SCHUSTER SLOPE LANDSCAPE MANAGEMENT PLAN. January 15, 2015
|
|
- Domenic Bridges
- 6 years ago
- Views:
Transcription
1 SCHUSTER SLOPE LANDSCAPE MANAGEMENT PLAN January 15,
2 WHY DO WE NEED A LANDSCAPE MANAGEMENT PLAN? 2
3 PROCESS FOR DEVELOPING THE SCHUSTER SLOPE LANDSCAPE MANAGEMENT PLAN 3
4 NORTH DOWNTOWN SUB AREA PLAN SLOPE DESIGN STANDARDS Adopted by City Council, October
5 PUBLIC OUTREACH July 16, 2014 Public Open House August / September Online Survey 5
6 USING BEST SCIENCE 6
7 A MANAGEMENT PLAN THAT ADDRESSES MANY INTERESTS 7
8 INTRODUCTION Presentation Outline Geologic setting Why we need a Landscape Management Plan A landscape approach to slope stability Balancing the objectives a plan to address many interests and site constraints Landscape Management Plan the details How can vegetation management accommodate views? Management Plan Implementation 8
9 GEOLOGIC SETTING 9
10 SLOPE STABILITY Definitions Slope morphology Geologic setting Slope processes GEOLOGIC SETTING 10
11 DEFINITIONS SLOPE TERMS Toe of slope Slope face Slope crest (top of slope) Upland area GEOLOGIC SETTING 11
12 DEFINITIONS SLOPE GRADIENT GEOLOGIC SETTING 12
13 DEFINITIONS ANGLE OF REPOSE The maximum slope at which loose soil will remain in place without sliding. 67% Slope 1:1.5 ft GEOLOGIC SETTING 13
14 PRO GLACIAL SLOPE Advancing continental ice sheet scoured our Commencement Bay Characteristic steep-side U shaped valley GEOLOGIC SETTING 14
15 POST GLACIAL SLOPE Retreating glaciers left behind over steepened slopes Slopes unstable Massing wasting process of erosion/sloughing, landsliding, etc. altering slope Slopes continuing to retreat in attempt to reach equilibrium conditions GEOLOGIC SETTING 15
16 PROJECT AREA GEOLOGY Glacial till/ice contact deposits Olympia beds Pre-Vashon glacial sediments Troost, K.G. In review. Geologic Map of the Tacoma North 7.5-Minute Quadrangle, Washington. U.S. Geological Survey Miscellaneous Field Investigation. Scale 1:24,000. GEOLOGIC SETTING 16
17 HISTORIC SLOPE INSTABILITY Two mapped landslides along Stadium Way LiDAR images show history of slope instability along entire slope GEOLOGIC SETTING 17
18 Mapped Landslides GEOLOGIC SETTING 18
19 Garfield Gulch Old RR ROW GEOLOGIC SETTING 19
20 Old Slide Scarps GEOLOGIC SETTING 20
21 Stadium HS Old Landslide GEOLOGIC SETTING 21
22 Old Landslide GEOLOGIC SETTING 22
23 SLOPE PROCESSES Mass wasting processes (rooting plants, borrowing animals and insects, freeze-thaw, and mechanical weathering) create a zone of weak, loose soil on slope face Thickness dependent on type of soil On steep slopes, zone of weak soil subjected to downslope movement as a result of gravity Slow downslope movement referred to as soil creep This weak layer of soil can also be subject to shallow debris flows or skin slides Debris flows remove the weak soil layer exposing the underlying parent soil Mass wasting begins and the process starts anew GEOLOGIC SETTING 23
24 SOIL CREEP Soil moving downslope due to gravity GEOLOGIC SETTING 24
25 EFFECTS OF SOIL CREEP GEOLOGIC SETTING 25
