Sinkholes along the Dead Sea Coast and their Development. Boris SHIRMAN and Michael RYBAKOV

Similar documents
Sinkholes of Dead Sea in Satellite Image Time Series

Hazard Mapping Along the Dead Sea Shoreline

New Modes of Sinkhole Formation along the Dead Sea Shorelines (Israel): Observations from InSAR, LiDAR, Time-lapse Camera, and Water Analysis

Development of geophysical investigation for verifying treatment efficiency of underground cavities

Lecture 15: Subsidence

ambiguity in earth sciences IESO Geophysics Section Eddy hartantyo, Lab Geofisika FMIPA UGM

The three-year mapping and monitoring of underground cavity expansion with 2D resistivity survey: What has revealed?

PUBLICATIONS. Journal of Geophysical Research: Earth Surface. Salt dissolution and sinkhole formation: Results of laboratory experiments

IAEA SAFETY STANDARDS Geotechnical Aspects of Site Evaluation and Foundations in NPPs, NS-G-3.6

Geodetic monitoring of surface deformation along the western shores of the Dead Sea using GPS and InSAR observations


Chapter 14: Groundwater. Fig 14.5b

WATER ON AND UNDER GROUND. Objectives. The Hydrologic Cycle

Directed Reading. Section: Types of Maps

Need of Proper Development in Hilly Urban Areas to Avoid

PALEOGEOGRAPHY of NYS. Definitions GEOLOGIC PROCESSES. Faulting. Folding 9/6/2012. TOPOGRAPHIC RELIEF MAP of NYS GRADATIONAL TECTONIC

THE DEAD SEA RIFT VALLEY

Prof. Stephen A. Nelson EENS 111. Groundwater

b Blackwell Science Environmental Geology PRINCIPLES AND PRACTICE

Ground subsidence is a worldwide problem especially

LOT S CAPTIVITY AND RESCUE

Name Class Date. Study Guide for 7 th Grade Final Exam (Semester One)

Chapter 13. Groundwater

' International Institute for Land Reclamation and Improvement. 2 Groundwater Investigations. N.A. de Ridder'? 2.1 Introduction. 2.

Last Time. Today s s Agenda. Geophysics. Geophysics. Geophysics. MAS 603: Geological Oceanography. Lecture 21: Geophysics 1: Gravity

Unit 7.2 W.E.D. & Topography Test

Land Subsidence. Land subsidence is defined as the lowering of the land surface.

Soluble rocks. November Overview. What are soluble rocks? What are the hazards from soluble rocks? What is the cost to the UK economy?

STUDY GUIDE FOR CONTENT MASTERY. Movement and Storage of Groundwater

Electrical Resistivity Survey for Delineating Seawater Intrusion in a Coastal Aquifer

A Case Study of High-Resolution Gravity and Wenner-Schlumberger Resistivity for Geotechnical Engineering: An Example from North Jordan

INTRODUCTION. Climate

EMERGENCY INVESTIGATION OF EXTREMELY LARGE SINKHOLES, MAOHE, GUANGXI, CHINA

Finding Large Capacity Groundwater Supplies for Irrigation

DATA ACQUISITION METHODS FOR GROUNDWATER INVESTIGATION AND THE SITING OF WATER SUPPLY WELLS

GEOTECHNICAL ENGINEERING INVESTIGATION HANDBOOK Second Edition

Subsidence is the sinking or collapse of a portion of the land surface. The movement involved in subsidence is essentially vertical; little or no

GEOELECTRICAL INVESTIGATIONS OF MARINE INTRUSIONS ON THE ROMANIAN BLACK SEA SHORE

Land subsidence due to groundwater withdrawal in Hanoi, Vietnam

Controls on the Distribution of Drift Filled Hollows in London

Laboratory and Numerical Study of Sinkhole Collapse Mechanisms

Evaluation of the hydraulic gradient at an island for low-level nuclear waste disposal

CCR Rule Compliance: Innovative Use of Geophysics to Certify Landfill Stability and Site Groundwater Monitoring Wells

State of Israel Ministry of Housing and Construction Survey of Israel. The Hydrological project case

Overview of Consequences of the Tsunami in Thailand and Roles and Activities of the Department of Mineral Resources after the 26 December 2004 Tsunami

A Case Study on Ground Subsidence Using Ground Penetrating Radar

An Introduction to Field Explorations for Foundations

6.1 Water. The Water Cycle

Environmental Geology Lab 5 - Mass Wasting Hazards

PUBLICATIONS. Journal of Geophysical Research: Earth Surface

Notes and Summary pages:

Geophysical Exploration in Water Resources Assessment. John Mundell, P.E., L.P.G., P.G. Ryan Brumbaugh, L.P.G. Mundell & Associates, Inc.

