Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5780454 | Journal of South American Earth Sciences | 2017 | 33 Pages |
Abstract
The bathymetry and geomorphological characteristics of Udaeta Lake are herein presented. This lake is located in the central-eastern portion of Isla Grande de Tierra del Fuego and it fills a structural depression originated along a section of the Magallanes-Fagnano Fault System. Based on a bathymetric survey, the depth data of the lake allowed for describing it by means of several morphometric parameters. Udaeta Lake has an area of 159Â ha, a perimeter of 4.911Â m, and a maximum depth of 25.9Â m. Two sub-basins can be recognized within the Udaeta Lake: a large-size (ca. 953Â ÃÂ 1012Â m), deep (25.9Â m), and asymmetric basin located to the east and a smaller (175Â ÃÂ 317Â m), shallower (17Â m) sub-basin to the west. The Udaeta Lake is characterized as a geomorphologic feature of the Magallanes Fagnano Fault System, i.e. as an active pull-apart basin. In this paper, we provide information that may help to the geomorphological characterization and interpretation of the neotectonic genesis of Udaeta Lake.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
M. Romina Onorato, Andrea Coronato, Laura P. Perucca, Jorge Rabassa, Ramiro López,