Geometry.Net - the online learning center
Home  - Basic_L - Landslides
e99.com Bookstore
  
Images 
Newsgroups
Page 6     101-120 of 136    Back | 1  | 2  | 3  | 4  | 5  | 6  | 7  | Next 20
A  B  C  D  E  F  G  H  I  J  K  L  M  N  O  P  Q  R  S  T  U  V  W  X  Y  Z  

         Landslides:     more books (100)
  1. Risk Assessment Methodologies with Application to Selected Large Landslides in Europe
  2. Landslides
  3. Landslides/Landslide Mitigation (Reviews in Engineering Geology) by James E. Slosson, Arthur G. Keene, et all 1992-12
  4. Estimating the costs of landslide damage in the United States (Geological Survey circular) by Robert W Fleming, 1980
  5. GOVERNING PARTY WINS LANDSLIDE VICTORY IN GUBERNATORIAL, LEGISLATIVE, & MAYORAL ELECTIONS IN COAHUILA STATE.: An article from: SourceMex Economic News & Analysis on Mexico
  6. Landslide: The How and Why of Nixon's Victory by Arthur Pearl, 1973-06
  7. The Landslide by Stephen Gilbert, 1944
  8. Crumbling Earth: Erosion & Landslides (Turbulent Planet) by Mary Colson, 2005-07
  9. Landslides: Mass Wasting, Soil, and Mineral Hazards (The Hazardous Earth) by Timothy, Ph.D. Kusky, 2008-04-30
  10. Large landslides, composed of megabreccia, interbedded in Miocene basin deposits, southeastern Arizona (Geological Survey professional paper ; 1008) by Medora Louise Hooper Krieger, 1977
  11. Asonada electoral. (elecciones, Venezuela)(TT: Electoral landslide) (TA: elections, Venezuela): An article from: Siempre! by Gerardo Yong, 1998-12-10
  12. Landslides by Griffiths, 1999-01-01
  13. Landslides 1st European by Rybar, 2002-01-01
  14. Landslide by Desmond Bagley, 1967

101. Dark Peak Fieldwork - Geography In The Peak District
Virtual tour through the Dark Peak. Covers the geographical themes of peat formation and erosion, vegetation, geology, water quality and landslides. Research from the School of geography, Manchester University.
http://www.art.man.ac.uk/Geog/fieldwork
@import url(darkpeak.css); Jump to Main Menu Sitemap WebCT Dark Peak Fieldwork
The Dark Peak Field Guide
What's what in the Dark Peak Field Guide...
Background Where is the Peak District? Why is it so special? These questions are answered here... Virtual Tour A transect which runs from Alport Moor and Snake Pass on the A57 to Torside Reservoir in the Longdendale valley. Themes More in-depth information on the topics of water quality geology vegetation landslides and spatial data Research Group Some of the research undertaken in the School of Geography's Upland Environments Research Unit. Data Archive Downloads of datasets and images of the Dark Peak (Not Yet Available). Glossary Don't know its meaning? The Glossary defines the technical terms / words and phrases used.
Also contains a Vegetation Glossary (under construction) describing the plants commonly found throughout the Dark Peak. Bibliography The Bibliography contains papers and books to follow up topics in more detail. Links The page highlights the interesting, fun and useful sites about the Peak District and other broader interests.
Where is the Virtual Tour area?

102. ScienceMaster - JumpStart - Volcanic Landslides
JumpStart Earth Science. Volcanic landslides. Volcanic landslides can be sudden and deadly. Start of landslide. What are volcano landslides?
http://www.sciencemaster.com/jump/earth/slides.php

