Inside the Earth
... earth. They are caused by the release of stored energy in earths outer layer.This release of energy causes sudden shifts of rocks along faults ...
... earth. They are caused by the release of stored energy in earths outer layer.This release of energy causes sudden shifts of rocks along faults ...
Unit C: Earth Science Chapter 1: The Changing Earth Lesson 1
... Plate Tectonics 1. This is the theory of how continents move 2. The earth's surface is broken into about twenty sections or plates 3. Plates are large sections of the earth's surface made of the crust and the top rigid portion of the mantle 4. They fit together but keep changing because they are slo ...
... Plate Tectonics 1. This is the theory of how continents move 2. The earth's surface is broken into about twenty sections or plates 3. Plates are large sections of the earth's surface made of the crust and the top rigid portion of the mantle 4. They fit together but keep changing because they are slo ...
Key Terms/People Overview - DC Everest Website has moved!
... Isoline- a map line that connects points of equal/similar values. Time space convergence – As communication increases efficiency the distance between two places is effectively diminished. Gravity Model – Formula based on population and distance and how it effects interaction between two places. Geoi ...
... Isoline- a map line that connects points of equal/similar values. Time space convergence – As communication increases efficiency the distance between two places is effectively diminished. Gravity Model – Formula based on population and distance and how it effects interaction between two places. Geoi ...
Review for Earth Science Test
... It is the shaking that results from the movement of rock beneath Earth’s surface. 6. What is streak? It is the color of a mineral’s powder. 7. What is Mohs’ Hardness Scale? It is the scale used by scientists to classify minerals according to their hardness. 8. What is the rock cycle? It is a series ...
... It is the shaking that results from the movement of rock beneath Earth’s surface. 6. What is streak? It is the color of a mineral’s powder. 7. What is Mohs’ Hardness Scale? It is the scale used by scientists to classify minerals according to their hardness. 8. What is the rock cycle? It is a series ...
Earth Science SOL Review Facts Word document
... Contour lines form V's and point upstream of rivers and creeks. The altitude of Polaris (the north star) equals your Latitude. Mercator Maps take a round, 3 dimensional surface and places it on a 2 dimesional map. When this happens, the areas at the poles get distorted. ...
... Contour lines form V's and point upstream of rivers and creeks. The altitude of Polaris (the north star) equals your Latitude. Mercator Maps take a round, 3 dimensional surface and places it on a 2 dimesional map. When this happens, the areas at the poles get distorted. ...
The Layers of the EarthPowerPoint Fill-in-the
... The crust and the upper layer of the mantle _____________________ make up a zone of rigid, brittle rock called the __________________________. The crust is composed of two rocks. The continental crust is mostly _______________. The oceanic crust is ________________. Basalt is much _________________ ...
... The crust and the upper layer of the mantle _____________________ make up a zone of rigid, brittle rock called the __________________________. The crust is composed of two rocks. The continental crust is mostly _______________. The oceanic crust is ________________. Basalt is much _________________ ...
Why study geography?
... increase or decrease you clock by 1 hour for each time zone you cross when traveling. If you head West, you lose an hour for each time zone you cross. If you head East, you add an hour for each time zone you cross. Each zone you cross is called a Standard Time Zone. ...
... increase or decrease you clock by 1 hour for each time zone you cross when traveling. If you head West, you lose an hour for each time zone you cross. If you head East, you add an hour for each time zone you cross. Each zone you cross is called a Standard Time Zone. ...
Earth`s outer layer has moved.
... • Distinct properties define Earth’s three main layers: crust, mantle, and core. • The crust is the rigid outer layer that makes up the continents and sea floors. • The lithosphere is a region formed by the crust and the rigid outer layer of the mantle. • The asthenosphere is the fluid-like layer of ...
... • Distinct properties define Earth’s three main layers: crust, mantle, and core. • The crust is the rigid outer layer that makes up the continents and sea floors. • The lithosphere is a region formed by the crust and the rigid outer layer of the mantle. • The asthenosphere is the fluid-like layer of ...
Layers of Earth Notes
... • Made of solid nickel and iron • So hot it melts everything in the outer core • Spins at a speed faster than the Earth rotates • Densest layer of the Earth • Average temperature 5000o 6000o ...
