karst processes and landforms. objectives discuss processes producing karst landscapes and...
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Karst Processes and Landforms
Objectives
• Discuss processes producing karst landscapes and influencing environmental factors
• Analyze landscapes characterizing karst landscapes and describe their formation
• Relate karst process to development of undeground cave systems
Introduction
• Through dissolution of rocks landscapes are formed
• Karst is name for landscapes and landforms produced and processes causing them
• Most karst landforms beneath ground– Limestone caves are examples
Karst Processes
• Rock must be soluble in water– Most karst develop in limestones• Limestone must be less than 20-30% other minerals• More porosity favors karst
– Also in gypsum, dolomite, even sandstone
Role of Water and Climate
• Karst forms slowly in dry climates, faster in humid one
• Carbonation is important process– More CO2 in water favors dissolution
Relief• Flat rocks slow underground drainage and karst
development• High relief causes more rapid water movement• Deepening valleys lower water table causing varying levels
of karst
Groundwater
• Karst forms large pathways for rapid groundwater flow
• Dyes can trace water flow
• Contaminants move quickly
Karst Landforms and Landscapes—Temperate Karst
• Slower forming karst with:– Disappearing
streams– Jagged rock masses– Solution
depressions– Extensive cave
networks
Karst Landforms and Landscapes—Tropical Karst
• Rapidly forming karst characterized by:– Larger solution features– More vegetation cover• More organic acids and biogenic action
– Steep sided hills
Karst Landforms and Landscapes—Caribbean Karst
• Forms in few locations such as Florida
• Hills feed water to flat lying limestones near sea level– Conduits form. Collapse
form surface depressions
Disappearing Streams and Sinkholes
• Streams disappear in swallow holes– Holes formed by dissolution
along fault or joint• Solution sinkholes may be
large and area may contain thousands
• Collapse sinkholes form through collapse of roof– Include collapse and suffusion
sink– Two or more sinkhole coming
together form large depression called uvala
Karst Towers
• Cone-shaped, steep-sided hill
• Main feature in tropical karst
• Maybe 100s of meters tall• Form through lack of soil
and vegetation cover on parts of limestone bedrock– Surrounding area lowered
through dissolution
Karst and Caves• Form through dissolution
along joints/fractures– Consist of portal and
termination– Cave network depends on
stratigraphy, faulting, jointing– Large areas form chambers
or rooms– Stalactites (hanging) and
stalagmites (standing) form