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Beyond_the_Beach
Beyond_the_Beach

... continental and oceanic plates move toward each other examples – margins around Pacific Ocean contain: coastal mountain range, volcanoes, earthquakes narrow, steep continental shelf continental slope and submarine trench ...
earth science literacy principles - University of Calgary Geoscience
earth science literacy principles - University of Calgary Geoscience

... energy and mineral resources, changing climates, water shortages—directly relating to the Earth sciences. There are many difficult decisions that governments, local and national, will have to make concerning these issues, and how well humans survive the twenty-first century will depend upon the success ...
Chapter 3 section 1 2015
Chapter 3 section 1 2015

... • The Earth’s surface is continually battered by wind and scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natur ...
Plate Tectonic Theory
Plate Tectonic Theory

... Younger rocks near mid-ocean ridges. Older near continents. Ocean floor age mirrored on each side of mid-ocean ridge ...
1. Continental drift? What evidence did Alfred Wagner use to
1. Continental drift? What evidence did Alfred Wagner use to

... thermal convection in the earth’s mantle could cause continents to move, but they suggested that the continents didn’t move but were by larger pieces of the earth’s crust called tectonic plates. And it let to the development of plate tectonics. 4. What are the three different types of plate boundari ...
• • • • • • • • • • • • • • • • • • • • • • •
• • • • • • • • • • • • • • • • • • • • • • •

...  Explain how the water cycle circulates Earth's water supply in an unending cycle  Explain how the water cycle is kept in balance  Describe the ability of a stream to erode and transport material  Compare and contrast the changes in gradient and discharge between a stream's headwaters and mouth ...
Objective Recovery Packet Unit 2
Objective Recovery Packet Unit 2

... Step 2 (Star 2): You have two options (just pick one!): Draw the rock cycle, including each of the three different types of rock and the forces that drive the rock cycle; OR write a paragraph as if you are a rock, who has lived a long life and been transformed into each different type of rock over t ...
EARTH SCIENCE LITERACY PRINCIPLES
EARTH SCIENCE LITERACY PRINCIPLES

... energy and mineral resources, changing climates, water shortages—directly relating to the Earth sciences. There are many difficult decisions that governments, local and national, will have to make concerning these issues, and how well humans survive the twenty-first century will depend upon the succ ...
Understanding Regional Ecosystem Patterns to Design Monitoring Networks and Sustainable Landscapes
Understanding Regional Ecosystem Patterns to Design Monitoring Networks and Sustainable Landscapes

... Classifying metropolitan areas by ecoregion forms a baseline for selecting native plants for landscaping or to restore natural conditions, as well as transferring information among similar cities. A source of native plant information can be found in Description of the Ecoregions of the United States ...
Rock Your World
Rock Your World

... Geology)is)a)science)that)deals)with)the)history)of)the)earth)and)its)life,)especially)as) recorded)in)rocks.)In)this)unit,)students)will)learn)about)how)the)land)around)them)(both)at) Calvin)Crest)and)at)home))was)formed.)They)will)see)evidence)of)slow)geological)processes) and)changes)to)the)earth ...
The Dynamic Earth - Model High School
The Dynamic Earth - Model High School

... The Geosphere • Most is located in Earth’s interior • Use seismic waves to learn about interior -wave is altered by the material it travels through ...
Weathering - Liceo Galvani
Weathering - Liceo Galvani

... precipitate out forming evaporite deposits. • Calcium carbonate (calcite, limestone), sodium chloride (salt), and calcium sulfate (gypsum) are particularly vulnerable to solution weathering. ...
crust - River Dell Regional School District
crust - River Dell Regional School District

... Earth has layered structures with solid rock at the surface and partly liquid rock material below. When scientists understand the Earth’s structure, they can help predict when a geyser or a volcano will erupt, or how a river will change course over time. ...
Planets Notes 5 - 1 Notes 5: Planetary Interiors 5.1 Layers The
Planets Notes 5 - 1 Notes 5: Planetary Interiors 5.1 Layers The

... to the high pressure. The outer core is liquid, and the motion of the material in the outer core helps produce the Earth’s magnetic field. Material is estimated to move at a rate of 0.02 cm/s in the outer core. On top of the core is the rocky mantle. This is comprised of siderophile rich rocks (iro ...
3 How does the movement of lithospheric plates cause major events
3 How does the movement of lithospheric plates cause major events

... magma – hot fluid or semi fluid material below or within the earth's crust fossil - a remnant or trace of an organism from the past, such as a skeleton or leaf imprint, embedded and preserved in the earth's crust subduction – the sideways and downward movement of the edge of a plate of the earth's c ...
Rock Cycle Powerpoint with pictures
Rock Cycle Powerpoint with pictures

... Heat and Pressure WITHOUT MELTING Crystals form (again) ...
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves

... is a weaker, viscous layer of upper mantle, called the asthenosphere, which is thought to lubricate the movement of overriding lithospheric plates. Although the base of the lithosphere is commonly thought of as a first-order boundary or structural discontinuity, there are no strong a priori physical ...
course outline - H-W Science Website
course outline - H-W Science Website

... 5. Describe the following parts of a stream system: channel, divide, flood plain, headwaters 6. Describe the changes in a stream valley over time, from young to mature and old. 7. Describe drainage patterns and explain why each develops: dendritic, trellis, radial 8. Explain how a stream flows, tran ...
surface features and plate tectonics (modified for adeed)
surface features and plate tectonics (modified for adeed)

... sea-floor spreading - happens at the mid-oceanic ridge where a divergent boundary is causing two plates to move away from one another resulting in spreading of the sea floor. As the plates move apart, new material wells up and cools onto the edge of the plates shear stress - the stress component par ...
Chapter 2
Chapter 2

... convection (對流). Convection can happen in gases, in liquids, or, given enough time, in ductile solids. A prerequisite condition for mantle convection is the thermal expansion (熱膨脹) of hot rock. Convective heat is transported with the motion of ductile rock. ...
Final Earth Pacing
Final Earth Pacing

... 9 Weeks (2 Weeks) ...
Weather $100
Weather $100

... Which of the following statements best describes the formation of new crust along the boundary of a tectonic ...
The 10000-Foot High Great Escarpment Southeast
The 10000-Foot High Great Escarpment Southeast

... by the geomorphology of the coastal plain with steep perpendicular valley sides and steep river profiles showing that the rivers are not in equilibrium.16 These are young rivers according to the uniformitarian paradigm. King remarked on the significance of such steep rivers: “So recent have the late ...
Essentials of Geology Plate Tectonics: A Unifying Theory
Essentials of Geology Plate Tectonics: A Unifying Theory

... This reconstruction is consistent with fossil and climatologic evidence from Laurasia ...
Erosion, Himalayan Geodynamics, and the Geomorphology of
Erosion, Himalayan Geodynamics, and the Geomorphology of

... JANUARY 2001, GSA TODAY ...
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Geomorphology



Geomorphology (from Greek: γῆ, ge, ""earth""; μορφή, morfé, ""form""; and λόγος, logos, ""study"") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical or chemical processes operating at or near the earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphology is practiced within physical geography, geology, geodesy, engineering geology, archaeology and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field.
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