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Metamorphism
Metamorphism

... metamorphism at high pressures and temperatures. During the metamorphic transition, the augite (pyroxene), plagioclase and olivine in the basalt is transformed into garnet (red), omphacite (green) and clinozoisite (white). A densification of the rock from a density of about 2.9 g/cm3 to about 3.5 g/ ...
Earth and Environmental Science Final Exam Prep
Earth and Environmental Science Final Exam Prep

... 5. What is the difference between porosity and permeability? Porosity refers to the amount of space between individual soil particles (the more space, the more open pores and the higher the porosity); Permeability refers to how well water flows through the soil (the more pore space/higher porosity, ...
Ms. Destin Earth /Space Science Lesson Plans
Ms. Destin Earth /Space Science Lesson Plans

... Bell Ringer: Describe one way in which the biosphere and atmosphere interact. Teacher: Introduce layers of the Earth with power point. Teacher/students: Hypothesize which sodas will be more dense. Test. Students: 1. Produce a tree map from power point notes. Provide a written explanation of thinking ...
phase_4_ip_for_sci101
phase_4_ip_for_sci101

... The magnetized minerals also show the direction to the Earth’s magnetic poles and provide a means of determining their latitude of origin. Polar wandering, which is the apparent movement of the magnetic poles illustrated in rocks, indicates that continents have moved. This is shown in polar wanderin ...
Making Oceans and Continents
Making Oceans and Continents

... Seafloor spreading occurs along relatively narrow zones, called rift zones, located at the crests of ocean ridges called Mid-Ocean Ridges (MOR’s). These are above hot rising mantle. As plates pulled apart, cracks allow low pressure and water to hit mantle. Causes partial melting. Magma moves into fr ...
Happy Valentine`s Day!
Happy Valentine`s Day!

... K migrate into the melt, while Mg and Fe stay put. The magma rises, preferentially separating out these elements. Additionally, minerals with lots of Mg and little Si crystallize out first, the second step in the mantle’s Mg loss prevention program ...
Geo Time Vocab
Geo Time Vocab

... characteristic; several hundred million years period = subdivision of an era epoch = subdivision of a period trilobite = extinct marine arthropod that occurred abundantly during the Paleozoic era, with a carapace over the forepart, and a segmented hind part ...
EARTH AS A PLANET
EARTH AS A PLANET

... and other pre-biological molecules from primitive Earth atmosphere - mainly CO2 (No O2). ...
Geol 101: Physical Geology Spring 2002
Geol 101: Physical Geology Spring 2002

... 43. The most volcanically active body in the solar system is: A. Earth B. Triton C. the Moon D. Io E. Mars 44. Which of the following statements accurately accounts for why there were no advanced life forms on Earth early in its geologic history? A. initially the atmosphere contained mostly water va ...
12.2 PPT - gessramsey
12.2 PPT - gessramsey

... C. Continental-continental plate convergence  Since both are continental plates, their densities are similar.  As they collide, their edges fold and crumple, forming mountain ranges.  The Himalayas are the world’s youngest (and tallest) mountain range, formed as Asia and Africa plates collided 4 ...
12.2 PPT
12.2 PPT

... C. Continental-continental plate convergence  Since both are continental plates, their densities are similar.  As they collide, their edges fold and crumple, forming mountain ranges.  The Himalayas are the world’s youngest (and tallest) mountain range, formed as Asia and Africa plates collided 4 ...
2 Precambrian Geology
2 Precambrian Geology

... •4 bya: mostly deep water clastic deposits such as mudstones and muddy sandstones. –high concentration of eroded volcanic minerals (Sandstones called Graywackes). ...
Activity: A Plate Tectonic Puzzle - American Museum of Natural History
Activity: A Plate Tectonic Puzzle - American Museum of Natural History

... Activity: A Plate Tectonic Puzzle Introduction The Earth’s crust is not a solid shell. It is made up of thick, interconnecting pieces called tectonic plates that fit together like a puzzle. They move atop the underlying mantle, a really thick layer of hot flowing rock. By examining evidence such as ...
Chapter 2: The Earth
Chapter 2: The Earth

