Forest Slope Stability Project, Phase II

Total Page:16

File Type:pdf, Size:1020Kb

Forest Slope Stability Project, Phase II 1 , .., r-; · ':::iv ' \ ! GEOLOG'/ ?J . OLYf,/lPIA. WA::JHii\iGTON 00504 FOREST SLOPE STABILITY PROJECT PHASE II VOLUME I WDOE 81-14 SEPTEMBER. 1981 Donald W. Moos Director COVER PHOTO Big Slump Mountain and Clearwater Creek, Middle Fork of the Nooksack River area V '.,,' •.' ~ FOREST SLOPE STABILITY PROJECT PHASE II for Washington State Department of Ecology WDOE 81-14 by Allen J. Fiksdal and Matthew J. Brunengo 1981 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, WA 98504 This study was conducted under a grant from the United States Environmental Protection Agency with funds from Section 208 of the Federal Clean Water Law (Public Law 95-217). The contents of this paper do not necessarily reflect the views and policies of EPA and WDOE, nor does mention of trade names of commercial products constitute endorsement or recommendation for use, PREFACE To assist forest managers in the identification of potential sediment sources, landforms keyed to mass wasting features and potential were ~apped in parts of five river basins in western Washington State. The study areas were chosen as representative of the different geologic, geomorphic, and climatic regions found in western Washington so that extrapolation of this study could be carried to adjoining drainages. The following report on methods used and findings is accompanied by orthophoto maps (scale 1:24,000) for the Middle Fork of the Nooksack, Green, South Fork of the Toutle, Clear­ water, and Grays Rivers. The maps have mass wasting features delineated and landforms outlined. The landforms relate to the geology and erosional processes and are rated for slope instability potential~low, moderate, or high. (The orthophoto maps that accompany this report are bound separately, Volume II.) III CONTENTS Page· Preface . .......... , ....... , .............................. , .................... , ...... , III Introduction ... , ............. , ... , ........................... , ............... ,........ 1 Mapping procedures and products ..•..•••.. , , , , , .• , • . • . • . • • • . • . • • . • • • • . • • . • • 2 Mass wasting ................................. , ............................. , . 3 Slump-earthflows ...... , ............ , ... , .. , , . 3 Debris avalanches ....•.•••..... , , , .•....••.. , •.• , . • • . • . • . • . • . • . • 4 Debris torrents . ........ , , ................ , ................. , .... , .. , , .. , 5 Stream erosion, ..... , .•..•......•...•.....• , . • . • • . • • • . • . • . • . • . • . • 6 Rock slide . ..................................................... , . 6 Rockfall ... , ....... ,.................................................... 6 Snow avalanche chutes, .••• ,, .....•.....•...•••.•...•..•.•...........• ,, 7 Road sidecast failure ..•.•.. , ... , ...•...•...•.•.. , ••. , ..•....••. , . • • • • • . 7 Roadcut backslope failure. , ••..•.•.••. , .•.• , ...•......••••.....•....••. , 7 Summary............................... ,....................................... 8 Landforms ... , ............. , , ................ , , .................... , , .. , .. , ... , ... , . , . 8 Alluvial-glacial terrain •. ,.,, .........•...••.•.. , .........•...............•..• ,. '9 Bedrock terrain .. , , .•....•........ , ......•• , , , , , • . • . • . • • . • . • . • . • • • . 10 Landslide terrain .•.... , . , ••....•.•...•...•. , .............. , •.•.•...•...• , • • . • 13 North Cascades-Middle Fork of the Nooksack River area •..•••. , ••••.•.• , •• , .•• , • , , , • , 14 Alluvial-glacial terrain .. ,., ••• , ...•........••.•.....•. ,., ••.. ,, ••.• , ..•.••.. ,.. 16 Floodplains ...... , . , .. , ........... , .... , ........................ , . 