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The image illustrates a cyclical geological process beginning with average volcanic eruptions occurring three times yearly, where magma formation is driven by internal heat and tectonic movements, with subduction and melting at temperatures of 3200°C and pressure of 2400 atm leading to cooling and solidification into granite and basalt, weathering and erosion fragment rocks in the first 7 months via chemical and mechanical causes, transferring rock sediments primarily by weather to deposition areas such as river turns where lithification accumulates cement forming metamorphic rocks.
Given the complexity of the image, the above description may not be entirely accurate.
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The illustration provides details on how the natural cycle of stone formation happens.
Overall, the sequence unfolds in eight steps, starting with weathering and erosion and ending with cooling and solidification.
In the first 7 months, rocks break down into smaller pieces due to chemical and mechanical causes. With the help of weather the sediments of rocks are transferred. Then these elements get depositioned by the process of lithification, which later will form metamorphic rocks with accumulated cement.
In the fifth stage of the sequence, rocks will be subducted and melted in 2400 units of pressure at a high temperature of 32000 Celsius. Later, with the help of internal heat and tectonic movements, magma will be formed. At this point, volcanic eruptions happen 3 times a year. Finally, the magma thrown from the volcano cools and solidifies at the top of basalt and granite.
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