Due to the driving forces of the rock cycle, plate tectonics and the water cycle, rocks do not remain in equilibrium and change as they encounter new environments. Rock particles are deposited in lakes and seas. Both compaction and cementation help in the formation of sedimentary rocks. Before we dive into the processes which transform the three different rock types into one another, it would be helpful to define some terms. A rock that cools within the Earth is called intrusive or plutonic and cools very slowly, producing a coarse-grained texture such as the rock granite. These cycle of rock formation and wearing out is constantly recycled the earth’s minerals. Soon, they melt and give rise to melted rocks called lava. Want to know more? Every rock you see, from the smooth stones in the riverbed to the mountains in the distance, is part of the ongoing cycle. The cooling and solidification of magma that happens over time creates igneous rocks. At times some of the metamorphosed downgoing slab may be thrust up or obducted onto the continental margin. Stay tuned with BYJU’S for more such interesting articles. In uralitization, secondary hornblende replaces augite; chloritization is the alteration of augite (biotite or hornblende) to chlorite, and is seen in many diabases, diorites and greenstones. The continental plates which lie on the Earth’s mantle are moving. The tectonic plates which collide with each other are by necessity pulling away from each other in other areas. The pressure and/or heat is so intense that it can transform the basic properties of another type of rock. Sediment is any type of geological particles, particles made out of Earth, that are small enough to be carried off and moved around by wind or water. streams, rivers, and oceans to a distant place from their origin. For example, an igneous rock such as basalt may break down and dissolve when exposed to the atmosphere, or melt as it is subducted under a continent. This involves the carbon cycle as a part of the overall rock cycle. 2) Formation of Sedimentary Rock – Weathering, Erosion, Sedimentation, After the particles build up they can join together and harden into a single sedimentary rock. This is caused by compression and tension. The rock cycle basic definiton is transitions among the three main rock types, which are metamorphic, igneous and sedimentary rocks. The information provided should not be used as a substitute for professional services. Offspring frequently have long maternal dependence periods during […], We have domesticated many species of animals for work and our own pleasure. The rock cycle explains how the three rock types are related to each other, and how processes change from one type to another over time. This is called the rock cycle. The phenomenon of seafloor spreading also plays a role in the rock cycle.

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