This document provides an overview of geology and soils issues that should be addressed in a CEQA environmental review document. It discusses various seismic hazards in California like fault rupture, ground shaking, liquefaction, landslides, and hazardous minerals. It describes laws like the Alquist-Priolo Earthquake Fault Zoning Act and Seismic Hazards Mapping Act. Common geologic hazards are defined, like different types of landslides and ground failure. Guidelines are provided for analyzing project impacts related to geology and soils.
Landslides Represent Permanent Deformation Caused By The Downward And Outward Movements Of Large Volumes Of Soil And/Or Rock Under The Influence Of Gravity. Landslides Occur Naturally. Landslides Can Be Triggered And/Or Exacerbated By: 1) Water (From Precipitation During A Tropical Storm, Hurricane, Or Typhoon), Or 2) Vibrations (From Ground Shaking) During An Earthquake. Millions Of Communities Are Not Resilient To Landslide Disasters. The International Community Often Provides Millions To Billions Of Dollars In Relief To Help “pick Up The Pieces, ” But This Strategy Is Not Enough By Itself To Ensure Disaster Resilience. The Challenge Is To Create, Adjust And Realign Programs, Partners And People Until One Has Created The Kind Of "Turning Points" Needed For Moving Towards Landslide Disaster, Resilience. Using Educational Surges Containing The Past And Present Lessons To Foster And Accelerate The Creation Of Turning Points. Integration Of Scientific And Technical Solutions With Political Solutions For Policies On Preparedness, Protection, Early Warning, Emergency Response, And Recovery. Presentation courtesy of Dr. Walter Hays, Global Alliance For Disaster Reduction
Definition, classification & types of landslideTarikIslam9
General Information about Bangladesh
Bangladesh is consisted of a total land area of 147570 km² with hilly areas of 17,342 km² (8.5% of total area of Bangladesh).
Chattagram Hill tracts is the wide ranging hilly area in the southeastern part of the country. Rangamati, Bandarban and Khagrachari are three unique geographical and cultural landscape administrative districts in this region.
Landslides are a common hazard in the Chittagong Hill Districts (CHD) of Bangladesh. The communities that live on dangerous hill slopes in CHD repeatedly experience landslide hazards during the monsoon season, with casualties, economic losses and property damage.
Landslides Represent Permanent Deformation Caused By The Downward And Outward Movements Of Large Volumes Of Soil And/Or Rock Under The Influence Of Gravity. Landslides Occur Naturally. Landslides Can Be Triggered And/Or Exacerbated By: 1) Water (From Precipitation During A Tropical Storm, Hurricane, Or Typhoon), Or 2) Vibrations (From Ground Shaking) During An Earthquake. Millions Of Communities Are Not Resilient To Landslide Disasters. The International Community Often Provides Millions To Billions Of Dollars In Relief To Help “pick Up The Pieces, ” But This Strategy Is Not Enough By Itself To Ensure Disaster Resilience. The Challenge Is To Create, Adjust And Realign Programs, Partners And People Until One Has Created The Kind Of "Turning Points" Needed For Moving Towards Landslide Disaster, Resilience. Using Educational Surges Containing The Past And Present Lessons To Foster And Accelerate The Creation Of Turning Points. Integration Of Scientific And Technical Solutions With Political Solutions For Policies On Preparedness, Protection, Early Warning, Emergency Response, And Recovery. Presentation courtesy of Dr. Walter Hays, Global Alliance For Disaster Reduction
Definition, classification & types of landslideTarikIslam9
General Information about Bangladesh
Bangladesh is consisted of a total land area of 147570 km² with hilly areas of 17,342 km² (8.5% of total area of Bangladesh).
Chattagram Hill tracts is the wide ranging hilly area in the southeastern part of the country. Rangamati, Bandarban and Khagrachari are three unique geographical and cultural landscape administrative districts in this region.
Landslides are a common hazard in the Chittagong Hill Districts (CHD) of Bangladesh. The communities that live on dangerous hill slopes in CHD repeatedly experience landslide hazards during the monsoon season, with casualties, economic losses and property damage.
There are many different means of investigating the landslide-prone areas. Two types of landslide hazard evaluation methods are available. One is the direct observation and the other one is the use of technological tools. One of the guiding principles of geology is that the past is the key to the future. In evaluating landslide hazards, the future slope failures could occur as a result of the same geologic, geomorphic, and hydrologic situations that led to past and present failures. Based on this assumption, it is possible to estimate the types, frequency of occurrence, extent, and consequences of slope failures that may occur in the future. A landslide susceptibility map goes beyond an inventory map and depicts areas that have the potential for landsliding.
