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1987
Spring is a points of natural, concentrated discharge of groundwater at a rate high enough to maintain flow on the surface. Generally springs are formed where water table intersects with the earth’s surface, or groundwater rises to the surface through rock faults, fractures or depressions.
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Spring is a points of natural, concentrated discharge of groundwater at a rate high enough to maintain flow on the surface. Generally springs are formed where water table intersects with the earth’s surface, or groundwater rises to the surface through rock faults, fractures or depressions.
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2017
This chapter describes the extent and formation of karst in Kentucky: how the dissolution of limestone by water shapes the underground and surface of over half of Kentucky; the ways that hydro geologists map karst aquifers, including illustrative examples. The beauty of caving in the Mammoth Cave area and throughout Kentucky karst is illustrated.
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This chapter describes the extent and formation of karst in Kentucky: how the dissolution of limestone by water shapes the underground and surface of over half of Kentucky; the ways that hydro geologists map karst aquifers, including illustrative examples. The beauty of caving in the Mammoth Cave area and throughout Kentucky karst is illustrated.
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Karst and karst groundwater resources in the Mediterranean
Environmental Earth Sciences, 2015Karst landforms were first described and studied in Mediterranean regions, where these common landforms display their main hydrological characteristics. For this reason, Mediterranean karst is often considered to be the common reference. However, when we examine the general settings of Mediterranean karst and their groundwater resources more carefully,
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Karst spring catchment: an example from Dinaric karst
Environmental Earth Sciences, 2015Definition of karst spring catchment or basin area and boundaries belongs to one of the greatest problems of karst hydrology and hydrogeology, not adequately solved until now. This paper tries to address main problems in defining this crucial parameter. The theoretical aspect of this issue is discussed in the first two chapters.
Bonacci, Ognjen, Andrić, Ivo
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Sustainability of the karst environment - Dinaric karst and other karst regions
2010The objective of the international interdisciplinary scientific conference “Sustainability of the karst environment - Dinaric karst and other karst regions”, organized by Centre for Karst, Gospić, Croatia, was to give a theoretical and practical contribution to the concept of sustainable development in karst regions, with a special emphasis on the ...
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Karst Terminology and Karst Types in China
1995Before discussing the main karst types in China, some aspects of Chinese karst terminology should be described. In geomorphology, Chinese geographers and hydrogeologists are more concerned with groupings of landforms than with the origins of individual forms.
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Karst and karst water recourses of Albania and their management
Carbonates and Evaporites, 2020Albania is situated in the western part of Balkan Peninsula, on the eastern coast of the Adriatic and the Ionian Sea, which is one of the most water−rich regions of the world. The karst landscape in Albania covers about 2750 km2 consisting of nearly 24% of the countries territory. Karstic aquifers are the richest in the country.
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