PRELIMINARY INVESTIGATIONS OF SUBSIDENCE, COLLAPSE, AND POTENTIAL FOR CONTINUED GROWTH OF THE DAISETTA SINKHOLE, LIBERTY COUNTY, TEXAS

RESISTIVITY IMAGING AND BOREHOLE INVESTIGATION OF THE BANTING AREA AQUIFER, SELANGOR, MALAYSIA. A.N. Ibrahim Z.Z.T. Harith M.N.M.

TYPICAL METHODS FOR FORECASTING KARST COLLAPSE IN CHINA

What we will cover. The Hydrologic Cycle. River systems. Floods. Groundwater. Caves and Karst Topography. Hot springs

INVESTIGATIONS OF LARGE SCALE SINKHOLE COLLAPSES, LAIBIN, GUANGXI, CHINA

Module 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes

process is taking place. In addition, Nepal is a seismic prone country and the risk it faces from earthquakes is very high (Figure 2). Historical reco

Amistad Dam Investigation and Oversight: Karst- Founded Dam on the USA-Mexico Border

4.9 GEOLOGY AND SOILS

ENCE 3610 Soil Mechanics. Site Exploration and Characterisation Field Exploration Methods

Chapter 8 Fetter, Applied Hydrology 4 th Edition, Geology of Groundwater Occurrence

Does the SDCP need inputs from geology?

Rogun Hydropower Project

Horizontal gradient and band-pass filter of aeromagnetic data image the subsurface structure; Example from Esh El Mellaha Area, Gulf of Suez, Egypt.

Guidelines for Site-Specific Seismic Hazard Reports for Essential and Hazardous Facilities and Major and Special-Occupancy Structures in Oregon

5 Further Case Histories

Soils, Hydrogeology, and Aquifer Properties. Philip B. Bedient 2006 Rice University

Tips for Success on a Test

LOCATING AND CHARACTERIZING ABANDONED MINES USING MICROGRAVITY by Richard C. Benson 1, Ronald D. Kaufmann 1, Lynn Yuhr 1, Richard Hopkins 2 ABSTRACT

Mapping Earth. How are Earth s surface features measured and modeled?

FUNDAMENTALS OF ENGINEERING GEOLOGY

Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s

Geophysical Methods for Screening and Investigating Utility Waste Landfill Sites in Karst Terrain

Electrical imaging techniques for hydrological and risk assessment studies

Pre-Lab Reading Questions ES202

What is weathering and how does it change Earth s surface? Answer the question using

Before writing the discipline examinations, candidates must have passed, or have been exempted from, the Basic Studies Examinations.

Oil & Gas. From exploration to distribution. Week 1 V05 Origin of hydrocarbon resources part 1. Jean-Pierre Deflandre

Geo-hazard Potential Mapping Using GIS and Artificial Intelligence

ENVIRONMENTAL AND ENGINEERING GEOPHYSICS

Tectonically conditioned brine leakage into usable freshwater aquifers implications for the quality of groundwater exploited in central Poland

Land subsidence induced by groundwater extraction in the Alto Guadalentín aquifer, SE Spain.

