1 ENV-3A1Y: Natural Hazards: 2006 - 7 Landslide Hazards N.K. Tovey Н.К.Тови Landslide on Main Highway at km 365 west of Sao Paulo: August 2002 14,607 days.

Slides:



Advertisements
Similar presentations
Tectonic Hazards A PowerPoint of images to accompany the notesheet.
Advertisements

ENV-2E1Y: Fluvial Geomorphology:
ENV-2E1Y: Fluvial Geomorphology:
1 ENV-3A1Y/ENVF3A1Y: Natural Hazards: Landslide Hazards N.K. Tovey Н.К.Тови Landslide on Main Highway at km 365 west of Sao Paulo: August 2002.
The Aberfan Disaster 21 October 1966.
Agenda 2/10 Warm-Up: Have you ever seen geologic problems in California on the news? What types of events make life more challenging on the West Coast?
UNDERSTANDING LANDSLIDES Dr. Walter Hays, Global Alliance For Disaster Reduction.
Mass Movements at Earth’s Surface
EROSION Erosion is the process by which natural forces move weathered rock and soil from one place to another.
LET’S LOOK AT PAGE 32 OF NEW GEO.  Mass movement is the movement of any loose weathered material down a slope under the influence of gravity.
Forces wear down and build up earth’s surface
Earthquake induced LIQUEFACTION by Jimmy McLauchlan Peat Nicholas Case study: Mexico City, 1985.
Guided Notes for Mass Movements
Section Two Collapsing slopes. What is a landslide? soil layer rock layer wet soil Landslide takes place when large masses of loose rocks and soil move.
Mass Movements at Earth’s Surface
Landslides Causes.
Liquefaction: Behavior Evidence, Prediction, and Prevention.
1 N.K. Tovey Н.К.Тови Landslide just west of Maracas Beach, Trinidad December 2002 Types of Landslide Why Landslides occur Landslide Hazards.
Types of Mass Movement By Tony, Ed, Steven Introduction In mass movement of soil gravity is the force acting to move surface materials such as soil and.
Weather Air Masses and Fronts. Air Masses Function of location (arctic – A, polar – P, tropical – T) and surface type (continental – c and maritime –
1 ENV-3A1Y/ENVF3A1Y: Natural Hazards: Landslide Hazards N.K. Tovey Н.К.Тови Landslide on Main Highway at km 365 west of Sao Paulo: August 2002.
Mass Movement (Mass Wasting) Chapter 8 Mass movements occur when the shearing stress acting on rocks or soil exceeds the shear strength of the material.
Coping with earthquakes and eruptions
13A.3 – Natural Hazards.
California’s Natural Hazards Chapter 13A, Section 3.
California’s natural hazards
These sessions will introduce the basic natural processes, historical geographic ranges, and potential impacts of the natural hazards that are not as unique.
California’s Natural Hazards
Section 3: Earthquakes and Society
By:Markquinesha Owens Ms.McBryde 2 nd Period How Do Tsunamis Occur? Most tsunamis occur in a zone known as “The Ring of Fire". The Ring of Fire is located.
Mass Wasting Chapter 8 “The mountains are very high and steep about Carson, Eagle, and Washoe valleys – very high and very steep, and so when the snow.
Volcanoes and Earthquakes
1.Landslides - brittle failure Modeling Landscapes - Force Balance Rockslide spawns debris flow in British Columbia, GSC.
FACTOR OF SAFETY Determining slope stability in Holtwood, PA in the aftermath of Hurricane Sandy Kristina Lofman November 27, 2012 EPS 109.
Mass Wasting Sculpturing Earth’s Landscape. What is Mass Wasting? The downslope movement of material under the influence of gravity May occur at rates.
Location and map of region Tectonic activities Mechanism of earthquake Damage Risks.
Welcome to Science 12/2 1. Science News 2. Ch. 12 Section 4 on Erosion 3. Question of the Day 4. Skills Lab.
Landslides - brittle failure Modeling Landslides - Force Balance Rockslide spawns debris flow in British Columbia, GSC.
Mass Wasting. Introduction While landslides are a normal part of erosion and surface processes, they can be very destructive to life and property Mass.
Geological Engineering University of Wisconsin-Madison
1 Natural Disasters Mass Wasting: Landslides
SCI TIP Describe the differences of Sand, Silt, & Clay Which sediment travels by wind furthest? Why? What is a Loess Deposit? How did it get there?
Warm Up 1) The part of a water project that carries (moves) fresh water to where it is needed is a(n) a. hydroelectric plant.c. desalination plant. b.
ABERFAN DISASTER 1966 …this is short, but VERY serious…
{ The Effect of Gravity on Erosion and Deposition Agents of Weathering and Erosion.
Recap Recap what the following terms mean Natural Hazard Disaster Risk
California’s Natural Hazards. California’s geology has unique natural hazards that goes along with its natural beauty.
DEVASTATING LANDSLIDE IN THE PHILIPPINES INDUCED BY HEAVY RAIN 22 MINERS TRAPPED, BUT ONLY 3 DEATHS 2:30 am, GOOD FRIDAY, APRIL 22, 2011 Walter Hays, Global.
Changing Earth’s Surface
What is the connection between these pictures?
Environmental Health Natural Disasters.
A PowerPoint of images to accompany the notesheet
Introduction to Mass Movement
Air photo showing rockfall in 1999
Ground Stability Issues Cause and Effect
Session 9: Geological Natural Hazards
BACKGROUND FOR THE 2011 HURRICANE SEASON
A B 1.What is / has happened in each photo
NATURAL DISASTERS! EARTHQUAKES WILDFIRES VOLCANIC ERUPTIONS TORNADOES
Changing Earth’s Surface
HIGHLIGHTS OF NOTABLE DISASTERS OF 2012 PART 6: LANDSLIDES
M7.6 EARTHQUAKE STRIKES 140 KM FROM SAMAR PROVINCE ON EAST COAST OF THE PHILIPPINES 34 KM DEEP 8:47 PM AUGUST 31, 2012 Walter Hays, Global Alliance.
LANDSLIDE BURIES VILLAGE IN CHINA JANUARY 11, 2013
Mass movements Falls, slumps flows Landslide scar/scarp
California’s Natural Hazards
Po Shan Road, Hong Kong, 18 June 1972
Title: 8.1 Types of Mass Movements Page #: 68 Date: 2/4/2013
Tropical cyclones movement
Lecture 25 Mass wasting and landslide mechanics.
Civil Engineering Dept.
Presentation transcript:

