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This is equivalent to 30,000 metres or 30 kilometres. At 1 mm/y, 30,000,000 mm would accumulate over that 30 million years.Since the age of the Earth is 4570 Ma, this represents 150 ÷ 4,570 = 0.033 or 3.3% of geological time. The magma produced moves upward into cracks in the crust and is extruded onto the sea floor. Hot mantle rock moving toward the surface partially melts because the pressure is reduced.Mantle convection creates the traction that can force plates to move around on the surface.Because the mantle is plastic, this lower-density material tends to rise toward the surface, and cooler denser mantle material moves in to take its place. When heated, the rock expands and its density is reduced. Transfer of heat from the core to the mantle leads to heating of lower mantle rock.
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The main component of Earth’s core is iron (Fe).Rocks are made out of minerals, and most rocks contain several different types of minerals. A mineral has a specific chemical composition and lattice structure.Halite is composed of sodium (Na) and chlorine (Cl) with the Na+ and Cl− ions alternating with one another in all three directions within a cubic structure.Geologists provide information to reduce the risk of harm from hazards such as earthquakes, volcanoes, and slope failures they play a critical role in the discovery of important resources they contribute to our understanding of life and its evolution through paleontological studies and they play a leading role in the investigation of climate change, past and present and its implications.Paleontology is an important aspect of geology and requires an understanding of biology, including evolution, the physiology of animals and plants and ecological relationships.Geology involves integration of various different sciences (chemistry, physics, and biology for example), but also requires an understanding of the importance of billions of years of geological time.Answers to the exercises are provided in Appendix 3. The following are suggested answers to the review questions at the end of chapters in Physical Geology.
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