Seismic study of land subsidence and Vulnerability of Rural Buildings by using geophysics methods, near Shiraz city

11/22/2010. Groundwater in Unconsolidated Deposits. Alluvial (fluvial) deposits. - consist of gravel, sand, silt and clay

GRAVITY EXPLORATION (Gph 301) Chokri Jallouli 2014/2015

Downloaded 11/20/12 to Redistribution subject to SEG license or copyright; see Terms of Use at

UGRC 144 Science and Technology in Our Lives/Geohazards

Chapter 2 Geography. Getting to know Earth

Publication n 121 of the International Association of Hydrological Sciences Proceedings of the Anaheim Symposium, December 1976

EASTON, CA POLLUTANT PLUMES. By Dr. David Cehrs. April 2012

Chapter 14. Groundwater

Prentice Hall EARTH SCIENCE

- Groundwater Supply (Fanny Bay to Nanoose Bay)

Canary in the Coal Mine: Subsidence in Coastal Louisiana Press Conference

High Resolution Seismic Reflection Investigation of Salt Dissolution Features in Kansas

GEOPHYSICAL SITE CHARACTERIZATION IN SUPPORT OF HIGHWAY EXPANSION PROJECT

COURSE OUTLINE Physical Geology

GEOCHEMISTRY UNIFORM SYLLABUS

Transcription:

Sinkholes along the Dead Sea Coast and their Development Boris SHIRMAN and Michael RYBAKOV Over the past several years, the coastal area around the declining Dead Sea has undergone a catastrophic collapse. One of the major expressions of this process is the sudden appearance of hundreds of collapse sinkholes, causing a severe threat to the future of this region. We shall touch briefly on the sinkhole phenomenon and center our attention on micromagnetic techniques in which the authors were involved. 1

The Phenomenon Sinkholes Location: Dead Sea coastlines in Israel and Jordan within a narrow strip of 60 km long and about 1 km wide Concentration: in clusters, parallel to the general direction of the Dead Sea fault system Period: started appearing in the early 1980s Development: since 2000 accelerated, with a rate of 150-300 per year Total today: more than 1,700 Shape: well (gravel holes) or crater (mud holes) Size: can reach a diameter of more than 30 m and a depth of 20 m Occurrence: collapse of upper ground layer Sinkholes in the pictures a c d b e a (Shalem b (Samar (c Hever (d,e En-Gedi Sinkholes were going on: a,b in mudflats c,d,e in alluvial fan (Yechieli et all, 2005) 2

The formation of these sinkholes is connected to the dramatic drop of the Dead Sea water level and associated groundwater levels. -380 Dead Sea level decline since 1930 Dead Sea level, m -390-400 -410 17 cm/year 1930-1973 62 cm/year 1974-1979 (Abelson et al., 2007) 79 cm/year 1981-1991 100 cm/year 1994-2001 -420-419.5 1930 1940 1950 1960 1970 1980 1990 2000 Years Dead sea level, m -420-420.5-421 -421.5 117 cm/year 2007-2008 -422 SOI measurements -422.5 1 3 5 6 8 10 12 2 4 6 8 10 12 2 Months 2007 2008 The contributing factor for this decline in succeeding years was the interception of the freshwater flow to the Dead Sea upstream by agricultural, industrial and other needs of surrounding countries. Location of sinkholes (white squares) Dead Sea level decline and sinkholes number changes The sinkholes have evolved due to the dramatic decline of the Dead Sea level, which exceed 30 m since the early 1930's 2000 300 Number of sinkholes 1600 1200 800 400 Number of sinkholes Growth rate 250 200 150 100 50 Growth rate (sinkholes/year) 0 0 1980 1985 1990 1995 2000 2005 2010 Number and growth rate of sinkholes since 1980 Shaded relief by John Hall GIS data processing: The sinkhole development significantly accelerated since 1997; currently there are more than 1700 sinkholes and their number increases by a rate of 200-300 per year.(abelson et all, 2007) 3

Hazard Collapse-sinkholes are an environmental hazard. An alarming case occurred recently in the resort area, on Highway 90, and at the Israeli and Jordanian potash plants. 4

5 The Earth opened its mouth

METHODS TO INVESTIGATE AND PREDICT SINKHOLES Geodesy Geophysics Aerial photography InSAR (Interferometer Synthetic Aperture Radar) Seismic refraction Geoelectric survey Microgravity Micromagnetics Boreholes Hydrogeology Geology The Geological Survey of Israel and Geophysical Institute of Israel employed a variety of tools such as seismic reflection and refraction, electrical methods, drilling and groundwater sampling. Also, the Survey of Israel made a contribution to sinkhole investigation in aerial photograph interpretation, micromagnetic techniques development and following the Dead Sea level decrease in recent years. 6