26 DEBRIS FLOWS/LANDSLIDING GEOLOGIC SETTING 26
27 SLOPE PROCESSES Lower slope dominated by skin slides Upper slope dominated by soil creep, but potential for debris flows if slope not properly managed. GEOLOGIC SETTING 27
28 WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 28
29 MANAGEMENT ELEMENTS Slope Stability Stormwater Benefit Forest Health Public Safety Views WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 29
30 SLOPES Slope stability Soil binding root systems Site constraints Over half project area >60% slopes Shallow failures Difficult plant establishment WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 30
31 SLOPES WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 31
32 STORMWATER BENEFIT Reduce surface impact/flow Evergreen, multilayered vegetation Site constraints Deciduous trees Sparse understory Erosion WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 32
33 FOREST HEALTH Restore native vegetation Target ecosystem Site constraints Invasives Lack of diversity Lack of rejuvenation Tree disease WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 33
34 PUBLIC SAFETY Create safe environment Vegetation management Site constraints Irregular users Hazard trees Slope stability WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 34
35 VIEWS Opportunity to provide views Pruning and species selection Site constraints Mismanagement Lack of species diversity Invasives WHY WE NEED A LANDSCAPE MANAGEMENT PLAN 35
36 LANDSCAPE MANAGEMENT PLAN THE DETAILS 36
37 LANDSCAPE MANAGEMENT PLAN LANDSCAPE MANAGEMENT PLAN DETAILS 37
38 SLOPES Engineering solutions Erosion control Additional requirements may apply based on slope conditions LANDSCAPE MANAGEMENT PLAN DETAILS 38
39 STORMWATER BENEFIT 2 out of every 3 trees evergreen Layered understory Dense root network LANDSCAPE MANAGEMENT PLAN DETAILS 39
40 FOREST HEALTH Invasive removal Plant diversity Natives, >90% LANDSCAPE MANAGEMENT PLAN DETAILS 40
41 PUBLIC SAFETY Crime Prevention Through Environmental Design Natural surveillance Natural access control Tree assessments LANDSCAPE MANAGEMENT PLAN DETAILS 41
42 VIEWS Phased approach Establish layered understory and canopy Pruning and maintenance Select tree removal LANDSCAPE MANAGEMENT PLAN DETAILS 42
43 VIEWS LANDSCAPE MANAGEMENT PLAN DETAILS 43
44 44
45 45 45
46 46 46
47 47 47
48 48
49 49 49
50 VIEWS LANDSCAPE MANAGEMENT PLAN DETAILS 50
51 CONCLUSIONS Geologic settings Why we need a Landscape Management Plan Landscape Management Plan Details Slope Stability Stormwater Benefit Forest Health Public Safety Views 51
52 MANAGEMENT PLAN IMPLEMENTATION 52
Day 3 Weathering and Erosion.notebook. October 02, Section 7.2. Erosion and Deposition. Objectives
Objectives Describe the relationship of gravity to all agents of erosion. Contrast the features left from different types of erosion. Analyze the impact of living and nonliving things on the processes
More informationGG101 Lecture 22: Mass Wasting. Soil, debris, sediment, and broken rock is called regolith.