... The total amount of water on Earth doesn’t change, however, the Earth’s water is constantly moving– from the oceans to the air, to the ground and finally back to the oceans, this is known as the Water Cycle. The sun drives the cycle by evaporating water from Earth’s surface. Evaporation is the chang ...
Anyone who has attended elementary school knows Earth is layered
Anyone who has attended elementary school knows Earth is layered

... Sometimes compared to the skin of an apple or peach, Earths’ crust is the thinnest layer. It is composed of two types of crustal material; continental and oceanic. Landmasses are composed predominately of continental crustal material, while oceanic crust is the material that typically makes up the f ...
Layering in the wall rock of Valles Marineris: intrusive and extrusive
Layering in the wall rock of Valles Marineris: intrusive and extrusive

... and those that occur in mafic layered intrusions such as the Stillwater complex in the Western United States which exhibit similar mineralogic trends and may have formed in an analogous manner [Raedeke and McCallum, 1980]. [12] Large intrusions of basaltic magma within the Earth’s crust are known to ...
Species and Areas: History of Ideas Earth History: Plate Tectonics
Species and Areas: History of Ideas Earth History: Plate Tectonics

... west and east. Rock dating indicated that the youngest rocks were in the middle and got progressively older going both west and east ...
Species and Areas: History of Ideas
Species and Areas: History of Ideas

... The concept of plate tectonics explains the movements of the continents. The earth’s crust is divided into 7 major and a number of smaller plates. The plates are rigid and contain areas of continental crust. ...
Mid-Ocean Ridges
Mid-Ocean Ridges

... Magma plumes develop into volcanoes that can build up and eventually become a volcanic island or mountain. Hot spots occur far from plate boundaries, yet tell us how fast and in what directions plates are moving. The Hawaiian Islands and Yellowstone are examples of hot spot ...
Continental Drift
Continental Drift

... Numbers represent average rates of relative movement, cm/yr ...
Volcano - Simpson
Volcano - Simpson

... Steam also comes out. ...
9-28 Plate Tectonics1.notebook
9-28 Plate Tectonics1.notebook

... • Plate boundaries extend deep into the lithosphere. • There are 3 kinds of plate boundaries. ...
PLATE TECTONICS AND SEA-FLOOR SPREADING REVIEW
PLATE TECTONICS AND SEA-FLOOR SPREADING REVIEW

... CREATING MOUNTAINS (EX: HIMALAYAS CREATED BY INDIA COLLING WITH ASIA) 9. ___SUBDUCTION___ occurs when old oceanic crust is forced back into the mantle. 10. Where is new oceanic crust being formed? __AT MID OCEAN RIDGES (SEA- FLOOR SPREADING)_____ ...
Chapter 13 Notes Worksheet
Chapter 13 Notes Worksheet

... What are the continents made out of? Why is that important? ...
When drilling stopped in 1994, the hole was over seven miles deep
When drilling stopped in 1994, the hole was over seven miles deep

... brought on by intense heat and pressure, or metamorphic rock. Even more surprisingly, this deep rock was found to be saturated in water which filled the cracks. Because free water should not be found at those depths, scientists theorize that the water is comprised of hydrogen and oxygen atoms which ...
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Geology



Geology (from the Greek γῆ, gē, i.e. ""earth"" and -λoγία, -logia, i.e. ""study of, discourse"") is an earth science comprising the study of solid Earth, the rocks of which it is composed, and the processes by which they change. Geology can also refer generally to the study of the solid features of any celestial body (such as the geology of the Moon or Mars).Geology gives insight into the history of the Earth by providing the primary evidence for plate tectonics, the evolutionary history of life, and past climates. Geology is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources, understanding of natural hazards, the remediation of environmental problems, and for providing insights into past climate change. Geology also plays a role in geotechnical engineering and is a major academic discipline.
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