My first blog

• Feb. 3, 2008 - Mammoth cave

  • Karst Geology
  • The Ancient World
  • was located much closer to the equator. A shallow
  • sea covered most of the southeastern United States,
  • and its warm water supported a dense population of
  • tiny organisms whose shells were made of calcium
  • carbonate (CaCO3). As these creatures died, their
  • shells accumulated by the billions on the sea fl oor.
  • In addition, calcium carbonate can precipitate from
  • the water itself. The build-up of material continued
  • for 70 million years accumulating seven hundred
  • feet of limestone and shale followed by sixty feet of
  • sandstone that was deposited over much of the area
  • by a large river system fl owing into the sea from the
  • north.
  • About 280 million years ago the sea level started to
  • fall exposing the layers of limestone and sandstone.
  • Additional tectonic forces caused the earth’s crust
  • to slowly rise causing cracks to form in and between
  • the limestone and sandstone formations. As the uplift
  • continued, rivers developed which over millions
  • of years have created the sandstone-capped plateau
  • above the Green River and the low, almost fl at limestone
  • plain which extends southeast of I-65.
  • 350 million years ago the North American continent
  • Beneath the surface of South Central Kentucky
  • dark, seemingly endless passageways. The geological processes which formed this world
  • referred to as Mammoth Cave began hundreds of millions of years ago and continue
  • today.
  • lies a world characterized by miles of
  • Look Beneath
  • “Acid Rain”
  • seeped downward through cracks in the limestone
  • and began to dissolve and create the labyrinth
  • of passages we know as Mammoth Cave. As the
  • land continued to rise slowly, Green River eroded
  • its channel deeper and deeper, passages created
  • drained through the limestone toward the river
  • which became the out-source for waters creating
  • the cave. Because the major drains carried the most
  • water, they enlarged faster. As Green River eroded
  • its channel deeper into the bedrock, cave passages
  • continued dropping to the same level as the Green
  • River. Upper level passages drained and became
  • dry. At the present water table, cave passages are still
  • forming.
  • Rain water, acidifi ed by carbon dioxide in the soil
  • Surface Clues
  • existence of caves. Road cuts along the highway
  • expose vast amounts of soluble limestone which
  • display solutionally enlarged vertical cracks, an indicator
  • that caves are forming. The undulating landscape
  • along the interstate is created by crater like
  • depressions called “sinkholes’, which funnel surface
  • water into the passages below. It is referred to as the
  • “Land of 10,000 sinks” or the Sinkhole Plain. At the
  • southeast edge of the Sinkhole Plain, surface streams
  • suddenly sink underground joining the drainage
  • from thousands of sinkholes and continuing to the
  • Northwest where they become the underground rivers
  • in Mammoth Cave. Soluble limestone, sinkholes,
  • sinking streams and caves create a landform called
  • Karst Topography.
  • As you approach the park, several clues suggest the
  • Mammoth Cave
  • U.S. Department of the Interior
  • Mammoth Cave
  • National Park
  • National Park Service
  • Driving Northwest from Cave City or Park City, you
  • climb the Chester Escarpment which rises some 300
  • feet above the sinkhole plain. Beyond the top of the
  • escarpment the plateau is divided into fl at sandstone
  • capped ridges separated by steep, limestone-fl oored
  • The Uplands
  • capped ridges that protect the cave.
  • valleys with many sinkholes. It is the sandstone
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    I'm 7 yr. old and this is where I go to journal and do some of my "school work."

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