The rock cycle is very important to us because it explains the way the different types of rocks are formed on earth. The rocks currently visible on the Earth’s surface have moved through transition stages that transformed them from one form into another. The importance of the rock cycle lies in how it forms and recycles the various layers that make up the Earth. To do this‚ the cycle moves through three different stages that produce three different types of rock. Igneous rock makes up the foundation
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The Rock Cycle & Classification of Rocks The rock cycle is the formation‚ breakdown and reformation of a rock as a result of sedimentary‚ igneous‚ and metamorphic processes. The rock cycle is an illustration that is used to describe how the three rock types are related and how Earth processes change a rock from one type to another over time. Each group contains a collection of rock types that differ from each other on the basis of the size‚ shape and arrangement of mineral grains. Due to the driving
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Formation of Rocks The three main ways rocks are formed: • Sedimentary rocks are formed through the gradual accumulation of sediment: for example‚ sand on a beach or mud on a river bed. As the sediment is buried it is compacted as more and more material is deposited on top. Eventually the sediment will become so dense that it is essentially rock. This process is known as lithification. • Igneous rocks are rocks which have crystallized from a melt or magma. The melt is made up of various components
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The rock cycle involves of a chain of continual progressions through which earth materials change from one form to another over time. Some processes in the rock cycle happen over millions of years and others occur much more quickly. There is no real starting or completion to the rock cycle; however‚ it may be appropriate to begin investigating the rock cycle with magma (Bergman 2005). Magma‚ or molten rock‚ forms only at certain locations within the earth‚ mostly along plate boundaries. Magma crystallizes
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Incredible Igneous Rocks Granite is one of the most well-known and commonly found types of igneous rock. Granite batholiths are a common rock type found in Richmond‚ VA. These larger igneous‚ intrusive rocks are found near my grandparents’ home in Richmond‚ and as a child I would constantly climb and play on them. Looking at granite in class always reminds me of these batholiths by my grandparents’ home. Granite consists mostly of the minerals quartz‚ mica and feldspar‚ which give granite its typical
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Metamorphic Rock Metamorphism means to change form; this is exactly what metamorphic rocks do. This paper will take a look at the Earth’s rock cycle to examine exactly where the metamorphic rock fits into it. It will also look at how metamorphic rocks are formed and the relationship between metamorphic rocks and igneous rock and sedimentary rocks. This paper will examine the geological characteristics and materials of metamorphic rocks‚ and examine some examples of metamorphic rocks and will describe
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Minerals and Rocks Minerals Minerals: Minerals are elements or compounds found in the earth. The elements or compounds are called minerals if they have five features. They are solids. They are formed naturally in the earth. They have the same chemical makeup throughout They are not alive or made of living things. They have definite arrangement of atoms. 3‚000 different minerals are found in the earth. Some are common but most are rare. Aluminum‚ quartz‚ feldspar
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Level Material History of Rock Worksheet Leah Bechtel 12/09/2012 SCI/245 Robert Dillon Write a 500- to 750-word explanation regarding the role of plate tectonics in the origin of igneous rocks. The role of plate tectonics in the origin of igneous rock is extremely important. Igneous rock is formed from magma that reaches the continental and oceanic crust or through hot spots that are around the world. There are three different places where igneous rocks can form; where the lithospheric
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A joint is defined as a fracture in a rock between the sides of which there is no observable relative movement. They are present is most consolidated rocks of igneous‚ metamorphic and sedimentary origin. Joints may form as a result of either diastrophism or contraction. Description: (i) A series of parallel joints is called a ’joint set’. (ii) Two or more joint sets intersecting each other produce a ’joint system’. (iii) Two sets of joints nearly at right angles to one another‚ produced by the
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The purpose of this paper is to propose an annual rock climbing training “action” plan (macrocycle) for teaching and developing a young athlete through the use of an integrated neuromuscular training program with three “periodization” mesocycles (4 months) in a distributed block framework paralleling Fitts’ three stages of learning. This plan will focus on developing the core six components of INT which are dynamic stabilization‚ coordination‚ strength‚ plyometrics‚ speed/agility‚ and fatigue resistance
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