GG101 Lecture 22: Mass Wasting Mass Wasting is the movement of rock and soil down a slope due to the force of gravity. Soil, debris, sediment, and broken rock is called regolith. Mass wasting creates broad
More informationClass Notes: Surface Processes
Name: Date: Period: Surface Processes The Physical Setting: Earth Science Class Notes: Surface Processes I. Weathering and Soils Weathering -! Sediments -! Weathering occurs when rocks are exposed to:
More informationMass Wasting. Revisit: Erosion, Transportation, and Deposition
Mass Wasting Revisit: Erosion, Transportation, and Deposition While landslides are a normal part of erosion and surface processes, they can be very destructive to life and property! - Mass wasting: downslope
More informationThe Earth s Crust. Weathering & Erosion
The Earth s Crust Weathering & Erosion ! Soil begins with rocks so how is rock turned into soil?! How does soil travel and move?! Without sediments our planet would decline, perhaps ceasing to exist Inside
More informationMass Wasting: The Work of Gravity
Chapter 15 Lecture Earth: An Introduction to Physical Geology Twelfth Edition Mass Wasting: The Work of Gravity Tarbuck and Lutgens Chapter 15 Mass Wasting The Importance of Mass Wasting Slopes are the
More informationUNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land
UNIT SEVEN: Earth s Water Chapter 21 Water and Solutions Chapter 22 Water Systems Chapter 23 How Water Shapes the Land Chapter Twenty-Three: How Water Shapes the Land 23.1 Weathering and Erosion 23.2
More informationMass Movements. Rock Weathering. Accumulation of Debris on Slopes. Landslides 12/8/2014
Mass Movements Already talked a little about landslides with earthquakes AKA mass wasting A mass movement is any displacement of large amounts of soil down slopes over (often) a comparatively short period
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 informationGeog 1000 Lecture 17: Chapter 10
Geog 1000 Lecture 17: Chapter 10 Landslides and Mass Movements Link to lectures: http://scholar.ulethbridge.ca/chasmer/classes/ Today s Lecture 1. Assignment 2 Due Pick up Assignment 1 if you don t have
More informationMass Wasting. Mass Wasting. Earth s s External Processes
1 Mass Wasting Presentation Modified from Instructor Resource Center on CD-ROM, Foundations of Earth Science, 4 th Edition, Lutgens & Tarbuck Mass Wasting 2 Down-slope movement of rock, loose material
More informationMass Wasting Landslides, Mudflows. Chapter 7. Geology of the Hawaiian Islands. Any Questions? Mass wasting. Mass wasting.
Geology of the Hawaiian Islands Class 17 9 March 2004 Any Questions? Mass Wasting, Mudflows Chapter 7 Mass wasting Transportation of large masses of rock Downslope movement of rock and soil debris under
More information3/22/2014. Earth s subsystems or cycles. Outline for next couple weeks. Weathering (breakdown of rock) Erosion
and Erosion Earth s subsystems or cycles Outline for next couple weeks 1. and Erosion 2. Surface water systems (rivers) 3. Groundwater systems 4. Groundwater in-class activity (grade) (breakdown of rock)
More informationGeology 101. Reading Guides for Chapters 5 and 14 Weathering: the Breakdown of Rocks (p. 142)
Geology 101 Name Reading Guides for Chapters 5 and 14 Weathering: the Breakdown of Rocks (p. 142) Please read the introduction to the chapter. What is the difference between weathering and erosion? Weathering
More informationChapter 12 Weathering and Erosion
Chapter 12 Weathering and Erosion Multiple Choice Select the definition that most nearly defines the given word. 1. Landform A. chemical combination of metallic elements with oxygen B. layer of weathered
More informationClyde River Landslide
Clyde River Landslide Department of Geology, Perkins Hall, University of Vermont, Burlington, VT 05405 Abstract: This paper investigates a landslide on the Clyde River in Newport, Vermont. The landslide
More information3 Erosion and Deposition by Ice
CHAPTER 12 3 Erosion and Deposition by Ice SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: What are glaciers? How do
More informationLandscape. Review Note Cards
Landscape Review Note Cards Last Ice Age Pleistocene Epoch that occurred about 22,000 Years ago Glacier A large, long lasting mass of ice which forms on land and moves downhill because of gravity. Continental
More information9/13/2011 CHAPTER 9 AND SUBSIDENCE. Case History: La Conchita Landslide. Introduction
