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Name: Earth Space Spiraling Questions Earth`s Structure 1. The
Name: Earth Space Spiraling Questions Earth`s Structure 1. The

... b. Inner core and lithosphere c. Core and mantle d. Crust and outer core 6. Deforestation occurs when large areas of trees are cut down. Which of the following ...
Study Guide Chapt 7: Solid Earth
Study Guide Chapt 7: Solid Earth

... Crust Continental (20 -40 km thick mostly of granite type rock) , and Oceanic (~10 km thick basalt type rock) Since Basalt is more dense on average than granite ocean plates tend to move below continental plates when there is a collision. Because of this rocks in oceanic crust are not very old relat ...
Study Guide Chapt 7
Study Guide Chapt 7

... Crust Continental (20 -40 km thick mostly of granite type rock) , and Oceanic (~10 km thick basalt type rock) Since Basalt is more dense on average than granite ocean plates tend to move below continental plates when there is a collision. Because of this rocks in oceanic crust are not very old relat ...
Brain POP - Volcano
Brain POP - Volcano

Plate tectonics, earthquakes, and volcanoes 1. Hypothesis that
Plate tectonics, earthquakes, and volcanoes 1. Hypothesis that

... 1. Hypothesis that states that the continents have moved around the earth into their present positions. 2. The boundary between two tectonics plates that are moving away from each other. 3. The driving force in plate tectonics in which lava from the mantle rises to the lithosphere, moves horizontall ...
Geography 12
Geography 12

... (continents) moving apart from each other? He looked at the shape of the continents and concluded that because they look like the fit together they must have drifted apart. Later, scientists theorized thatThe supercontinent acted as a thermal cap, allowing thermal activity to increase under the supe ...
Geomorphology Final Exam Study Guide
Geomorphology Final Exam Study Guide

... Within the Basin and Range Province, the Earth’s crust has been stretched up to 100% of its original width. The entire region has been subjected to extension that Thinned and cracked the crust as it was pulled apart. ...
The History of Life
The History of Life

... method used to determine the age of rocks by comparing them with those in other layers. ...
How the Continents Move (910L)
How the Continents Move (910L)

... would fit together like pieces of a jigsaw puzzle? Back in 1620, Sir Francis Bacon thought so. Off and on ever since, there have been scientists who believed all the continents were once part of a single, big land mass that split apart. Mostly these scientists were laughed at--until about twenty-fiv ...
Chapter 4: Origin and Evolution of Igneous Rocks
Chapter 4: Origin and Evolution of Igneous Rocks

... Evolution of Igneous Rocks • Magmas change over time. • Chemistry of the magma changes as crystals form. • Mineralogy changes as crystals react with magma. • Crystals settle out or separate from the magma (fractionation). • Magma mixes with other magmas. • Magma incorporates wall rock (assimilation ...
Study Guide: Academic Standard 8-3 Earth`s Structure and Processes
Study Guide: Academic Standard 8-3 Earth`s Structure and Processes

... Igneous: Forms when molten rock cools and hardens. If cooling takes place slowly beneath Earth’s surface, the igneous rock is called intrusive and the mineral crystals that form are large. If cooling takes place rapidly on Earth’s surface, the igneous rock is extrusive and the mineral crystals are s ...
1st Semester Study Guide
1st Semester Study Guide

... pressure of a metamorphic rock or the melting of igneous rock would ______________________ them. Most fossils are found when living things are buried by sediment. The sediment ______________________________________________________________ _____________________________________________________________ ...
PRESENTSS
PRESENTSS

... Deriving its name from the Greek word asthenos (without strength) and contained entirely in the upper mantle is the asthenosphere. This zone is known as a plastic zone because of the sometimes semi-solid nature of its materials. The asthenospheres lack of rigidity is because the temperature is so cl ...
Layers of the Earth Vocabulary
Layers of the Earth Vocabulary

... The transfer of heat by movements of fluids The layer of rock that forms Earth’s surface The movement of energy from a warmer object to a cooler object A dense sphere of solid iron and nickel in the center of the Earth A rigid layer made up of the uppermost part of the mantle and the crust The molte ...
Layers of the Earth Vocabulary
Layers of the Earth Vocabulary

... The transfer of heat by movements of fluids The layer of rock that forms Earth’s surface The movement of energy from a warmer object to a cooler object A dense sphere of solid iron and nickel in the center of the Earth A rigid layer made up of the uppermost part of the mantle and the crust The molte ...
Chapter Test A The Dynamic Earth
Chapter Test A The Dynamic Earth

The Earth - Cardinal Newman High School
The Earth - Cardinal Newman High School

... Interior ...
Chapter 5 Notes: Plate Tectonics  Earth’s Interior Direct
Chapter 5 Notes: Plate Tectonics Earth’s Interior Direct

... o Plates: a section of the lithosphere that slowly moves over the Asthenosphere carrying pieces of the continental and oceanic crust  Combined continental drift and sea floor spreading into a scientific theory o Scientific Theory: well tested concept that explains a wide range of observations  Ide ...
The Story of the Wissahickon Rocks Tienne Moriniere
The Story of the Wissahickon Rocks Tienne Moriniere

... American, Pacific, African, Eurasian, Australian-Indian, and Antarctic. These plates rest on a region in the mantle known as the asthenosphere. The asthenosphere is composed of rocks that are near their melting temperature. The result is a very weak zone that allows the lithosphere to detach from th ...
Sixth Grade Science Standards
Sixth Grade Science Standards

... climate and weather. Elements: a. Demonstrate that land and water absorb and lose heat at different rates and explain the resulting effects on weather patterns. b. Relate unequal heating of land and water surfaces to form large global wind systems and weather events such as tornados and thunderstorm ...
Lab: Metamorphism: minerals, rocks and plate tectonics!
Lab: Metamorphism: minerals, rocks and plate tectonics!

... (1) Protoliths that are rich in aluminum and potassium. Possible protoliths include clay-rich sedimentary rocks such as shale and siltstone, and some felsic volcanic rocks. Metamorphic rocks formed from these rock types tend to contain abundant biotite and muscovite. They also contain one or more of ...
Fieldex receives drill permit and commences drilling program on the
Fieldex receives drill permit and commences drilling program on the

... One grab sample notably recovered 2.5% Cu, 14.0 g/t Ag and 0.5g/t Au. Each north-east line of the cut–lines grid was only 600 metres in length and did not cover the property entirely. However, the IP survey exhibits a strong chargeability anomaly over a length of 1.4 kilometres and a width varying b ...
Igneous Rocks - Mrs. GM Earth Science 300
Igneous Rocks - Mrs. GM Earth Science 300

...  Extrusive – made when magma flows on the earth's surface.  Intrusive - produced when magma solidifies deep beneath the earth. How do they form?  Extrusive rocks cool faster than intrusive. Some rocks are shot into the air and cool pretty fast, others into waterways (also fast cooling).  Some ro ...
metamorphic rock reading and questions
metamorphic rock reading and questions

... Every metamorphic rock is a rock that has changed its form. In fact, the word metamorphic comes from the Greek words meta, meaning “change,” and morphosis, meaning “form.” But what causes a rock to change into metamorphic rock? The answer lies inside Earth. Heat and pressure deep beneath Earth’s su ...
Section 1 - Pelham City Schools
Section 1 - Pelham City Schools

... ________________________, & living things AIR that interact with each other • Divided WATER into 4 parts: LIVING THINGS ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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