Landscape Development
|
|
- Noah Moore
- 5 years ago
- Views:
Transcription
1 Landscape Development
2 Slopes Dominate Natural Landscapes Created by the interplay of tectonic and igneous activity and gradation Deformation and uplift Volcanic activity Agents of gradation Mass wasting Streams Wind Glaciers
3 Slope Formation Slopes are temporary, in the context of geologic time Change may result from renewal of the activity which created them, or by other actions Change may be rapid, but, overall, is typically quite slow Earthquakes, eruptions, floods, landslides, glaciation Creep: the very slow downward adjustment of hillsides Geologists attempt to understand landforms in light of their formation and continued adjustments
4 The hydrologic cycle Figure 16.3
5 Slope Formation Rainsplash, sheetflow, rills, runoff and streams Water falls on the land and quickly enters (forms) small channels These join together in a drainage network to remove the water Channels lengthen by headward erosion, intercept other channels and grow in size and flow volume An efficient drainage system is developed
6 Longitudinal profile of a stream Figure 16.7
7 Running water Changes from upstream to downstream Profile Profile is a smooth curve Gradient decreases downstream Factors that increase downstream Velocity Discharge Channel size
8 Running water Changes from upstream to downstream Factors that decrease downstream Gradient Channel roughness Base level and graded streams Base level is the lowest point to which a stream can erode
9 Running water Base level and graded streams Two general types of base level Ultimate (sea level) Local or temporary Changing conditions causes readjustment of stream activities Raising base level causes deposition Lowering base level causes erosion
10 A waterfall is an example of a local base level
11 Adjustment of base level to changing conditions Figure 16.9
12 Drainage basin Figure 16.30
13 The drainage basin of the Mississippi River
14 Watershed of Chesapeake Bay
15 Drainage patterns Figure 16.32
16
17 Running water Stream valleys The most common landforms on Earth s surface Two general types of stream valleys Narrow valleys» V-shaped» Downcutting toward base level» Features often include rapids and waterfalls
18 Erosion in Fast-moving Streams Figure 7-7 A Steep-Gradient Stream Gradients are steep in headwaters, and streams flow fast, cut steep-sided channels, erode vigorously, and carry coarse sediment. Figure 7-8 Rivers Erode the Geosphere Arizona s Grand Canyon is an example of how effective river erosion can be. In this case the Colorado River downcut rapidly In response to uplift on the Colorado Plateau.
19 Sideways Erosion Cutbanks Figure 7-9 Erosion along River Cutbanks Can Be Hazardous Rivers obviously erode downward but they also erode sideways or laterally, especially if the gradient is lower. On the outside bend of a stream a channel may be eroded; this is called the cutbank (the stream cuts into the bank here). Opposite the cutbank is the pointbar a focus of deposition rather than erosion as streams migrate laterally.
20 Running water Stream valleys Two general types of stream valleys Wide valleys» Stream is near base level» Downward erosion is less dominant» Stream energy is directed from side to side forming a floodplain
21 Running water Stream valleys Features of wide valleys often include Floodplains» Erosional floodplains» Depositional floodplains Meanders» Cut bank and point bar» Cutoffs and oxbow lakes
22 Erosion and deposition along a meandering stream Figure Link: Map of Licking River
23 Erosion and Deposition Low Gradient Streams Near Base Level Broad loops and curves are common along the lower reaches of rivers, near their base levels. These bends, or meanders (Fig. 7-10a), change as a result of erosion and deposition working hand in hand. Figure 7-10 Meanders and Oxbow Lakes (a) Meanders erode banks where river s gradient is low. (b) If a river cuts across narrow neck of a meander loop, sedimentation may seal off the loop, transforming it into an oxbow lake.
24
25 Sediment Transport Loads Bedload, is dragged, rolled, skipped, or bounced over the river bottom the latter is referred to as the process of saltation Finer particles carried along in the river water itself are the suspended load. Dissolved minerals and some organic materials leached from soil/rock make up the dissolved load. Figure 7-11 Mechanisms of Sediment Transport Gravel-rich bedload is dominant along steeper river gradients, whereas suspended and dissolved loads are common at lower gradients.