CHAPTER 9 SLOPE PROCESSES, LANDSLIDES, AND SUBSIDENCE Case History: La Conchita Landslide La Conchita: small coastal community 80 km (50 mi) northwest of Los Angeles Landslide occurred on January 10, 2005
More informationSurface Processes on the Earth. Rocks, Weathering, Erosion and Soil
Surface Processes on the Earth Rocks, Weathering, Erosion and Soil ROCKS AND ROCK CYCLE Rock types Three main types of rock Igneous Metamorphic Sedimentary Igneous Form when magma or lava cools and hardens
More informationNeed of Proper Development in Hilly Urban Areas to Avoid
Need of Proper Development in Hilly Urban Areas to Avoid Landslide Hazard Dr. Arvind Phukan, P.E. Cosultant/Former Professor of Civil Engineering University of Alaska, Anchorage, USA RI District Governor
More informationPHYSICAL GEOGRAPHY. By Brett Lucas
PHYSICAL GEOGRAPHY By Brett Lucas WEATHERING & MASS WASTING Denudation Disintegration, wearing away, and removal of rock material Involves three activities: Weathering is the break down of rocks into smaller
More informationMass Wasting. Requirements for Mass Wasting. Slope Stability. Geol 104: mass wasting
Mass Wasting Movement of earth materials downslope, driven by Gravitational Forces. Landslides - general term for rock or soil movement. In U.S., on average, mass wasting causes 1 to 2 billion dollars
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 informationMass Movements, Wind, and Glaciers
Mass Movements,, and Glaciers SECTION 8.1 Mass Movement at Earth s Surface In your textbook, read about mass movement. Use each of the terms below just once to complete the passage. avalanche creep landslide
More informationChapter 11 10/30/2013. Mass Wasting. Introduction. Factors That Influence Mass Wasting. Introduction. Factors That Influence Mass Wasting
Introduction Chapter 11 Mass wasting - The downslope movement of material resulting from the force of gravity. Mass Wasting Mass wasting results when the force of gravity acting on a slope exceeds the
More informationSoil Formation. Lesson Plan: NRES B2-4
Soil Formation Lesson Plan: NRES B2-4 1 Anticipated Problems 1. What are five different factors that affect soil formation? 2. What are some different types of parent material that affect soils? 3. What
More informationContrasting Behaviour of Two Recent, Large Landslides in Discontinuous Permafrost Little Salmon Lake, Yukon, Canada
Contrasting Behaviour of Two Recent, Large Landslides in Discontinuous Permafrost Little Salmon Lake, Yukon, Canada Ryan R. Lyle BGC Engineering Inc. Kamloops, British Columbia D. Jean Hutchinson Queen
More informationEngineering Geology ECIV 3302
Engineering Geology ECIV 3302 Instructor : Dr. Jehad Hamad 2019-2018 Chapter (5) Weathering & Soil Chapter 5: Weathering, Soil, and Mass Wasting External processes include : (1) Weathering (2) Mass wasting
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 informationSLOPE FAILURE SLOPES. Landslides, Mudflows, Earthflows, and other Mass Wasting Processes
GEOL g406 Environmental Geology SLOPE FAILURE Landslides, Mudflows, Earthflows, and other Mass Wasting Processes Read Chapter 5 in your textbook (Keller, 2000) Gros Ventre landslide, Wyoming S. Hughes,
More informationPreliminaries to Erosion: Weathering and Mass Wasting
Preliminaries to Erosion: Weathering & Mass Wasting All things deteriorate in time. Virgil 1 Preliminaries to Erosion: Weathering and Mass Wasting Denudation The Impact of Weathering and Mass Wasting on
More informationGateway Trail Project
Gateway Trail Project Debris Flow Hazard Assessment By: Juan de la Fuente April 30, 2010 Background- On April 22, 2010, the Shasta-Trinity National Forest (Mt. Shasta-McCloud Unit) requested a geologic
More informationThe Importance of Mass Wasting
Mass Wasting: The Work of Gravity Earth Chapter 15 Chapter 15 Mass Wasting The Importance of Mass Wasting Slopes are the most common elements in our physical landscape Slopes may appear to be stable, but
More informationWeathering, Mass Wasting and Karst
Weathering, Mass Wasting and Karst Capable of wearing down anything that the internal processes can build. Gravity, water, wind and ice Denudation - the overall effect of disintegration, wearing away and
More informationSection 3. Slopes and Landscapes. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 4 Surface Processes Section 3 Slopes and Landscapes What Do You See? Learning Outcomes In this section, you will Calculate the angle of repose for different kinds of soils and other granular materials.
