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Plate Tectonics Study Guide
Plate Tectonics Study Guide

... That all the continents were once connected in a supercontinent called Pangaea 4. What evidence is there to support Wegener’s theory? List 3 things. 1. Fossils 2. Land Features 3. Climate change 5. Where do we find evidence of sea-floor spreading? At mid-ocean ridges 6. What causes the earth’s plate ...
Grade 6 Curriculum Map - Bibb County School District
Grade 6 Curriculum Map - Bibb County School District

... specifically identify the expectations for student learning for the Bibb County School District. This curriculum is expected to be followed by all teachers to ensure that learning goals are met for all students and state standards. ...
Chapter 2 Physical Geography: A Living Planet
Chapter 2 Physical Geography: A Living Planet

... 8 planets 1 dwarf planet (Pluto) Other celestial bodies that orbit the sun – Comets > spheres covered with ice and dust that leave trails of vapor as they race through space – Asteroids > large chunks of rocky material found in space ...
Powerpoint Presentation Physical Geology, 10th ed.
Powerpoint Presentation Physical Geology, 10th ed.

... uppermost mantle • Makes up Earth’s tectonic “plates” ...
Continental Drift: The Beginning of Plate Tectonics
Continental Drift: The Beginning of Plate Tectonics

... Idea that all continents were all pieced together 245 million years ago Pangaea = “All Earth” ...
Notes: Plate Tectonics - Riverdale Middle School
Notes: Plate Tectonics - Riverdale Middle School

... • A system is a group of parts that work together as a whole. • The constant flow, or cycling, of matter through the Earth system is driven by energy. • Energy is the ability to do work. • Energy that drives the Earth system has two main sources: 1.) heat from the sun 2.) heat flowing out of Earth a ...
Plate Tectonics - Faculty Perry, Oklahoma
Plate Tectonics - Faculty Perry, Oklahoma

... The layer in Earth’s upper mantle and directly under the lithosphere in which rock is soft and weak because it is close to melting. ...
Earths Interior- Milky Way
Earths Interior- Milky Way

... CRUST or LITHOSPHERE – thin, brittle, hard, cold, solid outer shell INNER CORE – hot, solid (very high pressure, contains heavy metals) OUTER CORE – so hot, even pressure can’t force it into a solid. This layer is a liquid Cut the Milky Way bar in half: Label the three layers of the bar according to ...
Check for Understanding
Check for Understanding

... • Inner Core- Believed to be composed primarily of iron and nickel; because it is able to deflect seismic waves, it must behave as a solid in some fashion. Avg Temperatures of 4,300c • Outer Core- Outer core surrounds the inner core and is believed to be a liquid composed of iron mixed with nickel ...
Fall Semester Exam ReviewAnswers Old
Fall Semester Exam ReviewAnswers Old

... Atlantic coastal plain; waterfalls are common; used by many communities for power 57. Faults: cracks in the earth’s crust 58. Prairie: an inland grassland area (grasses can reach 12 feet high); common in the Great Plains 59. Timberline: elevation above which it is too cold for trees to grow 60. Tund ...
Carrying Capacity
Carrying Capacity

... Is it hospitable? It most resembles Earth in size, density and distance from the Sun, but atmosphere is rich in carbon dioxide and caustic sulfuric clouds fill the sky. Lead would melt at the surface…why so different then Earth? ...
inner core - Denton ISD
inner core - Denton ISD

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
L2 - School of Earth Sciences
L2 - School of Earth Sciences

... – cooling and expansion – nebulae formation (gas cloud patches) – centers of high gravity and began to grow, build heat, and spin forming protostars (200 my) – star ignites (true star) (800 my) and stellar nucleosynthesis – No fuel: star dies (supernova explosions) ...
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 ...
File
File

... • If this plate gets stuck it causes a lot of pressure on surrounding rocks. • When this pressure is released it produces shock waves. These are called seismic waves. This is an earthquake. • The waves spread out from the point where the earthquake started - the focus. More damage is done near the f ...
Chapter 1 Notes
Chapter 1 Notes

... Brainstorm a way 2 of the systems interact with each other and write it in your notebook. You are going to share this idea with a partner in 1 minute. With your partner, come up with a way that 3 of the system interact. You will share your idea with another pair in 1 minute. ...
Chapter 1: Introduction
Chapter 1: Introduction

... Earth as a system The Earth system is also powered by the Earth’s interior • Heat remaining from the formation and heat that is continuously generated by radioactive decay powers the internal processes that produce volcanoes, earthquakes, and mountains ...
Convection Currents and Hot Spots
Convection Currents and Hot Spots

... • http://www.pbslearningmedia.org/resource/ nvdv.sci.earth.yellowvolc-1/volcanism-atyellowstone/ 5:45 min • http://www.pbslearningmedia.org/resource/ ess05.sci.ess.earthsys.hawaii/platetectonics-the-hawai699ian-archipelago/ - hotspot (4:36) ...
HOT SPOTS - Norwich High School
HOT SPOTS - Norwich High School

... • http://www.pbslearningmedia.org/resource/ nvdv.sci.earth.yellowvolc-1/volcanism-atyellowstone/ 5:45 min • http://www.pbslearningmedia.org/resource/ ess05.sci.ess.earthsys.hawaii/platetectonics-the-hawai699ian-archipelago/ - hotspot (4:36) ...
The Earth
The Earth

... • At the right distance from the Sun to have liquid water. • Only planet in the solar system to have open oceans. Because water can dissolve CO2, the Earth was saved from a “runaway greenhouse effect.” (Compare with Venus.) • O2-rich atmosphere (21% O2 by volume) • Magnetic field that protects the p ...
Earth`s crust is made up of moving plates
Earth`s crust is made up of moving plates

... the mountains up. – The mountains are probably smaller than they were before because they have been weathered by wind and rain. – The river probably eroded some of the land. – The area was once underwater. The fish died and was buried by sediments, and after a long time the water went away. • After ...
The Living Planet PPT
The Living Planet PPT

...  Waves: swells or ridges produced by wind  Tides: created by gravitational pull of moon or sun ...
Chapter 5 Plate Tectonics-Section 1 Earth`s Interior Exploring Inside
Chapter 5 Plate Tectonics-Section 1 Earth`s Interior Exploring Inside

... structure. Samples that are taken allow geologists to make inferences about conditions deep inside Earth where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide more information about the interior. Ev ...
Chapter 2 Section 2
Chapter 2 Section 2

... Richter developed this scale to measure the amount of energy released by an earthquake. ...
DYNAMIC EARTH NOTES
DYNAMIC EARTH NOTES

... PLATE TECTONICS: The theory that the earth’s crust is divided into plates that move over top of the earth’s mantle. I. CONTINENTAL DRIFT: ALFRED WEGNER - 1920’s - Did NOT explain plate motion a. Continental Puzzle: The earth’s continents look as if they fit together like a puzzle (ex. Africa & S. Am ...
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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.
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