26 Stream Carrying Capacity At a specific velocity and discharge, a stream has a maximum amount of bed and suspended load it can carry = capacity. Capacity with Velocity and Discharge, therefore more erosion and sediment transport occurs during flooding. Material transported in large rivers consists mainly of suspended load, such as silt. Figure 7-12 The World s Muddiest River China s Huang Ho (Yellow River) carries a tremendous suspended load of silt up to 70% of the river s volume. Its watershed has much loess, a silt-rich windblown sedimentary deposit.
27 Running water Incised meanders and stream terraces Incised meanders Meanders in steep, narrow valleys Caused by a drop in base level or uplift of the region Terraces Remnants of a former floodplain River has adjusted to a relative drop in base level by downcutting
28 A meander loop on the Colorado River
29 Running water Headward erosion and stream piracy A stream can lengthen its course by either Building a delta Headward erosion Headward erosion may result in stream piracy the diversion of the drainage of one stream into another
30
31
Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College
Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College Hydrologic Cycle The hydrologic cycle is a summary of the circulation of Earth s water supply. Processes involved in the hydrologic
More informationStreams. Stream Water Flow
CHAPTER 14 OUTLINE Streams: Transport to the Oceans Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. Streams Streams are the major geological agents
More informationES 105 Surface Processes I. Hydrologic cycle A. Distribution % in oceans 2. >3% surface water a. +99% surface water in glaciers b.
ES 105 Surface Processes I. Hydrologic cycle A. Distribution 1. +97% in oceans 2. >3% surface water a. +99% surface water in glaciers b. >1/3% liquid, fresh water in streams and lakes~1/10,000 of water
More informationStreams. Water. Hydrologic Cycle. Geol 104: Streams
Streams Why study streams? Running water is the most important geologic agent in erosion, transportation and deposition of sediments. Water The unique physical and chemical properties of water make it
More informationErosion Surface Water. moving, transporting, and depositing sediment.
+ Erosion Surface Water moving, transporting, and depositing sediment. + Surface Water 2 Water from rainfall can hit Earth s surface and do a number of things: Slowly soak into the ground: Infiltration
More informationEarth Science Chapter 6 Section 2 Review
Name: Class: Date: Earth Science Chapter 6 Section Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Most streams carry the largest part of their
More informationFinal Exam. Running Water Erosion and Deposition. Willamette Discharge. Running Water
Final Exam Running Water Erosion and Deposition Earth Science Chapter 5 Pages 120-135 Scheduled for 8 AM, March 21, 2006 Bring A scantron form A calculator Your 3 x 5 paper card of formulas Review questions
More informationFresh Water: Streams, Lakes Groundwater & Wetlands
Fresh Water:, Lakes Groundwater & Wetlands Oct 27 Glaciers and Ice Ages Chp 13 Nov 3 Deserts and Wind and EXAM #3 Slope hydrologic cycle P = precip I = precip intercepted by veg ET = evapotranspiration
More informationLecture Outlines PowerPoint. Chapter 5 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 5 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationRunning Water: The Geology of Streams and Floods Running Water Chapter 14
Geology 800 Today Running Water: The Geology of Streams and Floods Running Water Chapter 14 Next Class Oceans and Coasts 15 Stream Flow Streams Ribbons of water that flow down channels. Runoff Water in
More information6.1 Water. The Water Cycle
6.1 Water The Water Cycle Water constantly moves among the oceans, the atmosphere, the solid Earth, and the biosphere. This unending circulation of Earth s water supply is the water cycle. The Water Cycle
More informationRivers and Landslides
Rivers and Landslides Path of desire or path of least resistance? Desire Path: A term in landscape architecture used to describe a path that isn t designed but rather is worn casually away by people finding
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Running Water and Groundwater Running Water The Water Cycle Water constantly moves among the oceans, the atmosphere, the solid Earth, and the biosphere. This
More informationSTREAM SYSTEMS and FLOODS
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Runoff Transpiration Earth s Water and the Hydrologic Cycle The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationPrecipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration
STREAM SYSTEMS and FLOODS The Hydrologic Cycle Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle Runoff Transpiration The Hydrologic Cycle The Hydrologic Cycle Oceans not filling
More informationSTUDY GUIDE FOR CONTENT MASTERY. Surface Water Movement
Surface Water SECTION 9.1 Surface Water Movement In your textbook, read about surface water and the way in which it moves sediment. Complete each statement. 1. An excessive amount of water flowing downslope
More informationPHYSICAL GEOGRAPHY. By Brett Lucas
PHYSICAL GEOGRAPHY By Brett Lucas FLUVIAL PROCESSES Fluvial Processes The Impact of Fluvial Processes on the Landscape Streams and Stream Systems Stream Channels Structural Relationships The Shaping and
More informationRivers. Regents Earth Science Weathering & Erosion
Regents Earth Science Weathering & Erosion Name: Rivers Use your notes, the handout Weathering and Erosion and your review book to answer the following questions on Rivers. Be sure to read the information
More informationSurface Water and Stream Development
Surface Water and Stream Development Surface Water The moment a raindrop falls to earth it begins its return to the sea. Once water reaches Earth s surface it may evaporate back into the atmosphere, soak
More informationFLUVIAL PROCESSES 13 MARCH 2014
FLUVIAL PROCESSES 13 MARCH 2014 In this lesson we: Lesson Description Look at river profiles, river grading, river rejuvenation as well as the identification, description and formation of fluvial landforms.
