The author of this book has been working in different types of karren landscapes for more than fifteen years. The book summarizes the scientific results of syst-. Karren: cave: Pavement karst: These are collectively known as karren. Karren include solutionally widened joints (kluftkarren, or cleftkarren), small runnels. Karst is a term used to describe landscapes that are formed by chemical weathering process . Karren: small hollow that forms on the surface of a limestone clint.

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In southern Saskatchewancollapse-solution cavities in salt have extended through as much as 1, m of overlying insoluble rocks to produce shallow sinkholes at the surface. Medium-sized surface karreen may include sinkholes or cenotes closed basinsvertical shafts, foibe inverted funnel shaped sinkholesdisappearing streams, and reappearing springs.

Alpine Karst

In this case the water enters the crack and does not stay on the surface. Each direction shows one stage in the tectonic history of the limestone. Carbonic acid is formed when rain picks up CO 2 as it falls through the atmosphere. List of karst areas.

Archived copy as title CS1 maint: Thousands of sinkholes exist in southern Canada, from gypsum terrains in western Newfoundland to limestones on Vancouver Island. Retrieved from ” https: Overloaded or malfunctioning septic tanks in karst landscapes may dump raw sewage karsy into underground channels. Kegelkarst is a type of tropical karst terrain with numerous cone-like hills, formed by cockpits, mogotesand poljes and without strong fluvial erosion processes.

Search The Canadian Encyclopedia. The karstification of a landscape may result in a variety of large- or small-scale features both on the surface and beneath. Sinkholes often occur in lines or clusters. This reaction chain forms gypsum.


Karst Landform

Karst formations are cavernous and therefore have high rates of permeability, resulting in reduced opportunity for contaminants to be filtered. The world’s largest limestone karst is Australia’s Nullarbor Plain. Forces in the rock typically produce many parallel fissures.

There are many large, spectacular examples in Wood Buffalo National Parkin the Franklin Mountains, and west of Great Bear Lake where limestones and dolomites have collapsed into cavities in gypsum. Karst landforms are created by water sinking and circulating underground, and the resulting chemical erosion of bedrock.

Water always takes the direction of the highest gradientwhich is commonly described by the term steepest slope.

Karstgeology: Karren – Lapies

Interstratal karst is a karstic landscape which is developed beneath a cover of insoluble rocks. Some of the modern spring water is believed to have travelled as much as 70 km underground. Very similar dissolution effects produce limestone pavements. Examples include lava caves and granite tors —for example, Labertouche Cave in VictoriaAustralia —and paleocollapse features.

These are a hazard to settlement on gypsum terrains in parts of Newfoundland and Nova Scotia. Views Oarst Edit View history.

Individual features are rarely longer or deeper than 10 m, but frequently they are densely clustered and dissect larger marst, referred to as limestone pavement. By using this site, you agree to the Terms of Use and Privacy Policy.

In English both terms are used equally and synonymously. For other uses, see Karst disambiguation. The length or diameter of sinkholes ranges from 10 to 1, m.

Karren | geology |

Large limestone surfaces get cut into pavements. In some karsts their frequency exceeds per km 2giving the terrain a shell-pitted appearance. In metropolitan Winnipegapproximately 3, km 2 of limestone pavement is preserved beneath glacial-lake clays see Lake Agassiz and serves as an important industrial water store.


Many other springs are known with peak discharges exceeding 10 m 3 per second. Karren are formed when water runs down a rock surface with a slope, dissoluting the rock while it runs.

The soils may be fertile enough, and rainfall may be adequate, but rainwater quickly karreen through the crevices into the ground, sometimes leaving the kkarst soil parched between rains. Glacier action has eroded or infilled much karst. Pseudokarsts are similar in form or appearance to karst features but are created by different mechanisms. The landforms pose some hazard to forestry practices, while clear-cutting may severely damage both surface and underground karst.

A karst landform is a geological feature created on the earth’s surface by the drainage of water into the ground. Rivers in karst areas may disappear underground a number of times and spring up again in different places, usually under a different name like Ljubljanicathe river of seven names.

The sinking water is discharged 16 km northwest at some 60 springs in the floor of Maligne Canyon. Most are formed by chemical solution in the funnel or larst collapse of the roof of an underlying cave. Ford, The Canadian Encyclopedias.