Post on 30-Dec-2015
Introduction to Geology Geology ”Knowlege or study of the Earth."
Physical geology examines the materials and processes of the Earth.Historical geology examines the origin and evolution of our planet through time.
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USES OF ROCK
Source of power
Source of minerals
Source of soil
Source of building and road making materials
Source of industrial raw materials
Source of gems and precious metals
Geology in the News
• Two die in 6.5 magnitude Earthquake near San Lois Obispo California
• Earthquake triggers mudslides
http://news.nationalgeographic.com/news/2003
Geologic Hazards
San Andreas Fault
“Major Quake Likely to Strike San Francisco Bay Region Between 2003 and 2032”
• Assessing Risks• Avoiding Risks• Preventing
Damage• Predicting Impact
Dealing withGeologic Hazards:
http://quake.wr.usgs.gov/research/seismology/wg02/
Geology in the News 2
Earthquake Bam, Iran• A Magnitude 6.5
Earthquake hits a stone- and mud-house city of 100,000 in Iran 12-26-03– 30,000 Dead– 30,000 Refugees
• US sends aid and releases sanctions
• Relations improved
Photos from AP
Geological HazardsVolcanoes
Landslides
Earthquakes
Geology in EngineeringSlope Failure Risk Assessment and Control
To prevent slope failure engineers must understand the geology that forms and controls the slope
Geology in Engineering
Committee member John Burland, an engineer, promoted soil extraction as the best way to save the tower.
In Pisa the tilted one is back in business after an 11-year effort to keep it from collapsing
The Leaning Tower Straightens Up
www.smithsonianmag.si.edu
Engineers use knowledge of geology to design, protect and correct structures
What's the first thing that you notice about our planet when you see this image?
ESS
What are some of the interactions between these spheres?
The Earth System
The Earth System
Hydrosphere: The oceans cover ~71% of our planet and represent 97% of all the water on our planet.
Atmosphere: The thin blanket of air that covers our planet. It is not only the air we breathe, but protects us from harmful radiation from the sun.
ESS
The Earth System
Biosphere: includes all life on Earth - concentrated at the surface. Plants and animals don't only respond the their environment but also influence it.
Solid Earth (Lithosphere): The majority of the Earth system.
ESS
Nebular Hypothesis: The Earth, the other 8 planets and the Sun accreted from a vast cloud of dust and gas (nebula).
1. Gravitational contraction (5 BYA) Rotates and flattens.
1. Solar fusion (4BYA) 2. Newly formed planets begin to
differentiate a) heavier elements and chemical
components sink to the center and rocky material formed the crust.
The Origin of the Earth
The Earth's interior is characterized by a gradual increase in temperature, pressure and density with depth.
At only 100 km depth, the temp is ~1300°C.
At the Earth's center, the temperature is >6700°C.
The pressure in the crust increases ~280 bars for every kilometer depth.
Earth's Internal Structure
The Earth consists of 3 major regions marked by differences in chemical composition.
Crust (Lithosphere): rigid outermost layer of the Earth. Consists of two types:
1. oceanic - 3-15 km thick and is composed of basalt (igneous). Young (<180 million years old).
2. continental - up to 70 km thick and composed of a wide variety of rock types (ave. granodiorite). Ranges from young to old (>3.8 billion years old).
Earth's Internal Structure
Mohorovicic Discontinuity The “slip surface” boundary between the crust and the mantle.
Mantle: comprises ~82% of the Earth by volume and is ~2900 km thick.
• Change in composition occurs.
• Asthenosphere is the soft, solid but “ductile” region just below the lithosphere.
• The mantle is able to flow (plasticity) at very slow rates.
Earth's Internal Structure
Core: composed of iron, nickel and other minor elements. • Outer core is liquid, capable of flow and source of the Earth's magnetic field.• Inner core is solid Fe-Ni. There is no major chemical difference between the outer and inner core.
Earth's Internal Structure