... • Made of solid nickel and iron • So hot it melts everything in the outer core • Spins at a speed faster than the Earth rotates • Densest layer of the Earth • Average temperature 5000o 6000o ...
Ch 17 PP
... • Distinct properties define Earth’s three main layers: crust, mantle, and core. • The crust is the rigid outer layer that makes up the continents and sea floors. • The lithosphere is a region formed by the crust and the rigid outer layer of the mantle. • The asthenosphere is the fluid-like layer of ...
... • Distinct properties define Earth’s three main layers: crust, mantle, and core. • The crust is the rigid outer layer that makes up the continents and sea floors. • The lithosphere is a region formed by the crust and the rigid outer layer of the mantle. • The asthenosphere is the fluid-like layer of ...
Plate Tectonics - Arlington Public Schools
... *fossil, *inner core, lava, magma, *mantle, *outer core, • Humans have varying degrees of impact on Earth’s *iron, *nickel, *sliding boundary, also known as strike-slip surface through their everyday activities. With careful or transform boundary (slip past each other horizontally), planning, the im ...
... *fossil, *inner core, lava, magma, *mantle, *outer core, • Humans have varying degrees of impact on Earth’s *iron, *nickel, *sliding boundary, also known as strike-slip surface through their everyday activities. With careful or transform boundary (slip past each other horizontally), planning, the im ...
Plate Tectonics Jeopardy Game
... This is the boundary caused by plates moving past each other in opposite directions. ...
... This is the boundary caused by plates moving past each other in opposite directions. ...
Dynamic Planet Unit Test Study Guide (Answers)
... 4. List the Earth’s layers from the center to the surface. • Inner core, outer core, mantle, crust 5. What is the difference between the inner core and the outer core? The outer core is made of high-temperature liquid iron. The inner core is solid. 6. What can an earthquake on the sea floor produce? ...
... 4. List the Earth’s layers from the center to the surface. • Inner core, outer core, mantle, crust 5. What is the difference between the inner core and the outer core? The outer core is made of high-temperature liquid iron. The inner core is solid. 6. What can an earthquake on the sea floor produce? ...
Section 1 - WordPress.com
... • A magnetic compass can indicate direction because Earth has magnetic properties as if a powerful barshaped magnet were buried at Earth’s center at an angle to Earth’s axis of rotation. • The areas on Earth’s surface just above where the poles of the imaginary magnet would be are called the geomagn ...
... • A magnetic compass can indicate direction because Earth has magnetic properties as if a powerful barshaped magnet were buried at Earth’s center at an angle to Earth’s axis of rotation. • The areas on Earth’s surface just above where the poles of the imaginary magnet would be are called the geomagn ...
Chemistry Unit Test Study Guide
... 4. List the Earth’s layers from the center to the surface. Inner core, outer core, mantle, crust 5. What is the difference between the inner core and the outer core? The outer core is made of high-temperature liquid iron. The inner core is solid. 6. What can an earthquake on the sea floor produce? ...
... 4. List the Earth’s layers from the center to the surface. Inner core, outer core, mantle, crust 5. What is the difference between the inner core and the outer core? The outer core is made of high-temperature liquid iron. The inner core is solid. 6. What can an earthquake on the sea floor produce? ...
Crosby_LiDAR_edu_dis..
... Develop descriptions, explanations, predictions, and models using evidence; Think critically and logically (Grades 5-8); Design and conduct scientific investigations; Use technology to improve investigations; Scientists rely on technology to enhance gathering and manipulation of data (Grades 9-12). ...
... Develop descriptions, explanations, predictions, and models using evidence; Think critically and logically (Grades 5-8); Design and conduct scientific investigations; Use technology to improve investigations; Scientists rely on technology to enhance gathering and manipulation of data (Grades 9-12). ...
Golf
... A road cut reveals layers in the soil. Why does soil have layers? A. It has been sorted by particle size and density B. It is made from rock and other particles C. It was placed in layers by humans D. The layers have always been there ...
... A road cut reveals layers in the soil. Why does soil have layers? A. It has been sorted by particle size and density B. It is made from rock and other particles C. It was placed in layers by humans D. The layers have always been there ...
Golf
... A road cut reveals layers in the soil. Why does soil have layers? A. It has been sorted by particle size and density B. It is made from rock and other particles C. It was placed in layers by humans D. The layers have always been there ...