More informationMASS MOVEMENTS, WIND, AND GLACIERS
Date Period Name MASS MOVEMENTS, WIND, AND GLACIERS SECTION.1 Mass Movements In your textbook, read about mass movements. Use each of the terms below just once to complete the passage. avalanche creep
More informationAN APPROACH TO THE CLASSIFICATION OF SLOPE MOVEMENTS
Training/workshop on Earthquake Vulnerability and Multi-Hazard Risk Assessment: Geospatial Tools for Rehabilitation and Reconstruction Effort 13 31 March 2006, Islamabad, Pakistan AN APPROACH TO THE CLASSIFICATION
More informationAppendix F4.11 Geologic Unit Summaries, Hazard Areas, and Boring Locations
Appendix F4.11 Geologic Unit Summaries, Hazard Areas, and Boring Locations Appendix F4.11 Geologic Unit Summaries and Hazard Areas TABLE F4.11-1 Summary of Geologic Units and their Engineering Properties
More informationLAB 5: LANDSLIDE RECOGNITION AND MAPPING
Geology 350 1 LAB 5: LANDSLIDE RECOGNITION AND MAPPING OBJECTIVES: a. to learn to recognize and classify landslides on airphotos and topographic maps b. to learn to recognize landslide topography on topographic
More informationWeathering, Erosion and Deposition
Weathering, Erosion and Deposition Shaping the Earth s Surface Weathering the process of breaking down rocks into smaller fragments Erosion the transport of rock fragments from one location to another
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 informationHow does Rock become Exposed to the Surface?
Weathering How does Rock become Exposed to the Surface? Most rocks, like granite, form under earth s surface. The rocks uplift and eventually make their way to earth s surface. Conditions on the surface
More informationEarth Science, 10e. Edward J. Tarbuck & Frederick K. Lutgens
Earth Science, 10e Edward J. Tarbuck & Frederick K. Lutgens Weathering, Soil, and Mass Wasting Chapter 3 Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College Earth's external processes
More informationThe landforms of Svalbard
The landforms of Svalbard Content Periglacial landforms -) ice-wedges -) rock glaciers -) pingos -) solifluction -) avalanches -) debris flows -) rock falls -) nivation -) aeolian landforms Glacial landforms
More informationEXTERNAL LAND FORMING PROCESSES
NAME SCHOOL INDEX NUMBER DATE EXTERNAL LAND FORMING PROCESSES WEATHERING 1 1998 Q 7 (a) (i) What is the difference between weathering and mass wasting (ii) List five processes involved in chemical weathering
More informationUnsafe Ground: Landslides and Other Mass Movements
Unsafe Ground: Landslides and Other Mass Movements Mass Movements Downslope motion of earth materials by gravity. Mass movements are a type of natural hazard. Natural feature of the environment. Can cause
More informationThe Effect of Weather, Erosion, and Deposition in Texas Ecoregions
The Effect of Weather, Erosion, and Deposition in Texas Ecoregions 7.8B: I can analyze the effects of weathering, erosion, and deposition on the environment in ecoregions of Texas Weathering The breakdown
More informationWearing Down Landforms
Wearing Down Landforms Denudation Denudation has also been called gradation. It is the Natural loss of soil and rock debris, blown away by wind or washed away by running water, laying bare the rock below.
