APES Monday, April 13 th, 2015 Reminders: EVERYONE: APES Math Review Worksheet – due tomorrow! AP Testers: Princeton Review Assignment (not due till after AP Test) Ocean Acidification Lab: need from Jamie & Destiny APES Exam is Monday, May 4 8:00 am; LEOCT is Friday, May 8 th Today’s Schedule: Get Back Graded Work Get Unit 12 Vocab List: due with quiz Monday, April 20 th Start Unit 12 Guided Notes
Geology & Mineral Resources Chapters 16
Geology Earth is dynamic planet whose surface & interior are constantly changing 3 Main Layers of the Earth 1. Core 2. Mantle 3. Crust
Geology Layers of the Earth
Geology Layers of the Earth Continental crust: under continents km (15–56 mi) thick Oceanic crust: under oceans. Thinner than continental km thick ( miles) Lithosphere: Outer part of earth. Combination of crust & upper mantle. Rigid layers. Asthenosphere: Part of the mantle. Very hot, partially melted rock. Like silly putty. ~180 km thick (112 miles)
Geology Layers of the Earth Mesosphere: Part of the mantle. Partially melted rock – very hot. Mesosphere ends ~1,800 mi down Outer core: Liquid metals. Extremely hot. ~2260 km (1400 mi) thick Inner core: Solid metal. Intense pressure keeps inner core solid km (1400 miles) thick
Geology Crust and Upper Mantle
Geology Internal Processes 2 kinds of movement occur in mantle’s asthenosphere: 1. Mantle plumes – mantle rock flows slowly upward in a column When reaches the top, it moves out in radial pattern 2. Convection cells/ currents that move large volumes of rock & heat in loops
Geology Internal Process
Geology Plate Tectonics Flow of energy & heated material in mantle’s convection cells cause 15 tectonic plates to move slowly across earth’s surface Move from cm per year Plate Tectonics = theory explaining movements of plates & the processes that occur at their boundaries (updated version of continental drift) Throughout earth’s history, continents have split & joined as plates have very slowly drifted thousands of km back & forth across the planet’s surface
Geology Plate Tectonics
Geology Plate Tectonics: 3 Types of boundaries 1. Divergent Boundary: 2 plates moving away from each other 2. Convergent Boundary: 2 plates pushed together; Subduction Zone: when a convergent boundary occurs between a continental plate and oceanic plate continental plate rides up over denser oceanic plat and pushes it down into mantle (process called subduction) 3. Transform Fault: 2 tectonic plates slide & grind past each other horizontally, along a fracture in lithosphere
Geology Plate Tectonics
Geology External Processes = geological changes based on energy from sun & gravity While internal processes build up earth’s surface, external processes tend to wear it down Ex: Erosion: material is dissolved, loosened or worn away from one area & deposited elsewhere driven by water & wind; accelerated by human activities
Geology External Processes Include : Mechanical weathering: rocks broken down into smaller pieces Frost wedging: forcing apart of rocks by expansion of water as it freezes in fractures & pores Chemical weathering: rock is decomposed due to influence of water, oxygen, & carbon dioxide Biological weathering: breakdown of rock through action of plants & animals
Geology Geological Hazards Earthquake: shaking of ground from fracturing & displacement of rock, creating a fault Severity is measured by magnitude – measure of amount of energy released Scientists use Richter Scale – each unit represents an amplitude 10 times greater than next smaller unit; 6.0 quake is 100 times greater than 4.0 Volcano: where magma reaches earth’s surface through a central vent or long crack Can release debris, liquid lava, gases (water vapor, carbon dioxide, & sulfur dioxide)
Geology Natural Hazard: Earthquakes
Geology Mount St. Helens
Geology Rocks and Minerals Crust is source of fossil fuels, metallic minerals, & nonmetallic minerals Mineral: element or inorganic compound that occurs naturally & is solid w/ regular, crystalline structure Ex: gold, silver, diamond, sulfur; salts, quartz Rock: solid combination of one or more minerals that is part of crust Ex: limestone (CaCO 3 ) and quartzite (silicon dioxide, SiO 2 )
Geology Rock Cycle: interaction of physical & chemical processes that changes rocks from one type to another
Geology 3 Types of Rock: 1. Igneous rock: formed by solidification of molten magma (granite, lava rock) 2. Sedimentary rock: formed from layers of sediments produced by erosion of existing rock become compacted (sandstone from sand; limestone from compacted shells & skeletons; coal from plant remains ) 3. Metamorphic rock: formed when rock is subjected to high pressure &/or heat (marble, slate) Video
Mineral Resources Mineral Resources Two major types Metallic minerals Nonmetallic minerals Are NONRENEWABLE Resources!