More informationThe Hydrologic Cycle STREAM SYSTEMS. Earth s Water and the Hydrologic Cycle. The Hydrologic Cycle. Hydrologic Cycle
STREAM SYSTEMS Earth Science: Chapter 5 Reading pages 114-124 The Hydrologic Cycle Oceans not filling up Evaporation = precipitation System is balanced Earth s Water and the Hydrologic Cycle Earth s Water
More informationWhat do you need for a Marathon?
What do you need for a Marathon? Water and a snack? What about just a normal day? 1 flush = 3.5 gallons 1 flush = 3.5 gallons 10 minute shower = 20 gal 1 flush = 3.5 gallons 10 minute shower = 20 gal Jeans
More informationRivers and Streams. Streams. Hydrologic Cycle. Drainage Basins and Divides. Colorado River Drainage Basin. Colorado Drainage Basins.
Chapter 14 Hydrologic Cycle Rivers and Streams Streams A stream is a body of water that is confined in a channel and moves downhill under the influence of gravity. This definition includes all sizes of
More informationGEOL 1121 Earth Processes and Environments
GEOL 1121 Earth Processes and Environments Wondwosen Seyoum Department of Geology University of Georgia e-mail: seyoum@uga.edu G/G Bldg., Rm. No. 122 Seyoum, 2015 Chapter 6 Streams and Flooding Seyoum,
More information11/12/2014. Running Water. Introduction. Water on Earth. The Hydrologic Cycle. Fluid Flow
Introduction Mercury, Venus, Earth and Mars share a similar history, but Earth is the only terrestrial planet with abundant water! Mercury is too small and hot Venus has a runaway green house effect so
More informationmountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output
mountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output strong interaction between streams & hillslopes Sediment Budgets for Mountain Rivers Little
More informationYear 6. Geography. Revision
Year 6 Geography Revision November 2017 Rivers and World knowledge How the water cycle works and the meaning of the terms evaporation, condensation, precipitation, transpiration, surface run-off, groundwater
More informationSurface Water Short Study Guide
Name: Class: Date: Surface Water Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The three ways in which a stream carries
More informationEnvironmental Geology Chapter 9 Rivers and Flooding
Environmental Geology Chapter 9 Rivers and Flooding Flooding in Pakistan 2010-1600 killed/20000 affected The hydrologic cycle is powered by the Sun The cycle includes evaporation, precipitation, infiltration,
More informationLaboratory Exercise #3 The Hydrologic Cycle and Running Water Processes
Laboratory Exercise #3 The Hydrologic Cycle and Running Water Processes page - 1 Section A - The Hydrologic Cycle Figure 1 illustrates the hydrologic cycle which quantifies how water is cycled throughout
More informationChapter 10. Running Water aka Rivers. BFRB Pages
Chapter 10 Running Water aka Rivers BFRB Pages 101-116 Stream Erosion and Transportation Running water is all precipitation (rain, snow, etc) that falls on Earth and is pulled downhill by gravity. Running
More information3/3/2013. The hydro cycle water returns from the sea. All "toilet to tap." Introduction to Environmental Geology, 5e
Introduction to Environmental Geology, 5e Running Water: summary in haiku form Edward A. Keller Chapter 9 Rivers and Flooding Lecture Presentation prepared by X. Mara Chen, Salisbury University The hydro
More informationWeathering, Erosion, Deposition, and Landscape Development
Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into
More informationA floodplain is the flat land immediately surrounding a stream channel and innundated at 5mes of high flow.