More informationSLOPE PROCESSES, LANDSLIDES, AND SUBSIDENCE
CHAPTER 9 SLOPE PROCESSES, LANDSLIDES, AND SUBSIDENCE La Conchita slide January 10, 2005 Triggered by heavy rainfall, reactivation along an older landslide surface (35,000 years ago, 6000 years ago, and
More information2/23/2009. Visualizing Earth Science. Chapter Overview. Deserts and Drylands. Glaciers and Ice Sheets
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 6 Deserts, Glaciers and Ice Sheets Chapter Overview Deserts and Drylands Glaciers and Ice Sheets Deserts Geography Categorization of deserts
More informationSedimentation Rate Change in the Winooski River Delta
Sedimentation Rate Change in the Winooski River Delta Chris Ricker and Brian Connelly Abstract Historical air photographs, from 1937 show the Winooski River Delta extended much farther into Lake Champlain
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 informationEssentials of Geology, 11e
Essentials of Geology, 11e and s Chapter 5 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Jennifer Cole Northeastern University Earth
More informationNatural Shoreline Landscapes on Michigan Inland Lakes
Natural Shoreline Landscapes on Michigan Inland Lakes Excerpts from Chapters 2 and 3 Photo Photo by Jane by Jane Herbert Herbert Did you know? Twenty-four species of amphibians, 25 species of reptiles,
More informationTime allowed: 1 hour 30 minutes
SPECIMEN ASSESSMENT MATERIAL: SET 2 GCSE GEOGRAPHY Paper 1 Living with the physical environment Specimen Materials For this paper you must have: a pencil a ruler. Time allowed: 1 hour 30 minutes Instructions
More informationWhat factors affect the angle of a slope?
Climate Rock type and Structure What factors affect the angle of a slope? Aspect Fast mass movements Slides: Slides are movements along the SLIP PLANE, i.e. a line of weakness in the rock or soil structure.
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 informationUnit E: Basic Principles of Soil Science. Lesson 2: Understanding Soil Formation
Unit E: Basic Principles of Soil Science Lesson 2: Understanding Soil Formation Important Terms Alluvium Bedrock Chemical weathering Climate Glacial till Loess Native vegetation Organic matter Outwash
More informationSCIENCE TEST1 (VWILLIAMSSCIENCETEST1)
Name: Date: 1. In which of the following areas would soil erosion MOST LIKELY occur if they received the same amount of rainfall? A. a forest B. flat agricultural lands C. agricultural lands on steep slopes
More informationLecture 10 Glaciers and glaciation
Lecture 10 Glaciers and glaciation Outline Importance of ice to people! Basics of glaciers formation, classification, mechanisms of movement Glacial landscapes erosion and deposition by glaciers and the
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 informationWeathering, Soil, and Mass Movements
Tarbuck Lutgens Weathering, Soil, and Mass Movements 5.1 Weathering Mechanical Weathering Mechanical weathering occurs when physical forces break rock into smaller and smaller pieces without changing the
More informationChapter 16 Weathering, Erosion, Mass Wasting. Chapter 16 Weathering, Erosion, Mass Wasting. Mechanical Weathering
Weathering, Erosion and Mass Wasting Weathering is the the breakdown of solid rock at or near the Earth's surface. Chapter 16 Weathering, Erosion, Mass Wasting Does weathering of rock remove or add CO
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 informationLandslides & Debris Flows
T.#Perron# #12.001# #Landslides#&#Debris#Flows# 1# Landslides & Debris Flows Many geologic processes, including those shaping the land surface, are slowacting, involving feedbacks that operate over many
More informationThe Seattle-area geologic mapping project and the geologic framework of Seattle
The Seattle-area geologic mapping project and the geologic framework of Seattle Troost, K.G., D.B. Booth, S.A. Shimel, and M.A. O Neal, Univ. of Washington, Seattle 98195 Introduction The Puget Lowland
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 informationWeathering and Erosion
Weathering and Erosion OBJECTIVE: Explain how erosion and deposition shape Earth s surface by matching and using models How do erosion and deposition shape Earth s surface? Deposition Formation Transported
More informationGeology 101. Reading Guides for Chapters 6 and 12
Geology 101 Name Chapter 6: Weathering and Soils (p. 160): Reading Guides for Chapters 6 and 12 This chapter is about the processes involved in the disintegration of rock. Weathering is often mistaken
