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  5. Geomorphologic Map of Northeastern Sector of San Jorge Gulf (Chubut, Argentina)
 
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Geomorphologic Map of Northeastern Sector of San Jorge Gulf (Chubut, Argentina)

Author(s)
Isola, I.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Bini, M.  
Dipartimento di Scienze della Terra, University of Pisa, Pisa, ITALY  
Ribolini, A.  
Dipartimento di Scienze della Terra, University of Pisa, Pisa, ITALY  
Pappalardo, M.  
Dipartimento di Scienze della Terra, University of Pisa, Pisa, ITALY  
Consoloni, I.  
Dipartimento di Scienze della Terra, University of Pisa, Pisa, ITALY  
Fucks, E.  
Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, INGEA, La Plata, ARGENTINA.  
Boretto, G.  
CICTERRA (Centro de Investigaciones en Ciencias de la Tierra) Avenida Vélez Sárfield 1611. CP 5016. Córdoba, ARGENTINA.  
Ragaini, L.  
Dipartimento di Scienze della Terra, University of Pisa, Pisa, ITALY.  
Zanchetta, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Language
English
Obiettivo Specifico
1.10. TTC - Telerilevamento
3.7. Dinamica del clima e dell'oceano
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Maps  
Issue/vol(year)
/2011( 2011)
Pages (printed)
476-485
Date Issued
2011
DOI
10.4113/jom.2011.1203
URI
https://www.earth-prints.org/handle/2122/7499
Subjects
03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatology  
04. Solid Earth::04.04. Geology::04.04.02. Geochronology  
04. Solid Earth::04.04. Geology::04.04.03. Geomorphology  
Subjects

Geomorphology

Remote sensing

Sea level

Abstract
This paper presents a 1:100,000 scale geomorphologic map of the Northeastern sector of San Jorge Gulf
(Chubut Province) in Patagonia, Argentina, covering more than 1,000 km2. Derived from remote sensing
data and validated by three field surveys, it has been compiled in order to understand the past and recent evolution of the area with particular reference to sea-level oscillation studies, for which this map is the
basic tool. The very low human impact and rates of dynamic landscape change allow the preservation
of extensive palaeo deposits and landforms, including those indicative of sea-level variations. The relative
change of sea level dominates landscape evolution, allowing the formation of widespread marine
and lagoon deposits often interfingering with fluvial deposits and reworked by aeolian process in the framework of consequent beach progradation.
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