Homework Helper
Jumpstart Science Topics Learning Galleries
Today is
JumpStart - Earth Science
Volcanic Landslides
Volcanic landslides can be sudden and deadly
Looking downstream along the Upper Toutle, at Mount St. Helens' debris avalanche.
Photograph by Lyn Topinka on February 2, 1984
USGS/Cascades Volcano Observatory
Start of landslide
What are volcano landslides?
Volcano landslides range in size from less than 1 km to more than 100 km , reached speeds of 50-80 m/s (180-288 km/hr), and surged up and over a 400 m tall ridge located about 5 km from the volcano!
Landslide enters valley
Illustrations by B. Myers
How are volcano landslides generated?
Landslides are common on volcanoes because their massive cones (1) typically rise hundreds to thousands of meters above the surrounding terrain; and (2) are often weakened by the very process that created themthe rise and eruption of molten rock. Each time magma moves toward the surface, overlying rocks are shouldered aside as the molten rock makes room for itself, often creating internal shear zones or oversteepening one or more sides of the cone. Magma that remains within the cone releases volcanic gases that partially dissolve in groundwater, resulting in a hot acidic hydrothermal system that weakens rock by altering rock minerals to clay. Furthermore, the tremendous mass of thousands of layers lava and loose fragmented rock debris can lead to internal faults and fault zones that move frequently as the cone "settles" under the downward pull of gravity.

103. Mining & Geological Engineering - University Of Arizona
Earth Engineering is a field critical to sustaining and improving the quality of life for people in the US, and all over the world. Whether it is designing an environmentally safe copper mine, predicting the danger posed by landslides and earthquakes, or building a tunnel under the English Channel; Mining and Geological Engineers play an integral role in addressing the important problems of an environmentally conscious society.
http://www.mge.arizona.edu/
The University of Arizona
1235 E. North Campus Dr., Mines 229
P.O. Box 210012
Tucson, AZ 85721
Ph: 520-621-6063
Fax: 520-621-8330 email: mgedept@email.arizona.edu Questions, Comments, Suggestions?
Contact MGE Webmistress
Elsa Morales at elsam@u.arizona.edu Last updated 2/05/2004 s="na";c="na";j="na";f=""+escape(document.referrer)

104. Landslides And Mass-Wasting
landslides and MassWasting. Gravity is a constant force, always pulling towards the center of the Earth. This tireless force moves
http://www.geo.arizona.edu/geo2xx/geo218/UNIT6/lecture18.html
Landslides and Mass-Wasting
Gravity is a constant force, always pulling towards the center of the Earth. This tireless force moves material "down hill" in a process known as mass-wasting . Most people think of mass wasting in terms of landslides , which is a rapid displacement of rock and soil (which is a major hazard almost 2 billion dollars per year losses in the US alone!). However, mass-wasting covers many different phenomena, some of which are quite slow. Classifications of Mass-wasting A slump is a type of slope failure which involves the rotational movement of soil or rock a fall is a sudden, nearly vertical movement of rock or soil for example from an overhanging cliff. A slide is similar to a slump except the material does not rotate. Block slides have coherent blocks move down the hill side, while a debris slide is a jumble of material. A flow is the rapid movement of a mixture of rock/soil with a significant component of water or air. Creep is an imperceptibly slow flow. Factors controlling Mass-wasting hazards
Disaster occurs when mass wasting interacts with human society. In general, this means that certain factors conspire to cause a

105. CNN.com - Ecuadorean Rains Leave More Than 40 Dead - June 13, 2001
CNN
http://cnn.com/2001/WORLD/americas/06/13/ecuador.landslides/index.html
MAIN PAGE WORLD U.S.
WEATHER
...
ABOUT US

CNN TV what's on
show transcripts

CNN Headline News

CNN International
...
askCNN

EDITIONS CNN.com Asia
CNN.com Europe

set your edition
Languages Time, Inc. Time.com People Fortune EW
Ecuadorean rains leave more than 40 dead
QUITO, Ecuador (CNN) Thirty-six people died in a landslide Tuesday, buried under mud and rocks that tumbled from a mountain onto a highway in the province of Napo, the Ecuadorean Red Cross said. The accident brings the number of people killed in the country to 41 as a result of heavy rains, which began last Friday. Tuesday's victims were waiting for the reopening of the road that leads to Baeza, 30 miles east of the capital. It was shut down Monday as a result of several landslides. None of those caused any injuries. Elsie Andrade, a National Civil Defense spokeswoman, said the victims "had set up an improvised camping ground, where they were waiting for the highway to be reopened when the mountain fell on top of them." Communication with the remote area, where cell phones and radio transmissions do not work, was difficult. Red Cross workers, fire officials and police were searching for any possible survivors, trying to recover the victims' bodies, and said more dead could be buried under the mountains of mud which covered the narrow highway, a rural road that leads to the Amazon.

