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Earth Science Warm ups week ending 9/16
Earth Science Warm ups week ending 9/16

... 1- Has the surface of the earth changed over time? If yes why? 2- Has there ever been a single land mass on earth? Thursday 1- What is one evidence of continental drift? 2- Who came up with the theory of Pangaea? Friday 1- Contrast or compare the movement Divergent and Convergent plate boundaries. 2 ...
RHV_Margins_Mini_Lesson.v8
RHV_Margins_Mini_Lesson.v8

... Look at a map of the Earth’s lithospheric plates and identify the overriding and subducting plate for each of the three Margins Focus areas mentioned here. Look at a list of historic tsunamis and determine in which subduction zones the earthquakes that triggered these events occurred. Look at the Na ...
Geologic Time and the Fossil Record
Geologic Time and the Fossil Record

... Each volcano has two main parts, the magma chamber below ground and the vents (cracks in the surface through which lava is escapes). Magma is called lava after it reaches the surface. Its composition, what chemicals it as made up of, can affect how it erupts. -If it has a lot of water dissolved in ...
Earth`s Structure
Earth`s Structure

...  subduction – This occurs where plates move together and one of the plates is driven down into the mantle. ...
Passwords: Social Studies Vocabulary
Passwords: Social Studies Vocabulary

... the seven continents. A continent is one of the seven large areas of land ...
Interior of the earth
Interior of the earth

... state of gravitational equilibrium between the earth's lithosphere and asthenosphere such that the tectonic plates "float" at an elevation which depends on their thickness and density. This concept is invoked to explain how different topographic heights can exist at the Earth's surface. When a certa ...
Earth Science Literacy Principles
Earth Science Literacy Principles

... physical changes in Earth’s materials and living organisms. For example, large amounts of carbon continually cycle among systems of rock, water, air, organisms, and fossil fuels such as coal and oil. ...
Earth Science Literacy Principles
Earth Science Literacy Principles

... physical changes in Earth’s materials and living organisms. For example, large amounts of carbon continually cycle among systems of rock, water, air, organisms, and fossil fuels such as coal and oil. ...
Dynamic Earth
Dynamic Earth

... • Wegener and Taylor, early 1900’s, proposed continental drift and Pangaea • Evidence supporting the idea that the continents had drifted. – Geographic fit of continents ...
How does the Earth`s crust move?
How does the Earth`s crust move?

... incredibly large amounts of active volcanoes. • Most of the active volcanoes on Earth are located here! ...
1 The Growing Earth David de Hilster 1360 Redondo Ave. #301
1 The Growing Earth David de Hilster 1360 Redondo Ave. #301

... drew the first known map where the continents were purposely drawn together. 1888: Ivan Osipovich Yarkovsky, a Russian-Polish civil engineer, suggested that some sort of aether is absorbed within the earth and transformed into new chemical elements, forcing the celestial bodies to expand. 1889 and 1 ...
Layers of the Earth PowerPoint
Layers of the Earth PowerPoint

... • Very dense ...
Core
Core

... Layer below Lithosphere Pieces of lithosphere (tectonic plates) move along this layer. Made of solid rock, soft layer of the mantle ...
Why is the Earth Moving?
Why is the Earth Moving?

... E. As the magma warms it expands and becomes less dense. F. It are these currents that create friction with the crust above and causes it to move. G. Magma (semi-molten rock) near the outer core is heated. H. As the magma nears the crust it begins to cool. ...
Why Questions Topics
Why Questions Topics

... 119. How did the Devil’s Tower form the way it is? How did it get that way? 120. Why haven’t our mountains collapsed? 121. Why do volcanoes stay dormant? 122. Why do tectonics plates move so slowly or move at all? 123. Why don’t volcanoes exist in less tropical areas like Colorado? 126. How long doe ...
Bundle 1
Bundle 1

... Although active geologic processes, such as plate tectonics and erosion, have destroyed or altered most of the very early rock record on Earth, other objects in the solar system, such as lunar rocks, asteroids, and meteorites, have changed little over billions of years. Studying these objects can pr ...
AUGURY, Reconstructing Earth`s mantle convection
AUGURY, Reconstructing Earth`s mantle convection

... In an effort to accurately reconstruct the evolution of Earth’s mantle, Professor Nicolas Coltice is collaborating with researchers across the globe, using data assimilation and tectonic observations in a novel geological approach that will help inform a range of disciplines Our results will give be ...
What we`re gonna do today
What we`re gonna do today

... need to look to find the oldest rocks? What we’re gonna do today Video: Plate Tectonics Reflect Please write a one paragraph summary of the video. In your paragraph, please also give a critique of the video. Please be honest and appropriate. Homework Have a wonderful weekend! ...
test - Scioly.org
test - Scioly.org

... d. It disappears from Earth. 72 What is a magnetic field reversal? a. when Earth's magnetic field suddenly disappears for short periods of time b. when Earth's magnetic field leaves the north pole and enters the south pole c. when Earth's magnetic field suddenly runs east/west instead of south/north ...
Earth
Earth

... UV is blocked by the atmosphere at about 30 km above the surface UV is absorbed => 3 Oxygen atoms to bind into O3 (ozone) human activity => sharp drop in ozone 1950 - 1980 decreased by 1/2 ...
ContinentalDrift
ContinentalDrift

... Probably one of the most obvious pieces of evidence for continental drift is the fact that many of the continents appear as though they may have once fit together One scientist who put a lot of thought into this idea of cont. drift was Alfred Wegener (1880-1930) ...
File
File

... show HOW the plates move. • Back then, we had no GPS (global position satellites) nor did we know much about atomic radiation nor CONVECTION! ...
Chapter 7_Part 1
Chapter 7_Part 1

... analyses and the lack of a physical mechanism • How could continents plow their way through the solid rock of the seafloor? ...
To demonstrate how Young Fold Mountains are
To demonstrate how Young Fold Mountains are

... Fig. 6: Mark the wrinkling created by the ‘push’ of your fingers. This represents folding of the SIAL, SIMA, and also a bit of the Mantle. ...
Mr. Handerson - WordPress.com
Mr. Handerson - WordPress.com

... First evidence is, by making observations of the seismic waves. Seismic waves causes by earthquakes. Scientist observes how the seismic waves travel through the earth. As if there was an earthquake in Italy. The seismic waves would first start in the place where the earthquake happened and would tra ...
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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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