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Introduction To World Geography
Introduction To World Geography

... • Physical Characteristics – Features of the Earth’s surface, such as landforms, water systems, climate patterns, and plant and animal life. • Physical Processes – Physical processes are nature's methods of operation that produce, maintain, or alter Earth's physical systems. • Physical processes ca ...
Name: Date: Period: ______ Chapter 13 Study Guide 1. What is soil
Name: Date: Period: ______ Chapter 13 Study Guide 1. What is soil

... Geosphere: includes the thin layer of soil and rocks on Earth’s surface and all of the underlying layers of Earth; example a cliff, the largest reservoir of carbon can be found here. Biosphere: all the living things on Earth; example people 4. What is the least dense layer of the geosphere? Outer cr ...
Unit 3 study Guide
Unit 3 study Guide

... 21.) What are the different types of seismic waves? Give information about each type. Body Waves: P-waves – bend slightly when they travel from one layer to another ------ S-waves – cannot travel through liquid material Surface Waves: travel along the surface * They all travel outwards in all direc ...
Chapter 14
Chapter 14

... gigantic jigsaw puzzle. The plates have three types of boundaries. Natural hazards such as earthquakes and volcanoes are likely to be found at plate boundaries. ...
Table of Contents - Milan Area Schools
Table of Contents - Milan Area Schools

... • In some lineages, periods of gradual evolution have been interrupted by periods in which changes in the physical or biological environment created conditions favorable for the rapid evolution of new traits. ...
oceanic - geography and history 1eso social studies
oceanic - geography and history 1eso social studies

... WEATHERING NEED NOT INVOLVE THE MOVEMENT OF MATERIAL ...
World Regions in Global Context: Peoples, Places, and
World Regions in Global Context: Peoples, Places, and

... 1) Identify spatial patterns in certain phenomena. 2) Analyze the spatial patterns and ask why they exist. 3) Determine what processes led to a specific spatial pattern. 4) Analyze how this process operates, which allows for prediction. 5) Analyze how this spatial process interacts with other phenom ...
Mineral Resources
Mineral Resources

... Enrichment by chemical weathering – Other minerals are removed leaving ore ...
Teacher Pre-assessment
Teacher Pre-assessment

... d. Its density 31. Which of these is most likely formed when a continental and oceanic plate collide? a. An alpine glacier b. A rain shadow desert c. A rift valley d. A subduction zone 32. If a planet was discovered that had tectonic plates that moved more rapidly than those on Earth, which of the f ...
Landform
Landform

... As water moves, it carries away sediment. This sediment is eventually dropped in a new location. Wind also picks up sediment as it blows across the land. A good image of erosion and deposition by wind is a sand dune. One side is eroded while the sand is deposited on the other side. Glaciers scrape a ...
Earth: Chapter 1
Earth: Chapter 1

... 1. waves break when they reach __________ water a. breaking waves release a tremendous amount of _____; they can ______ and ______________ rock, eventually turning it into _______ C. Waves can create a variety of features along a ____________ 1. sea stacks = offshore columns of _________________ 2. ...
weathering?
weathering?

... 50.) A hot spot is an area where material deep inside earth’s crust rises creating volcanoes. ...
Integrated Science Chapter 19 Name
Integrated Science Chapter 19 Name

... materials exposed at Earth’s surface Z. a crack in the Earth created when rocks on either side of a break ...
Lesson Title: Tectonic Forces World Geography, Module 1, Lesson 6
Lesson Title: Tectonic Forces World Geography, Module 1, Lesson 6

... Another physical process is called erosion. Erosion in all of its forms reshapes landforms and coastal regions, as well as riverbeds and riverbanks. Erosion occurs when weathered material is moved by the action of wind, water, ice, or even gravity. For erosion to take place, a transporting agent (su ...
Clastic (detrital)
Clastic (detrital)

... • Can be from glacial activity • Are rarer than Ss and Sh because they are usually deposited in a system that has not reached ...
CH 5 Earth`s Phys Enviro
CH 5 Earth`s Phys Enviro

... Def: periodic large scale warming of surface waters of tropical eastern Pacific Ocean ...
Ch. 5 Lecture Power Pt
Ch. 5 Lecture Power Pt

... Def: periodic large scale warming of surface waters of tropical eastern Pacific Ocean ...
Name ____________ Date ______________ Period ________
Name ____________ Date ______________ Period ________

... Fault - A crack within Earth’s rocky crust, where rock has been fractured, and where rocks move past each other. ...
Contribution of glacial-isostatic adjustment to tectonic
Contribution of glacial-isostatic adjustment to tectonic

... Charles University in Prague, Czech Republic ...
Final Exam - UTEP Geology Homepage
Final Exam - UTEP Geology Homepage

... expansion & fracturing, abrasion, organic activity  Chemical weathering: dissolution, oxidation, hydrolysis  Primary “agents” of erosion: wind, water, gravity, ice Determining Geologic Ages:  Relative ages: Principles of Original Horizontality, Superposition, Crosscutting Relationships, Faunal Su ...
Light: The Cosmic Messenger
Light: The Cosmic Messenger

... • Was Earth’s geology destined from birth? – Many of Earth’s features determined by size, distance from Sun, and rotation rate – Reason for plate tectonics still a mystery. – Maybe to the authors of our textbook, but wet rocks behave differently than dry rocks. This is well known to seismologist, ge ...
Chapter 2: The need for Earth Heritage Conservation
Chapter 2: The need for Earth Heritage Conservation

... Understanding how processes have operated in the past – the climate system, soil formation, desertification and the evolution and extinction of plants and animals – contributes to understanding the problems of the present. We may be able to use this knowledge to forecast volcanic activity, earthquak ...
Keynote Solid Earth: Imaging Earth`s interior
Keynote Solid Earth: Imaging Earth`s interior

... Permanent exchange of material recycled between surface and depth (water, rocks, gaz) ...
Michelle Mindick
Michelle Mindick

... buckle  and  break,  is  that  they  form  large  mountain  ranges.   ...
1st Semester Post Test Study Guide 2010 – 2011 KEY 1. Define
1st Semester Post Test Study Guide 2010 – 2011 KEY 1. Define

... The shaking from the movement of rock beneath Earth’s surface; release of energy 33. What is a volcano? Weak spot in crust where magma has come to the surface 34.Explain the two types of weathering. Give examples of each. chemical and mechanical processes that break down the surface Mechanical weath ...
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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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