16 Terraces ............. , ........ , ...................... , .. , . , ......... , , . 16 Valley benches . , , • , ..•...••.......••••.....•.• , ..••••••.• , •• , , •• , .••. , , 16 Alluvial fans and cones ..•••.......••.•. , . • . • • . • . • . • . • . • • . 16 Continental glacial deposits .....•.•••....• , , .•. , • • . • . • . • . • • . • . • • 17 Glaciated valleys ....••..............••. , •...••.• , . • . • . • • • . • . • • . • 17 Cirque floors . ............................. , ............. , , . , . 17 Cirque headwalls •.•.....•••• , .•....•...• , • . • • . • • . • . • . • • . • 17 Mature bedrock terrain • • • . • . • . • . • • • • . • . • • . • . • . • . • . • . • . 17 Moderate slopes .... , ............................................... , . 17 Steep slopes . .......... , ....... , , ............................ , ........ , . 18 Twin Sisters foothills ..•....•......•..••..•.•...• , •.••.. , ...•.. , ...• , . 18 Twin Sisters alpine zone ...... , .. , ..•..•..• , ..• , .....•.•...••.•..... , .. , 18 Sandstone-shale terrain ••..•.•. , , •.•... , ..... , .•.•.•.• , , •... , .• , •.••......•... , . 18 Dip slopes. , ....... , . , ... , , . 19 Scarp slopes, •.•.•...••.••••... , , ••....••••.•..•..••....•.•... , .• , , , .. , • 19 Ribbed slopes ..... , ........................................ , ........... 20 Undercut slopes • , , , •......•.....••.••.. , .•... , . , .•.•....••..•...•.• , • • . 20 V Page North Cascades-Middle Fork of the Nooksack River area--Continued Landslide terrain .......•.... , • . • . • . • . • . • 20 Slump landforms ........ ,, ..• ,,,.,., .. , ....... ,,., •.. ,,,., ..•...•....... 20 Incised valleys , , • , .....• , , ... , , , ... , , , •.. , . , •...•...•.. , ....... , , , • • . • . 21 General instability and hazards , ... , , ..••. , ... , , • . • . • . • . • . 23 Central Cascades-Green River area ..••..............•.....•...•.•.•.........••.•.••. 23 Alluvial-glacial terrain .•...•....•...•.•.. , •..... , .....•.••..•..••.............. 25 Floodplains .•.•.•...•.... , ..•......•.... , ....... , . • • . • . • . 25 Tributary valleys, . • . • . • . • • . • . • . • . • . • • . • 25 Terraces , ........•.....•..•..... , ....•• , ...• , , ....••. , . • . 25 Benches ...•...•..•..••.•...•. , •..•.•... , ..•.•...•... , .. ,., ......•.....• 26 Alluvial fans .....•..••...•.................... , • , ........•.•.. , . • 26 Glaciated valleys .•............••....• , .....•.....•.• , • . • . • . 26 Cirque floors .......•....... , •...•. , ... , .........•.. , . • . • . 26 Headwalls ..•....... , ... , •.. , ... , .. , ......•.. , ..•.••....•...•... , . • • . 26 Volcaniclastic terrain. ...•... , .. , ...•...•..•...•..... , .....• , ....•..........•... 26 Flat bedding attitudes ....•.••.... , ....••..............•.. , . • . • 26 Dip slopes ••...•.•...•••.•......•••....... , ...... , ....•••.•....... , .. ,.. 26 Scarp slopes •.......• , . , ....•. , . , ..••...• , ...••••. , • . • . • . • . • 27 Eagle Gorge terrain •.....•.•.....•... ,, .....•......... , ..... , ............•..... 27 Dip slopes .......• , ... , •.•.•....••. , ......•.....•...... , , . • • . 27 Scarp slopes ....•.... , ....•.............•...•. ,, .. ,..................... 28 Snow Creek terrain. , .•.......•...... , ..•. , .•.....•...•.•... , .•..•.... , . • • . 28 Snow Creek slopes ................ , ......••. , ....•...................... 28 Intrusive terrain. .... , •...•.... , ... ,.,, ..... ,, .. , ..... , ..•.........•....... , .. , 28 Intrusive terrain. ............ , ..... , •...•............. ,, ..••... ,........ 28 Landslide terrain • , .. , .. , ...•.. , ...••.... , . • . • . • . • . • . • . 29 Slumps on volcaniclastic rocks ....•.•. , . • . • . • . • 29 Slumps in Eagle Gorge terrain .............•.....••.•.....•...•.•. , ....• 29 Incised valleys •.•......•.....•....... , .