Video: Colliding Continents - National Geographic Name: https
... noticed ______________fossils were discovered oceans away from each other. 19. When he first proposed his theory of continental drift, why did the scientific community reject his ideas? 20. Heat escaping from the core creates ____________ _______________ in the next layer of the Earth, the _________ ...
... noticed ______________fossils were discovered oceans away from each other. 19. When he first proposed his theory of continental drift, why did the scientific community reject his ideas? 20. Heat escaping from the core creates ____________ _______________ in the next layer of the Earth, the _________ ...
Practice Questions 1) 2) 3) 4) 1. Which pie graph correctly shows the
... shows the general movement of air within a portion of Earth’s atmosphere located between 30° N and 30° S latitude. Numbers 1 and 2 represent different locations in the atmosphere. ...
... shows the general movement of air within a portion of Earth’s atmosphere located between 30° N and 30° S latitude. Numbers 1 and 2 represent different locations in the atmosphere. ...
Earth Science - Center Grove Schools
... 4. Your scale is 1:20,000,000 (one to twenty million), or 1cm = 200km. The Earth has a radius of about 6371 km. Hence, your “Slice” will be 63.7cm ÷ 2 or 32cm, or one 20 millionth as large as the Earth. 5. Make a mark on the “crust” which is 32cm from the “Center of Earth” mark. See Figure Above. 6. ...
... 4. Your scale is 1:20,000,000 (one to twenty million), or 1cm = 200km. The Earth has a radius of about 6371 km. Hence, your “Slice” will be 63.7cm ÷ 2 or 32cm, or one 20 millionth as large as the Earth. 5. Make a mark on the “crust” which is 32cm from the “Center of Earth” mark. See Figure Above. 6. ...
Earth Space Science
... Earth’s crust consists of major and minor tectonic plates that move relative to each other. A combination of constructive and destructive geologic processes formed Earth’s surface. Evidence of the dynamic changes of Earth’s surface through time is found in the geologic record. ...
... Earth’s crust consists of major and minor tectonic plates that move relative to each other. A combination of constructive and destructive geologic processes formed Earth’s surface. Evidence of the dynamic changes of Earth’s surface through time is found in the geologic record. ...
National Geographic – Colliding Continents Video
... 18. The world’s last supercontinent is known as _____________________. 19. How many years ago did the supercontinent Pangaea begin breaking up? ___________ years ago 20. During the break-up of Pangaea, South America split off from ______________, North America split off from ________________, and Au ...
... 18. The world’s last supercontinent is known as _____________________. 19. How many years ago did the supercontinent Pangaea begin breaking up? ___________ years ago 20. During the break-up of Pangaea, South America split off from ______________, North America split off from ________________, and Au ...
guide
... 7. Base of the lithosphere (~100 km) – The Earth’s plates (lithosphere) are moving at centimeters per year! 8. The asthenosphere (150 km) – Partially molten mantle and convection currents here. ...
... 7. Base of the lithosphere (~100 km) – The Earth’s plates (lithosphere) are moving at centimeters per year! 8. The asthenosphere (150 km) – Partially molten mantle and convection currents here. ...
Chapter 15 Outline
... b. Contains most of the Earth’s _____________ c. No one has ever been to the _____________ 4. _____________ a. Center of the _____________ b. Mostly ____________ and _____________ B. Physical _____________ of the _________________ 1. ___________ physical layers 2. Lithosphere: Divided into pieces ca ...
... b. Contains most of the Earth’s _____________ c. No one has ever been to the _____________ 4. _____________ a. Center of the _____________ b. Mostly ____________ and _____________ B. Physical _____________ of the _________________ 1. ___________ physical layers 2. Lithosphere: Divided into pieces ca ...
The Physical world
... solid ball, it is really more like a series of shells that float on one another.—Think of an egg! • Core – solid metallic center made of nickel and iron • Mantle – soft layer of molten rock (magma) • Crust – thin layer of rock on earth’s surface ...
... solid ball, it is really more like a series of shells that float on one another.—Think of an egg! • Core – solid metallic center made of nickel and iron • Mantle – soft layer of molten rock (magma) • Crust – thin layer of rock on earth’s surface ...
final_exam - Winthrop Chemistry, Physics, and Geology
... 10. [True or False] Seismic P-waves can’t travel through the liquid outer core of the Earth but Swaves can. This results in a P-wave shadow on the side of the Earth opposite an earthquake. 11. To reach its dew point temperature, a packet of unsaturated air must usually be [ heated / cooled ]. (circl ...
... 10. [True or False] Seismic P-waves can’t travel through the liquid outer core of the Earth but Swaves can. This results in a P-wave shadow on the side of the Earth opposite an earthquake. 11. To reach its dew point temperature, a packet of unsaturated air must usually be [ heated / cooled ]. (circl ...
Wind Patterns
... Wind Patterns on a Spherical Earth At the same time, cold air is flowing from the poles to the equator. By the time the air reaches 60º, it has warmed enough to begin to rise again. The result, three distinct closed patterns of air ...
... Wind Patterns on a Spherical Earth At the same time, cold air is flowing from the poles to the equator. By the time the air reaches 60º, it has warmed enough to begin to rise again. The result, three distinct closed patterns of air ...
Day 10 - Ch. 5
... Earth’s Interior The mantle is about 80% of the volume of the Earth. It is mostly a rocky material (basalt). The core is believed to be mostly iron and nickel, but could have many of the heavier elements. There is certainly some uranium and other radioactive elements which produce heat that keeps t ...
