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Crust - www .alexandria .k12 .mn .us
Crust - www .alexandria .k12 .mn .us

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Earth’s Interior PowerPoint - Marcia's Science Teaching
Earth’s Interior PowerPoint - Marcia's Science Teaching

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Plate Tectonics PowerPoint plate_tectonics_2011
Plate Tectonics PowerPoint plate_tectonics_2011

... – Thousands of layers of sedimentary rock provide evidence that allows us to determine the age of Earth’s changing surface and to estimate the age of fossils found in the rocks. (6-8 ES3B) – In most locations sedimentary rocks are in horizontal formations with the oldest layers on the bottom. Howeve ...
File
File

... plates ride on the asthenosphere like blocks of wood float on water ...
AP Chapter 8 - Madeira City Schools
AP Chapter 8 - Madeira City Schools

... 2. Fill in the chart below for the layers of the earth. Do your best given that several of the layers overlap. Layer ...
No Slide Title
No Slide Title

... “orbital” ...
Dynamic Earth
Dynamic Earth

... stripes of normal and reverse polarity at the mid-ocean ridge. ...
EarthTestReview_Coelho
EarthTestReview_Coelho

... Fossil fuels come from buried dead/decayed organisms changed by increased heat & pressure from rock layers (takes longer than a lifetime to MILLIONS of years to form) **If FF don’t have enough heat, pressure, & time then they won’t form** ...
What Is Inside Earth?
What Is Inside Earth?

... eologists are scientists who study Earth. They want to know about the materials that Earth is made of and how Earth has changed during its history. Geologists cannot drill deep enough to study Earth’s interior. The deepest well ever drilled is only about 12 kilometers (7.5 miles) deep. But the dista ...
Unit 2: Physical Geography  Study Guide for Test  Learning Targets:   
Unit 2: Physical Geography  Study Guide for Test  Learning Targets:   

... 3. Explain factors that affect the climate of an  area (including latitude, elevation, wind and  ocean currents, and landforms).  a. What is the climate of the  high­latitudes like? Why?  b. What is the climate of the low­latitude  like? Why?  c. What is the climate of the  mid­latitudes like? Why?  ...
Geology and Nonrenewable Minerals
Geology and Nonrenewable Minerals

... • The forces produced at these plate boundaries can cause earthquakes, erupting volcanoes and mountains to form. • Oceanic plates move apart from one another allowing magma, to flow up between them. • Much of the geologic activity at earth’s surface takes place at the boundaries between tectonic pla ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... area is known as a subduction zone. It forms when continental land masses collide with ocean plates, or when two ocean plates collide with each other. 4 Movement of the plates does not just cause trenches and ridges on the ocean floor. It can also form mountains on land. When two continental plates ...
CTY Course Syllabus: Dynamic Earth
CTY Course Syllabus: Dynamic Earth

... magnitude and intensity, scope of global plate movement, How global networks work together to monitor earthquakes, Law of Superposition, unconformities, nonconformities, using strata to identify formation of rocks in the lithosphere ...
Ch 7 study guide answers
Ch 7 study guide answers

... Core – (inner and outer) inner core has the most iron 7. List some evidence that proved continental drift did occur? Seafloor Spreading Magnetic Reversals 8. Earthquakes mainly are associated with what one boundary? Transform Plate Boundaries 9. Draw and label all the layers and sub layers of the Ea ...
Continental Drift and Plate Tectonics
Continental Drift and Plate Tectonics

... moving apart and new crust is created by magma pushing up from the mantle. The best known of the divergent boundaries is the Mid-Atlantic Ridge. This submerged mountain range, which extends from the Arctic Ocean to beyond the southern tip of Africa, is but one segment of the global mid-ocean ridge s ...
Document
Document

... The arrival of plate tectonics was a scientific revolution: Plate tectonic theory states that the Earth's surface is broken into rigid lithospheric plates that slide on top of asthenospheric mantle. The boundary between these lithosphere and asthenosphere is based on rheology (typically defined by ...
Volcanoes
Volcanoes

... D. Shield volcano 16. If geologist detect many small earthquakes in the area of a volcano what can they infer? ...
Chapter 5: Earthquakes and Volcanoes
Chapter 5: Earthquakes and Volcanoes

... When sudden energy is released from Earth’s crust breaking or moving which cause vibrations.  If the vibrations are large enough they are felt as earthquakes. ...
Geology and Nonrenewable Minerals
Geology and Nonrenewable Minerals

... • The forces produced at these plate boundaries can cause earthquakes, erupting volcanoes and mountains to form. • Oceanic plates move apart from one another allowing magma, to flow up between them. • Much of the geologic activity at earth’s surface takes place at the boundaries between tectonic pla ...
petrology of continental rocks
petrology of continental rocks

... billion years. If the erosion is restricted to the present area of land, the depth becomes 150 km. Clearly the erosion never reached such depths. The figure simply proves that extensive recycling must have taken place. During the geologic history of our globe a total mass perhaps many times that of ...
The Physical World
The Physical World

... Continental Drift- theory that the continents were once joined and have slowly drifted apart ...
Deforming the Earth`s Crust
Deforming the Earth`s Crust

... 2. Normal Fault = the hanging wall slides down the foot wall ...
Late - to post-orogenic tectonic processes and exhumation
Late - to post-orogenic tectonic processes and exhumation

... From late to post orogenic tectonics in continental collision zones to rifts The end of a Wilson cycle does not mark the end of the tectonic activity in a mountainbelt. In many orogenic belts high-grade rocks formed by the crustal-thickening during collision get quickly exhumed. In many instances t ...
Earth Science Regents Review
Earth Science Regents Review

... If the travel time of an S-wave is 9 minutes 40 seconds, what is the epicenter distance?______________ If the difference in arrival times of the P- and Swaves is 6 minutes 20 seconds, how far is the distance to the epicenter? ________________ A P-wave arrived at 3:32:00 p.m. and the S-wave arrived a ...
File 8th Grade Science Vocabulary Review GAME!.
File 8th Grade Science Vocabulary Review GAME!.

... A bond that results from the attraction between the nuclei of atoms where the electrons are shared by the atoms ...
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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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