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Wellesley Elementary Schools. Grade Four Geology Training By: Lisa Moore. Training Objectives. To provide necessary information for parent volunteers, in preparation for leading students on the fourth grade geology field investigation. - PowerPoint PPT Presentation

Text of Wellesley Elementary Schools

  • Wellesley Elementary SchoolsGrade Four Geology TrainingBy: Lisa Moore

  • Training ObjectivesTo provide necessary information for parent volunteers, in preparation for leading students on the fourth grade geology field investigation.

    To familiarize parent volunteers with important geological sites in Wellesley.

  • Presentation OutlineBackground information Layers of the earth, plate tectonics, the rock cycleMineral identificationThree types of rocks Igneous, Sedimentary, and MetamorphicGeologic time scale Geologic history of Wellesley

  • The layers of the earthCrust Relatively cold, thin, brittle solid, fractures with earthquakes. Made of calcium, sodium, and aluminum silicate minerals. 5-20miles(8-32km) thick, thickest at mountains, thinnest at ocean floorMantle An elastic solid, making up most of the Earths mass. Made of iron, magnesium, Aluminum, silicon, and oxygen. Convection currents within mantle cause crustal plates to move.(1832 F or 1000 C), 1800miles (2896km) thickLiquid outer core Made of iron and sulfur.(6692 F or 3700 C), 1400miles (2252km) thick Solid inner core Made of iron. Remains solid due to immense pressure, even at high heat. (9000 F or 5000 C), 800 miles (1287km) to center

  • Plate TectonicsPlate tectonics is the movement of the earths crustal plates due to convection currents in the mantle. As plates move they may collide, pull apart or rub past each other. The earths land masses sit atop these crustal plates and are deformed by crustal motion.Demo mantle elasticity.Demo plate tectonics.

  • Tectonic plate boundaries and the Pacific ring of fire

  • Minerals Naturally occurring, homogenous, inorganic solid with definite chemical composition, crystal structure and specific physical properties Minerals are the building blocks for all rocks.A mineral may be a pure element, like gold or a complex compound, like quartz. A rock is made up of one or more minerals physically or chemically combined. The type of rock formed will be determined by the type of minerals present and how it was formed.Scientists use characteristics of crystal shape, color, luster, hardness and streak to identify minerals.Demo mineral identification techniques.

  • Three types of rocksIgneous formed when molten rock, magma or lava, cools and hardens.

    Sedimentary formed when sediments are compacted and cemented together.

    Metamorphic formed when existing rock is put under intense heat and pressure, physically or chemically changing the rock.

  • The rock cycle - a model that shows how minerals are recycled through continuous geologic processes on earth.

  • Igneous rocks - from Latin meaning fireIntrusive igneous rock formed from magma deep within the earths crust. These rocks cool slowly, resulting in coarse grained texture with large visible crystals. (granite and diorite)Extrusive igneous rock formed when lava cools at the earths surface. These rocks cool quickly, resulting in a fine grained or smooth texture. Air bubbles may be present. (basalt, obsidian, pumice)

  • Extrusive igneous rock examples: Top left is a lava flow & below it is Basalt Intrusive igneous rock examples: Top right is Granite & below it is an igneous intrusion

  • Sedimentary rockMade from sediments; bits and pieces of rock and organic matter, being cemented and compacted togetherSediments transported by wind, water, and glaciersEvidence of layering, ripple marks, fossils, and rounding of particles of sediment

  • Sedimentary rocks Breccia, a fossil, Roxbury puddingstone, sandstone

  • Metamorphic rockFormed when existing rock is put under intense pressure and/or heat and is changed physically and/or chemically.Regional metamorphism and contact metamorphism.May see banding, rock is very hard.

  • Examples of metamorphic rock and what they changed from.Top: left is the igneous rock granite, at right after heat and pressure, becomes gneissBottom: left is sedimentary shale, at right after heat and pressure becomes slate

  • Can you name the types of rock seen below?

  • The geologic time scale : A trip through Wellesleys geologic history

  • Word bank of terms to knowRockMineralCrystalCrustMantleIntrusive igneous rockExtrusive igneous rock Sedimentary rockMetamorphic rockBedrockWeatheringErosion

  • Final thoughts:Every rock tells a story of how it formed and what has happened to it. Dont worry about specific rock names but be able to look for identifying traits for each type of rock. (Igneous visible crystals, Metamorphic banding, Sedimentary layers, fossils, rounded particles) Understand what a rock, or rock formations, tell you about the geologic history of the area. (i.e. glacial activity, volcanic activity, crustal motion, water action) Generate excitement and curiosity as you learn about Wellesleys history through its rocks, exploring its volcanic past, glacial past and present day geology.

  • Jany_Finkielsztein@wellesley.k12.ma.us781 446 6210 xt 1411

    Outdoor: Friday October 15, Tuesday October 19,Friday October 22 and Tuesday October 26(8:50-11:45am, meet at Kelly Memorial Park on Elmwood next to the Baptist Church)

    Geology Video