Geology and Earth Resources

Slides:



Advertisements
Similar presentations
Changes to the Earth’s surface
Advertisements

Layers of the Earth.
Chapter 2 Section 2 Forces Of Change.
Earth Structure and Composition Layers, Rocks, Minerals and the Rock Cycle.
ESC110 Chapter Eleven Environmental Geology & Earth Resources
Minerals and the Environment. The Rock Cycle Definitions Mineral –a solid homogenous (crystalline) chemical element or compound; naturally occurring.
Environmental Science PowerPoint Lecture Principles of Environmental Science - Inquiry and Applications, 2nd Edition by William and Mary Ann Cunningham.
1 Geology and Earth Resources. 2 Earth is a Dynamic Planet A Layered Sphere  Core - interior composed of dense, intensely hot metal, mostly iron. Generates.
Environmental Geology
1 William P. Cunningham University of Minnesota Mary Ann Cunningham Vassar College Copyright © The McGraw-Hill Companies, Inc. Permission required for.
AP Environmental Science Mr. Grant Lesson 20
The Earth Notes. Water, Land, and Air About 70% of our planet’s surface is water Oceans, lakes, rivers, and other bodies of water make up the hydrosphere.
GEOLOGIC TIME SCALE Organizes Earth’s 4.6 billion years of history into subgroups Subgroups: Eons Eras Periods Epochs 4 Major Eons…
Mining and related Issues Chapter 14 Lecture #3 Sections
1 Principles of Environmental Science Inquiry and Applications Third Edition Cunningham Chapter 11 Lecture Outlines* *See PowerPoint Image Slides for all.
1920 – land sold at public auction
1 Principles of Environmental Science Inquiry and Applications Third Edition Cunningham Chapter 11 Lecture Outlines* *See PowerPoint Image Slides for all.
1 Geology and Earth Resources
Geology and Nonrenewable Minerals Chapter What Are the Earth’s Major Geological Processes and Hazards?  Concept 14-1A: Gigantic plates in the.
1 Geology and Earth Resources. 2 Earth is a Dynamic Planet A Layered Sphere  Core - interior composed of dense, intensely hot metal, mostly iron. Generates.
1 William P. Cunningham University of Minnesota Mary Ann Cunningham Vassar College Copyright © The McGraw-Hill Companies, Inc. Permission required for.
Lecture #1 Section 14.1 & Section 14.1 Earth is a Dynamic Planet A Layered Sphere – Core - interior composed of dense, intensely hot metal, mostly.
Geology and Earth Resources By: Michela Griffin. Earth as a Layered Sphere Core: Interior of the earth; composed of a dense, intensely hot mass of metal.
Earth Notes Chapter 2 ~ Section 2 Forces of Change.
The Solid Earth. Earth’s Structure Core Mantle Crust.
Plate Tectonics. What is Plate Tectonics? The Earth’s crust and upper mantle are broken into sections called plates Plates move around on top of the mantle.
Vocabulary Click Below to start with a video – when the window opens be sure to click download.
Geology Review.
Introduction to Geology, Various Rx and Minerals.
The Earth’s Interior Composed of 4 layers Crust Mantle Outer Core
Geology and Nonrenewable Mineral Resources
Geology and Nonrenewable Mineral Resources. Key Concepts  Major geologic processes  Minerals, rocks, and the rock cycle  Earthquakes and volcanoes.
Students type their answers here
Geology and Nonrenewable Minerals
Chapter 8 Earth Systems and Resources.  Core - the innermost zone of the planet made of nickel and iron.  Mantle - above the core containing magma 
Geology and Nonrenewable Mineral Resources
1 Geology and Earth Resources. 2 Outline Tectonic Processes Rocks and Minerals  Rock Cycle Economic Geology and Mineralogy Environmental Effects of Resource.
Sedimentary rock forms when sediment is carried away by wind, ice or water and deposited in layers under pressure Sediment is any fragments of rock,
1 William P. Cunningham University of Minnesota Mary Ann Cunningham Vassar College Chapter 14 Lecture Outline Copyright © McGraw-Hill Education. All rights.
Geology and Nonrenewable Mineral Resources
Earth’s interior layers.
Chapter 22: The Earth’s Crust
AP Environmental Science
Earth Systems.
Ch 15 Geology Part 1.
Geology and Earth Resources
14-2 How Are the Earth’s Rocks Recycled?
Jeopardy! Vocabulary 1 Misc. Erosion & Weathering Earth’s Interior
The Rock Cycle
The Rock Cycle and Changes in the Earth
WEATHERING AND EROSION
Geology and Nonrenewable Mineral Resources
Intro to World Geography
Chapter 14 Lecture Outline*
Classifying Rocks Rocks
Question of the Day How are volcanoes formed?
Navo middle school science
Geology Notes Part 6.
Earth Systems & Resources
Earth’s Layers Three main layers Crust, Mantle, and Core
AP Environmental Science New England Geology
Forces that Shape the Earth
Understanding and identifying minerals
Geology and Nonrenewable Mineral Resources
Physical Geology Composition of materials, tectonic cycle, Formation and identification of rock types.
Chapter 8 Earth Systems Friedland and Relyea Environmental Science for AP®, second edition ©2015 W.H. Freeman and Company/BFW AP® is a trademark registered.
Unit 1 Lesson 2 The Rock Cycle
Bell Ringer Igneous rocks are classified by their ________ composition and their ________ size. If you were given a rock high in silica and with small.
Geology and Nonrenewable Minerals
Earth Structure and Composition
Presentation transcript:

Geology and Earth Resources

Outline Tectonic Processes Rocks and Minerals Rock Cycle Economic Geology and Mineralogy Environmental Effects of Resource Extraction Mining Reclamation Conserving Geologic Resources Geologic Hazards

A DYNAMIC PLANET A Layered Sphere Core - Interior composed of dense, intensely hot metal. Generates magnetic field enveloping the earth. Mantle - Hot, pliable layer surrounding the core. Less dense than core. Crust - Cool, lightweight, brittle outermost layer. Floats on top of mantle.

