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The Mantle
The Mantle

... 2. Fossils of the same species found on different continents 3. Mountains chains, like the Appalachians, begin on one continent and match up to another continent 4. Evidence of glaciers discovered on continents close to the equator ...
GEOLOGY CURRICULUM Unit 1: Introduction to Geology
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... ● Running water is the single most important agent sculpturing the earth’s land surface. ● Identify and describe the zones of erosion, transportation, and deposition in river systems. ● Discuss factors that impact the velocity of running water. ● Identify the depositional landforms and explain the p ...
Rocks and the Rock Cycle
Rocks and the Rock Cycle

... 3. The nucleus is tiny, so most of an atom is empty space!! 4. There is a good diagram of an atom's structure on page 30 of the text. E. Atomic number = the number of protons in an atom's nucleus. It is this number that dictates what element an atom is. F. Mass number - the number of protons and neu ...
section 12.2
section 12.2

... • The island of Hawaii sits on top of a hot spot. • The hot spot has formed the Mauna Loa and Kilauea volcanoes on the island. • Currently, the hot spot is making the undersea volcano Loihi to the A hot spot is making Loihi southeast of the island. bigger, so Hawaii is growing. ...
Key Ideas
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... The Earth’s Interior: Studies of seismic waves (vibrations produced by earthquakes) show that the Earth has a small, solid inner core surrounded by a liquid outer core. The outer core is surrounded by the dense mantle, which in turn is surrounded by the thin lowdensity crust. Seismologists deduce th ...
WGCh2NotetakingKey
WGCh2NotetakingKey

... 2. This type of freshwater comes from rain and snow that has filtered through the soil and rock and accumulated below the Earth’s surface. Some water from lakes and rivers may also become part of the groundwater. 3. People often dig wells and use springs that tap into this type of freshwater. ...
LEARNING FROM GLOBAL DISASTER LABORATORIES PART 8
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Document
Document

... Draw a profile of the velocity vectors parallel to the SAF. Define the Azimut of the Pa/NA plate motion in Los Angeles Region, What is the Azimut of The SAF ? What can you tell about the components of GPS velocity vectors perpendicular to the Pa/NA direction ? ...
slide1
slide1

... Are KT boundary chromites terrestrial or extra-terrestrial? Terrestrial isotopic signatures for Raton Basin KT boundary chrome spinels would also corroborate evidence for mantle or ultramafic material in KT boundary ejecta as proposed by:  DePaolo, Kyte, Marshall, O’Neil & Smit; EPSL Vol. 64, Sept. ...
Convection currents
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... The transfer of heat by the movement of a heated fluid is called convection. Fluids include liquids and gases. During convection, heated particles of a fluid begin to flow, transferring heat energy from on part of the fluid to another. Heat transfer by convection is caused by differences in temperat ...
6. A Pre-Assessment
6. A Pre-Assessment

... 5. How  are  volcanoes  formed?  Magma  reaches  the  surface  through  volcanic  structures.   Volcano  eruptions  can  be  of  various  types:  quiet  and  explosive.  Volcanoes  are  classified   by  how  they  are  formed  (quiet  or ...
Episodic Tremor and Slip The Cascadia Subduction Zone
Episodic Tremor and Slip The Cascadia Subduction Zone

... On Vancouver Island, episodes of deep slip are accompanied by seismic tremors that are recorded by the same network of seismographs used to measure earthquakes. Unlike an earthquake’s shockwaves, ETS tremors persist like background chatter for the duration of the event. These chattering tremors, com ...
Types of Rocks - Sikkimsprings
Types of Rocks - Sikkimsprings

...  We shall consider only the ones which have some bearing on ground water and its movement. ...
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... The large underground pool of molten rock lying immediately under the crust is known as the magma chamber. Temperatures in this area reach over 2500oF. ...
accepted manuscript
accepted manuscript

... The breakup of Pangaea in the Early Cretaceous led to the separation and drift of the South American and African continents. That event, called the Wealdenian Reactivation by Almeida (1967), created an ...
lithosphere_42344
lithosphere_42344

... 1) The high velocity of the lid can not be explained by temperature alone. This suggests a compositional component to the lithosphere and associated properties. Likely sources of compositional differences wrt the deeper mantle are: - depletion in volatiles - existence of an eclogite phase 2) The LVZ ...
Document
Document

... are large pyroclasts. When solid rock has been blasted apart by a volcanic explosion, the pyroclastic fragments are angular, with no rounded edges or corners and are called blocks. If lava is ejected into the air, a molten blob becomes streamlined during flight, solidifies, and falls to the ground a ...
Forces Within Earth
Forces Within Earth

... Identifying Tectonic Plate Movement • Plate tectonic theory, 1915 when Alfred Wegener "continental drift" • Coastlines look like they fit together like a puzzle ...
to Ch. 8 Notes
to Ch. 8 Notes

... - Seismic waves that travel along Earth’s outer layer - Shake particles at right angles to the direction that they travel - Travel only through solids - __________________velocity than P waves  A __________________shows all three types of seismic waves—surface waves, P waves, and S waves  Earthqua ...
Earthquakes - Science Learning Hub
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Formation of plate boundaries: The role of mantle volatilization
Formation of plate boundaries: The role of mantle volatilization

... which prevents subduction and leads to heating-up of the Earth's mantle and a shift back to a magma ocean (Sleep, 2000). In this paper, we present a scenario where H2O and CO2 play a role in the initiation of plate boundaries in the context of realistic tectonic situations. We propose that subductio ...
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c. Section 4.3 Seismology (powerpoint)

... • Each point represents vibrations that are 10 times greater than the point below it. • Each tenfold increase in vibrations means 30 times more energy released. ...
Unit Quiz - mariewatson
Unit Quiz - mariewatson

... 9. Why is soil in Egypt different from soil in Germany? ...
Milky-Way-Plate-Tectonics2
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The Ocean floor Foldable Notes
The Ocean floor Foldable Notes

... • Can occur in chains or ridges and often have an active volcanic island at one end. • Hawaiian Islands are the best example. ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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