A floodplain is the flat land immediately surrounding a stream channel and innundated at 5mes of high flow. Aggrada5on occurs when deposi5on is greater than erosion. Aggrada&on of the Rivière des Ha! Ha!
More informationTrue or False: The Earth s surface has stayed the same for thousands of years
True or False: The Earth s surface has stayed the same for thousands of years True or False: The Earth s surface has stayed the same for thousands of years The Earth s surface is always changing! Weathering
More informationChapter 11. Rivers: Shaping our landscape
Chapter 11 Rivers: Shaping our landscape Learning outcomes In this presentation you will learn: Common terms associated with rivers About the three stages of a river About the processes of river erosion
More informationSummary. Streams and Drainage Systems
Streams and Drainage Systems Summary Streams are part of the hydrologic cycle and the chief means by which water returns from the land to the sea. They help shape the Earth s surface and transport sediment
More informationREVIEW. There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL. What is WEATHERING? The breakdown of rocks at or near Earth s surface
REVIEW What is WEATHERING? Def: The breakdown of rocks at or near Earth s surface There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL CHEMICAL WEATHERING EXAMPLES: 1. OXIDATION (rust) CHEMICAL WEATHERING
More informationWhat is weathering and how does it change Earth s surface? Answer the question using
7 th Grade Lesson What is weathering and how does it change Earth s surface? Answer the question using the sentence frame. You have 4 minutes. Weathering is. This changes the Earth s surface because. 1
More informationEROSION AND DEPOSITION
CHAPTER 8 EROSION AND DEPOSITION SECTION 8 1 Changing Earth s Surface (pages 252-255) This section explains how sediment is carried away and deposited elsewhere to wear down and build up Earth s surface.
More informationLectures Hydrology & Fluvial Geomorphology. Gauley River Images. Ancients' (= Biblical) Model of Water (Hydrologic) Cycle
Lectures 11-13 13 Hydrology & Fluvial Geomorphology Gauley River Images http://www.youtube.com/watch?v=eulmuyegtz4&feature=related Ancients' (= Biblical) Model of Water (Hydrologic) Cycle Stream Water
More informationGeography Notes for Plonk Meeting
Geography Notes for Plonk Meeting Hydrologic Cycle 1. Rainfall Water falls as rain or snow if the air is cold enough. 2. Groundwater Water that seeps into the ground may be absorbed by plants or flow into
More informationRiver Processes. A) Write definitions for the terms erosion, transportation & deposition.
River Processes Lesson Aims To learn what is erosion, transportation and deposition. To learn which processes carry out erosion, transportation and deposition in river systems. Within rivers a number of
More informationWATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle
WATER ON AND UNDER GROUND Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin. Describe how floods occur and what factors may make
More information1. Any process that causes rock to crack or break into pieces is called physical weathering. Initial product = final product
Weathering 1. Any process that causes rock to crack or break into pieces is called physical weathering. Initial product = final product End Result of physical weathering is increased surface area. 2. Physical
More informationWhat are the different ways rocks can be weathered?
Romano - 223 What are the different ways rocks can be weathered? Weathering - the breakdown of rocks and minerals at the Earth s surface 1. 2. PHYSICAL WEATHERING Rock is broken into smaller pieces with
More information1. The map below shows a meandering river. A A' is the location of a cross section. The arrows show the direction of the river flow.
1. The map below shows a meandering river. A A' is the location of a cross section. The arrows show the direction of the river flow. Which cross section best represents the shape of the river bottom at
More informationNATURAL RIVER. Karima Attia Nile Research Institute
NATURAL RIVER CHARACTERISTICS Karima Attia Nile Research Institute NATURAL RIVER DEFINITION NATURAL RIVER DEFINITION Is natural stream of water that flows in channels with ih more or less defined banks.
More informationRIVERS, GROUNDWATER, AND GLACIERS
RIVERS, GROUNDWATER, AND GLACIERS Delta A fan-shaped deposit that forms when a river flows into a quiet or large body of water, such as a lake, an ocean, or an inland sea. Alluvial Fan A sloping triangle
More informationWeathering & Erosion
Weathering & Erosion Weathering and Erosion Weathering - processes at or near Earth s surface that cause rocks and minerals to break down Erosion - process of removing Earth materials from their original
More informationThe Active River. Rivers: Agents of Erosion. Key Concept Water running downhill is the dominant process in shaping the landscape.
