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Two Common mineral bonds & example |
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ionic- donates electron to an atom (Halite) Covalent- share electrons (Diamond) |
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Naturally occurring, inorganic solid with a well defined and orderly crystalline structure |
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Common use: Bauxite Hematite Sphalerite |
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Abundant elements in earth's crust |
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Causes of seismicity for Mt.Pinatubo |
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Rising Magma Mountain Letting off steam tectonic stress |
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Volcano type for Colombia River Basalt |
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Paracutin, Mexico volcano type |
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Melting at ocean spreading ridges |
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Decompression- pressure decreases and solids can liquify and become new rock/mineral |
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Melting at convergent plate boundaries |
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Pressure increases and heat increases to change the rock |
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Types of data collected at Mt.Pinatubo |
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seismic activity from volcano gas levels of sulfur at the cone or head of volcano |
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section of origin rock surrounded by a different type of rock and is cut off from similar rock (island) |
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Original though of land mass that was first then split and drifted to locations today |
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Plutonic continental crust |
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Volcanic convergent boundaries |
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2 reasons why convergent margin volcanoes are more explosive than ocean ridge |
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more pressure built up and released at once lower temperatures |
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Igneous structures at Devils Tower, Ship Rock |
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Ropy basaltic lava flows in Hawaii |
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Two ores in WI mines and issues |
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Copper,iron, zinc- waste materials can contaminate and leech into the aquifers and can be toxic to humans and animals |
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Hazard for Fibrous amphibole |
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can get into lungs because they are very fine and cause lung cancer |
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Hazard for Montmorillonite clay |
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building on clay is hazardous can expand and sink depending on moisture |
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Two most common MINERALS of earth |
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Fine grained, microscopic crystals |
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Two sized crystals, only one is visible |
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Two size crystals, both are visible |
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Frothy texture due to gases escaping magma |
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How minerals solidify and the way the will |
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Tubular igneous bodies that parallel rock layers |
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Polygonal dikes formed by cooling of mafic magma |
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Linear Magnetic Anomolies |
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Fred Vine and Drummond Matthews |
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Magma diversification: some of the rock is melted and produces a new rock |
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Magma diversification: formation of crystals removes chemical cmponents of crystal from liquid and changes composition |
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Positively Charged and are in nucleus |
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Neutral charged particle and located in nucleus |
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Protolight of Mica Schist |
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Sediments originally deposited horizontally |
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The oldest layer is on the bottom, each layer above that is younger |
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Law of cross cutting/intrusion |
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Dikes and intrusions are younger than the rock cut into it |
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Resource value of Greenstones |
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weathering is the breakdown of the rocks and erosion is the transportation of the particles by wind,water etc. |
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Chemical process where feldspars decompose to clay |
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Chemical process where limestone weathers |
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two protons and neutrons are lost, atomic number decreases by two and atomic mass decreases by four |
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Sandstone- formed in a beach environment |
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Diagnostic rocks and structures from streams |
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Rounded stones and sandstone, ripple marks form and indicate a stream in the rock beds |
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Sedimentary rocks and structures from desert |
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Evaporates like rock salts |
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Sedimentary rocks and structures from floodplain |
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Silts from the fine grained sand |
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Limestone weathering product |
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soil has high concentrations of shell and calcium carbonate |
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high concentrations of clay from decomposed feldspars |
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Mechanical weathering agent |
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ice wedging, water fills in cracks in the rock and freezes, the water expands and the rock breaks appart |
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% Chance of 50 year flood |
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% chance of 20 year flood |
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Two rock types where Karst Topography develops |
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Two potential aquifer rocks |
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Regions that receive less than 25cm of precipitation per year |
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How to calculate stream discharge |
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Stream width x Stream depth x Stream velocity |
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Capacity- rate of permeability |
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Hydraulic gradient- ability of water to travel through sediments |
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mass of ice originating on land from compaction and recrystallization of snow that shows evidence of past/present flow |
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Last glacial advance peak |
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Years ago last glacial advance ended |
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Located in western us and has over pumping and risk of saltwater intrusion |
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Origin of sedientary deposits in Stevens Point |
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Beach environment to shallow marine environment |
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Global sea rise last 15,000 years |
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Ag impacted floods along mississippi |
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Working the soil created loose sediments which were able to be carried away. Farmers needed natural levees to protect farmland from natural flood cycles |
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2 Geographic reasons Southwest US is a desert |
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Rain shadow from the mountains No permanent streams |
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Eccentricity- change in shape of earth's orbit around the sun Obliquity- changes in the angle of earth's axis towards or away from the sun |
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2 stabilization projects the ACOE develops on the coast |
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Dunes- create dunes to try and hold the sand in place Breakwaters- ledges or walls out seaward to slow down waves |
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Waves that decrease velocity in outer core |
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Waves of highest velocity |
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Waves that don't penetrate the outer core |
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Crust-Mantle seismic boundary |
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Geologic environment where coal forms |
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Swampy environment where vegetation falls and is covered up |
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Located in Wyoming and is the largest coal mine in the U.S, provides majority of coal for our country |
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Suggested fracking of the shale deposits to extract natural gas |
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stress accumulates, is released from one area along a fault and is transferred farther down the fault |
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earth, moon and sun are aligned |
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earth, moon and sun are at right angles |
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four causes:earthquakes, landslides,volcanic erruption, meteorite impacts |
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steep slope, doesn't break the wave, rolls onto the beach |
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moderate slopes, wave curls into tunnel until wave breaks |
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gentle beach, waves break far from the beach, surf rolls over the front of the wave |
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force along ocean and volcano, ocean water has a negative and voclano side is positive gradual force |
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East pacific ocean plate was largely subducted |
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Modern day remnant of farallan plate |
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3 Orogenies of the Appalachian Mountains |
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Taconic, Acadian and Alleghenian |
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