... A road cut reveals layers in the soil. Why does soil have layers? A. It has been sorted by particle size and density B. It is made from rock and other particles C. It was placed in layers by humans D. The layers have always been there ...
Slide 1
... Continental crust: The second smallest area of the Earth making up only 0.374% of the Earth's mass and extending a short depth of 0 - 31 miles (050 kilometers). Looking at the percent by composition, the continental crust makes up only 0.554% of the mantle-crust mass. The layer is composed primarily ...
... Continental crust: The second smallest area of the Earth making up only 0.374% of the Earth's mass and extending a short depth of 0 - 31 miles (050 kilometers). Looking at the percent by composition, the continental crust makes up only 0.554% of the mantle-crust mass. The layer is composed primarily ...
Take Home 12 Complete the following on your own paper. Do not
... the atmosphere in the early 1800’s. This gas and dust caused weather extremes, crop failure and major climatic change worldwide for over a year following the eruption. The link between these changes and the volcano’s eruption were not understood for years. What is this an example of? A. Understandin ...
... the atmosphere in the early 1800’s. This gas and dust caused weather extremes, crop failure and major climatic change worldwide for over a year following the eruption. The link between these changes and the volcano’s eruption were not understood for years. What is this an example of? A. Understandin ...
sxES_G6_RNG_ch04-A_070-073.fm
... This section explains sea-floor spreading and describes evidence supporting its occurrence. The section also explains subduction and describes how subduction affects Earth’s oceans. ...
... This section explains sea-floor spreading and describes evidence supporting its occurrence. The section also explains subduction and describes how subduction affects Earth’s oceans. ...
Structure of the Earth
... Around the Outer Core is the Mantle The Mantle is divided into two major layers, the Lower and Upper Mantle The Lower Mantle is made of solid rock, but very high pressure inside the Earth makes it act like a liquid. The Mantle goes from 65- 2890 km below ground ...
... Around the Outer Core is the Mantle The Mantle is divided into two major layers, the Lower and Upper Mantle The Lower Mantle is made of solid rock, but very high pressure inside the Earth makes it act like a liquid. The Mantle goes from 65- 2890 km below ground ...
The Earth
... •Sunlight not reflected by clouds reaches the Earths surface (about 50%) •The heated earth re-radiates this light in the form of infrared radiation •Infrared light is partially blocked by the Earth’s carbon dioxide (and water vapor) •So, only part of the IR light goes into space, part goes back to e ...
... •Sunlight not reflected by clouds reaches the Earths surface (about 50%) •The heated earth re-radiates this light in the form of infrared radiation •Infrared light is partially blocked by the Earth’s carbon dioxide (and water vapor) •So, only part of the IR light goes into space, part goes back to e ...
EARTH AS A PLANET
... up CO2 and produce O2 - photosynthesis. O2 in atmosphere 2 billion years ago. ...
... up CO2 and produce O2 - photosynthesis. O2 in atmosphere 2 billion years ago. ...
Spherical Earth
The concept of a spherical Earth dates back to around the 6th century BC, when it was mentioned in ancient Greek philosophy, but remained a matter of philosophical speculation until the 3rd century BC, when Hellenistic astronomy established the spherical shape of the earth as a physical given. The paradigm was gradually adopted throughout the Old World during Late Antiquity and the Middle Ages. A practical demonstration of Earth's sphericity was achieved by Ferdinand Magellan and Juan Sebastián Elcano's expedition's circumnavigation (1519−1522).The concept of a spherical Earth displaced earlier beliefs in a flat Earth: In early Mesopotamian mythology, the world was portrayed as a flat disk floating in the ocean and surrounded by a spherical sky, and this forms the premise for early world maps like those of Anaximander and Hecataeus of Miletus. Other speculations on the shape of Earth include a seven-layered ziggurat or cosmic mountain, alluded to in the Avesta and ancient Persian writings (see seven climes).The realization that the figure of the Earth is more accurately described as an ellipsoid dates to the 18th century (Maupertuis).In the early 19th century, the flattening of the earth ellipsoid was determined to be of the order of 1/300 (Delambre, Everest). The modern value as determined by the US DoD World Geodetic System since the 1960s is close to 1/298.25.