1 What You Will Learn Moving water shapes the surface of Earth by the process of erosion. The sun is the major source of energy that drives the water cycle. Three factors that affect the rate of stream
More informationErosion and Deposition
Erosion and Deposition Erosion Sediment natural forces move rock/soil from one place to another. gravity, water, wind, glaciers, waves are causes material moved by erosion Deposition when erosion lays
More informationChapter 12: River Systems and Landforms
Chapter 12: River Systems and Landforms Base Levels: Local and Ultimate Figure 12.6 Figure 12.2 A Drainage Basin Rills and Gullies feeding into small Streams in Iowa North American Drainage Basins Figure
More informationRiver Processes. Learning Objective: Discover how a river erodes, transports and deposits material
River Processes Learning Objective: Discover how a river erodes, transports and deposits material Learning Outcomes: Compare vertical and lateral erosion Describe how a river erodes, transports and deposits
More informationChapter 2. Wearing Down Landforms: Rivers and Ice. Physical Weathering
Chapter 2 Wearing Down Landforms: Rivers and Ice Physical Weathering Weathering vs. Erosion Weathering is the breakdown of rock and minerals. Erosion is a two fold process that starts with 1) breakdown
More informationSection 5. Low-Gradient Streams. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 4 Surface Processes Section 5 Low-Gradient Streams What Do You See? Learning Outcomes In this section, you will Use models and real-time streamflow data to understand the characteristics of lowgradient
More informationPage 1. Name:
Name: 1) Which event is the best example of erosion? dissolving of rock particles on a limestone gravestone by acid rain breaking apart of shale as a result of water freezing in a crack rolling of a pebble
More informationChanging Earth s Surface
Name Date Class Changing Earth s Surface What processes wear down and build up Earth s surface? What causes the different types of mass movement? Erosion is the process by which natural forces move weathered
More informationEARTH S CHANGING SURFACE
EARTH S CHANGING SURFACE Weathering Together, weathering and erosion work continuously to wear down the material on Earth s surface. weathering process that breaks down rock and other substances of Earth
More informationTeacher s Pack Key Stage 3 GEOGRAPHY
Teacher s Pack Key Stage 3 GEOGRAPHY Geography Key Stage 3 Fieldwork Worksheet Rivers: 1. Is the water fresh or salty? (test its resistance or specific gravity) 2. Do you know where the water is coming
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 14: Sedimentary Rocks Part 2: Alluvial Fans and Rivers Instructor: Dr. Douglas W. Haywick Last Time 1) Types of Sediment 2) Sedimentary Rock
More informationMountain Rivers. Gutta cavat lapidem. (Dripping water hollows out a stone) -Ovid, Epistulae Ex Ponto, Book 3, no. 10, 1. 5
Mountain Rivers Gutta cavat lapidem (Dripping water hollows out a stone) -Ovid, Epistulae Ex Ponto, Book 3, no. 10, 1. 5 Mountain Rivers Fixed channel boundaries (bedrock banks and bed) High transport
More informationFluvial Systems Lab Environmental Geology Lab Dr. Johnson
Fluvial Systems Lab Environmental Geology Lab Dr. Johnson *Introductory sections of this lab were adapted from Pidwirny, M. (2006). "Streamflow and Fluvial Processes". Fundamentals of Physical Geography,
More informationTopic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p ) Workbook Chapter 4, 5 WEATHERING
Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p. 95-125) Workbook Chapter 4, 5 THE BIG PICTURE: Weathering, erosion and deposition are processes that cause changes to rock material
More informationEROSION, DEPOSITION AND SEDIMENTARY ROCKS. Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages Chapter 3: pages 52-54, 61-69
EROSION, DEPOSITION AND SEDIMENTARY ROCKS Reading: Earth Science Tarbuck and Lutgens Chapter 5: pages 124-133 Chapter 3: pages 52-54, 61-69 Base Level Resistant bed Resistant bed creates a local base level
More informationName. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown.
Name 1. In the cross section of the hill shown below, which rock units are probably most resistant to weathering? 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different
More information1. Base your answer to the following question on the map below, which shows the generalized bedrock of a part of western New York State.
