A preliminary comparison between boring from Pocala Cave and an unroofle cave at Borgo Grotta Gigante, Trieste Karst

dc.contributor.author	Tremul, A.
dc.contributor.author	Calligaris, R.
dc.date.accessioned	2010-01-25T09:38:43Z
dc.date.available	2010-01-25T09:38:43Z
dc.date.issued	2001
dc.identifier.citation	Cadernos do Laboratorio Xeolóxico de Laxe, 2001, 26: 503-507 ISSN: 00213-4497	es_ES
dc.identifier.issn	0213-4497
dc.identifier.uri	http://hdl.handle.net/2183/6527
dc.description.abstract	[Abstract] In 2000 five boring were performed in a unroofle cave at Borgo Grotta gigante, the third in particular is correlable with the boring outside Pocala Cave. The first result has been obtained by observing the absence of collapsed rocks, in particular in the unroofle cave of Borgo Grotta Gigante. Clearly limestones have dissolved
dc.language.iso	eng	es_ES
dc.publisher	Universidade da Coruña	es_ES
dc.subject	Pocala Cave	es_ES
dc.subject	Unroofle cave	es_ES
dc.subject	Borgo Grotta Gigante	es_ES
dc.subject	Boring	es_ES
dc.title	A preliminary comparison between boring from Pocala Cave and an unroofle cave at Borgo Grotta Gigante, Trieste Karst	es_ES
dc.title.alternative	Comparación preliminar entre el sondeo de Pocala y una cueva innominada en Borgo Grotta Gigante, Karst de Trieste
dc.type	info:eu-repo/semantics/article	es_ES
dc.rights.access	info:eu-repo/semantics/openAccess