Landslides Represent Permanent Deformation Caused By The Downward And Outward Movements Of Large Volumes Of Soil And/Or Rock Under The Influence Of Gravity. Landslides Occur Naturally. Landslides Can Be Triggered And/Or Exacerbated By: 1) Water (From Precipitation During A Tropical Storm, Hurricane, Or Typhoon), Or 2) Vibrations (From Ground Shaking) During An Earthquake. Millions Of Communities Are Not Resilient To Landslide Disasters. One Of The Myths Of Disasters Is That Landslide Disasters, Which Occur Annually In Every Nation, Should Be Enough To Make All Nations Adopt And Implement Policies That Will Lead To Landslide Disaster Resilience. But The Fact Of The Matter Is, This Premise Is Wrong; It Usually Takes Multiple Disasters Before A Stricken Nation Will Adopt Policies To Move Towards Disaster Resilience. Lesson: The Timing Of Anticipatory Actions Is Vital. The People Who Know: 1) What To Expect (E.G., Rock Falls, “quake Lakes,” Mud Flows, Etc.), 2) Where And When It Will Happen, And 3) What They Should (And Should Not) Do To Prepare Will Survive. The People Who Have Timely Early Warning In Conjunction With A Modern Monitoring System, And A Community Evacuation Plan That Facilitates Getting Out Of Harm’s Way From The Risks Associated With Rock Falls, Mudflows, Etc. Will Survive. Engineering To Stabilize Slopes Will Reduce Damage To Buildings And Infrastructure And Help Sustain Their Functions And Save Lives. Presentation courtesy of Dr. Walter Hays, Global Alliance For Disaster Reduction
After attending this lesson, the user would be able to understand the nature and causative factors of landslides, their characteristics, classifications, triggering mechanisms, and effects. The methods of controlling the effects of landslides, and avoiding their menace are also highlighted. Disaster management methods are to be adopted to mitigate the never ending natural hazards. This lesson is an important topic in disaster management.
is a form of mass wasting that includes a wide range of ground movements, such as rockfalls, deep failure of slopes, and shallow debris flows. Landslides can occur underwater, called a submarine landslide, coastal and onshore environments. Although the action of gravity is the primary driving force for a landslide to occur, there are other contributing factors affecting the original slope stability. Typically, pre-conditional factors build up specific sub-surface conditions that make the slope area prone to failure, whereas the actual landslide often requires a trigger before being released. Landslides should not be confused with mudflows, a form of mass wasting involving very to extremely rapid flow of debris that has become partially or fully liquefied by the addition of significant amounts of water to the source material.
Prepared By
Md. Arifuzzaman Arif
MSc in Disaster Management
Department of Geography and Environment
University of Dhaka
BSc in Forestry & Wood Technology Discipline
Khulna University
There are many different means of investigating the landslide-prone areas. Two types of landslide hazard evaluation methods are available. One is the direct observation and the other one is the use of technological tools. One of the guiding principles of geology is that the past is the key to the future. In evaluating landslide hazards, the future slope failures could occur as a result of the same geologic, geomorphic, and hydrologic situations that led to past and present failures. Based on this assumption, it is possible to estimate the types, frequency of occurrence, extent, and consequences of slope failures that may occur in the future. A landslide susceptibility map goes beyond an inventory map and depicts areas that have the potential for landsliding.
Landslides Represent Permanent Deformation Caused By The Downward And Outward Movements Of Large Volumes Of Soil And/Or Rock Under The Influence Of Gravity. Landslides Occur Naturally. Landslides Can Be Triggered And/Or Exacerbated By: 1) Water (From Precipitation During A Tropical Storm, Hurricane, Or Typhoon), Or 2) Vibrations (From Ground Shaking) During An Earthquake. Millions Of Communities Are Not Resilient To Landslide Disasters. One Of The Myths Of Disasters Is That Landslide Disasters, Which Occur Annually In Every Nation, Should Be Enough To Make All Nations Adopt And Implement Policies That Will Lead To Landslide Disaster Resilience. But The Fact Of The Matter Is, This Premise Is Wrong; It Usually Takes Multiple Disasters Before A Stricken Nation Will Adopt Policies To Move Towards Disaster Resilience. Lesson: The Timing Of Anticipatory Actions Is Vital. The People Who Know: 1) What To Expect (E.G., Rock Falls, “quake Lakes,” Mud Flows, Etc.), 2) Where And When It Will Happen, And 3) What They Should (And Should Not) Do To Prepare Will Survive. The People Who Have Timely Early Warning In Conjunction With A Modern Monitoring System, And A Community Evacuation Plan That Facilitates Getting Out Of Harm’s Way From The Risks Associated With Rock Falls, Mudflows, Etc. Will Survive. Engineering To Stabilize Slopes Will Reduce Damage To Buildings And Infrastructure And Help Sustain Their Functions And Save Lives. Presentation courtesy of Dr. Walter Hays, Global Alliance For Disaster Reduction
After attending this lesson, the user would be able to understand the nature and causative factors of landslides, their characteristics, classifications, triggering mechanisms, and effects. The methods of controlling the effects of landslides, and avoiding their menace are also highlighted. Disaster management methods are to be adopted to mitigate the never ending natural hazards. This lesson is an important topic in disaster management.