•....... , . • . • . • . • . • 29 General instability and hazards . • . • . • • . • • . • . • • • 29 Southern Cascades-South Fork of the Toutle River area ..•......•....... , .•..•.... , . 31 Alluvial-glacial terrain ......................................•..•........ ,...... 34 Mudflow-alluvial valley .. , ..............•...•.• , . , ..• , ...•.... , ... , . • 34 Older mudflows or pyroclastic flows ............ , ... , .... , ... , .. , ... , . 34 Terraces and benches.. , ..... , •. , .. , ... , ........ , ............. , ..... , . 34 Glaciated valleys ...•....... , •. , .•.......•.•....•.. , ... , . , ... , .. , . , , . 34 Glacial headwalls-valley sides ..•.. , .•• , . , . , .•.. , ..• , . , . , . , .. , , ... , . , ... , 35 VI Page Southern Cascades-South Fork of the Toutle River area--Continued Dissected volcanic terrain, .......•.•••••••...•.••••••..•• , •.•. , , •.• , , .• , ••• , • • • 35 Dissected slopes •.•..•.••....•.•.•.•...•••.•.• , , ••..••..•••..•••••. , •• , . 35 Dip slopes, , , . , . , , , • , , • , . , , • , , . , , , , • , , , , •. , • , , • , , , .•. , , , .••• , , , , , , . , • , • • 35 Scarp slopes.,., •. ,,.,., ••• ,,,,,,.,.,,,,,,.,,,,,,,,.,,,.,,,,, .••• ,., .•• , 35 Ohanapecosh terrain . 36 Ohanapecosh dip slopes, • , , , • , , , . , • , , , , .• , , , , • , . , , , , , • , • , •.• , , .•. , , , • , , • 36 Ohanapecosh scarp slopes •. , . , • , • , , , , , , , , , • , , •••••. , , , , , , • , , , , , .•• , , •. , , 36 Bedrock terrain. , , , , • , •.•. , , • , , , , , , • , , .. , . , •• , • , , , , , , , , , , , , • , , • , . , •. , , ... , • . • • . 36 Lava flow ....... , ........ ,............................................... 37 Goat mountain intrusion •• , , , , , •. , , , , , , , , , , , , , , , , , , •• , • , • , • , , •• , , • • • • . • . • 37 Landslide terrain , , • , , ..• , . , , • , , . , , . , , , . , , • , , • , , , . , , , .• , • , ••• , •• , . , ..• , . • . • • . 37 Incised valleys ..••• , , .•..• , • , , , , ••••.. , .. , •.. , , ... , ..• , , •. ·, , • . • . • • • • 37 Eroding
Recommended publications
  • ACTIVITY 7 – MARKING GUIDELINE: 1. a – Cuesta B – Homoclinal Ridge C
    ACTIVITY 7 – MARKING GUIDELINE: 1. A – Cuesta B – Homoclinal ridge C – Hogsback 2. Sedimentary 3. Inclined rocks with different resistance to erosion. Soft rock erodes away more quickly than hard rock. 4. The dip slope is 10–25° to the horizontal. Folding can result in cuesta basins and cuesta domes. 5. Farming can take place on dip slopes. Roads and railways can be built parallel to these landscapes. Gaps or poorts between homoclinal ridges can be good sites to build dams. Cuesta basins yield artesian water. Cuesta domes may contain oil and natural gas (fracking). Fertile valleys and plains between cuestas are suitable for human settlements. These ridges are used for forestry, tourism, recreation and nature conservation. These ridges can be used for defence purposes. (Accept any relevant answer) ACTIVITY 8 – MARKING GUIDELINE: 1. It occurs when strata are subjected to stress (compression, tension, volcanic intrusion, or tectonic movement) and they become tilted relative to their original (horizontal) position. Faulting or folding causes the strata to be tilted. The beds may be inclined in any direction with the angle of the dip slope between 0º to 90º. 2. Cuesta dome 3. The scarp slope faces inward, and dip slopes faces outward. 4. HOMOCLINICAL RIDGE: HOGSBACK: 5. HOMOCLINICAL RIDGE: HOGSBACK: • The angle of the dip slope lies 25º – 45º; • The angle of the dip slope is more than 45º; • Rivers cut poorts through the ridges; • There is very little difference in the gradient of the scarp and dip slopes ACTIVITY 9 – MARKING GUIDELINE: 1. A ridge that develop in tilted sedimentary rock characterised by a gentle slope and a steep slope 2.