1. Base your answer to the following question on the map below, which shows the generalized bedrock of a part of western New York State. 3. The table below describes the deposits that an observer saw while
More informationEarth Science Chapter 9. Day 6 - Finish Capillary Action Lab - Quiz over Notes - Review Worksheets over Sections 9.2 and 9.3
Earth Science Chapter 9 Day 1 Day 2 Day 3 Read Section 9.1 Surface Water Chapter 9 Term Sheet Notes over Section 9.1 Surface Water Section 9.1 Review Worksheets Quiz over Section 9.1 Notes Virtual Lab
More informationRiver/Stream Erosion Notes
Name Date ES per Mr. Williams River/Stream Erosion Notes Erosion: the of weathered material. FACT: Running water moves more sediment than ANY other type of erosion. 1. The Water Cycle What happens when
More informationNATURE OF RIVERS B-1. Channel Function... ALLUVIAL FEATURES. ... to successfully carry sediment and water from the watershed. ...dissipate energy.
1 2 Function... Sevier River... to successfully carry sediment and water from the watershed....dissipate energy. 3 ALLUVIAL FEATURES 4 CHANNEL DIMENSION The purpose of a stream is to carry water and sediment
More informationSurface Processes Focus on Mass Wasting (Chapter 10)
Surface Processes Focus on Mass Wasting (Chapter 10) 1. What is the distinction between weathering, mass wasting, and erosion? 2. What is the controlling force in mass wasting? What force provides resistance?
More information10/27/2014. Surface Processes. Surface Processes. Surface Processes. Surface Processes. Surface Processes
Hewitt/Lyons/Suchocki/Yeh Conceptual Integrated Science Chapter 25 Surface or surficial processes originate at Earth's surface and reshape its contours. Surface processes include: Weathering Erosion Deposition
More information1. Erosion by Running Water Most powerful cause of erosion
I. Destructive Forces Notes: Destructive force: a process in which land is destroyed or changed such as weathering and erosion. All landforms are a result of a combination of constructive and destructive
More information27. Running Water I (p ; )
27. Running Water I (p. 424-436; 440-444) Hydrosphere How much of the Earth s surface is covered by water? Earth's water is collectively called the and is stored in a number of so-called as follows: 1.
More informationGLG362/GLG598 Geomorphology K. Whipple October, 2009 I. Characteristics of Alluvial Channels
I. Characteristics of Alluvial Channels Self-formed morphology set by entrainment, transport, and deposition They move unconsolidated sedimentary materials present in the valley fill flood plain/bank flow
More information4. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom.
1. Sediment is deposited as a river enters a lake because the A) velocity of the river decreases B) force of gravity decreases C) volume of water increases D) slope of the river increases 2. Which diagram
More informationOverview of fluvial and geotechnical processes for TMDL assessment
Overview of fluvial and geotechnical processes for TMDL assessment Christian F Lenhart, Assistant Prof, MSU Research Assoc., U of M Biosystems Engineering Fluvial processes in a glaciated landscape Martin
More informationFLUVIAL LANDFORMS. Floodplains
FLUVIAL LANDFORMS Floodplains fairly flat & continuous surface occupying much of a valley bottom normally underlain by unconsolidated sediments subject to periodic flooding (usually once every year or
More informationRiparian Assessment. Steps in the right direction... Drainage Basin/Watershed: Start by Thinking Big. Riparian Assessment vs.
Riparian Assessment vs. Monitoring Riparian Assessment What is a healthy stream? Determine stream/riparian health Determine change or trend, especially in response to mgmt Classification = designation
More informationRiver Systems. Physical Geography Lecture - GEOG B1. Accessible on:
River Systems Physical Geography Lecture - GEOG B1 Accessible on: www.cherylnail.com Hydrology Hydrology is the scientific study of the movement, distribution, and properties of water on Earth (and other
More informationSURFACE WATER. Thompson Higher Education 2007; Monroe, Wicander, and Hazlett, Physical Geology en.wikipedia.org
SURFACE WATER Thompson Higher Education 2007; Monroe, Wicander, and Hazlett, Physical Geology www.google.com en.wikipedia.org KATRINA April 29, 2005 KATRINA April 29, 2005 Golden Canyon, Death Valley,
More informationBell Ringer. Are soil and dirt the same material? In your explanation be sure to talk about plants.
