This is not a question.
The rock cycles are used to understand how rocks are made and how they change from metamorphic to sedamentary and so on. It is a chart to explain it.
Weathering can cause different layers of rock to erode at different rates based on their composition and susceptibility to weathering processes such as freeze-thaw cycles or chemical weathering. This can lead to the formation of distinct layers or textures in the rock, creating a stratified appearance over time.
No, not all rocks follow the rock cycle. The rock cycle is a continuous process of formation, transformation, and reformation of rocks through different geological processes. Some rocks may not experience all stages of the rock cycle, while others may undergo multiple cycles over millions of years.
Two cycles determine how mineral deposits are formed-the rock cycle and the tectonic cycle. Heat from the Earth's interior melts some of the rocks in the crust (the upper part of the lithosphere).
The size of a rock or rock particle is a general indicator of the distance it has travelled from the point of origin of the parent rock formation.
Igneous Rock Metamorphic Rock Sedimentary Rock
revolving or cecurring in cycles; characterized by recurrence in cycles Rock on!!
Movement of the plates takes rock and sediment into different geologic spaces. Convergence and subduction zones push some rock up, while dragging other rock down. This causes changes in the mineral component.
The: Rock Cycle Water Cycle Nitrogen Cycle Oxygen Cycle Carbon Cycle
revolving or cecurring in cycles; characterized by recurrence in cycles Rock on!!
Freeze-thaw weathering occurs when water seeps into cracks in rocks, freezes, expands, and breaks the rock apart. Over time, this process weakens the rock, causing it to fragment and break into smaller pieces. The repeated cycles of freezing and thawing can lead to the formation of scree slopes as the broken rock fragments accumulate at the base of steep slopes.
The cycles are molten rock, lava, and then hardened lava like obsidian.