Aerial photograph Hamei Shalem site 1993 Mapping was carried out using ortho-rectified aerial photographs from the archive of the Survey of Israel from: 1990, 1992, 1993, 1995 and 1997. It was shown (Itamar and Raizman, 2000), that sinkholes are not distributed randomly but concentrated in clusters along the Dead Sea shore. Scale: from 1:1000 to 1:40000 (GSI-Report \22\2000 ) Hamei Shalem 1995 1999 Sinkholes grew in number and in size in 1999 compared with 1995 7

From the SOI Data base Hamei Shalem 2006 100m Ortho-rectified aerial photographs Hamei Shalem 2003-2008 Green spots in the pictures are defined as sinkholes filled by water: 2003 some isolated spots; 2006 the central spots merged together; 2008- a merged spot expanded to the North. 2003 8 2006 2008

Gravimetry The method is based on the assumption that density in a sinkhole area is lower than in the surrounding area The gravimeter with resolution of 0.005 mgal can detect a void of 8 m in size filled by salt water at a depth of 16 m or filled by air at a depth of 24 m. (Rybakov et. All., 2001) Magnetometry The technique is based on revealing negative anomalies using magnetic mapping at a bounded region. Modeling shows that susceptibility of sediments of 14-16 16 micro sgs allows us to detect hollowness at a depth of about 10-15 15 m. 9

Field magnetic measurements The magnetic measurements (field equipment) 05.05.2004 Zohar site: Two small sinkholes (~1.5 m in diameter and ~ 7m in depth) have recently opened (photo) and their development 1 1 / 2 year after. High-resolution magnetic map (contour interval 2 nt) shows magnetic anomalies caused by the sinkholes. (Rybakov et. All., 2001) 15.11.2005 10

Assael site (mud flat ) Magnetic anomalies located out of the sinkhole cluster suggest a subsurface mass deficiency which will cause future ground collapse. Such locations are shown by gray polygons bounded by dashed black lines. (Rybakov et. All., 2001) Magnetometry (cont.) View of anomaly location in 2004 07-07 07-2004 New crater view 15-11-05 Predicted sinkhole ASSAEL SITE Micromagnetic survey 2004 Predicted and documented in Rybakov et al., 2005 sinkhole collapse in the Assael mud flat were confirmed there later (Rybakov( et al., 2006). 11

Mechanism of sinkhole generation from (Abelson, 2005) 1. Hydrological factor There is a hydrological connection between the Dead Sea and freshwater levels. Dead Sea decline is responsible for freshwater decrease. The primary cause of sinkhole formation is dissolution of the salt layer by groundwater. 2. Effect The Role of Land Subsidence and Faults The decline of the Dead Sea level increases the effective stress and generates differential compaction of the aquiclude layers. The differential compaction results in shear deformation of the aquiclude layers, confining the salt layer along pre-existing faults. 12

3 Destabilization of cavities The increase in effective stress due to the Dead Sea level drop also directly destabilizes cavities in the salt layer, promoting the collapse of overlying sediments. This effect serves as a catalyst for sinkhole collapse rather than causing new underground cavities. (Abelson, 2005) Was the sinkhole phenomenon encountered in the past? "And the vale of Siddim was full of slimepits; and the kings of Sodom and Gomorrah fled, and fell there; and they that remained fled to the mountain." (Genesis, Abram and Lot part: 14-10) 10) Valley of Siddim and the surrounding region (from Biblos.com) 13

RESULTS The formation of sinkholes is attributed to the dissolution of subsurface salt layer by fresh groundwater due to the drop Dead Sea and associated groundwater level. Appearance of sinkholes started in the yearly 1980s when the Dead Sea level was about -400 regarding Israeli leveling system. Human activity seriously affected on the Dead Sea ecosystem. From other hand, there are evidences (Frumkin, 2002; Bookman-KenTor et al., 2004) that Dead Sea level like in the modern period and even lower encounter during the last several thousands years. 14

Nowadays, some effectively technique were developed to understand better sinkholes generation and even to predict their appearance. One such technique is micromagnetic method cave detection near Dead Sea. Acknowledgments We thank the collaborators of the aerial photograph division for help in the data base search and Dr. Meir Abelson ( Geological Survey) for the updated sinkhole statistical data Thank you 15