facts and concepts that you need to know to pass the earth science
... The same substance always has the same density, even if you cut it in half or change its shape. As pressure increases, density increases. As temperature increases, density decreases. Most substances, except water, expand when they are heated. Water expands as it freezes. Water is most dense at 4oC, ...
... The same substance always has the same density, even if you cut it in half or change its shape. As pressure increases, density increases. As temperature increases, density decreases. Most substances, except water, expand when they are heated. Water expands as it freezes. Water is most dense at 4oC, ...
Modeling Earth Interior
... physical model. We will also scale the data to make an accurate model of Earth. At times it is difficult to visualize the relationships among numbers if they are in an inconvenient form or very big like Earth. The data table on the left contains a list of measurements. This raw data can be converted ...
... physical model. We will also scale the data to make an accurate model of Earth. At times it is difficult to visualize the relationships among numbers if they are in an inconvenient form or very big like Earth. The data table on the left contains a list of measurements. This raw data can be converted ...
Document
... formed as a direct result of the “Solar Nebula Hypothesis”, which states, “a great cloud of gas and dust shrank under its own gravitation and transformed into the planets and natural satellites that make up the present solar system” Text Reference: pages 19 – 20 Copyright © 2014 All rights reserved, ...
... formed as a direct result of the “Solar Nebula Hypothesis”, which states, “a great cloud of gas and dust shrank under its own gravitation and transformed into the planets and natural satellites that make up the present solar system” Text Reference: pages 19 – 20 Copyright © 2014 All rights reserved, ...
GEOG - Unit 1
... The geography and structure of the earth are continually being changed by internal forces, like plate tectonics, and external forces, like the weather. ...
... The geography and structure of the earth are continually being changed by internal forces, like plate tectonics, and external forces, like the weather. ...
Earth as a System - Bakersfield College
... • well-tested hypothesis – widely accepted view that explains observable facts ...
... • well-tested hypothesis – widely accepted view that explains observable facts ...
File
... Dating the Solar System Meteorites (the original planetismals) sometimes fall to Earth. We can get an age for the meteorites by radioactive dating (more on this later). The meteorites, which are left over pieces from the formation of the solar system, have an average age of ...
... Dating the Solar System Meteorites (the original planetismals) sometimes fall to Earth. We can get an age for the meteorites by radioactive dating (more on this later). The meteorites, which are left over pieces from the formation of the solar system, have an average age of ...
Earth as a System Section 1 Earth`s Interior, continued
... of water known as the global ocean. • Shape = oblate sphere, or a slightly flattened sphere. (Earth’s pole-to-pole circumference is 40,007 km. Its equatorial circumference is 40,074 km.) • Earth’s average diameter is 12,756 km. ...
... of water known as the global ocean. • Shape = oblate sphere, or a slightly flattened sphere. (Earth’s pole-to-pole circumference is 40,007 km. Its equatorial circumference is 40,074 km.) • Earth’s average diameter is 12,756 km. ...
Scaling down the Earth
... Thickness/Radius and Composition: The total radius of the Earth’s thickness is approximately 6,370 km and each layer has its own characteristics. Crust: this layer is solid and comprises the continents and ocean basins. It has a variable thickness, anywhere from 35-70km thick in the continents and 5 ...
... Thickness/Radius and Composition: The total radius of the Earth’s thickness is approximately 6,370 km and each layer has its own characteristics. Crust: this layer is solid and comprises the continents and ocean basins. It has a variable thickness, anywhere from 35-70km thick in the continents and 5 ...
Historical Geology - FacultyWeb Support Center
... – interpreting many aspects of Earth on a global scale – relating many seemingly unrelated phenomena – interpreting Earth history ...
... – interpreting many aspects of Earth on a global scale – relating many seemingly unrelated phenomena – interpreting Earth history ...
Science, 4th 9 weeks
... 2016.17 Seventh Grade, Quarter 4 Big Ideas/Key Concepts: Major geologic events that occur over eons or brief moments in time continually shape and reshape the surface of the Earth, resulting in continuous global change. Standards ...
... 2016.17 Seventh Grade, Quarter 4 Big Ideas/Key Concepts: Major geologic events that occur over eons or brief moments in time continually shape and reshape the surface of the Earth, resulting in continuous global change. Standards ...
Inside the earth - Northside Middle School
... The Earth is made up of three layers—the crust, the mantle, and the core—based on chemical composition. Less dense compounds make up the crust and mantle. Denser compounds make up the core. ...
... The Earth is made up of three layers—the crust, the mantle, and the core—based on chemical composition. Less dense compounds make up the crust and mantle. Denser compounds make up the core. ...