Earth’s Cross Section

Tectonic Processes Upper layer of mantle contains convection currents that break overlaying crust into a mosaic of tectonic plates. Slide slowly across earth’s surface. Ocean basins form where continents crack and pull apart. Magma forced up through cracks in oceanic crust form mid-oceanic ridges.

Tectonic Plates

Tectonic Processes Earthquakes are caused by grinding and jerking as plates slide past each other. Mountain ranges pushed up at the margins of colliding plates. When an oceanic plate collides with a continental landmass, the continental plate will ride up over the seafloor and the oceanic plate will subduct down into the mantle. Deep ocean trenches mark subduction zones.

Tectonic Plate Movement

Pangea Geologists suggest that several times in earth’s history most, or all, of the continents gathered to form a single super-continent, Pangea, surrounded by a single global ocean.

Continental Shift

ROCKS AND MINERALS A mineral is a naturally occurring, inorganic, solid element or compound with a definite chemical composition and regular internal crystal structure. A rock is a solid, cohesive, aggregate of one or more minerals. Each rock has a characteristic mixture of minerals, grain sizes, and ways in which the grains are held together.

Rock Types Rock Cycle - Cycle of creation, destruction, and metamorphosis. Three major rock classifications: Igneous Sedimentary Metamorphic

Rock Cycle

Igneous Rocks Most common type of rock in earth’s crust. Solidified from magma extruded onto the surface from volcanic vents. Quick cooling of magma produces fine-grained rocks. Basalt Slow cooling of magma produces coarse-grained rocks. Granite

Weathering and Sedimentation Mechanical - Physical break-up of rocks into smaller particles without a change in chemical composition. Chemical - Selective removal or alteration of specific components that leads to weakening and disintegration of rock. Oxidation Sedimentation - Deposition of loosened material.

Sedimentary Rock Deposited materials that remain in place long enough, or are covered with enough material for compaction, may again become rock. Formed from crystals that precipitate out of, or grow from, a solution. Shale Sandstone Tuff

Metamorphic Rock Pre-existing rocks modified by heat, pressure, and chemical agents. Chemical reactions can alter both the composition and structure of rocks as they are metamorphosed. Marble (from limestone) Quartzite (from sandstone) Slate (from mudstone and shale)

ECONOMIC GEOLOGY AND MINERALOGY Metals Metals consumed in greatest quantity by world industry (metric tons annually): Iron (740 million) Aluminum (40 million) Manganese (22.4 million) Copper and Chromium (8 million ea) Nickel (0.7 million)

Non-Metal Mineral Resources Gemstones and Precious Metals Supports despots, criminal gangs, terrorism, inhumane labor conditions, and environmental destruction. Sand and Gravel Brick and concrete construction, paving, sandblasting and glass production. Limestone Concrete and building stone Evaporites Gypsum and Potash Sulfur Sulfuric Acid

ENVIRONMENTAL EFFECTS OF RESOURCE EXTRACTION Mining Placer Mining - Hydraulically washing out metals deposited in streambed gravel. Destroys streambeds and fills water with suspended solids. Strip-Mining or Open Pit Mining Large scars on land surface. Tailings Toxic runoff

Mining Underground Mining Extremely Dangerous Gas Inhaling Particulate Matter Tunnel Collapse

Restoration Surface Mining Control and Reclamation Act (1977) requires better restoration of strip-mined lands, especially if land classed as prime farmland. Difficult and expensive. Complete reclamation often costs more than $10,000 / hectare. 50% of U.S. coal is strip mined.

Processing Metals are extracted from ores by heating or treatment with chemical solvents. Smelting - Roasting ore to release metals. Major source of air pollution. Heap-Leach Extraction - Crushed ore piled in large heaps and sprayed with a dilute alkaline cyanide solution which percolates through the pile to dissolve the gold. Effluent left behind in ponds.

CONSERVING GEOLOGIC RESOURCES Recycling Aluminum must be extracted from bauxite by electrolysis. Recycling waste aluminum consumes one-twentieth the energy of extraction from raw ore. Nearly two-thirds of all aluminum beverage cans in U.S. are recycled. Other metals commonly recycled: Platinum, gold, copper, lead, iron, steel.

Substituting New Materials For Old Reduce metal consumption by using new materials or new technologies. Plastic pipes in place of metal pipes. Fiber-optics in place of metal wires. Metal alloys in place of traditional steel.

GEOLOGIC HAZARDS Earthquakes - Sudden movements of the earth’s crust that occur along faults where one rock mass slides past another. Gradual movement - creep. When friction prevents creep, stress builds up until eventually released with a sudden jerk. Frequently occur along subduction zones. Tsunami - Seismic sea swells.

Volcanoes Volcanoes and undersea magma vents are the sources of most of the earth’s crust. Many of world’s fertile soils are weathered volcanic material. Human / Environmental Dangers Volcanic Ash Mudslides Sulfur Emissions

Mass Wasting Materials are moved downslope from one place to another. Many human activities such as forest clearing and building homes on unstable slopes increase both frequency and damage done by landslides.

Summary Tectonic Processes Rocks and Minerals Economic Geology and Mineralogy Strategic Resources Environmental Effects of Resource Extraction Mining Reclamation Conserving Geologic Resources Geologic Hazards