Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Matti J. Rossi"'
Publikováno v:
Jökull. 51:1-16
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da775bde28ef3b429e5fc35a85fe5d96
https://doi.org/10.33799/jokull2002.51.001
https://doi.org/10.33799/jokull2002.51.001
Publikováno v:
Geoarchaeology. 17:633-648
Chullpas are pre-Columbian burial towers built by indigenous Aymaras on the Bolivian Altiplano. Bolivian chullpas date back to the Late Intermediate Period (A.D. 1000–1476) and the Late Horizon (A.D. 1476–1532). We recorded 228 chullpas among 84
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed69d98d70df3db079da6649797a5e59
https://doi.org/10.1002/gea.10032
https://doi.org/10.1002/gea.10032
Autor:
Matti J. Rossi
Publikováno v:
Geomorphology. 20:95-112
An open-channel lava flow of olivine tholeiite basalt, 9 km long and 1–2 km wide, formed in a volcanic eruption that took place in the Krafla volcano, Iceland, on the 4–18 September 1984. The eruption started with emplacement of a pahoehoe sheet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e6c0ddaa4260ab0e38a65da42d9160c
https://doi.org/10.1016/s0169-555x(97)00007-x
https://doi.org/10.1016/s0169-555x(97)00007-x
Autor:
Matti J. Rossi
Publikováno v:
Bulletin of Volcanology. 57:530-540
Postglacial Icelandic shield volcanoes were formed in monogenetic eruptions mainly in the early Holocene epoch. Shield volcanoes vary in their cone morphology and in the areal extent of the associated lava flows. This paper presents the results of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::760dbb56f5b1285f29325a1ed22706e8
https://doi.org/10.1007/bf00304437
https://doi.org/10.1007/bf00304437
Publikováno v:
Technical University of Denmark Orbit
[1] Images of the Northern plain on Mars have revealed up to 1500 km long lava flows. The low density of impact craters on the lava flows implies that these lava flows were formed during the most recent volcanic activity on Mars. Estimates of the age
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c4300ea1094f6f25487af0e9c9ad7b0e
https://doi.org/10.1029/2005je002536
https://doi.org/10.1029/2005je002536
Autor:
Henning Haack, Thorvaldur Thordarson, Stephen Self, Alfred S. McEwen, Marie-Noëlle Guilbaud, Matti J. Rossi, Laszlo P. Keszthelyi
Publikováno v:
Geochemistry, Geophysics, Geosystems. 5
We report on new field observations from Icelandic lava flows that have the same surface morphology as many Martian flood lava flows. The Martian flood lavas are characterized by a platy-ridged surface morphology whose formation is not well understoo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b25d4892da5e09c24223d658c6e14fef
https://doi.org/10.1029/2004gc000758
https://doi.org/10.1029/2004gc000758