Limestone is a biological sedimentary rock formation composed mostly of calcite, a calcium carbonate mineral, and often resembles concrete. It forms as shells, corals, algae, fecal matter and other organic debris settle and accumulate on the bottom of a waterbody. Because of the conditions of its formation, limestone may hold fossils from a time long ago. According to Otonabee Conservation the limestone bedrock of the Warsaw area was laid down in the Paleozoic Era when shallow seas covered the region over 350 million years ago. Many organisms, from corals to microscopic foraminifera that grew shells from the carbonates in the water, contributed their carbonate shells when they died, accumulating in the sediments of the shallow seas. This sediment then lithified into limestone.
Geology.com writes that “cementation” is an important step in the transformation of a sediment into rock with precipitated calcium carbonate contributing as much as 50% and as little as a few percent of the rock by volume.
The calcium carbonate of the sea or freshwater may also crystallize out of solution during evaporation to form chemical limestones; but this process is more rare and not observed at Warsaw Caves. Evaporative limestones form the kind of caves most of us imagine when we think of caves. These form stalactites, stalagmites and other cave formations (often called “speleotherms”). Such caves are often huge and the limestone is known as “travertine,” a chemical sedimentary rock that can exist as “tufa,” at a hot spring or on the shoreline of a lake in an arid area.
Action of Glaciers
Millennia ago, a series of Pleistocene epoch glaciations, including the Wisconsin ice age, covered the Warsaw Caves area with ice sheets up to three kilometers. When the glaciers began their final retreat 12,000 years ago, meltwaters created Lake Algonquin (the present-day upper Great Lakes and Lake Simcoe) and Lake Iroquois (present-day Lake Ontario). The flow of glacial meltwater from the two lakes formed the Kirkfield Spillway, which included the Indian and Otonabee Rivers. Deep and swift, these glacier-fed rivers shaped the landscape, creating caves, kettles, limestone cliffs and ledges, and underground channels.
Limestone’s distinctive crystal structure allows it to crack and fracture in a distinct pattern. On limestone cliffs you can easily make out the horizontal cracks called ‘bedding planes’ and the vertical cracks called ‘joints.’ These allow water to easily flow through the limestone rock.The slightly acidic river that flowed over the bedrock made its way into and through these cracks, dissolving the limestone over thousands of years and widening the natural cracks and rock fissures in a process called carbonation. Over time a karst topography formed in the porous limestone at Warsaw Caves as water dissolved the limestone through a process called karstification. This created deep fissures and sinkholes, underground caves and streams. The word ‘karst’ comes from the pre-Indo-European language in which ‘kar’ means ‘rock.’ In Slovenia the word ‘kras,’ later Germanised as ‘karst,’ comes from the name of a barren stony limestone area near Trieste, which is still considered the type area for limestone karst.
Nina Munteanu is a Canadian ecologist / limnologist and novelist. She is co-editor of Europa SF and currently teaches writing courses at George Brown College and the University of Toronto. Visit www.ninamunteanu.ca for the latest on her books. Nina’s bilingual “La natura dell’acqua / The Way of Water” was published by Mincione Edizioni in Rome. Her non-fiction book “Water Is…” by Pixl Press (Vancouver) was selected by Margaret Atwood in the New York Times ‘Year in Reading’ and was chosen as the 2017 Summer Read by Water Canada. Her novel “A Diary in the Age of Water” was released by Inanna Publications (Toronto) in June 2020.
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