is a form of mass wasting that includes a wide range of ground movements, such as rockfalls, deep failure of slopes, and shallow debris flows. Landslides can occur underwater, called a submarine landslide, coastal and onshore environments. Although the action of gravity is the primary driving force for a landslide to occur, there are other contributing factors affecting the original slope stability. Typically, pre-conditional factors build up specific sub-surface conditions that make the slope area prone to failure, whereas the actual landslide often requires a trigger before being released. Landslides should not be confused with mudflows, a form of mass wasting involving very to extremely rapid flow of debris that has become partially or fully liquefied by the addition of significant amounts of water to the source material.
Prepared By
Md. Arifuzzaman Arif
MSc in Disaster Management
Department of Geography and Environment
University of Dhaka
BSc in Forestry & Wood Technology Discipline
Khulna University
Geomorphology at a glance: Major landformsP.K. Mani
Geomorphology, Major landforms, Genetic landform classifications, Volcanic landforms, River Systems and Fluvial Landforms, Aeolian Landforms, Glacial Landforms
Hello! I've created this PowerPoint presentation as a requisite in Disaster Readiness and Risk Reduction subject during SY 2019–2020.
Other Geological Hazards
- Bolide Impact
- Ground Subsidence
- Coastal Erosion
Should you need a .pptx file, kindly email me at rd.chrxlr@gmail.com.
1. ESP 179- Winter 2012
Geology and Soils
January 24, 2012
Instructor: Trevor Macenski
2. Outline
Review CEQA Checklist Questions
Seismic Hazards in CA
Alquist-Priolo Earthquake Fault Zoning Act
Seismic Hazards Mapping Act
Common Geologic Hazards
Impact Analysis Approach
Sample Discussion and Analysis
3. Geology and Soils
Appendix G Checklist: Geology and Soils
Expose people or structures to substantial adverse effects
Alquist-Priolo Fault Zone
Seismic ground Shaking
Ground failure/Liquefaction
Landslides
Loss of top soil
Lateral Spreading
Expansive Soils
Soils and Septic System
6. Seismic Hazards
Pose a substantial danger to property and
human safety.
Seismic hazards present in California
include:
Ground rupture along faults
Strong seismic shaking
Liquefaction, Lateral Spreading, Lurching
Landsliding
Slope failure
Hazardous Minerals
Tunamis
7. Fault Rupture
Fault rupture is a seismic hazard that
affects structures sited above an
active fault.
The hazard from fault rupture is the
movement of the ground surface
along a fault during an earthquake.
Creep= Slower moving fault action
Earthquakes-
Strike-slip
Normal
Thrust
Infrastructure often can’t handle Creep or Earthquakes
8. Ground Shaking
Ground shaking depends on several
variables:
Earthquake magnitude
Epicenter distance
Local geology and Soils Thickness
Seismic wave-propagation properties of
unconsolidated
Materials
Groundwater conditions
Topographic setting
Sample Modeling
9. Richter vs. MMI
Richter Scale
Measurement comparison between earthquakes
Evaluates magnitude used for scientific comparison
Only accounts for the actual slip that is generated
Actual damage= Propagation of seismic or ground
waves as a result of initial failure
Loose materials tend to amplify ground waves,
while hard rock can quickly attenuate them,
causing little damage to overlying structures.
10. Richter vs. MMI
Modified Mercalli Intensity (MMI)
Scale provides a useful qualitative assessment
of ground shaking.
The MMI Scale is a 12-point scale of
earthquake intensity:
Local effects experienced by people
Structures
Earth materials.
