Continental crust is formed through a process called continental accretion, where smaller landmasses collide and merge to form larger continents. This process involves the accumulation of various types of rocks over millions of years.
Understanding the composition, characteristics, and formation of continental crust is essential for comprehending the Earth's structure and the processes that have shaped its surface over millions of years.