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Publication Date

2011

Publication Title

Speleogenesis and Evolution of Karst Aquifers

Issue Number

10

Abstract

Blomstrandsøya, at Kongsfjord (78 0 57’N), Spitsbergen, is within the high arctic, a completely permafrozen zone. The bedrock consists of Paleozoic marbles and has yielded a surprising amount of karst features. Early phases of hydrothermal, possibly Caledonian, speleogenesis and subsequent Devonian karstification with redbed deposits is well documented. 62 active seacaves, and more than 30 relict karst caves were found in the coastal cliffs and in escarpment faces around the island. All caves have very limited extent; they are either quite short, like most of the active sea caves, or they are soon choked by frozen sediments and ground ice after a few meters. The deepest penetration was some 34 m into the surface cliff. Many of the relict caves are scalloped and display well-defined paragenetic wall and ceiling half-tubes, implying that they are indeed conduits, leading further into the rock mass, beyond their present permafrozen terminations. Most of the speleogenetic volume of the relict caves is ascribed to sub-glacial conditions during stadials, when the site was covered beneath thick ice sheets. In many cases, the present caves were formed by reactivation of pre-existing paleokarst voids. Due to the present intense gelifraction and erosion in the littoral zone, and the relatively constant sea level during the past 9.5 kyr, most of the volume of the sea caves can be explained by processes acting during the Holocene.

Keywords

Karst, Speleogenesis, Arctic, Permafrost, Quaternary, Subglacial

Geographic Subject

Kongsfjord (Norway)

Document Type

Article

Language

English

Identifier

K26-04225

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Article Location

 
COinS

Latitude

79.00518749999999

Longitude

11.7149375
 
 

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