106. Landslides - King County Emergency Services
Prepare Respond Go up one level, You re in Emergency Services » Prepare Respond » Hazards Disasters » landslides. landslides.
http://www.metrokc.gov/prepare/preparerespond/hazardsdisasters/landslides.aspx
Emergency Services Office of Emergency Management
Search this section only Contact Us Print You're in Emergency Services Landslides King County Office of Emergency Management
3511 NE 2nd Street
Renton, WA 98056
Landslides
We have seen the power of landslides as a secondary hazard associated with the severe winter storm that hit the Puget Sound region in December 1996 and January 1997. Heavy snowstorms were followed by a warming trend that caused quick melting, runoff and flooding. This period was then followed by rain. This lead to over 100 slides in King County over the subsequent two-month period. King County was also hard hit by landslide damage in 1972. The Seattle area was particularly hard hit due to urbanization and geologic conditions.
Although landslides can and do occur in almost any part of the state, the most vulnerable areas are the Puget Sound Basin and King County. Due to the high population density and the fact that many structures are built either on top of or below bluffs and slopes subject to land sliding, more lives are endangered and there is a greater potential for damage or destruction to private and public property. Many of the major valleys and shoreline bluffs of Puget Sound are bordered by steeply sloping unconsolidated glacial deposits that are highly susceptible to landslides. Other vulnerable areas include the Cascade Mountain passes leading to eastern Washington.

107. CNN.com - Rain Triggers Mountain Collapse In Northern India - August 11, 2000
CNN
http://www.cnn.com/2000/ASIANOW/south/08/11/india.landslides.ap/index.html
asianow Editions myCNN Video ... Feedback
CNN Sites CNN CNN Europe CNNfn CNNSI myCNN CNNfyi AllPolitics Languages
Search
AsiaNow TIME Only Asiaweek Only CNN.com CNNSI.com CNNfn.com The Web
ASIANOW

TOP STORIES
Faith, madness, magic mix at sacred Hindu festival

MORE

TOP STORIES
Tanker spills remaining fuel near Galapagos as captain detained

Final two Texas fugitives make first court appearance
Gore accepts visiting professor post at Columbia Lott calls Justice Department 'cesspool,' Ashcroft foes 'extremists' ... MORE MARKETS 4:30pm ET, 4/16 DJIA NAS SPORTS Jordan says farewell for the third time ... LOCAL EDITIONS: CNN.com Europe change default edition MULTIMEDIA: video video archive audio multimedia showcase ... more services E-MAIL: Subscribe to one of our news e-mail lists Enter your address: DISCUSSION: chat feedback CNN WEB SITES: CNNfyi.com CNN.com Europe AsiaNow Spanish ... Korean Headlines TIME INC. SITES: Go To ... Time.com People Money Fortune EW CNN NETWORKS: CNN anchors transcripts Turner distribution SITE INFO: help contents search ad info ... jobs WEB SERVICES:
Rain triggers mountain collapse in northern India
August 12, 2000

108. Nearctica - Geophysics - Avalanches And Landslides
Avalanches and landslides. Click Here. Special Segments. Current avalanche conditions in Canada and accident information. landslides AND MUDSLIDES.
http://www.nearctica.com/geology/avalan.htm
Avalanches and Landslides Special Segments Butterflies of North America Conifers of North America Eastern Birds List of N.A. Insects Home Eastern Wildflowers General Topics Natural History Ecology Family Environment Evolution Home Education Home Conservation Geophysics Paleontology Commercial Organizations Return to Geophysics Main Page AVALANCHES Cyberspace Snow and Avalanche Center . Jim Frankenfield. This site is a good place to start if you are interested in avalanches. You'll find articles on avalanches and avalanche safety. Current conditions are also featured along with an index to photographs of avalanches on the web. There is a little of everything here. Recommended. Avalanche Information . Rocky Mountain Hiking. An introduction to avalanches, stability evaluation, and avalanche safety. Recommended. Avalanche . Nova Online. This web site is primarily a history of the making of a show for NOVA on PBS. It also has, however, segments on avalanches in general and a primer on avalanche safety. Westwide Avalanche Network . A miscellaneous collection of information and links related to avalanches and avalance safety. Swiss Federation Snow and Avalanche Research Davos . This site is a great resource for the physics of avalanches and avalance safety. Colorado Avalanche Information Center . Basic avalanche information, current avalanche conditions in Colorado, and some very nice avalanche photographs.

