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The Rock Cycle What is a rock? Answer • A naturally occurring solid mixture of 1 or more minerals/organic matter • Rocks are always changing • New rocks form from old rocks = ROCK CYCLE How can rocks help Humans? HMMMMMMM… Human Usage of Rocks • Used for tools – Hammers, knives, arrowheads, spear points, scrapers • Roads + monuments – Pyramids, capitol buildings Weathering • IS H2O, wind, ice, and heat break down rock • Breaks rocks down into fragments • These fragments will become part of sedimentary rocks Erosion • Sediment is removed from its source • This is caused by H2O, wind, ice, + gravity Deposition • Process in which sediment moved by erosion is dropped and comes to rest is this. • Sediment is deposited in bodies of water or areas of low-lying land • Sediment will be pressed and cemented together to form sedimentary rock Example of this • Bryce Canyon is an example of weathering, erosion, and deposition Heat and Pressure • Sedimentary rock can also form when sediment is buried and squeezed by weight • IF add heat to the process then the sediment rock can change to metamorphic rock • If HOT enough to melt then will create magma when MAGMA cools then have igneous rock Uplift • Buried rock will eventually be exposed to Earth due to uplift and erosion • Uplift is movement within the Earth that causes rocks inside the Earth to be moved to the surface • Uplifted rocks will then go through weathering, erosion, and deposition Rock cycle steps/paths 1. sedimentary rock -grains of sand and other sediments erode from hills and Mts—wash into rivers—oceans—form the ocean floor—compacted together to form this 2. Metamorphic rock -Earth’s crust collide (tectonic plates) some rock is forced downward—get intense heat + pressure= m. Rock 3. Magma -Hot Liquid forms when rock is melted 4. Igneous Rock -Magma rises (is less dense), cools= I. rock 5. Sediment -Uplift and Erosion expose the Igneous Rock—weathers, wears back into Sedimentary rock Rocks changing • So rocks are continually changing what time they’re due to the Earth’s process – Igneous –Sedimentary-Metamorphic • The location of the rock is a huge factor is what the rock will change into – Surface- have weathering, erosion, deposition – Deep down- heat and pressure Rock Classification • Rocks are first divided into igneous, metamorphic, and sedimentary by how they form • But then will divided them down even farther – Ex. Igneous- if cooled on Earth’s surface or below • 2 main items scientist use is the composition and texture of rock to identify them Composition • Minerals that make up the rock • Look @ pg. 95 Texture • The size, shape, and position of the grains that make up the rock = texture of it – Sedimentary= fine-medium, or coarse- depends on size of grains – Igneous= fine to coarse-depends on how time magma has to cool – Metamorphic = fine or coarse- depends on temperature and pressure rock gets – Texture can also tell how rock was formed-look on pg. 96