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Evidence for Continental Drift
Evidence for Continental Drift

... Name ...
Science 4th Unit 2 4-ESS2-2
Science 4th Unit 2 4-ESS2-2

final exam study guide KEY
final exam study guide KEY

... size, small, taste, acidity, magnetism, density….  Which properties are good for identifying minerals? Which properties are not as useful? Hardness and density are good properties but they are more specific measurements. Color is not useful because a mineral can come in a variety of colors AND many ...
Earth`sInterior
Earth`sInterior

... • If Earth were made of the same materials throughout, seismic waves (energy released from earthquakes) would travel in straight lines at a constant speed. • However, seismic waves speed up and refract (bend) when they reach the mantle as it is more dense (due to increased pressure). • Scientists ca ...
Plate Tectonics - Down To Earth Science
Plate Tectonics - Down To Earth Science

...  If a more dense oceanic plate slides under a less dense continental plate or another oceanic plate, there is a subduction zone, and some crust is destroyed  If two continental plates converge, both plates buckle and push up into mountain ranges ...
1 - TeacherWeb
1 - TeacherWeb

... 12. The scientist who proposed the Theory of Continental Drift was a. James Hutton. c. Charles Lyell. b. Alfred Wegener. d. Charles Darwin. 13. A plate boundary at which two plates slide past each other horizontally is a a. divergent boundary. c. convergent boundary. b. transform boundary. d. subdu ...
6.3 Notes Deforming the Earth’s Crust
6.3 Notes Deforming the Earth’s Crust

... 6.3 Notes Deforming the Earth’s Crust ...
Answers to Spring Final Review
Answers to Spring Final Review

... rises, cools and any water in it condenses and falls as rain (the windward side is usually cool and damp). As the air sinks down the other side (leeward side) it warms and can hold more water so the weather is usually clear and dry. ...
File
File

... (if planet’s gravity is strong enough, it pulls the gases in & keeps them near surface) • Venus, Earth, Mars had gravity strong enough to hold heavy gases such as CO2. (Mars/Venus are mostly CO2) • Atmosphere moves from warmer places to cooler places. Keeps planet surface warmer & stable between day ...
lecture notes
lecture notes

...  Seismicity is the frequency. Magnitude, and distribution of earthquakes  Earthquakes are concentrated along oceanic ridges, transform faults, trences and island arcs  Tectonism refers to the deformation of Earth’s crust  Benioff Zone is an area of increasingly deeper seismic activity, inclined ...
CHapter 14 APES Test
CHapter 14 APES Test

... d. valuable deposits are found nearly everywhere. ...
Notes: The Theory of Plate Tectonics
Notes: The Theory of Plate Tectonics

...  Wegener said that when ___________ ___________, ___________ ranges formed  When ___________ separated or ___________, ocean __________ formed.  Continental Drift Theory provided answers to some big mysteries. Like…  The apparent ______________ fit of the ____________. This had been noticed sinc ...
Plate Tectonics
Plate Tectonics

... The main features of plate tectonics are: •The Earth's crust is broken into a series of plates or pieces. •The ocean floors are continually, moving, spreading from the center, sinking at the edges, and being regenerated. •Convection currents beneath the plates move the crustal plates in different ...
Chapter 7
Chapter 7

... 3. Ophiolite suite - Piece of descending oceanic plate that was scraped off and incorporated into the accretionary wedge. Contains: – Deep-sea sediments – Submarine basalts (pillow lavas) – Metamorphosed mantle rocks (serpentinized peridotite) 4. Blueschists – metamorphic minerals (glaucophane and l ...
Earthquakes
Earthquakes

... Earthquakes Why do earthquakes happen? Two of the crusts plates rub against each other and stick in one place. Pressure builds up as they try and move past each other. Suddenly, the pressure is too much and the plates jerk past each other. The place where this happens is called the focus. Vibrations ...
IGNEOUS ACTIVITY AND ROCKS
IGNEOUS ACTIVITY AND ROCKS

... – no quartz, abundant ferromagnesian minerals – Dark colored Andesite- intermediate INTRUSIVE STRUCTURES Bodies that solidified underground Volcanic neck- shallow intrusion Fills cracks- tabular bodies – DIKE• If no layering in country rock • If country rock is layered- Discordant – Sill- less commo ...
Plate Tectonics
Plate Tectonics

... • Plate tectonics – theory that earth’s crust is made of plates that move driven by convection currents in the asthenosphere and sea floor spreading. ...
Unit 4 Overview, Obduction
Unit 4 Overview, Obduction

... As time goes by, the soft layers get eroded and the hard layers form the ridges. GEOSC 10 - Geology of the National Parks ...
CompositionoftheEarth
CompositionoftheEarth

... Earthquakes occur at ​transform ​plate boundaries. They can happen elsewhere, but that is fairly rare. The spot where an earthquake starts is called the ​epicenter​. Earthquakes form when jagged rocks get caught on one another causing ​pressure/stress​ to build until the rocks ​break​ and move sudde ...
Earth System Science: The Big Ideas
Earth System Science: The Big Ideas

... Big Ideas plate tectonics • the way by which the plates of the Earth’s crust move and interact with one another at their boundaries. ...
Week 21: Plate Tectonics
Week 21: Plate Tectonics

... Spreading theories led to the current Plate Tectonic Theory a. If new ocean floor is being created at the Mid-Ocean Ridges as Harry Hess suggested, and the Earth isn’t getting any larger, then somewhere in the world old ocean crust must be getting destroyed  SUBDUCTION. b. The mid-ocean ridges are ...
Metamorphism and Metamorphic Rocks
Metamorphism and Metamorphic Rocks

... •Those metamorphic rocks that lack foliation are referred to as nonfoliated •Develop in environments where deformation is minimal •Typically composed of minerals that exhibit equidimensional crystals •Porphyroblastic textures •Large grains, called porphyroblasts, surrounded by a fine-grained matrix ...
divergent boundaries - Thomas C. Cario Middle School
divergent boundaries - Thomas C. Cario Middle School

... 1. Oceanic-Continental When a continental plate collides with an oceanic plate, the less dense plate will continue on its course while the denser plate will sink under the continental plate and into the . As the descending plate increases in depth, the heat generated causes partial melting of the ma ...
1 Section 4.4 - Sea- Floor Spreading Directions
1 Section 4.4 - Sea- Floor Spreading Directions

... process by which ocean floor gets pushed back into the mantle 51) What happens at deep ocean trenches? Subduction occurs here -- process by which ocean floor gets pushed back into the mantle; Acts like a giant conveyor belt 52) Where are the youngest rocks in the ocean floor found? Why? At the mid-o ...
power point notes
power point notes

... Mauna Loa, comprising over half of the Big Island, is the largest shield volcano on the planet. The measurement from the base locally depressing the sea floor in the Hawaiian Trough to its peak is about 17 km Sea Level to peak of Everest is 8,848 (56,000 feet) meters (29,028 feet) ...
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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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