http://www.cnr.it/ontology/cnr/individuo/prodotto/ID41726
Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings (Articolo in rivista)
- Type
- Label
- Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings (Articolo in rivista) (literal)
- Anno
- 2010-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1029/2009GL041821 (literal)
- Alternative label
Wall S., A. Hayes, C. Bristow, R. Lorenz, E. Stofan, J. Lunine, A. Le Gall, M. Janssen, R. Lopes, L. Wye, L. Soderblom, P. Paillou, O. Aharonson, H. Zebker, T. Farr, G. Mitri, R. Kirk, K. Mitchell, C. Notarnicola, D. Casarano, B. Ventura (2010)
Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings
in Geophysical research letters
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Wall S., A. Hayes, C. Bristow, R. Lorenz, E. Stofan, J. Lunine, A. Le Gall, M. Janssen, R. Lopes, L. Wye, L. Soderblom, P. Paillou, O. Aharonson, H. Zebker, T. Farr, G. Mitri, R. Kirk, K. Mitchell, C. Notarnicola, D. Casarano, B. Ventura (literal)
- Pagina inizio
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.agu.org/pubs/crossref/2010/2009GL041821.shtml (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Dipartimento Interateneo di Fisica, Bari; EURAC, Bolzano; Jet Propulsion Laboratory, Pasadena, California (literal)
- Titolo
- Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings (literal)
- Abstract
- Of more than 400 filled lakes now identified on Titan,
the first and largest reported in the southern latitudes is
Ontario Lacus, which is dark in both infrared and
microwave. Here we describe recent observations including
synthetic aperture radar (SAR) images by Cassini's radar
instrument (l = 2 cm) and show morphological evidence
for active material transport and erosion. Ontario Lacus
lies in a shallow depression, with greater relief on the
southwestern shore and a gently sloping, possibly wavegenerated
beach to the northeast. The lake has a closed
internal drainage system fed by Earth-like rivers, deltas
and alluvial fans. Evidence for active shoreline processes,
including the wave-modified lakefront and deltaic
deposition, indicates that Ontario is a dynamic feature
undergoing typical terrestrial forms of littoral modification. (literal)
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- Autore CNR
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