Goal-directed Instructional Design Plan
... Goal-directed Instructional Design Plan Plate Tectonics: I Feel the Earth Move Under My Feet Author - Ryan Brown 1. A problem or a need – there must be a problem of practice or an educational need that should be addressed during the lesson. In what ways can Earth processes be explained as interactio ...
... Goal-directed Instructional Design Plan Plate Tectonics: I Feel the Earth Move Under My Feet Author - Ryan Brown 1. A problem or a need – there must be a problem of practice or an educational need that should be addressed during the lesson. In what ways can Earth processes be explained as interactio ...
Chapter 2
... Hydrosphere – 71% of earth’s surface. 97% of water is salt water. The 3% that is fresh is found in lakes , streams, aquifers and ice. Geosphere – Rock, soil, continents and oceanic floor and the molten portion of the earth. Biosphere – The volume 8km above the earth’s surface to 8km below the earth’ ...
... Hydrosphere – 71% of earth’s surface. 97% of water is salt water. The 3% that is fresh is found in lakes , streams, aquifers and ice. Geosphere – Rock, soil, continents and oceanic floor and the molten portion of the earth. Biosphere – The volume 8km above the earth’s surface to 8km below the earth’ ...
PowerPoint Review
... •A trench forms above the subduction zone in water •A volcanic mountain chain forms on land ...
... •A trench forms above the subduction zone in water •A volcanic mountain chain forms on land ...
Earth`s Layers Ppt
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
ppt presentation
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
earth`s thickest layer between the outer core and crust made of
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
... is broken into tectonic plates Asthenosphere – the layer in earth’s upper mantle directly under the lithosphere in which rock is soft and weak because it is close to melting ...
Essentials of Geology, 9e
... interacting parts or spheres Parts of the Earth system are linked It is characterized by processes that ▪ Vary on spatial scales from fractions of a millimeter to thousands of kilometers ▪ Have time scales that range from milliseconds to billions of years ...
... interacting parts or spheres Parts of the Earth system are linked It is characterized by processes that ▪ Vary on spatial scales from fractions of a millimeter to thousands of kilometers ▪ Have time scales that range from milliseconds to billions of years ...
Earth Systems Standards Aligned to National Science Education
... Earth systems have internal and external sources of energy, both of which create heat. The sun is the major external source of energy. Two primary sources of internal energy are the decay of radioactive isotopes and the gravitational energy from the earth's original formation. The outward transfer o ...
... Earth systems have internal and external sources of energy, both of which create heat. The sun is the major external source of energy. Two primary sources of internal energy are the decay of radioactive isotopes and the gravitational energy from the earth's original formation. The outward transfer o ...
DRAFT Expectation: Interactions of Earth`s Systems
... the properties of systems thinking to earth systems interactions. Define a system by: o specifying its apparent boundaries and subsystems o indicating its relation to other systems o Identifying inputs and outputs. Cite evidence to explain that if a system in equilibrium is disturbed, it may: o ...
... the properties of systems thinking to earth systems interactions. Define a system by: o specifying its apparent boundaries and subsystems o indicating its relation to other systems o Identifying inputs and outputs. Cite evidence to explain that if a system in equilibrium is disturbed, it may: o ...
Earth- information sheet Homework T4 Wk1
... hemisphere (meaning half of the Earth’s sphere) has winter. At this time the southern hemisphere is tilted very slightly towards the Sun and the southern hemisphere has summer. Winter in Britain means summer in New Zealand. Closer to the Equator there is much less difference between summer and winte ...
... hemisphere (meaning half of the Earth’s sphere) has winter. At this time the southern hemisphere is tilted very slightly towards the Sun and the southern hemisphere has summer. Winter in Britain means summer in New Zealand. Closer to the Equator there is much less difference between summer and winte ...
7th Grade Earth Science State and District Outcomes Summary
... 3.1a Gather, analyze, and communicate data that explains Earth’s plates, plate motions, and the results of plate motions 3.1b Identify, interpret, and explain models of plates motions on Earth 3.1c Use maps to locate likely geologic “hot spots”, using evidence of earthquakes and volcanic activity 3. ...
... 3.1a Gather, analyze, and communicate data that explains Earth’s plates, plate motions, and the results of plate motions 3.1b Identify, interpret, and explain models of plates motions on Earth 3.1c Use maps to locate likely geologic “hot spots”, using evidence of earthquakes and volcanic activity 3. ...
GLOBAL PLATE TECTONICS AND GEODYNAMICS
... Dynamic Earth: Plate motions and Earth history Mission: To explore the link between the lithosphere and the convecting mantle and quantify how palaeogeography and TPW have influenced the climate system. Main Hypothesis: Motion of tectonic plates is closely related to mantle dynamics and the mantle ...
... Dynamic Earth: Plate motions and Earth history Mission: To explore the link between the lithosphere and the convecting mantle and quantify how palaeogeography and TPW have influenced the climate system. Main Hypothesis: Motion of tectonic plates is closely related to mantle dynamics and the mantle ...
Lesson 1 - Earth`s Interior
... evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves. Rocks from inside Earth give geologists clues about Earth’s structure. To study Earth’s interior, geologists also study seismic waves. When earthquakes occur, they produce seismic wa ...
... evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves. Rocks from inside Earth give geologists clues about Earth’s structure. To study Earth’s interior, geologists also study seismic waves. When earthquakes occur, they produce seismic wa ...
Inside the Earth - ReedEarthScience
... up rock samples • Theses samples allow scientists to infer about conditions inside Earth ...
... up rock samples • Theses samples allow scientists to infer about conditions inside Earth ...
Internal External Forces
... • A special device called a seismograph can detect earthquakes. It measures the size of the waves created by an earthquake. ...
... • A special device called a seismograph can detect earthquakes. It measures the size of the waves created by an earthquake. ...
Tides
... • The moon creates tides through the pull of its gravity. • The pull isn’t strong enough to affect the crust or other landforms, but it is enough to cause a noticeable bulge in the ocean. • The high-tide bulge always stays with the moon as it travels around Earth. ...
... • The moon creates tides through the pull of its gravity. • The pull isn’t strong enough to affect the crust or other landforms, but it is enough to cause a noticeable bulge in the ocean. • The high-tide bulge always stays with the moon as it travels around Earth. ...
RESTLESS EARTH Chapter 3: Uniformitarianism~ A principle that
... processes shaping the Earth today have been at work throughout Earth’s history. These changes remain uniform or do not change over time. “The present is the key to the past” Catastrophism ~ A principle that states that all geologic change occurs suddenly. Mountains, canyons, and seas can be expl ...
... processes shaping the Earth today have been at work throughout Earth’s history. These changes remain uniform or do not change over time. “The present is the key to the past” Catastrophism ~ A principle that states that all geologic change occurs suddenly. Mountains, canyons, and seas can be expl ...
Introduction to Earth Science
... Other map projections: • A conic projection is made by wrapping a cone around the Earth at a particular line of latitude. (almost no distortion at that line) • A gnomonic projection is made by placing a sheet of paper on a globe so that it is touching only one spot. • See page 13 in text. ...
... Other map projections: • A conic projection is made by wrapping a cone around the Earth at a particular line of latitude. (almost no distortion at that line) • A gnomonic projection is made by placing a sheet of paper on a globe so that it is touching only one spot. • See page 13 in text. ...
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.