109. Landslides, Debris Flows, & Rockfalls - Utah Geological Survey
landslides Events Information. House damaged by the April 6, 2004 debris flow in Farmington, Utah. Damaging landslides 20012003.
http://geology.utah.gov/utahgeo/hazards/landslide/

ugs
utah geology geologic hazards / landslides
House damaged by the April 6, 2004 debris flow in Farmington, Utah. Landslides are common natural hazards in Utah. They often strike without warning and can be destructive and costly. Common types of landslides in Utah are debris flows, slides, and rock falls. Many landslides are associated with rising ground-water levels due to rainfall, snowmelt, and landscape irrigation. Therefore, landslides in Utah typically move during the months of March, April, and May, although debris flows associated with intense thunderstorm rainfall are common in July.
Recent Landslides
2001-2003 Landslides
Reduce Your Risk
UGS' Role
Recent Landslide Events
Damaging Landslides 2001-2003

110. PhysicsWeb - Probe To Predict Landslides And Earthquakes
Probe to predict landslides and earthquakes 17 January 2002. The discovery of geological electrical signals that precede seismic
http://physicsweb.org/article/news/6/1/10/1

Advanced site search
news
January February March April May June July August September October November December
Show summaries
quick search Search the news archive.
Previous News for January 2002 Next Probe to predict landslides and earthquakes
17 January 2002 et al Appl. Phys. Lett. Zimanowski and co-workers pressed together two pieces of volcanic rock and then slid one across the other. Electrodes in each rock monitored the electromotive force that built up between. Although the sliding force was constant, the researchers found that the electrical signal peaked periodically, shortly before any movement was detected. Based on this experiment, Zimanowski and colleagues developed a probe and used it to measure electrical signals at Mount Stromboli, an active volcano in Italy where landslides are frequent. The detector revealed a pattern in the signals similar to that in their experiment, and the team proposed a four-step process to explain it. Initially, the researchers believe, strain builds up between the layers of rock. 'Micro-cracks' then form at the rock surfaces as they creep over each other, exposing fresh rock. This causes electrical charge to accumulate, which generates the 'precursor signal'. Mechanical failure follows as the rocks slip past each other, and finally the interface relaxes and the electrical charge dissipates. According to the German team, this technique would be suitable for monitoring unstable mountainsides, in particular because it gives advance warning of landslides and volcanoes. 'The field probe is buried between 30 and 50 centimetres in the ground but its detection depth is presently one to two kilometres into the Earth's crust', Zimanowski told PhysicsWeb. Improvements to the probe could increase this to a depth of several kilometres, say the researchers, which could enable it to detect the precursor tremors of certain types of earthquake as well.

111. Landslides
landslides. landslides can contribute a significant amount of sediment to streams and can adversely affect fish habitat. Therefore
http://www.odf.state.or.us/DIVISIONS/protection/forest_practices/fpmp/landslides

112. PEI Elections: Liberal Landslides And Tory Tides - Politics And Economy - CBC Ar
Home Politics and Economy PEI Elections Liberal landslides and Tory tides. PEI Elections Liberal landslides and Tory tides.
http://archives.cbc.ca/IDD-1-73-906/politics_economy/elections_pei/
document.write(""); document.write(""); Search the Archives site
Advanced Search

Home
Politics and Economy Elections in Canada PEI Elections: Liberal landslides and Tory tides
PEI Elections: Liberal landslides and Tory tides Click to Activate Topic Timeline
If the province of PEI had a campaign slogan it would be of the "go big or go home" genre. From Liberal landslides to Tory sweeps, PEI elections have been showy and dramatic changings of the guard. But despite the spectacular overthrows, campaigns have been conducted as a sport of etiquette. CBC has covered the continuing electoral spectacle as Islanders waffled between the Liberal and Tory tides, confronted issues of party patronage, and elected the first woman and non-European premiers in Canada.
Educational activities about

PEI Elections: Liberal landslides and Tory tides
Stunning upheaval: Alex Campbell's victory The Million-Acre Farm ... A gentleman's sport
Young Liberal Alex Campbell woos voters with his visionary politics. (TV; runs 14:30)
Tory leader Angus MacLean seeks a rural renaissance. (TV; runs 1:20)

