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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1365-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1365/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1365/2010/tcd-4-1365-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1365/2010/tcd-4-1365-2010.pdf</fulltext_pdf>
	<start_page>1365</start_page>
	<end_page>1389</end_page>
	<publication_date>2010-08-23</publication_date>
	<article_title content_type="html">Application of ground penetrating radar (GPR) in Alpine ice caves</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Hausmann</name>
			<email>hausmann@mail.zserv.tuwien.ac.at</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Behm</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geodesy and Geophysics, Vienna University of Technology, Vienna, Austria</affiliation>
	</affiliations>
	<abstract content_type="html">Several caves in high elevated alpine regions host up to several meters
thick ice fillings. The age of the ice may exceed some hundreds or thousands
of years. However, structure, formation and development of the ice are not
fully understood and are subject to relatively recent investigation. The
application of ground penetrating radar (GPR) enables to determine
thickness, volume, basal and internal structure of the ice fillings and
provides as such important constraints for related studies. We present
results from four caves located in the Northern Calcareous Alps of Austria
and show that cave ice is far from being uniform. The transition from ice to
the ground has variable reflection signatures, which is related to the
deposit and size of debris. The internal structure of the ice fillings is
characterized by banded structures which are inclined or parallel to the
subsurface topography. These reflection signatures can result from thin
layers of calcitic minerals and might help to understand the ice formation
by representing isochrones.</abstract>
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</article>