    [Show full text]
  • Types of Landslides.Indd
    Landslide Types and Processes andslides in the United States occur in all 50 States. The primary regions of landslide occurrence and potential are the coastal and mountainous areas of California, Oregon, Land Washington, the States comprising the intermountain west, and the mountainous and hilly regions of the Eastern United States. Alaska and Hawaii also experience all types of landslides. Landslides in the United States cause approximately $3.5 billion (year 2001 dollars) in dam- age, and kill between 25 and 50 people annually. Casualties in the United States are primar- ily caused by rockfalls, rock slides, and debris flows. Worldwide, landslides occur and cause thousands of casualties and billions in monetary losses annually. The information in this publication provides an introductory primer on understanding basic scientific facts about landslides—the different types of landslides, how they are initiated, and some basic information about how they can begin to be managed as a hazard. TYPES OF LANDSLIDES porate additional variables, such as the rate of movement and the water, air, or ice content of The term “landslide” describes a wide variety the landslide material. of processes that result in the downward and outward movement of slope-forming materials Although landslides are primarily associ- including rock, soil, artificial fill, or a com- ated with mountainous regions, they can bination of these. The materials may move also occur in areas of generally low relief. In by falling, toppling, sliding, spreading, or low-relief areas, landslides occur as cut-and- La Conchita, coastal area of southern Califor- flowing. Figure 1 shows a graphic illustration fill failures (roadway and building excava- nia.
    [Show full text]
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]
  • Mass Wasting and Landslides
    Mass Wasting and Landslides Mass Wasting 1 Introduction 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 For convenience, definition of landslide includes all forms of mass-wasting movements Landslide and subsidence: naturally occurred and affected by human activities Mass wasting Downslope movement of rock and soil debris under the influence of gravity Transportation of large masses of rock Very important kind of erosion 2 Mass wasting Gravity is the driving force of all mass wasting Effects of gravity on a rock lying on a hillslope 3 Boulder on a hillside Mass Movement Mass movements occur when the force of gravity exceeds the strength of the slope material Such an occurrence can be precipitated by slope-weakening events Earthquakes Floods Volcanic Activity Storms/Torrential rain Overloading the strength of the rock 4 Mass Movement Can be either slow (creep) or fast (landslides, debris flows, etc.) As terrain becomes more mountainous, the hazard increases In developed nations impacts of mass-wasting or landslides can result in millions of dollars of damage with some deaths In less developed nations damage is more extensive because of population density, lack of stringent zoning laws, scarcity of information and inadequate preparedness **We can’t always predict or prevent the occurrence of mass- wasting events, a knowledge of the processes and their relationship to local geology can lead to intelligent planning that will help
    [Show full text]
  • General Geology
    BilimTook.com BilimTook.com BilimTook.com BilimTook.com BilimTook.com BilimTook.com BilimTook.com BilimTook.com BilimTook.com CHAPTER – 1 GENERAL GEOLOGY 1.1. GEOLOGY- A FASCINATING DISCIPLINE OF NATURAL SCIENCE Our home planet “The Earth” is a member of the solar system. Also known as the ‘Blue Planet’, it is the only heavenly body of revolution that has a delicate balance of physico-chemical conditions, which support sustenance of life that is unique and special. Geology is a natural scientific discipline and is a term derived from the summation of two ‘Greek’ words such as ‘Ge or Geo’ meaning the earth and ‘Logos’ meaning science or discourse. It pertains to the study of the earth as a whole or part thereof. In a broader sense, geology could be reframed as ‘Earth Science’ which considers the whole earth as closed system, which is ever dynamic and a mosaic of four interactive parts that are ever changeable both among and within them. These four parts are called four reservoirs of materials of the earth (Fig.1.1) which also represent the four open systems such as (i) THE ATMOSPHERE which surrounds the – earth’s surface as a continuous canopy (layer) composed of a gaseous mixture of nitrogen (N), oxygen (O), hydrogen (H), carbon Fig.1.1: Reservoirs of earth materials and transfer of energy - 1 - BilimTook.com dioxide (CO2) and water vapour (H2O↑). (ii) THE HYDROSPHERE which forms the storehouse of earth’s total water regime comprising the oceanic and sea water, stream (river) water, lake water, surface run-offs, frozen water in form of snow and ice, and underground water (iii) THE GEOSPHERE, which is the solid earth composed of soils, regolith (loosely cemented rock particles), solid rocks, layers of rock-metal association and metallic alloys (Fe-Ni), as is observed and interpreted from the top towards the centre of the earth.