113. Landslides
landslides. Landslide in Conecuh County, Alabama, 1997. WHAT IS A LANDSLIDE? A landslide is or surface runoff. TYPES OF landslides.
http://www.gsa.state.al.us/gsa/landslides.html
LANDSLIDES Landslide in Conecuh County, Alabama, 1997 WHAT IS A LANDSLIDE? A landslide is defined as a perceptible downward and outward movement of slope-forming soil, rock, and vegetation under the influence of gravity. WHAT CAUSES A LANDSLIDE? Landslides can be triggered by both natural and human-induced changes in the environment. These changes may result from weaknesses in the composition or structure of the rock or soil, heavy rain, or changes in ground-water level, seismic activity, or construction activity. Human- induced landslides may result from changes in slope caused by terracing for agriculture, cut-and-fill construction for highways, building construction, mining operations, and changes in irrigation or surface runoff. TYPES OF LANDSLIDES Rock falls are rapid movements of bedrock characterized by free-fall, bouncing, and rolling. A topple is a block of rock that tilts or rotates before falling to the slope below. Slides are movements of soil or rock along a distinct surface of rupture which separates the slide material from the more stable underlying material. The two major types of slides are rotational and translational slides Flows are mass movements of water-saturated material. Different types of flows include creep, debris flow, debris avalanche, earthflow, mudflow, and lahar.

114. Module 4 - Landslides
MODULE 4 landslides, SLOPE FAILURE, AND OTHER MASS WASTING PROCESSES By Anni Watkins and Scott Hughes. The Human Impact of landslides.
http://wapi.isu.edu/EnvGeo/EG4_mass_wasting/landslide2.html
Environmental Geology
GEOL 406/506 MODULE 4
LANDSLIDES, SLOPE FAILURE, AND OTHER MASS WASTING PROCESSES
By Anni Watkins and Scott Hughes Reading assignment: Chapter 6, p. 131-160; Keller. See Module Preview for initial information and a Powerpoint Presentation. Introduction - Heavy rains saturate the Portland, Oregon area. Slick, debris-filled mud slides down steep slopes blocking the scenic Columbia River Gorge Highway. - Warm rains rapidly melts snowpack. Snowmelt-induced debris flow threatens lives and damages property. - A major earthquake hits the West Coast. It triggers numerous landslides in a 200-mile radius. Each of these events represents some type of slope failure . Slope failure, also referred to as mass wasting , is the downslope movement of rock debris and soil in response to gravitational stresses. Three major types of mass wasting are classified by the type of downslope movement. The types of movement, falls, slides, and flows , will be covered in this module. In addition, another type of ground failure

115. KYRGYZSTAN More Landslides Predicted Following Quakes - OCHA IRIN
KYRGYZSTAN More landslides predicted following quakes. on Tuesday. There isn ta single day without landslides. landslides occurred
http://www.irinnews.org/report.asp?ReportID=40890&SelectRegion=Central_Asia&Sele

116. Is Montana At Risk? Landslides / Soil Failure
landslides / SOIL FAILURE. landslides are among the most common natural hazards. The hazards associated with landslides are as diverse as the types of failure.
http://www.discoveringmontana.com/dma/des/Soil.htm
Is Montana at Risk?
Identified Hazards for the State of Montana
Basic Disaster Information:
The Four Phases Hazardous Materials Severe Weather Flooding ... Miscellaneous
LANDSLIDES / SOIL FAILURE
Landslides are among the most common natural hazards. As with most natural hazards, they are often characterized by the catastrophic examples, such as the Hebgen Lake Quake Lake slide of 1959. Unlike most natural hazards, however, most damage is not caused by extreme events, but by uncounted (and often unreported) minor events. Slopes with the greatest potential for sliding are between 34 degrees and 37 degrees. Although steep slopes are commonly present where landslides occur, it is not necessary for the slopes to be long. Therefore, landslides are one major natural hazard that is as likely, or perhaps more likely, to occur in eastern Montana as in the mountainous western part of the state. Two criteria are typically used to classify landslides - types of movement and types of material. The types of movement are falls, topples, slides, spreads, flows, and combinations or two or more of these. Bedrock and soils are considered the principle material types. The soils type is further divided into debris and earth. Landslides occur when the shearing of forces exceed the resisting forces of earth materials. Several factors contribute to either increased shear stress or reduced shear strength, thus initiating the landslide process. Factors which can increase shear stress are:

