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Chapter_1_Section1
... 2. Destructive – forces that slowly wear away mountains and eventually every other feature on Earth’s surface Continents – 7 great landmasses surrounded by oceans Seismic Waves – the indirect evidence geologists use to study Earth's interior; created when earthquakes occur ...
... 2. Destructive – forces that slowly wear away mountains and eventually every other feature on Earth’s surface Continents – 7 great landmasses surrounded by oceans Seismic Waves – the indirect evidence geologists use to study Earth's interior; created when earthquakes occur ...
Closer to Poles (c)
... Air cools with altitude, clouds form and precipitation occurs (windward side) Dry air mass moves down opposite leeward side of mountain ...
... Air cools with altitude, clouds form and precipitation occurs (windward side) Dry air mass moves down opposite leeward side of mountain ...
Science Notes December 1, 2010 SOL 5.7 (b, c, d) Scientists are
... Convergent Boundaries – Occur when plates push together; cause mountain ranges to rise up from the Earth’s surface (example - Appalachian Mountains); however, deep in the Earth’s oceans, these boundaries force plates downward instead of upward and deep trenches are formed. Divergent Boundaries – ...
... Convergent Boundaries – Occur when plates push together; cause mountain ranges to rise up from the Earth’s surface (example - Appalachian Mountains); however, deep in the Earth’s oceans, these boundaries force plates downward instead of upward and deep trenches are formed. Divergent Boundaries – ...
Planet Earth/Atmosphere Name Learning Targets Period _____
... 12. Describe the evidence for plate tectonics, the different type of plate boundaries, and relate them to volcanoes and earthquakes. 13. Define an earthquake, the three types of seismic waves, and find the epicenter of an earthquake. 14. Describe and label the layers of the atmosphere. 15. Describe ...
... 12. Describe the evidence for plate tectonics, the different type of plate boundaries, and relate them to volcanoes and earthquakes. 13. Define an earthquake, the three types of seismic waves, and find the epicenter of an earthquake. 14. Describe and label the layers of the atmosphere. 15. Describe ...
Our Changing Earth Resource Page
... Sometimes when the plates move, they can either collide or bump into each other or one can slide under the other. These are called convergent boundaries. Sliding under one another is called subduction, and often results in volcanoes. If the crusts collide, mountains can be formed. ...
... Sometimes when the plates move, they can either collide or bump into each other or one can slide under the other. These are called convergent boundaries. Sliding under one another is called subduction, and often results in volcanoes. If the crusts collide, mountains can be formed. ...
The Earth
... Evolution of the Solid Earth •Accretion- material comes together to make the planet 4.6 Billion years ago (age of Sun). Earth was bombarded by interplanetary debris which made it hot. •Differentiation - different densities and compositions to the earth - Earth was molten, allowing higher-density ma ...
... Evolution of the Solid Earth •Accretion- material comes together to make the planet 4.6 Billion years ago (age of Sun). Earth was bombarded by interplanetary debris which made it hot. •Differentiation - different densities and compositions to the earth - Earth was molten, allowing higher-density ma ...
Unit A – Studying Soil Scientifically
... 5. Magma – Molten rock found beneath the earth’s surface. 6. Core – The innermost area of the earth’s interior. 7. Crust – The thin outermost “layer” of the earth. 8. Lava – Molten rock found on top of the earth’s surface. 9. Lithosphere – The rigid upper portion of the earth that is broken into pla ...
... 5. Magma – Molten rock found beneath the earth’s surface. 6. Core – The innermost area of the earth’s interior. 7. Crust – The thin outermost “layer” of the earth. 8. Lava – Molten rock found on top of the earth’s surface. 9. Lithosphere – The rigid upper portion of the earth that is broken into pla ...
Unit D Test Review - Bibb County Schools
... – The same kind of unusual fossils are found in South America and Africa. – The same kind of unusual rock layers are found in North America, Europe, and Africa. – The earth’s continents are moving at a rate of centimeters per year. ...
... – The same kind of unusual fossils are found in South America and Africa. – The same kind of unusual rock layers are found in North America, Europe, and Africa. – The earth’s continents are moving at a rate of centimeters per year. ...
The Composition of the Earth The Earth is divided into three layers
... layer of the Earth. 2. Is made up of 2 parts: a. crust b. the rigid upper part of the mantle. 3.The Lithosphere is divided into pieces called tectonic plates ...
... layer of the Earth. 2. Is made up of 2 parts: a. crust b. the rigid upper part of the mantle. 3.The Lithosphere is divided into pieces called tectonic plates ...
4 layers of Earth and Plate Activity notes
... Milky Way- cut in half • Chocolate- crust- thinnest layer made of rocks and soil (land we walk on and under the sea) • Caramel- mantle- holt molten rock, what would come out of a volcano • Light brown layer- outer core- liquid iron • Bottom layer of chocolate- inner core, solid iron and is the hott ...
... Milky Way- cut in half • Chocolate- crust- thinnest layer made of rocks and soil (land we walk on and under the sea) • Caramel- mantle- holt molten rock, what would come out of a volcano • Light brown layer- outer core- liquid iron • Bottom layer of chocolate- inner core, solid iron and is the hott ...
