👉 A peridendritic is a type of structure in the Earth's crust that forms when magma rises to the surface and cools, resulting in the formation of a new layer of rock. This process can be characterized by the presence of lava flows, which are usually composed of molten rock. The peridendritic rocks often have distinct features such as smooth surfaces and a characteristic shape, known as a "peridendritic curve." These rocks are typically found in areas where there is an active magma chamber