117. Devastating Landslides Strike Fiji
Devastating landslides Strike Fiji. Posted on Tue, 18 May 2004 161955 GMT Fiji Red Cross staff and volunteers have led the response
http://www.disasterrelief.org/Disasters/040419fiji/
Devastating Landslides Strike Fiji
Posted on Tue, 18 May 2004 16:19:55 GMT Fiji Red Cross staff and volunteers have led the response to a devastating storm that struck the Pacific nation last week, killing at least ten people with several more still missing. The tropical storm brought heavy rainfall and 90km/h winds to central areas of Fiji's largest island, Viti Levu, causing landslides and flooding in low-lying areas. In the worst fatal incident, a landslide pushed a bus carrying five people into the flooded Wainibuka River, north of Suva. According to Fiji's National Emergency Operations Centre, about 10,000 people have been directly affected by the storm, through extensive damage to infrastructure, crops and households. "With the tropical cyclone season almost over, we had been hoping that Fiji would escape any major natural disasters this season," said Fiji Red Cross Director-General Alison Cupit. "However, this storm has changed that, bringing a real dampener to Easter holiday celebrations." On the evening of Thursday 8 April, just hours after the storm had struck, Fiji Red Cross branch volunteers were providing immediate assistance in the field and at evacuation centers.

118. Table Of Contents
GEOPHOTO ALBUM Slope Stability. Earthquake-induced landslides. Earthquake-induced slides in mountains. Flow slides. Flow slide diversion walls.
http://cee.engr.ucdavis.edu/faculty/boulanger/geo_photo_album/Table of Contents/
G EO- P HOTO ... LBUM Slope Stability Earthquake-induced landslides Earthquake-induced slides in mountains Flow slides Flow slide diversion walls [see " Embankment dams " for more slides.]

119. Herald Sun: Landslides Cause Massive Oil Spill (archived)
landslides cause massive oil spill From correspondents in Quito ECUADOR was today trying to gauge the environmental damage caused by the spilling of thousands
http://www.heraldsun.news.com.au/common/story_page/0,5478,8964143%5E1702,00.html

Home
NEWS SECTIONS Breaking news State National World ... Learn OPINION Editorial Andrew Bolt COFFEE BREAK Daily horoscopes That's Life Trivia Quiz CLASSIFIEDS General CareerOne Announcements Cars Guide ... Casual advertising SERVICES / HELP About us Contact us Link to us Herald Sun Shop ... Home delivery SUNDAY FEATURES Sunday Gossip body+soul Faithworks Weddings
BREAKING NEWS This story is from our news.com.au network Source: AFP back PRINT-FRIENDLY VERSION EMAIL THIS STORY
Landslides cause massive oil spill
From correspondents in Quito
ECUADOR was today trying to gauge the environmental damage caused by the spilling of thousands of barrels of oil after landslides broke a pipeline running from the Amazon jungle to a Pacific port.
Oil exports remained indefinitely postponed as environmental workers and engineers began repairs that could last a month, said Pedro Espin, president of the state-owned Petroecuador. About 20,000 barrels of oil were spilled in an area near three rivers after two landslides fell on the Transecuadoran pipeline near the Amazon town of Baeza, some 70 kilometres southeast of the capital Quito. Petroecuador suspended exports to guarantee local supplies.

120. 8th ISL
bromhead landslide landslip rockslide coastal erosion analysis design remedial work landslides landslide landslide investigation residual peak strength
http://www.kingston.ac.uk/~ku00323/isl8-000.htm
8th International Symposium on Landslides
held in the UK in Cardiff, Wales, June 2000
SYMPOSIUM INFORMATION
Please note that while the links in the right hand column are under construction, you will get existing Bulletin items when you click on them! e.bromhead@kingston.ac.uk

A  B  C  D  E  F  G  H  I  J  K  L  M  N  O  P  Q  R  S  T  U  V  W  X  Y  Z  

Page 6     101-120 of 136    Back | 1  | 2  | 3  | 4  | 5  | 6  | 7  | Next 20

free hit counter