Each succeeding step on the scale
describes a progressively greater amount
of damage at a given point of observation.
11. Alquist-Priolo Earthquake
Fault Zoning Act
Passed in 1972
Intent: to mitigate the hazard of surface
faulting to structures for human occupancy
Purpose: Direct result of the 1971 San
Fernando Earthquake
Extensive surface fault ruptures that damaged
numerous homes, commercial buildings, and
other structures.
12. Alquist-Priolo Cont.
Requires the State Geologist to establish
regulatory zones (known as Earthquake Fault
Zones) around the surface traces of active faults
and to issue appropriate maps.
The maps are distributed to all
affected cities, counties, and state agencies for
their use in planning and controlling new or
renewed construction.
If an active fault is found, a structure for
human occupancy cannot be placed over the
trace of the fault and must be set back from
the fault (generally 50 feet).
Project will require site specific geotech mitigation
13. Seismic Hazards Mapping Act
Passed in 1990
Intent: Directs the Department of
Conservation, California Geological Survey
to identify and map areas prone to
liquefaction, earthquake-induced
landslides and amplified ground shaking.
Purpose: The SHMA was passed by the
legislature following the 1989 Loma Prieta
earthquake.
14. SHMA Cont.
Geologists in the Seismic Hazard Zonation
Program gather existing geological, geophysical
and geotechnical:
Produce the Seismic Hazard Zone Maps.
Designate as Zones of Required Investigation (ZORI)
Prone to liquefaction and earthquake–induced landslides.
The SHMA requires site-specific geotechnical
investigations within ZORI’s
To identify and evaluate seismic hazards and formulate
mitigation measures prior to permitting
16. Liquefaction
Liquefaction is a process by which sediments below the
water table temporarily lose strength during an earthquake
and behave as a viscous liquid rather than a solid.
Liquefaction is restricted to certain geologic and hydrologic
environments, primarily recently deposited sand and silt
in areas with high groundwater levels.
The process of liquefaction involves seismic waves passing
through saturated granular layers, distorting the granular
structure and causing the particles to collapse. This causes
the granular layer to behave temporarily as a viscous liquid
rather than a solid, resulting in liquefaction.
USGS has maps to identify areas: MAP
17. Lateral Spreading and Lurching
Lateral spreading
is lateral ground movement, with
some vertical component, as a result
of liquefaction.
The soil rides on top of the liquefied
layer
Lurching
is the movement of the ground
surface toward an open face when the
soil liquefies. An open face could be a
graded slope, stream bank, canal face,
gully, or other similar feature.
18. Landslide Hazard Mapping Act
Produced from 1986 through 1995, as
directed by the now-repealed Landslide
Hazard Mapping Act.
Online Resource: MAPs
19. Landslides
Categorized as either 1) rock, 2) soil, or 3)
rock and soil.
Rock= refers to hard or firm bedrock that
was intact and in place prior to slope
movement.
Soil=means unconsolidated particles or
poorly cemented rock or aggregates.
Soil is also distinguished further on the basis of
texture:
Debris (coarse fragments)
Earth (fine fragments)
20. Landslide Classification
1) Falls: Masses of soil or rock that dislodge from steep
slopes and free-fall, bounce, or roll downslope.
2) Topples: Move by the forward pivoting of a mass
around an axis below the displaced mass.
3) Spreads: Commonly induced by liquefaction of material
in an earthquake, move by horizontal extension and shear
or tensile fractures.
4) Slides: Displace masses of material along one or more
discrete planes.
Rotational: Sliding the slide plane is curved and the mass
rotates backwards around an axis parallel to the slope
Translational: Sliding the failure surface is more or less planar
and the mass moves parallel to the ground surface
5) Flows : mobilize as a deforming, viscous mass without
a discrete failure plane.
21. Hazardous Minerals of CA
Asbestos-Inhalation of asbestos fibers may
cause cancer.
Most commonly, asbestos occurrences are associated
with serpentinite and partially serpentinized ultramafic
rocks.
Mercury- Mercury from historic mercury mines
or gold mines has entered a number of
watersheds in California.
Radon- Gas is a naturally-occurring, radioactive
gas that is invisible and odorless. It forms from
the radioactive decay of small amounts of
uranium and thorium naturally present in rocks
and soils.
23. Significant Geology and Soil
Impacts?
What are a few types of projects?
Residential project close to a fault
Natural Gas Pipeline close to fault
Oceanfront Development
Other?