More informationENGINEERING EVALUATION OF THE STANLEY MINE ADVENTURE PARK AREA CLEAR CREEK COUNTY, COLORADO. Prepared for:
braun Braun Consulting Engineers ENGINEERING EVALUATION OF THE STANLEY MINE ADVENTURE PARK AREA CLEAR CREEK COUNTY, COLORADO Prepared for: STANLEY MINES ADENTURE PARK 3375 W. POWERS CIRCLE LITTLETON, COLORADO
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 informationScience and Health EFFECT OF EROSION ON THE CONDITION OF SOIL AND LAND SHAPE
4 Module 51 Science and Health EFFECT OF EROSION ON THE CONDITION OF SOIL AND LAND SHAPE A DepEd-BEAM Distance Learning Program supported by the Australian Agency for International Development To the Learner
More informationA Homeowner s Guide to Landslides for Washington and Oregon
Protect Your Home and Property 1 A Homeowner s Guide to Landslides for Washington and Oregon Washington Geological Survey and Oregon Department of Geology and Mineral Industries LANDSLIDES ARE ONE OF THE
More informationSESSION 6: FLUVIAL LANDFORMS
SESSION 6: FLUVIAL LANDFORMS KEY CONCEPTS: Fluvial Landforms Management of River Catchment Areas Slope Elements X-PLANATION: FLUVIAL LANDFORMS Rivers form landforms as they erode the landscape. These landforms
More informationEarth s Surface. Name Date. Key Concepts Choose the letter of the best answer.
Earth s Surface Key Concepts Choose the letter of the best answer. Unit Test A 1. A river starts as a steep channel in the mountains. It then leaves the mountains and enters a flatter area of land. It
More informationCHAPTER FIVE 5.0 STABILITY OF CUT SLOPES IN THE STUDY AREA. them limited by a thick canopy of vegetation and steep slope angles.
CHAPTER FIVE 5.0 STABILITY OF CUT SLOPES IN THE STUDY AREA 5.1. Introduction Ukay Perdana area is a developing community with continuous building activities and road construction. There are thus only left
More informationProf. B V S Viswanadham, Department of Civil Engineering, IIT Bombay
19 Module 5: Lecture -1 on Stability of Slopes Contents Stability analysis of a slope and finding critical slip surface; Sudden Draw down condition, effective stress and total stress analysis; Seismic
More informationSHORELINE AND BEACH PROCESSES: PART 2. Implications for Coastal Engineering
SHORELINE AND BEACH PROCESSES: PART 2 Implications for Coastal Engineering Objectives of the lecture: Part 2 Show examples of coastal engineering Discuss the practical difficulties of ocean engineering
More informationMatch up the pictures and key terms
Match up the pictures and key terms 1 Plucking Striations 3 Roche Mountonnees 2 Chatter Marks 4 What is the difference between plucking and abrasion? Glacial Processes Erosion, Weathering and Deposition
More informationWeathering, Erosion, Deposition
Weathering, Erosion, Deposition The breakdown of rocks at or near the Earth s Surface. Physical Chemical - The breakdown of rock into smaller pieces without chemical change. - Dominant in moist /cold conditions
More informationObjectives. Introduction to Soils. Terms to know: What is soil? Study of Soils. The Soil Body 11/9/2012
Objectives Explain what soil is and where it comes from Define a soil body List examples of the five soil-forming factors Explain how soils develop Introduction to Soils Terms to know: What is soil? Alluvial
More information9/23/2013. Introduction CHAPTER 7 SLOPE PROCESSES, LANDSLIDES, AND SUBSIDENCE. Case History: La Conchita Landslide
Introduction CHAPTER 7 SLOPE PROCESSES, LANDSLIDES, AND SUBSIDENCE Landslide and other ground failures posting substantial damage and loss of life In U.S., average 25 50 deaths; damage more than $3.5 billion
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 information3/8/17. #20 - Landslides: Mitigation and Case Histories. Questions for Thought. Questions for Thought
#20 - Landslides: Mitigation and Case Histories Web Exercise #3 (Volcanoes) Due Wednesday There is a 2-point penalty for every day the assignment is late. Exam 1 Scores Scores and exam key are posted Vaiont
More informationGuided Notes Surface Processes. Erosion & Deposition By: Glaciers
Guided Notes Surface Processes Erosion & Deposition By: Glaciers K. Coder 2015 26) How does moving ice erode and deposit sediments? Glaciers (Movement of Ice): a naturally formed mass of ice and snow that
More informationBeyond the Book. FOCUS Book
FOCUS Book Suppose your city wants to build a new housing development on a steep slope outside town. Design a model to test whether the land is safe from the types of landslides you read about in this
More information2011 Pearson Education, Inc.