    [Show full text]
  • Mass Movements General Anatomy
    CE/SC 10110-20110: Planet Earth Mass Movements Earth Portrait of a Planet Fifth Edition Chapter 16 Mass movement (or mass wasting) is the downslope motion of rock, regolith (soil, sediment, and debris), snow, and ice. General Anatomy Discrete slump blocks Head scarp Bulging toe Road for scale Disaster in the Andes: Yungay, Peru, 1970 Fractures rock, loosens soil particles. Seismic energy overstresses the system. Yungay, Peru, in the Santa River Valley beneath the heavily glaciated Nevado Huascarán (21,860 feet). May, 1970, earthquake occurred offshore ~100 km away - triggered many small rock falls. An 800-meter-wide block of ice was dislodged and avalanched downhill, scooping out small lakes and breaking off large masses of rock debris. Disaster in the Andes: Yungay, Peru, 1970 More than 50 million cubic meters of muddy debris traveled 3.7 km (12,000 feet) vertically and 14.5 km (9 miles) horizontally in less than 4 minutes! Main mass of material traveled down a steep valley, blocking the Santa River and burying ~18,000 people in Ranrachirca. A small part shot up the valley wall, was momentarily airborne before burying the village of Yungay. Estimated death toll = 17,000. Disaster in the Andes: Yungay, Peru, 1970 Before After Whats Left of Yungay. Common Mass Movements Rockfalls and Slides Slow Fast Debris Flows Slumping Lahars and Mudflows Solifluction and Creep These different kinds of mass movements are arranged from slowest (left) to fastest (right). Types of Mass Movement Different types of mass movement based on 4 factors: 1) Type of material involved (rock, regolith, snow, ice); 2) Velocity of the movement (slow, intermediate, fast); 3) Character of the movement (chaotic cloud, slurry, coherent mass; 4) Environment (subaerial, submarine).
    [Show full text]
  • Weathering, Erosion, and Mass-Wasting Processes
    Weathering, Erosion, and Mass-Wasting Processes Designed to meet South Carolina Department of Education 2005 Science Academic Standards 1 Table of Contents (1 of 2) Definitions: Weathering, Erosion, and Mass-Wasting (slide 4) (Standards: 3-3.8 ; 5-3.1) Types of Weathering (slide 5) (Standards: 3-3.8 ; 5-3.1) Mechanical Weathering (slide 6) (Standards: 3-3.8 ; 5-3.1) Exfoliation (slide 7) (Standards: 3-3.8 ; 5-3.1) Frost Wedging (slide 8) (Standards: 3-3.8 ; 5-3.1) Temperature Change (slide 9) (Standards: 3-3.8 ; 5-3.1) Salt Wedging (slide 10) (Standards: 3-3.8 ; 5-3.1) Abrasion (slide 11) (Standards: 3-3.8 ; 5-3.1) Chemical Weathering (slide 12) (Standards: 3-3.8 ; 5-3.1) Carbonation (slide 13) (Standards: 3-3.8 ; 5-3.1) Hydrolysis (slide 14) (Standards: 3-3.8 ; 5-3.1) Hydration (slide 15) (Standards: 3-3.8 ; 5-3.1) Oxidation (slide 16) (Standards: 3-3.8 ; 5-3.1) Solution (slide 17) (Standards: 3-3.8 ; 5-3.1) Biological Weathering (slide 18) (Standards: 3-3.8 ; 5-3.1) Lichen, Algae, and Decaying Plants (slide 19) (Standards: 3-3.8 ; 5-3.1) Plant Roots (slide 20) (Standards: 3-3.8 ; 5-3.1) Organism Activity: Burrowing, Tunneling, and Acid Secreting Organisms (slide 21) (Standards: 3-3.8 ; 5-3.1) Differential Weathering (slide 22) (Standards: 3-3.8 ; 5-3.1) 2 Table of Contents, cont. (2 of 2) Types of Erosion (slide 23) (Standards: 3-3.8 ; 5-3.1) Fluvial (slide 24) (Standards: 3-3.8 ; 5-3.1) Aeolian (slide 25) (Standards: 3-3.8 ; 5-3.1) Ice: Glacial and Periglacial (slide 26) (Standards: 3-3.8 ; 5-3.1) Gravity (slide
    [Show full text]
  • Alphabetical Glossary of Geomorphology
    International Association of Geomorphologists Association Internationale des Géomorphologues ALPHABETICAL GLOSSARY OF GEOMORPHOLOGY Version 1.0 Prepared for the IAG by Andrew Goudie, July 2014 Suggestions for corrections and additions should be sent to [email protected] Abime A vertical shaft in karstic (limestone) areas Ablation The wasting and removal of material from a rock surface by weathering and erosion, or more specifically from a glacier surface by melting, erosion or calving Ablation till Glacial debris deposited when a glacier melts away Abrasion The mechanical wearing down, scraping, or grinding away of a rock surface by friction, ensuing from collision between particles during their transport in wind, ice, running water, waves or gravity. It is sometimes termed