Mineral Resources Ore = rock that contains a large enough [ ] of a particular mineral to be profitable Can be considered high-grade (high [ ]) or low-grade (low [ ])
Mineral Resources Metallic Mineral Resources Aluminum (Al) – used for packaging, structural materials Iron (Fe) – used to make steel Steel – alloy of iron & other elements: Manganese (Mn) Cobalt (Co) Chromium (Cr) Copper (Cu) – wiring Gold (Au) – electrical equipment, coins, jewelry
Mineral Resources Nonmetallic Mineral Resources Sand – used to make glass, bricks, concrete Gravel – used for roads, to make concrete
Mineral Resources Types of Mining: Surface mining: removes shallow mineral deposits Materials lying over a deposit are removed to expose the resource for processing Surface mining is used to extract ~90% of nonfuel mineral resources & ~60% of coal in U.S.
Mineral Resources Types of Surface Mining: 1. Open-pit mining: machines dig large holes & remove metal ores Used for iron, copper, gold, sand, gravel, stone
Mineral Resources Types of Surface Mining: 2. Strip mining: extracting mineral deposits that lie in large horizontal beds close to earth’s surface; 2 types: 1. Area strip mining: when terrain is flat, an earthmover strips away overburden & a power shovel removes mineral deposit
Mineral Resources Types of Surface Mining : 2. Strip mining cont. 2. Contour strip mining: used to mine coal on hilly terrain
Mineral Resources Types of Surface Mining: 3. Mountaintop Removal: explosives, earth movers, power shoves, etc. are used to remove top of a mountain and expose seams of coal
Mineral Resources Subsurface Mining: Underground mineral resources are removed through tunnels & shafts Used to remove coal & metal ores
Mineral Resources The Damage of Mining: Scarring & disruption of the land Ex: area strip mining leaves spoil banks – no topsoil slow vegetative growth; high erosion Mountaintop removal puts waste into valleys destroys forests, buries streams Wastewater and toxic sludge produced when coal is processed can release toxins into water Produce lots of solid waste – contribute to water & air pollution Acid mine drainage: when rainwater seeps through a mine or spoil piles & carries sulfuric acid into streams and groundwater
Mineral Resources The Damage of Mining cont.: Water used to process ore contains sulfuric acid, mercury, arsenic contaminates freshwater Ore waste material is piled (called tailings) contaminates surface and groundwater Smelting: heating ores to extract metals Causes air pollution (sulfur dioxide, particles, greenhouse gases), water pollution, liquid & solid waste
APES Tuesday, April 13 th, 2015 Reminders: Unit 12 Vocab : due with quiz Monday, April 20 th Unit 12 TEST is definitely next week (Tues or Thurs) AP Testers: Princeton Review Assignment (not due till after AP Test) APES Exam is Monday, May 4 8:00 am; LEOCT is Friday, May 8 th Today’s Schedule: Cont. Unit 12 Guided Notes APES Math Review Worksheet Oreo Cookies Plate Techtonics
Mineral Resources
How long will supplies last? 5 countries supply most of world’s nonrenewable mineral resources: US, Canada, Russia, South Africa & Australia US imports all of its supplies of 20 key resources 4 strategic metal resources – manganese, cobalt, chromium, & platinum – are not available in US but important for economy & military
Mineral Resources How long will supplies last? Future supply depends on current supply and rate of use Supplies can become economically depleted – costs more than it is worth Depletion time = time it takes to use up a certain proportion of the reserves of a mineral at a given rate of use Usually set at 80% of reserves used
Mineral Resources How long will supplies last? Depletion time depends on: Recycling & reuse of supplies Technology Prices New discoveries Shortest depletion time from no recycling, no new discoveries Longest depletion time from recycling, reuse, better technology, new discoveries, etc.
Mineral Resources Solutions… Biomining: using genetically-engineered microorganisms that breakdown rock material and extract minerals Getting minerals from the ocean (such as copper, lead, zinc, etc.) Right now, it costs too much Substitute materials: plastics, fiber-optic glass cables Recycle & Reuse Ex: recycling aluminum can produces 95% less air pollution & uses 95% less energy Cleaner Production – pollution & waste prevention by companies