Weathering and Soil Earth - Chapter 6 Earth s External Processes Weathering the physical breakdown and chemical decomposition of rock Mass wasting the transfer of rock and soil downslope under the influence
More information2011 Pearson Education, Inc.
Weathering and Soil Earth - Chapter 6 Earth s External Processes Weathering the physical breakdown and chemical decomposition of rock Mass wasting the transfer of rock and soil downslope under the influence
More informationNumerical Study of Relationship Between Landslide Geometry and Run-out Distance of Landslide Mass
Numerical Study of Relationship Between Landslide Geometry and Run-out Distance of Landslide Mass Muneyoshi Numada Research Associate, Institute of Industrial Science, The University of Tokyo, Japan Kazuo
More informationWeathering, Erosion, and Deposition Guided Notes
1. Weathering, Erosion, and Deposition 2. Outline Section 1: Weathering Section 2: Erosion Section 3: Deposition Section 4: Case Study Weathering, Erosion, and Deposition Guided Notes 3. Section 1: Weathering
More informationAPPALACHIAN COLLUVIAL
LANDSLIDE PROBLEMS ON APPALACHIAN COLLUVIAL SLOPES Geohazards in Transportation in the Appalachian Region Charleston, WV August 5 7, 2008 RICHARD E. GRAY DIGIOIA, GRAY & ASSOCIATES, LLC. 570 BEATTY ROAD
More informationEarth s Dynamic Surface
Earth s Dynamic Surface Key Concepts What is the difference between physical and chemical weathering? How do water, ice, and wind change Earth s surface? Changing Earth s Surface What do you think? Read
More informationHILLSLOPE STABILITY. Focus in the Westfork Area of Washington County, Arkansas. Environmental Geology Dr. Paul Lowrey
Environmental Geology Dr. Paul Lowrey Team Members Christine Gossett Jennifer Lane Lauren Morrison Nicole Sage Focus in the Westfork Area of Washington County, Arkansas HILLSLOPE STABILITY INTRODUCTION
More informationChanging Landscapes: Glaciated Landscapes. How do glaciers move?
Changing Landscapes: Glaciated Landscapes How do glaciers move? What you need to know Differences between cold-and warm-based glaciers, their locations and rates of movement Glacier ice movement including
More informationSection 1: Weathering and Soil Formation. We will study some of the processes that contribute to soil formation
Section 1: Weathering and Soil Formation We will study some of the processes that contribute to soil formation ***Minerals form rocks. The decomposition of rocks and minerals will form soil. Minerals are
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 informationShoreline and Climate Change Adaptation Alternatives for The Letter Parcel, Bolinas Lagoon
Shoreline and Climate Change Adaptation Alternatives for The Letter Parcel, Bolinas Lagoon Scenic shoreline vista of Bolinas Lagoon and ridges, from Letter Parcel, March 2016 Peter Baye, Coastal Ecologist
More informationUsing Weather and Climate Information for Landslide Prevention and Mitigation
Using Weather and Climate Information for Landslide Prevention and Mitigation Professor Roy C. Sidle Disaster Prevention Research Institute Kyoto University, Japan International Workshop on Climate and
More informationTHE CHANGING SURFACE OF THE EARTH
THE CHANGING SURFACE OF THE EARTH Key words Drain geological agent weathering erosion Sediment deposition transport The landscape is a consequence of the action of two types of geological processes; internal
More information