corrosion Abrasion notch An elongated cliff-base hollow (typically 1-2 m high and up to 3m recessed) cut out by abrasion, usually where breaking waves are armed with rock fragments Abrasion platform A smooth, seaward-sloping surface formed by abrasion, extending across a rocky shore and often continuing below low tide level as a broad, very gently sloping surface (plain of marine erosion) formed by long-continued abrasion Abrasion ramp A smooth, seaward-sloping segment formed by abrasion on a rocky shore, usually a few meters wide, close to the cliff base Abyss Either a deep part of the ocean or a ravine or deep gorge Abyssal hill A small hill that rises from the floor of an abyssal plain. They are the most abundant geomorphic structures on the planet Earth, covering more than 30% of the ocean floors Abyssal plain An underwater plain on the deep ocean floor, usually found at depths between 3000 and 6000 m.
    [Show full text]
  • Open-File Report 08-03-1
    STATE OF MARYLAND Martin O’Malley, Governor DEPARTMENT OF NATURAL RESOURCES John R. Griffin, Secretary MARYLAND GEOLOGICAL SURVEY Jeffrey P. Halka, Director OPEN-FILE REPORT 08-03-1 By James P. Reger and Emery T. Cleaves Maryland Geological Survey 2008 STATE OF MARYLAND Martin O’Malley Governor Anthony G. Brown Lieutenant Governor DEPARTMENT OF NATURAL RESOURCES John R. Griffin Secretary Maryland Department of Natural Resources 580 Taylor Avenue, Annapolis, MD 21401 Toll-free in Maryland 1-877-260-8DNR Outside of Maryland 1-410-260-8400 TTY users call via Maryland Relay. http://www.dnr.Maryland.gov MARYLAND GEOLOGICAL SURVEY Jeffrey P. Halka Director Maryland Geological Survey 2300 St. Paul Street Baltimore, Maryland 21218 General MGS Telephone Number: 410-554-5500 http://www.mgs.md.gov Copies of this Open-File Report are available only as a PDF file from the Maryland Geological Survey at http://www.mgs.md.gov . For additional assistance and/or updates on this or other Maryland Geological Survey publications, please contact the Maryland Geological Survey at the address above. The facilities and services of the Maryland Department of Natural Resources are available to all without regard to race, color, religion, sex, age, national origin, or physical or mental disability. CONTENTS page ● Explanatory Text for the Physiographic Map of Maryland...............................................1 ▪ The Basics...................................................................................................................1 ▪ The Physiographic
    [Show full text]
  • Recognition and Identification of Landslides
    Chapter Four Recognition and Identification of Landslides Arthur M Ritchie The problems of recognition of land- movements have actually taken place or slides and identification of landslide are likely to do so in the future, and the types are as complex as are the ma- means of identifying the various types terials and processes that cause them. of landslides and their constituent parts. As treated more fully in Chapter Three, The application of these methods and the basic conditions that favor slides criteria to the solution of landslide prob- depend to a large extent on the char- lems appears in succeeding chapters, par- acter, stratigraphy and structure of the ticularly in Chapter Six. underlying rocks and soils, on the topog- .raphy, climate and vegetation, and on Evidence for Actual or Potential surface and underground waters. All of Landslides these factors vary widely from place to place; their variations are reflected in ENVIRONMENTAL FACTORS differences in the rate and kind of land- slide movements that result from their A knowledge of the general setting is interaction. essential in the recognition of either po- Because so many variables are in- tential or actual landslides. By setting is volved in the production of landslides, meant all the factors that make up the it is natural that many tools, theoretical physical environment - geology, soils, and practical, must be used in recogniz- topography, climate - for a difference in ing and classifying them. The selection any single factor, such as climate, can of methods and criteria for use in solu- have pronounced effect on the other fac- tion of a given problem is made with tors, hence on the probability of slides.