1 ENV-3A1Y: Natural Hazards: Landslide Hazards N.K. Tovey Н.К.Тови Landslide on Main Highway at km 365 west of Sao Paulo: August ,607 days ago today Exactly 40 years ago next Saturday

2 Lecture 1: Wednesday Week 42 –Introduction Landslides as a Hazard and their consequences background to why they occur Lecture 2: Thursday Week 4 12 – 13 EF 1.01 –Types of Landslide Lecture 3: Thursday Week –Landslide Warning systems Lecture 4: Wednesday Week 5 09 – 10 EF 1.01 –Landslide and Slope Management Field Excursion: Thursday Week 5 12 – 17 Bring Field Clothing and a packed lunch ENV-3A1Y: Natural Hazards:

3 Aims of the course An introduction to Landslide Hazard Management Factor of Safety the causes Why they occur Can we predict them the consequences The types of landslide Landslide Warning – Development of the Hong Kong System and what was learnt Strategic Planning for the future Slope management ENV-3A1Y: Natural Hazards:

4 Landslides as a Hazard Grossly Under Represented as a Hazard Often treated as a secondary issue e.g Rain Storm Disasters of 18 th June 1972 in Hong Kong 2 major landslides each killing over 60 people No one was killed by drowning/flooding ENV-3A1Y: Natural Hazards: Failure of slope above Po Shan Road in June 1972

5 Landslides associated with Heavy Rain (Tropical Cyclones) –~ 500+ landslides affected man in Hong Kong 28 th May to 2 nd June –As a result of NKT’s actions Yuen Mo village ceased to exist. Earthquakes –Cause liquefaction and rise of pore pressures Volcanic Eruptions ENV-3A1Y: Natural Hazards:

days ago today at 09:15 N K Tovey a second year PhD student was listening to a lecture by Andrew Schofield. Theme of lecture was Landslide Hazards At 09:15 he turned his attention to a landslide disaster which had occurred a few year earlier in Belgium. A colliery tip collapsed killing around 20 people in the village. At precisely the time he was speaking about the disaster >>>>>>>>>>>>>>>>>>>>>

7 Aberfan: 21 st October 1966 Tip 7 collapsed, engulfed Pantglas School and parts of the village killing 144 mostly children ENV-3A1Y: Natural Hazards:

8 Geotechnics – the discipline needed for detailed analysis "the application of the laws of mechanics and hydraulics to the mechanical problems relating to soils and rocks" Factor of Safety (F s ): Forces resisting landslide movement arising from the inherent strength of the soil. Forces trying to cause failure (i.e. the mobilizing forces). F s = ENV-3A1Y: Natural Hazards: F s > 1 stable But is it? F s = 1 just stable F s < 1 unstable But is it?

9 berms Heave at toe Landslide in man made Cut Slope at km 365 west of Sao Paolo - August 2002

10 berms Steep scar to rotational failure

11 Landslide Geochemistry