The diagrams show how dislodged fragments of rock and stones are carried to the sea, forming the sedimentary rock in coastal areas.
Overall, this process proves the real power of water, demonstrating how its influence forms geological features and affects the Earth’s relief over time.
First of all, rainwater soaks into fissures of a mountainside, leading to the expansion of these cracks. Once the water becomes frozen and breaks the rock, it starts rolling into the mountain river. Then, while crumbling and becoming small pebbles and sand grains, these stone fragments are being transported by downstream to the sea.
Next, these small pieces of rock settle down in layers on the seabed. Water and water-borne chemicals work between the pebbles and grains, gradually cementing them together. As a result of lithification, the sedimentary rock, also known as sandstone or mudstone, is formed, and can be seen during the low tide period.