    [Show full text]
  • Landslide Types and Processes
    Chapter Three Landslide Types and Processes David J. Varnes3 It is the purpose of this chapter to re- geology, and hence lie outside the prov- view the whole range of earth move- ince of the committee. ments that may properly be regarded as landslides and to classify these move- Types of Landslides ments according to factors that have some bearing on prevention or control. CLASSIFICATION As defined for use in this volume the term "landslide" denotes downward and Many classifications have already been outward movement of slope-forming ma- proposed for earth movements, based terials composed of natural rock, soils, variously on the kind of . material, type artificial fills, -or combinations of these of movement, causes, and many other materials. The moving mass may pro- factors. There are, in. fact, so many such ceed by any one of three principal types schemes embedded with varying degrees of movement: falling, sliding, or flowing, of firmness in geological and engineering or by their combinations. Parts of a literature that the committee has ap- landslide may move upward while other proached the question of a "new" classi- parts move downward. The lower limit fication with considerable misgivings. As of the rate of movement of landslide ma- Terzaghi has stated (1950, p. 88), "A terial is restricted in this book by the phenomenon involving such a multitude economic aspect to that actual or po- of combinations between materials and tential rate of movement which provokes disturbing agents opens unlimited vistas correction or maintenance. Normal sur- for the classification enthusiast. The re- ficial creep is excluded.
    [Show full text]
  • Mass Wasting
    Frank Press, Raymond Siever, John Grotzinger, and Thomas H. Jordan Mass Wasting Understanding Earth Process by which Fourth Edition material moves downslope under Chapter 12: Mass the force of gravity Wasting Copyright © 2004 by W. H. Freeman & Company 1 2 Factors Influencing Mass Movement Mass Movement is Classified on the Basis of: • Nature of slope materials • Nature of material • Steepness of slope • Velocity of movement • Water content • Nature of movement • Slope stability 3 4 Mass Movement Depends on Water Content 5 6 Water Content Lose of Steep slopes vegetations and in damp sand root systems maintained by increases moisture susceptibility of between soils to erosion grains and mass movement 7 8 Types of Rock Mass Movement • Rock fall • Rock slide • Rock avalanche 9 10 Rock Fall Rockfall in Zion National Park 11 12 Rockslide Rockslide The rapid movement of large blocks of detached bedrock sliding more or less as a unit 13 14 Rockslide Rock Avalanche The rapid* mass movement of broken rock material, often riding on a cushion of trapped air. Usually triggered b y an earthquake. *10’s to 100’s of km/hr 15 16 Rock Avalanches Triggered by an Rock Avalanche Earthquake (Nov. 3, 2002) in Alaska 17 18 Types of Unconsolidated Mass Creep Movement Unconsolidated Flows The downhill movement of soil and other debris, typically at rates of Creep about 1 to 10 mm/year Earth Flow Increased velocity Debris Flow Earth Flow 19 20 Evidence of Creep 21 22 Earthflow Earthflow A fluid movement of relatively fine‐ grained material, e.g. soil, weathered shale, and clay.
    [Show full text]