Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Philipp Häuselmann"'
Publikováno v:
International Journal of Speleology, Vol 49, Iss 2, Pp 107-118 (2020)
Karstic caves are created by water eroding and corroding rocks that can be dissolved. Since both the spring areas of caves (normally at the valley bottom) as well as the recharge is controlled by superficial processes, the morphology of the cave bear
Externí odkaz:
https://doaj.org/article/3f37d32dfa24447eaa86d5a1758ace16
Autor:
Francesco Sauro, Maria Giuditta Fellin, Andrea Columbu, Philipp Häuselmann, Andrea Borsato, Cristina Carbone, Jo De Waele
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Raponzolo is a paleo-phreatic cave explored in 2011 in the Brenta Dolomites (Trentino, Italy), at the remarkable altitude of 2,560 m a.s.l. Differently to all other caves of the area, it hosts well-cemented fine to medium sands of granitic-metamorphi
Externí odkaz:
https://doaj.org/article/b6a4ae3808474c7f8fc683c69b1f4978
Autor:
Philipp Häuselmann
Publikováno v:
International Journal of Speleology, Vol 46, Iss 2, p I (2017)
Externí odkaz:
https://doaj.org/article/9e5817644dcd4f8e841892df9a66f423
Autor:
Philipp Häuselmann
Publikováno v:
Acta Carsologica, Vol 31, Iss 3 (2016)
Predstavljen je seznam jamskih simbolov, ki jih Mednarodna speleološka zveza priporoča pri risanju načrtov podzemnih jam. Seznam simbolov so leta 1999 izvolili delegati iz dvanajstih držav. Kjer je potrebno, je poleg simbola še krajša razlaga.
Externí odkaz:
https://doaj.org/article/29c4c857676b4ee7aed1562eaa27a41a
Autor:
Philipp Häuselmann, Darryl E. Granger
Publikováno v:
Acta Carsologica, Vol 34, Iss 1 (2016)
Kozmični žarki povzročajo nastanek kozmogenih nuklidov na površini zemlje in tik pod njo. Za datiranje jamskih sedimentov sta posebej pomembna 10Be in 26Al, ki nastajata v kremenu. Ko je kamen na površini in izpostavljen kozmičnemu sevanju, nas
Externí odkaz:
https://doaj.org/article/98e1f34500da4408af6b975bac49aa41
Autor:
Philipp Häuselmann
Publikováno v:
International Journal of Speleology, Vol 37, Iss 2, Pp 107-111 (2008)
29 year old rock paintings in the Alpine karren field of Innerbergli (Siebenhengste, Switzerland) prevented the underlying rock from corrosion, while the surface nearby was corroded. Measurement of the steps indicates an average recent corrosion rate
Externí odkaz:
https://doaj.org/article/9615e187a76d4bdaaa81dc886bd6f603
Autor:
Philipp Häuselmann
Publikováno v:
Acta Carsologica, Vol 36, Iss 1 (2007)
A cave is a natural void in the rock. Therefore, a cave in itself cannot be dated, and one has to resort to datable sediments to get ideas about the age of the void itself. The problem then is that it is never very certain that the obtained age reall
Externí odkaz:
https://doaj.org/article/04f802c33d894f76861752b997bca514
Autor:
Philippe Audra, Alfredo Bini, Franci Gabrovšek, Philipp Häuselmann, Fabien Hobléa, Pierre-Yves Jeannin, Jurij Kunaver, Michel Monbaron, France Šušteršič, Paola Tognini, Hubert Trimmel, Andres Wildberger
Publikováno v:
Acta Carsologica, Vol 36, Iss 1 (2007)
Progress in the understanding of cave genesis processes, as well as the intensive research carried out in the Alps during the last decades, permit to summarize the latest knowledge about Alpine caves. The phreatic parts of cave systems develop close
Externí odkaz:
https://doaj.org/article/81080c0a2e66461e9610ea30d24c7a31
Autor:
Julia Rechenmacher, Marcel Ortler, Jasper Moernaut, Philipp Häuselmann, Markus Fiebig, Erwin Heine
Inner-Alpine lakes typically present a complex sedimentary record, with changing sediment dynamics and event deposits related to different natural hazards. Lake Altaussee (712 m asl; 2.4 x 1.0 km; max. 72 m deep) is a moderately sized lake located wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41b14451adc770006d999548e74e7fb0
https://doi.org/10.5194/egusphere-egu22-3952
https://doi.org/10.5194/egusphere-egu22-3952
Publikováno v:
International Journal of Speleology, Vol 49, Iss 2, Pp 107-118 (2020)
Karstic caves are created by water eroding and corroding rocks that can be dissolved. Since both the spring areas of caves (normally at the valley bottom) as well as the recharge is controlled by superficial processes, the morphology of the cave bear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d4e4d8f0c3202cf63bf789c6dcddeece
https://doi.org/10.5038/1827-806x.49.2.2303
https://doi.org/10.5038/1827-806x.49.2.2303