File - We All Love Science
... Do now: Base your answers to questions 15 and 16 on the United States time zone map shown below. The dashed lines represent meridians (lines of longitude). 16) The basis for the time difference between adjoining time zones is Earth’s a) 1° per hour rate of revolution b) 1° per hour rate of rotation ...
... Do now: Base your answers to questions 15 and 16 on the United States time zone map shown below. The dashed lines represent meridians (lines of longitude). 16) The basis for the time difference between adjoining time zones is Earth’s a) 1° per hour rate of revolution b) 1° per hour rate of rotation ...
Seismic tomography
... Thanks and/or apologies to Barbara Romanowicz, UC Berketey whose slides have been used liberally in this presentation. ...
... Thanks and/or apologies to Barbara Romanowicz, UC Berketey whose slides have been used liberally in this presentation. ...
C1b 6.1 Structure of the Earth
... • Challenge: This layer is not a liquid, but is often described as ‘syrupy’. Why is this? ...
... • Challenge: This layer is not a liquid, but is often described as ‘syrupy’. Why is this? ...
Power Point print view
... Earth’s surface over time. This is explained by the Theory of Plate Tectonics • Earth’s biota – all of living things – has evolved or changed through history and is explained by the Theory of Organic Evolution • All of the geologic processes take place within an extensive geologic time scale spannin ...
... Earth’s surface over time. This is explained by the Theory of Plate Tectonics • Earth’s biota – all of living things – has evolved or changed through history and is explained by the Theory of Organic Evolution • All of the geologic processes take place within an extensive geologic time scale spannin ...
Earth and Ocean Sciences
... The Jeanette Gillespie Memorial Prize in Earth Science is awarded annually to a student enrolled at the University who, in the year of the award, has taken at least two Level I courses in Earth Sciences for a first degree and who is academically the most meritorious student in Level I Earth Sciences ...
... The Jeanette Gillespie Memorial Prize in Earth Science is awarded annually to a student enrolled at the University who, in the year of the award, has taken at least two Level I courses in Earth Sciences for a first degree and who is academically the most meritorious student in Level I Earth Sciences ...
Curriculum Mapping: Integrating Magnet Theme with Ongoing Units
... Curriculum Mapping: Integrating Magnet Theme with Ongoing Units John Muir K-12 Magnet School for Global Citizenship Subject: Earth Science Grade level: 9 - 12 Teacher: V.Stevens Date: 4/14/09 Essential questions: How do we become globally aware? How do we draw together as a community to use our coll ...
... Curriculum Mapping: Integrating Magnet Theme with Ongoing Units John Muir K-12 Magnet School for Global Citizenship Subject: Earth Science Grade level: 9 - 12 Teacher: V.Stevens Date: 4/14/09 Essential questions: How do we become globally aware? How do we draw together as a community to use our coll ...
Unit 1 - Earth`s Dimensions Review Powerpoint
... on a globe of the Earth? A. Latitude lines are parallel and longitude lines meet at the poles B. Latitude lines are parallel and longitude lines meet at the equator C. Longitude lines are parallel and latitude lines meet at the equator D. Longitude lines are parallel and latitude lines meet at the p ...
... on a globe of the Earth? A. Latitude lines are parallel and longitude lines meet at the poles B. Latitude lines are parallel and longitude lines meet at the equator C. Longitude lines are parallel and latitude lines meet at the equator D. Longitude lines are parallel and latitude lines meet at the p ...
Earth - WordPress.com
... Long ago, people used to think the Earth was flat. They believed if they sailed a boat far out into the ocean, the boat would fall off the Earth! Now people know that this is not true. We know the Earth is not flat. It is shaped like a ball. The Earth only looks flat to us because it is so large. We ...
... Long ago, people used to think the Earth was flat. They believed if they sailed a boat far out into the ocean, the boat would fall off the Earth! Now people know that this is not true. We know the Earth is not flat. It is shaped like a ball. The Earth only looks flat to us because it is so large. We ...
History of geodesy
Geodesy (/dʒiːˈɒdɨsi/), also named geodetics, is the scientific discipline that deals with the measurement and representation of the Earth. The history of geodesy began in antiquity and blossomed during the Age of Enlightenment.Early ideas about the figure of the Earth held the Earth to be flat (see flat earth), and the heavens a physical dome spanning over it. Two early arguments for a spherical Earth were that lunar eclipses were seen as circular shadows which could only be caused by a spherical Earth, and that Polaris is seen lower in the sky as one travels South.