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Section 4 Deforming the Earth`s Crust
Section 4 Deforming the Earth`s Crust

... is called compression. • When compression occurs at a convergent boundary, large mountain ranges can form. ...
Unit 2 Review (CH 8, 10,11,12,13)
Unit 2 Review (CH 8, 10,11,12,13)

... 10. Define  the  term  half  -­‐life  and  how  is  it  related  to  radiometric  dating?   11. How  many  half  lives  has  an  isotope  been  through  if  you  started  with  40  grams  of  radioactive   material  but  now  have   ...
phy226 tutorial kit - Covenant University
phy226 tutorial kit - Covenant University

... the mass of materials in each ring would be too small to provide the gravitational attraction needed to cause the rings to condense into a planet. Also, as the nebula contrasted the largest part of the angular momentum would remain associated with the main mass condensed to form the Sun. But this di ...
Earth Layers Review
Earth Layers Review

... The largest layer of Earth. It makes up 82% of Earth’s volume. ...
Plate Tectonics Notes # 2
Plate Tectonics Notes # 2

... like silly putty , bread dough, or HONEY . This zone was discovered because it was found that seismic waves decrease in velocity from 100km to 700km below the Earth’s surface. (Seismic waves travel more slowly through liquids than solids). It is a plastic-like portion of the upper mantle that is par ...
GY111 Earth Materials
GY111 Earth Materials

... • All regional metamorphic rocks contain a foliation- in low grade (Low T) rocks the grains are microscopic so you can’t “see” the foliation • Cleavage in rocks is the tendency to split along smooth planes. Rocks with microscopic foliation tend to have excellent rock cleavage ...
Plate Tectonics and Earth`s Structure
Plate Tectonics and Earth`s Structure

... type and age. • Mountain ranges line up across the two continents as if these two continents were once joined. • Coal formed from tropical plants is found in North America and Antarctica. This implies they were both much closer to the equator at one time. ...
plates - Wilson`s Web Page
plates - Wilson`s Web Page

Geology of Tarnagulla area
Geology of Tarnagulla area

... slipped down under the Gondwanaland continent. As it did so, the softer layers of sediment which were around 12 to 15 km thick and on top of hard layers of basalt, were jammed up against the hard Gondwanaland continent and started to crumple. Think of them as being like layers of wet paper on top of ...
what`s inside the earth?
what`s inside the earth?

... broken into pieces called plates. The plates are moving at a rate of an inch or two a year, in a variety of directions, driven by the movement of magma within the earth's mantle. Plate movement is responsible for mountain building, volcanic eruptions, and the occurrence of earthquakes. The video cle ...
Chapter 14
Chapter 14

... Dolomite Limestone Lignite Bituminous coal ...
Chapter 19 - Heritage Collegiate
Chapter 19 - Heritage Collegiate

... the force of gravity created by the moon moved the continents). This was quickly proven not to be possible. He then explained that the continents cut through the ocean crust much like an icebreaker, but no evidence was found showing the ocean crust deformed where a continent moved through it. By 196 ...
The Living Machine - Annenberg Learner
The Living Machine - Annenberg Learner

... WEGENER DIED IN GREENLAND, LOST IN THE FAR REACHES OF FROZEN WILDERNESS, BUT HIS VISION OF MOVING CONTINENTS WOULD HAUNT THE SCIENTIFIC WORLD UNTIL NEW DISCOVERIES AT THE BOTTOM OF THE SEA REVIVED HIS CHALLENGING IDEAS. ...
Helpful Landform Websites
Helpful Landform Websites

... http://www.onegeology.org/extra/kids/home.html One Geology Kids A great website to learn about earthquakes, volcanoes, Earth processes, and geology (rocks and minerals) http://www.conservation.ca.gov/cgs/information/kids_geozone/Pages/Index.aspx CA.Gov Department of Conservation Go to links : “Geolo ...
Earth`s interior - Rochester Community Schools
Earth`s interior - Rochester Community Schools

... Background: Scientists have learned about the physical structure of Earth’s interior by measuring seismic waves. Seismic waves are an example of traveling waves, or mechanical waves that travel through a medium. Sound waves are the most familiar example of traveling waves. The speed of sound within ...
MS1_PNT_Geologyppt_V01
MS1_PNT_Geologyppt_V01

... Divergent Boundaries  At a spreading, or divergent boundary, two plates are ...
Earth`s Structure
Earth`s Structure

... The Earth’s Core – Outer Core • The outer core is also made of nickel and iron, but the nickel and iron are liquids in the outer core. • This layer is liquid because the temperature is still very high, but the pressure is not as great as it is in the ...
Review for Earthquakes Test
Review for Earthquakes Test

... Lesson 19 & 20 – Volcanoes Change The Landscape/Viscosity and Volcano Type 1. What is the difference between magma and lava? Magma is molten rock within the mantle (below Earth’s surface), lava is molten rock that has reached Earth’s surface. 2. What is viscosity? The ability of a liquid to resist f ...
660 km
660 km

... • Ocean water 0.025% of mass • Crust (Above the Moho) 0.5% of mass – Oceanic (7 to 10 km of basalt & gabbro) – Continental (30 to 60 km of granite) ...
What is the Earth? It is our planet and the only inhabited. It is in the
What is the Earth? It is our planet and the only inhabited. It is in the

... 4,500,000,000 Precambrian Azoica ...
Plate Tectonics Webquest
Plate Tectonics Webquest

... 4. Give the name of the last large supercontinent that included all of the current continents. _____________ 5. During which geologic era were the northern continents joined in to Laurasia and the southern continents joined into Gondwanaland? _____________ 6. Until the 1700s, most Europeans thought ...
Plate tectonics: why only on Earth?
Plate tectonics: why only on Earth?

... ridges by volcanic processes. There is little doubt that the concept of plate tectonics describes how the Earth operates now and how it operated in the last few hundred million years. A more difficult question is, how far plate tectonics reaches back in Earth´s 4.6 billion years of history. There is ...
Van Allen radiation belt
Van Allen radiation belt

... You can use a spring scale to measure gravity. Notice that when this is hanging without moving, the spring is stretched by a certain amount. If the mass is pulled down, it causes the spring to stretch further. A machine called a gravimeter can be built based on this principle to measure Earth's gra ...
Seismic Waves Webquest - Dublin City Schools Dashboard
Seismic Waves Webquest - Dublin City Schools Dashboard

... 1.   Go   to     http://aspire.cosmic-­‐ray.org/Labs/SeismicWaves/       you   can   also   access   this   website  in  the  resources  section  of  this  lesson.     2.    Spend  1-­‐2  minutes  playing  with  the  Mighty  Wave  Make ...
File
File

... Monoclines – an area of smoothly folded strata above a fault that forms a single “step” ...
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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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