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Unit Name: Earth`s History - Red Clay Secondary Science Wiki
Unit Name: Earth`s History - Red Clay Secondary Science Wiki

... The Earth’s surface has changed Differential erosion over time. Evidence for this is Rock sequences found in fossils, matching rock Rock correlation types, and the fit of the Law of Superposition continental coastlines. Fossils Index fossils Humans have only recently been Plate Tectonics present on ...
Ch 3, part 1
Ch 3, part 1

... Section 1 ...
10 Things to Know About Plate Tectonics
10 Things to Know About Plate Tectonics

... 2. Movement occurs because of convection currents in the asthenosphere, which move the lithosphere on top. Mantle heats up as it approaches the core, so it rises to the top, where it cools and cycles back down toward the core, and so on and so forth. 3. Divergent plate boundaries – two plates moving ...
Let`s Review
Let`s Review

... measured using the Richter Scale. The scale begins at 1 and has no upper limit... What was the largest earthquake ever recorded? ...
Inner Structure of the Earth 3. Mantle
Inner Structure of the Earth 3. Mantle

... Chemical Weathering • Carbonic Acid: CO2 from the air or soil combines with H2O to make carbonic acid. When the acidic water seeps into the cracks in certain rocks (limestone) it dissolves the rocks away. Examples: caves ...
Week 3 (Norton), part c (pdf, 4.5 MB)
Week 3 (Norton), part c (pdf, 4.5 MB)

... entitled “Earth’s plate tectonics from a Martian perspective,” he suggests that the problem faced by earthbound geologists is that they have been forced to study most of their subject backward, or wrong-way-round. By starting from trying to make sense of processes taking place right at their feet, t ...
Plate Tectonics Notes
Plate Tectonics Notes

... characteristics of rock – material that forms the Earth’s surface and crust. Geologists map where different rock types are – both above and below the surface. They describe landforms – both in terms of how and what created them. Geologists also collect and identify fossils to help determine the age ...
Chapter 1 Powerpoint Presentation
Chapter 1 Powerpoint Presentation

...  How and why did people come to occupy a particular place?  How do they assess the physical aspects of that place and then modify them to suit their particular needs?  How do people create environmental problems by the way they use a place?  How do people interact with other places? ...
See Q. “Sampler” on packet, pages 12
See Q. “Sampler” on packet, pages 12

... 2) Intergranular cement (also called matrix) *Their strength and other properties may be different from one another and may affect further weathering, infiltration, water storage, etc. Two Sedimentary Rock Types: 1) Detrital (aka Clastic): with rock fragments/grains and cement 2) Chemical: with solu ...
CHAPTER 1 - INTRODUCTION TO PHYSICAL GEOLOGY
CHAPTER 1 - INTRODUCTION TO PHYSICAL GEOLOGY

... Earth involved the process of differentiation which allowed materials of different densities to separate and create the internal structure of our planet consisting of core, mantle and crust. The crust and uppermost rigid mantle are broken into a number of lithospheric plates which move across the su ...
How old is that rock?
How old is that rock?

... As we have discussed, the Earth is not a static thing. Once crust is laid down, lots of things can change it. When magma pushes its way through the layers, it’s called intrusion. Intrusions are YOUNGER than the rock they are intruding upon. ...
The Earth`s Structure
The Earth`s Structure

... • Generally wear down the earth’s surface • Driven directly or indirectly by sun and gravity • Weathering • Physical, Chemical, and Biological ...
Geology - Rock Cycle Notes
Geology - Rock Cycle Notes

... • Generally wear down the earth’s surface • Driven directly or indirectly by sun and gravity • Weathering • Physical, Chemical, and Biological ...
Intro2-3
Intro2-3

... landforms. When two ocean plates collide, they may form deep valleys on the ocean’s floor. When ocean plates collide with continental plates, mountain ranges are formed. Mountains are also created when two continental plates collide. When plates separate, usually on the ocean floor, they cause gaps ...
5th Gr Earth Science Template Completed
5th Gr Earth Science Template Completed

... 3. Weather conditions change because of the uneven heating of Earth’s surface by the Sun’s energy. Weather changes are measured by differences in temperature, air pressure, wind and water in the atmosphere and type of precipitation ...
The solid, outer layer of Earth that consists of the crust and the rigid
The solid, outer layer of Earth that consists of the crust and the rigid

... The process of one tectonic plate sinking beneath another into the mantle at a convergent plate boundary ...
Internal Structure of the Earth and Lithosphere
Internal Structure of the Earth and Lithosphere

... Land Use Planning Land use planning is an essential tool for pollution control and prevention. Land use categories refer to the different socioeconomic activities in a certain area, the human behaviors they create and their effect on the environment. These activities take place at a local level but ...
Geology Rocks! - Billy B. Productions
Geology Rocks! - Billy B. Productions

... concepts relating to geology such as; the earth's composition, volcanoes, plate tectonics and erosion in an accurate manner. Geology is brought alive during this show. Students are given the opportunity to become part of the performance and through song and dance relate to the dynamic energy, moveme ...
Inside Earth: Chapter 1
Inside Earth: Chapter 1

... • 64.5 hours or about 2 ½ days! That’s about the time it would take to drive from here to Disney World. ...
Chapter 3 Geosphere
Chapter 3 Geosphere

... of rock that flows very slowly and allows tectonic plates to move on top of it. 3. Mesosphere: lower part of the mantle. 4. Outer core: made of liquid nickel and iron. 5. Inner core: sphere of solid nickel and iron. ...
Chapter 2 Physical Geography: A Living Planet
Chapter 2 Physical Geography: A Living Planet

... material and moves it downstream • Delta – sediment is deposited in a fan-like landform when a river enters an ocean ...
Changes Within the Earth
Changes Within the Earth

... 2. they found mountains, deep canyons, and wide plains much like what is above water 3. samples that they took showed that the rocks on the ocean floor were much younger than the rocks above water 4. seafloor spreading – molten rock from the mantle rises beneath the underwater ridge and breaks throu ...
Weathering
Weathering

... • Karst and corvettes • http://blog.hemmings.com/index.php/2014/ 02/12/breaking-news-eight-cars-damagedby-sinkhole-at-the-national-corvettemuseum/?refer=news ...
introduction to geography part 1
introduction to geography part 1

... zones ...
Science 7
Science 7

... major branches of scientific study: earth, life, and physical sciences; ...
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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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