2011
DOI: 10.17704/eshi.30.1.n76v556205141ux3
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Communication and ‘Forestructures’ at the Geological Intersection of Caves and Subsurface Water Flow: Hermeneutics and Parochialism

Abstract: The direction of cave and karst science throughout its history has been partly determined by communication-or, more commonly, the lack of communication-between non-scientist cavers and non-caving physical geologists writing about karst. Within each community, advancement of 'cave awareness' occurred through a hermeneutic circle in which 'forestructures' guided progress. One result was regionalism of speleo-genetic theories developed within karst science because of the weight of evidence placed upon local or re… Show more

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Cited by 7 publications
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“…In contrast, during times of higher Q , C/Cs values are < 1 and DIC concentrations drop below 0.8 mmol/l (Figure ). DIC flux increases linearly with Q (Figure ) and demonstrates the relative importance of infrequent storm events to solute flux and the thus landscape evolution (Groves and Meiman, ; Florea and Vacher, ). In fact, 48% of the 15 600–21 800 kg of DIC emerged from Redmond Creek aquifer during 12.8% of the duration of this study when Q > Q mean and the C/Cs values are low (Figure ).…”
Section: Discussionmentioning
confidence: 90%
“…In contrast, during times of higher Q , C/Cs values are < 1 and DIC concentrations drop below 0.8 mmol/l (Figure ). DIC flux increases linearly with Q (Figure ) and demonstrates the relative importance of infrequent storm events to solute flux and the thus landscape evolution (Groves and Meiman, ; Florea and Vacher, ). In fact, 48% of the 15 600–21 800 kg of DIC emerged from Redmond Creek aquifer during 12.8% of the duration of this study when Q > Q mean and the C/Cs values are low (Figure ).…”
Section: Discussionmentioning
confidence: 90%