The science of Geology
... understanding the workings of our dynamic planet Began in the early part of the twentieth century with a proposal called continental drift – the idea that continents moved about the face of the planet Later combined with sea-floor spreading The ...
... understanding the workings of our dynamic planet Began in the early part of the twentieth century with a proposal called continental drift – the idea that continents moved about the face of the planet Later combined with sea-floor spreading The ...
Social Studies
... Inner Core solid 2. Pangaea a. The name given to Earth’s landmasses when it formed one huge supercontinent. a. ...
... Inner Core solid 2. Pangaea a. The name given to Earth’s landmasses when it formed one huge supercontinent. a. ...
Dynamic Planet Vocabulary - Schurger
... moves sideways, cools and sinks; will move plates as it moves sideways Tectonic Plate Large sheets of the lithospheric crust that are moved by convection cells Dynamic Changing, A dynamic planet is a planet changes over time. Volcano A vent in the Earth’s lithosphere where magma, gases and ash escap ...
... moves sideways, cools and sinks; will move plates as it moves sideways Tectonic Plate Large sheets of the lithospheric crust that are moved by convection cells Dynamic Changing, A dynamic planet is a planet changes over time. Volcano A vent in the Earth’s lithosphere where magma, gases and ash escap ...
Slide 1
... The Earth’s surface is mostly covered by water called the: A. Crust B. Mantle C. Hydrosphere D. Atmosphere ...
... The Earth’s surface is mostly covered by water called the: A. Crust B. Mantle C. Hydrosphere D. Atmosphere ...
Layers of the Earth Study Guide
... 1. The first layer of the earth is called the crust. 2. It is the layer of the Earth where we live. 3. It is the outer most (outside) layer of the Earth. 4. It is a solid and is up to 100 kilometers thick. 5. It is the coolest in temperature of all the ...
... 1. The first layer of the earth is called the crust. 2. It is the layer of the Earth where we live. 3. It is the outer most (outside) layer of the Earth. 4. It is a solid and is up to 100 kilometers thick. 5. It is the coolest in temperature of all the ...
Origin of the Moon via giant impact
... Origin of the Moon via giant impact Canup (2004) made high-resolution simulations of the origin of the Moon via the impact of a Marssized object on the Earth, towards the end of the period when the Earth grew in mass by accretion of planetismals. Impact velocity ~9 km/s Impactor’s iron core is most ...
... Origin of the Moon via giant impact Canup (2004) made high-resolution simulations of the origin of the Moon via the impact of a Marssized object on the Earth, towards the end of the period when the Earth grew in mass by accretion of planetismals. Impact velocity ~9 km/s Impactor’s iron core is most ...
STUDY GUIDE FOR CHAPTER 1
... 5. Eventually the surface radiates so much energy that enough can get through the atmosphere to balance the amount of energy coming from the Sun. At that point the surface stops heating up. However its temperature is higher than it would be if no greenhouse gases were present and infrared radiation ...
... 5. Eventually the surface radiates so much energy that enough can get through the atmosphere to balance the amount of energy coming from the Sun. At that point the surface stops heating up. However its temperature is higher than it would be if no greenhouse gases were present and infrared radiation ...
The Solid Earth - cloudfront.net
... existence of an inner core that is distinct from the liquid outer core was discovered in 1936 by seismologist Inge Lehmann using observations of ...
... existence of an inner core that is distinct from the liquid outer core was discovered in 1936 by seismologist Inge Lehmann using observations of ...
The Solid Earth - Cloudfront.net
... existence of an inner core that is distinct from the liquid outer core was discovered in 1936 by seismologist Inge Lehmann using observations of ...
... existence of an inner core that is distinct from the liquid outer core was discovered in 1936 by seismologist Inge Lehmann using observations of ...
ASTRONOMY 161
... (solid but brittle). Beneath the lithosphere is the asthenosphere (plastic). The asthenosphere, heated from below, undergoes convection. ...
... (solid but brittle). Beneath the lithosphere is the asthenosphere (plastic). The asthenosphere, heated from below, undergoes convection. ...
History Channel`s How the Earth was Made Video Questions Name
... 3. How old did Lord Kelvin say the Earth was? (:07) 4. How has radioactive dating developed by Arthur Holmes in 1911 revolutionized our concept of how old the Earth really is? (:08) ...
... 3. How old did Lord Kelvin say the Earth was? (:07) 4. How has radioactive dating developed by Arthur Holmes in 1911 revolutionized our concept of how old the Earth really is? (:08) ...
Lesson 1 - Humanities.Com
... The Layers of the Earth Rap Throw your hands up for the layers of the Earth! Throw your hands up for what’s below the surface! Throw your hands up and let’s discuss… The inner core, outer core, mantle and crust! As you listen to the rap, write down five NIFs (new interesting facts) about the layers ...
... The Layers of the Earth Rap Throw your hands up for the layers of the Earth! Throw your hands up for what’s below the surface! Throw your hands up and let’s discuss… The inner core, outer core, mantle and crust! As you listen to the rap, write down five NIFs (new interesting facts) about the layers ...