Bell Ringer Are soil and dirt the same material? In your explanation be sure to talk about plants. 5.3 Mass Movements Triggers of Mass Movements The transfer of rock and soil downslope due to gravity is
More information1/6/ th Grade Earth s Surface. Chapter 3: Erosion and Deposition. Lesson 1 (Mass Movement)
Lesson 1 (Mass Movement) 7 th Grade Earth s Surface Chapter 3: Erosion and Deposition Weathering the chemical and physical processes that break down rock at Earth s surface Mechanical weathering when rock
More informationChapter 3 Erosion and Deposition. The Big Question:
Chapter 3 Erosion and Deposition The Big Question: 1 Design a way to represent and describe the 4 types of mass movement. You may use pictures, diagrams, list, web, chart, etc 2 Chapter 3: Erosion and
More informationStream Geomorphology. Leslie A. Morrissey UVM July 25, 2012
Stream Geomorphology Leslie A. Morrissey UVM July 25, 2012 What Functions do Healthy Streams Provide? Flood mitigation Water supply Water quality Sediment storage and transport Habitat Recreation Transportation
More informationRivers T. Perron
1 Rivers T. Perron 12.001 After our discussions of large-scale topography, how we represent topography in maps, and how topography interacts with geologic structures, you should be frothing at the mouth
More informationChapter 2. Denudation: Rivers and Ice
Chapter 2. Denudation: Rivers and Ice DENUDATION: process that lowers level of land - caused by rivers, glaciers, waves & wind - involves processes of WEATHERING & EROSION Weathering Def: breakdown of
More informationHigh-Gradient Streams
Chapter 4 Surface Processes Section 4 High-Gradient Streams What Do You See? Learning Outcomes In this section, you will Use models and real-time streamflow data to understand the characteristics of highgradient
More informationRiver Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation.
River Response River Response Sediment Water Wood Confinement Valley slope Channel morphology Bank material Flow obstructions Riparian vegetation climate catchment vegetation hydrological regime channel
More informationErosion and Deposition
CHAPTER 3 LESSON 2 Erosion and Deposition Landforms Shaped by Water and Wind Key Concepts What are the stages of stream development? How do water erosion and deposition change Earth s surface? How do wind
More informationWhat we will cover. The Hydrologic Cycle. River systems. Floods. Groundwater. Caves and Karst Topography. Hot springs
Fresh Water What we will cover The Hydrologic Cycle River systems Floods Groundwater Caves and Karst Topography Hot springs On a piece of paper, put these reservoirs of water in to order from largest to
More informationScience EOG Review: Landforms
Mathematician Science EOG Review: Landforms Vocabulary Definition Term canyon deep, large, V- shaped valley formed by a river over millions of years of erosion; sometimes called gorges (example: Linville
More informationLab 13: Fluvial Processes and Landforms
Name: Lab 13: Fluvial Processes and Landforms Geomorphology is the study of Earth s surface and of the processes acting to shape it. Streams, for example, are significant continental land-shaping agents.
More informationAnticipation guide # 3
Wind Anticipation guide # 3 Creep is a type of mass movement that happens slowly over many years Oxidation is a type of physical weathering A delta is a depositional feature that occurs with glaciers The
More informationWatershed concepts for community environmental planning
Purpose and Objectives Watershed concepts for community environmental planning Dale Bruns, Wilkes University USDA Rural GIS Consortium May 2007 Provide background on basic concepts in watershed, stream,
More informationCh 10 Deposition Practice Questions
1. Base your answer to the following question on the data table below. Six identical cylinders, A through F, were filled with equal volumes of sorted spherical particles. The data table shows the particle
More informationErosion and Deposition
Erosion and Deposition Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. Water erosion begins when runoff from rainfall flows in a thin layer over the land
More informationEssential Questions. What is erosion? What is mass wasting?
Erosion Essential Questions What is erosion? What is mass wasting? What is Erosion? Erosion The transportation of sediment from one area to another Caused mainly by running water but also caused by glaciers,
More informationPat Dryer Half Moon Lake: A True Oxbow Lake? Geography 364 April 1 st, 2007
Pat Dryer Half Moon Lake: A True Oxbow Lake? Geography 364 April 1 st, 2007 Appendix Abstract 2 Introduction 3 Methods 3 Results 3 Discussion 5 Conclusion 11 1 Abstract Half Moon Lake appears to be an
More informationWater Erosion (pages )
Water Erosion (pages 272 281) Runoff and Erosion (pages 273 274) Key Concept: Moving water is the major agent of the erosion that has shaped Earth s land surface. Falling raindrops can loosen and pick
More information