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Seismic Waves
Seismic Waves

... Earthquakes are movements or vibrations in the Earth. They are caused the release of stored energy in earth's outer layer. There is also an instrument that detects, measures, and records the energy of an earthquake.This is called a seismograph, and it produces seismograms. Pressure within the earth ...
476356_6341777079800..
476356_6341777079800..

... It's very stiff, and fractures if you push too hard The outer 75 km (with big variations between 10 and 300km) of the earth is a region which does not get heated up to near-melting because it is losing heat rapidly to the surface - it is stuck at a temperature close to 0°C. This relatively cool shel ...
Layers of Earth Notes On-Level
Layers of Earth Notes On-Level

... LAYERS OF THE EARTH • GEOLOGY – STUDY OF PLANET EARTH • INCLUDING SURFACE & INTERIOR • GEOLOGISTS – A PERSON WHO STUDIES INSIDE THE EARTH, TEMP, PRESSURE, HOW THEY AFFECT THE SURFACE OF THE EARTH. ...
Document
Document

... • This plate motion causes them to __________, ______ _______, or __________ against each other. • Each type of interaction causes a characteristic set of Earth structures or “tectonic” features. • The word, tectonic, refers to the ___________ of the crust as a consequence of plate interaction. ...
117 Ways to Pass the Earth Science Regents
117 Ways to Pass the Earth Science Regents

... 52. Capillarity increases when particle size decreases. ...
The Ocean Takes Shape
The Ocean Takes Shape

... 4. Students confuse the enhanced greenhouse effect with issues regarding the ozone hole. The enhanced greenhouse effect and ozone hole are often discussed simultaneously, and therefore, students incorrectly think that these two result in global climate change. In fact, the two phenomena are not clos ...
February 2015
February 2015

... made of rock, the crust is covered with dirt and water. The oceans and continents are located on the crust. The mantle is divided into two sections, the upper mantle pairs with the crust, forming the lithosphere. This is broken into plates, which is our next area of study. The lower mantle, also cal ...
The Earth’s Interior
The Earth’s Interior

...  The continental crust is the portion of Earth's crust that makes up the continents. ...
Layers of the Earth - Mrs. Rasmussen Science Class
Layers of the Earth - Mrs. Rasmussen Science Class

... mantle. The asthenosphere is about 180 km thick and much hotter than the crust (about 500 degrees Celsius). While it is technically still a solid, the rock in this layer is hot enough and under enough pressure that it flows like asphalt. A solid that can flow like this is called a plastic. Another e ...
Long term evolution of Earth`s magnetic field strength
Long term evolution of Earth`s magnetic field strength

... Here we present an approach that does not attempt to detect mean values, but accepts an inherent variability in the intensity of Earth’s magnetic field, especially on long time scales. Spectral analysis of all palaeointensity data and a quality-filtered dataset obtained from the palaeointensity data ...
Section: The Geosphere - Environmental Science
Section: The Geosphere - Environmental Science

... made of rock that flows very slow and allows tectonic plates to move on top of it. Beneath the asthenosphere is the mesosphere, the lower part of the mantle. The Earth’s outer core is a dense liquid layer. At the center of the Earth is the dense, solid inner core, which is made up mostly of the meta ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... Distance below surface: 6,370km Thickness: Thickest layer Because of it’s density ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... Distance below surface: 6,370km Thickness: Thickest layer Because of it’s density ...
Plate Tectonics - ESL Consulting Services
Plate Tectonics - ESL Consulting Services

... subducted plate, and rises toward the surface because it is less dense than the surrounding rock. The “Ring of Fire” around the Pacific Ocean is caused by this melting at subduction zones all around the Pacific. ...
Chapter One
Chapter One

... It's very stiff, and fractures if you push too hard The outer 75 km (with big variations between 10 and 300km) of the earth is a region which does not get heated up to near-melting because it is losing heat rapidly to the surface - it is stuck at a temperature close to 0°C. This relatively cool shel ...
Geography 1
Geography 1

... The squiggly lines show the rivers that flow from the mountain. In which town will the potential hazard for a lahar be greatest? -The town of Timberland (two rivers meet) followed by Tinytown (proximity). ...
What have earthquakes to do with the Earth`s climate?
What have earthquakes to do with the Earth`s climate?

... The cycle begins with volcanoes releasing carbon dioxide into the air.  As we all know, carbon dioxide as a major greenhouse gas keeps the Earth warm (otherwise, the Earth’s temperature will drop from an average of about 15 degrees Celsius to a staggering ­18 degrees Celsius!).  This warmth encourag ...
KEY for Tectonics Study Guide #1
KEY for Tectonics Study Guide #1

... continents or in the center of oceans instead of randomly. (They also showed that part of Earth’s core is liquid.) -GPS: showed not all mountains are growing taller. Goal 2: Describe Alfred Wegener’s Theory of Continental Drift. Explain the evidence he used to support his theory and tell why it was ...
Development of geological processes on the Earth and their impact
Development of geological processes on the Earth and their impact

... So, from ~2.35 Ga the tectonomagmatic processes started to involve previously absent geochemicalenriched material. Where this material stored and how it was activated? The established succession of events could be provided only by combination of two independent factors: (1) the Earth originally was ...
Handout
Handout

... gases (labeled as other gases on the diagram). Trace gases consist of compounds like carbon dioxide (CO2) and methane (CH4). Although trace gases are present in very small amounts, they play important roles in climate warming because they tend to absorb and reflect back to the surface long-wave radi ...
Chapter205.ppt
Chapter205.ppt

... gases (labeled as other gases on the diagram). Trace gases consist of compounds like carbon dioxide (CO2) and methane (CH4). Although trace gases are present in very small amounts, they play important roles in climate warming because they tend to absorb and reflect back to the surface long-wave radi ...
Earths Layers
Earths Layers

... mantle directly beneath the lithosphere – Due to heat and pressure ...
A Core Sample of Planet Earth I
A Core Sample of Planet Earth I

... 6. Use pages 391-392 in your book to put a very brief description of the composition/structure of each layer. Write words or phrases (not sentences). Include whether it is mostly rock or metal, the state of matter, and other important qualities (such as “rigid” for lithosphere and “weak, soft, flow ...
Earth
Earth

... Distance from the Sun where water is liquid as long as atmospheric pressure is high enough to stabilize it. ...
Earth`s Interior
Earth`s Interior

... materials like iron sank to center, while less-dense minerals rose toward surface. ...
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