Karst Processes, Landforms, and Landscapes. Karst Flow Diffuse vs. conduit flow Primary vs. secondary porosity.

Slides:



Advertisements
Similar presentations
Karst Processes and Landforms
Advertisements

GROUNDWATER. Groundwater The Hydrologic Cycle Groundwater.
Groundwater Chapter 16.
Karst Landscapes Lab 8.
Groundwater and Karst Topography
Click here for an animation
Chapter Fifteen Groundwater. Groundwater Earth’s hydrosphere extends from top of atmosphere to ~ 10 km (6 mi) below the Earth’s surface. Groundwater,
LIMESTONE Glossary by 2nd Year students Newlands 2009.
5th year Geography Ms Carr
Karst Landscapes Dev. due to: Hard jointed limestone… restricts path of water flow Low water table……….. stagnant water not shape landscape High rainfall……………
Carbonic Acid Most groundwater is slightly acidic due to carbonic acid. Carbonic acid forms when carbon dioxide gas dissolves in water and combines with.
KARST STRUCTURES AND GROUNDWATER FEATURES:
Karst and Karst Terranes Word is German form of the Yugoslavian term “Kras” means “bare stony ground” Named after investigating a region near the Adriatic.
Limestone features The Burren, Co. Clare The word Karst means exposed or bare ground. It is used mainly to describe a Limestone area where this karstic.
WHAT IS KARST? ITALY SLOVENIA. TWO DOMINANT TYPES OF KARST LANDSCAPE? Determined by the origin or “genesis” of the waters doing the solution.
Caves and Sinkholes 13/14 Nov.
Earth as a System The hydrologic cycle  Illustrates the circulation of Earth's water supply  What processes make up the water cycle?
Objectives: 1. To review the terms ‘denudation,’ ‘erosion,’ and ‘weathering’ (freeze-thaw action & carbonation), along with surface landforms found in.
Water Erosion Meander-bend in a river.
Aquifer Recharge, Lakes, and Springs
HIGHER GEOGRAPHY LITHOSPHERE LIMESTONE SCENERY. LIMESTONE -UNDERGROUND FEATURES Caves and Caverns Tunnels, passages and sumps Potholes, sinkholes, swallow.
Water Beneath the Surface
What is Karst? A terrain, generally underlain by carbonate rocks (limestone, dolomite), in which the topography is chiefly formed by the dissolving.
9 Karst Landscape The formation of karst landscapes
Weathering, Erosion and Distinctive Landscapes
Karst Definition by Jennings (1985) “A terrain with distinctive landforms and drainage arising from greater rock solubility in natural water that is found.
Water Resources. What is a Watershed ? Area of land that sheds (moves ) water from the highest to the lowest point.
Karst Cvijic (1893) - “krs [karst]” – rocky, bleak Dissolution, changing water table levels, subsidenceDissolution, changing water table levels, subsidence.
Groundwater. Porosity & Permeability Porosity: - the percentage of the total volume of a rock consisting of voids. - pore spaces: spaces between mineral.
Fresh Water and Karst Topography. Hydrologic cycle On a global basis: Water from atmosphere to earth (Precipitation) Water from earth to atmosphere (Evaporation.
Groundwater Main topics: Location of groundwater
Ground water.
McKnight's Physical Geography Karst and Hydrothermal Processes
Water Beneath the Surface
Chapter 14 Groundwater.
Groundwater Water Beneath the Surface. Groundwater Largest freshwater reservoir for humans.
The Water Cycle                                              
Introduction to Groundwater, Karst and the Edwards Aquifer Water color by Kathy Rottier.
Reporters: Allen June Buenavista Jambee Bernales.
Water Erosion: How do processes involving water change Earth’s surface? Part 3 1.
MAIN IDEA: LANDFORMS CAUSED BY THE CHEMICAL WEATHERING OF LIMESTONE ARE CALLED KARST TOPOGRAPHY. Chp 10.2 Notes Groundwater Erosion & Deposition.
Fig. 16-CO, p Study Guide Chapter Explain how the groundwater system operates. 2.Describe the zones of aeration and saturation. 3.Locate the.
Topic Physical and Chemical Weathering. Weathering vs. Erosion Weathering--Erosion--
El Salvador, Jan How can Factor of Safety (FS) Change? FS = RF/DF Safety Factor(FS) FS =1.25; minimum for slope FS = 10; minimum for a structure.
Effects of Groundwater on Topography By Diana L. Duckworth Rustburg High School Campbell County, VA.
Biology and Geology 4. Secondary Education THE LANDFORMS CREATED BY KARST MODELLING The modelling of landforms UNIT 11.
Caves A cave is defined as an underground passage large enough for a person to crawl into, naturally formed, and in complete darkness.
Groundwater Chapter 10 Notes.
DVD Clip from Fox News on Sinkholes---1 and ½ minutes DVD on the Giant Crystal Cave DVD…formed from Gypsum….500,000 years to form largest crystal in Mexico.
The Work of Groundwater
Carboniferous Limestone
Karst and Karst Terranes
BY Faizan Saleem BS-APPLIED GEOLOGY
LIMESTONE SCENERY.
Groundwater Groundwater: water that occupies pore spaces in sediment and rock in a zone beneath the Earth’s surface Largest reservoir of fresh water available.
GROUNDWATER.
Groundwater Erosion & Deposition
Ground water.
(Discussion and Worksheet – Groundwater Part 3)
GROUNDWATER SES3d. Relate the past and present actions of ice, wind, and water to landform distribution and landscape evolution. SES3e. Explain the.
Cavern and Mineral Deposits: How Caverns Form
Lecture Outlines PowerPoint
Groundwater Erosion and Deposition Nayiri, Eileen, Liz, Talin
Denudation: Weathering and erosion
Caves.
PROF. ROBINA KOUSER ASSISTANT PROFESSOR IN GEOGRAPHY
Water Beneath the Surface
Sinkholes Lecture 28.
Click here for an animation
Chapter 9: Karst Landscape
Presentation transcript:

Karst Processes, Landforms, and Landscapes

Karst Flow Diffuse vs. conduit flow Primary vs. secondary porosity

Karst Materials Carbonate Rocks Limestone Dolomite Other materials Salt Gypsum Ice Permafrost? GEOMORPHLIST Sandstone? Copyright © Carmen Krapf 2002 Cave in sandstone, Namibia

Porosity and Permeability Recrystallization of carbonate Calcite/ aragonite Faulting, jointing Bedding

Carbonate Geochemistry Low-temperature geochemistry Calcite and water; pH ~ 10, ppm Effectively insoluble! Calcite, water, and air CO 2 ; pH ~ 8.4, 50 ppm Very slow – like soil formation Calcite, water, and soil CO 2 ; pH ~ 4-7, <700 ppm H 2 O + CO 2  H 2 CO 3 [carbonic acid] H 2 CO 3  H + + HCO 3 - CaCO 3  Ca ++ + CO 3 -- CO H +  HCO 3 - Now that will eat rock!

Variables Affecting Karst Formation Precipitation Temperature Organic matter Turbulence Copyright © Frank Eckardt 2002

Effects of mixing “Two waters meetin’, limestone is eaten.” Water sources Water table Lakes, etc. Acid sources Cave types Meteoric (CO 2 ) Hydrothermal (H 2 S)

Cavern Formation Where max. solution? Surface Water table Confluence Effects of lithology/ structure

Cave Networks – Wind Cave Note structural control!

Lechuguilla Cave (Carlsbad, NM)

Geochemical transitions Charging w/ soil CO 2 Solution of carbonate Degassing Precipitation of CaCO 3

Speleothems Stalactites Stalagmites Columns Flowstone Cave bacon Cave popcorn Helictites Shields…

Speleothems Copyright © Stephane Veyrat-Charvillon 2002 Copyright © Lynn Fielding 2002

Distribution of Karst Typical of cratons Carbonate + evaporite deposition at high sea-stands

Distribution of Karst Typical of cratons Carbonate + evaporite deposition at high sea-stands Horizontal (diapirs?) Floridan, Interior plateaus, Edwards; Madison

Karst terminology Cvijic (1893) - “krs [karst]” – bleak, waterless Davis, Penck, Bretz Karren, lapies, grike and clint “Sinkholes” Dolines, cenotes, cockpits… Polje, Uvalas Kegelkarst, tower karst Drainage Sinks/springs Valleys – dry, pocket, blind, through Copyright © Jelena Calic-Ljubojevic 2002 Copyright © Andrew Goudie 2002

Karst landscapes

Inputs and outputs

Fundamental Karst Landforms Doline (sinkhole, cenote) Origins Solution Subsidence Collapse

Winter Park sinkhole (1981) 100 m across One day During drought (water table lowering?) On city Web page; now an urban lake.

Cenotes Yucatan, Florida… Developed during glaciations Flooded during interglaciations Explored by diving

Complex Forms Polje (oval); uvala (complex) Copyright © Jelena Calic-Ljubojevic 2002

Karst Landscapes Cockpit karst Tower karst Copyright © Frank Eckardt 2002

What types of karst depression does each of the following lakes occupy? Lake AltamahaTwin LakesCrystal Lake Lake SerenaLake Belle Lake Altamahasolution doline Twin Lakessolution or subsidence uvala Crystal Lakesolution doline Lake Serenasubsidence doline Lake Bellesolution or subsidence uvala

Karst Hydrology Sinks, Swallets, Swallow holes… EX: Map view

Karst Hydrology Sinks, Swallets, Swallow holes, Ponors… EX: Map view Sink Resurgence/spring

Case Study: Mammoth Cave Interior low plateaus Sinkholes and uvala Sinks and springs

Case Study: Mammoth Cave Interior low plateaus Sinkholes and uvala Sinks and springs

Sinkholes, Uvalas, and Caves

Geology Stratigraphy Structure

Block Diagram

Cave Exploration “The Longest Cave” Now over 300 miles of interconnected passages Best explored in drought! Mammoth Cave Flint Cave

Cave Exploration “The Longest Cave” Now over 300 miles of interconnected passages Best explored in drought! Mammoth Cave Flint Cave

Mammoth Cave Evolution Theoretical evolution (undated) Upper = older, lower = younger Incision = interglacial, stability/infilling = glacial TIME