... Earth’s Interior The mantle is about 80% of the volume of the Earth. It is mostly a rocky material (basalt). The core is believed to be mostly iron and nickel, but could have many of the heavier elements. There is certainly some uranium and other radioactive elements which produce heat that keeps t ...
Unit 1: Basics of Geography Chapter 2
... either one to dive under the other or the edges of both to crumple • Transform boundary- plates slide past one another ...
... either one to dive under the other or the edges of both to crumple • Transform boundary- plates slide past one another ...
1st nine weeks review - Okaloosa County School District
... Sediment- this happens when physical or chemical processes weather a rock on the earth’s surface ...
... Sediment- this happens when physical or chemical processes weather a rock on the earth’s surface ...
Primary Standards for Processes that Change the Earth
... Students will model the layers of the Earth, explain interactions between them and describe potential results of those interactions SC-07-2.3.2 Students will explain the layers of the Earth and their interactions. The use of models/diagrams/graphs helps illustrate that the Earth is layered. The lith ...
... Students will model the layers of the Earth, explain interactions between them and describe potential results of those interactions SC-07-2.3.2 Students will explain the layers of the Earth and their interactions. The use of models/diagrams/graphs helps illustrate that the Earth is layered. The lith ...
What on EARTH is going on here? (Mrs. Rodriguez tells the story of
... plates sort of shift around on top. When you look at the continents, don’t they look like puzzle pieces? ...
... plates sort of shift around on top. When you look at the continents, don’t they look like puzzle pieces? ...
The Earths interior overview
... The earth's interior is neither all solid nor is it all molten. There are layers with a different density, thickness and composition. Furthermore the earth's crust is not one continuous layer. It is broken into many sections known as plates. Some plates are quite small while others are quite large. ...
... The earth's interior is neither all solid nor is it all molten. There are layers with a different density, thickness and composition. Furthermore the earth's crust is not one continuous layer. It is broken into many sections known as plates. Some plates are quite small while others are quite large. ...
5 Themes of Geography Vocabulary:
... meridians - another term for longitude lines Prime Meridian - zero degrees longitude; passes through Greenwich, England International Dateline - 180 degrees longitude; this line designates where each new day begins. Mapmaker, Mapmaker, Make Me a Map! (Location cont.) migration - the movement of peop ...
... meridians - another term for longitude lines Prime Meridian - zero degrees longitude; passes through Greenwich, England International Dateline - 180 degrees longitude; this line designates where each new day begins. Mapmaker, Mapmaker, Make Me a Map! (Location cont.) migration - the movement of peop ...
Document
... A.Earth is divided into ___________ layers- the crust, mantle, and core. 1. Earth’s layers are arranged by their ___________________________ III. The Crust A.Crust- Earth’s outer layer. Also the _____________________________ layer 1. Solid rock that includes dry land and ocean floor. ...
... A.Earth is divided into ___________ layers- the crust, mantle, and core. 1. Earth’s layers are arranged by their ___________________________ III. The Crust A.Crust- Earth’s outer layer. Also the _____________________________ layer 1. Solid rock that includes dry land and ocean floor. ...
Layer Depth (km) Rigidity
... •Early H2 and He (light gases)-- “blown away” •Release of gases from interior N2, CO2, CH4, NH3, H2S, HCl, H2O vapor. •Evolution of atmosphere: (a) loss of reactive gases; (b) development of life – much later... CO2 removed and O2 accumulated. ...
... •Early H2 and He (light gases)-- “blown away” •Release of gases from interior N2, CO2, CH4, NH3, H2S, HCl, H2O vapor. •Evolution of atmosphere: (a) loss of reactive gases; (b) development of life – much later... CO2 removed and O2 accumulated. ...
The Dynamic Earth: Plate Tectonics (PowerPoint)
... http://smp.uq.edu.au/content/pitch-drop-experiment ...
... http://smp.uq.edu.au/content/pitch-drop-experiment ...
Theme 8 – The Dynamic Earth: Plate Tectonics
... http://smp.uq.edu.au/content/pitch-drop-experiment ...
... http://smp.uq.edu.au/content/pitch-drop-experiment ...
TERM 1 Final Exam – Study Guide
... A monarchy is government with a King or Queen in charge. A democracy is where all the citizens vote to establish the laws. ...
... A monarchy is government with a King or Queen in charge. A democracy is where all the citizens vote to establish the laws. ...
EARTH (¿)
... Formation of Earth: -accretion/collisions of smaller objects -great amounts of heat released -original Earth molten Earth became differentiated: -densest elements "sink" to center -iron, nickel -lightest elements "rise" to surface -silicon, oxygen compounds Today, slowly cooling off: Interior of Ea ...
... Formation of Earth: -accretion/collisions of smaller objects -great amounts of heat released -original Earth molten Earth became differentiated: -densest elements "sink" to center -iron, nickel -lightest elements "rise" to surface -silicon, oxygen compounds Today, slowly cooling off: Interior of Ea ...
Earth
... circumference by geometry. He used the length of a building shadow in Alexandria at noon on the summer solstice. He knew that, simultaneously, sunlight was hitting the bottom of a water well in Aswan. ...
... circumference by geometry. He used the length of a building shadow in Alexandria at noon on the summer solstice. He knew that, simultaneously, sunlight was hitting the bottom of a water well in Aswan. ...
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.