Geology/Rocks Study Guide Tentative Test Date: November 20, 2015 The rock cycle has an impact on the physical characteristics of the Earth. What is a rock? Rock A material made up of one or more minerals What is a mineral? Mineral A true mineral has 3 features: A solid material with particles arranged in a repeating pattern Usually made from material that was never alive (inorganic) Formed in nature (not man-made) Examples: Quartz Talc Hematite Sapphires & rubies Emeralds Diamonds Types of Data & Observations Quantitative Qualitative Data recorded using numbers and measurements Length, height, time, temperature, cost, age, etc. Descriptions of properties that can be observed but not measured Color, texture, smell, taste, etc. Properties of Minerals Property Hardness Luster Streak Scientists use properties of minerals to classify them. A characteristic of a substance, object, or organism We describe something or someone by its properties. Examples of properties below: A mineral’s ability to scratch another mineral, measured by the Mohs’ hardness scale How minerals reflect light, can be metallic, earthly, glassy, etc. The color left behind when a rock is rubbed across a streak plate The streak can be a different color than the observed color of the mineral Properties of Rocks Composition Grain size Color What mineral(s) a rock is made of How big the crystals of an igneous rock appear to be A property of rocks/minerals that you can easily see Types of Rock How do a rock’s properties determine how it is used in every day life? Classification Igneous Metamorphic Sedimentary The grouping of things by a set of rules A type of rock that forms when melted rock (magma or lava) hardens Examples: Granite Basalt A type of rock that forms when other rocks and/or minerals are changed by heat or pressure. Although heat is involved, the rocks don’t completely melt. Examples: Gneiss Marble Slate A type of rock formed by layers of sediments that were squeezed and stuck together over a long time. Sedimentary rock layers form on top of each other. The oldest layers are found at the bottom. Examples: Limestone Shale Sandstone Coal The Rock Cycle How does the rock cycle compare to other natural cycles? (like the water cycle) Rock Cycle Weathering Sediment Strata Volcano Magma Lava The slow, never-ending process of rock changes Rocks are being constantly changed chemically and physically The process of breaking rock into sediment (sand, soil & other tiny pieces) Small pieces of rock, sand and soil that have been broken off of larger pieces of rock by weathering Sediment can settle in layers to become sedimentary rock Sediment can also be moved from one place to another by wind and water Layers The different layers in sedimentary rock are sometimes called strata A mountain formed by lava and ash Melted rock from Earth’s mantle Magma when it is above Earth’s surface Diagram of the Rock Cycle Figure 1: The Rock Cycle, from http://www.cotf.edu/ete/modules/msese/earthsysflr/rock.html Rocks & the Past How do the physical characteristics of rocks help us understand the past? Erosion Fossil Trace Fossils Mold or Cast Fossils Index Fossils Fossil Fuels The process of moving sediment from one place to another The remains or traces of past life found in sedimentary rock Fossils that are not body parts, but show something an organism left behind (footprints, etc.) Fossils in the shape of an organism (dinosaur bones, shark teeth, fern imprints, etc.) Help identify how old a rock layer or other fossils are An energy rich resource formed from the buried remains of once-living organisms. Coal, Oil, Natural Gas, etc. Navigation Navigation Compass How to get from one place to another Device that uses Earth’s magnetic field to help in finding north for navigation Useful information from previous units Earth’s Structure Crust Mantle Outer Core Inner Core Question Research Hypothesis Observe Data Record Analyze & Conclusion The thin, outer layer of Earth The layer of rock beneath Earth’s crust The inner part of the mantle is very hot, which makes it soft The layer of melted iron beneath the mantle Source of Earth’s magnetic field The center layer of Earth, very hot The inner core is under very heavy pressure, so it stays solid, even though it is hot enough to be melted. Scientific Process Start with a question to answer or a problem to solve Find out what other people already have discovered about the topic An educated guess to answer your question. It should be stated in a way you can measure or observe To notice the properties of something. Observations can be made with your 5 senses. Observations can also be measured to get more exact information The information gathered from observing Collect your information in a clear way Once your experiment is complete, look at the recorded data and decide whether or not it supports your hypothesis