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  5. Remote sensing of volcanic terrains by terrestrial laser scanner: preliminary reflectance and RGB implications for studying Vesuvius crater (Italy)
 
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Remote sensing of volcanic terrains by terrestrial laser scanner: preliminary reflectance and RGB implications for studying Vesuvius crater (Italy)

Author(s)
Pesci, A.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia  
Teza, G.  
Universita' Padova  
Ventura, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Language
English
Obiettivo Specifico
1.10. TTC - Telerilevamento
3.5. Geologia e storia dei sistemi vulcanici
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Annals of Geophysics  
Issue/vol(year)
4/51 (2008)
Publisher
editrice compositori
Pages (printed)
633-653
Date Issued
August 2008
URI
https://www.earth-prints.org/handle/2122/3989
Subjects
04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks  
05. General::05.01. Computational geophysics::05.01.01. Data processing  
Subjects

Lidar

Vesuvius

Abstract
This work focuses on the use of terrestrial laser scanner (TLS) in the characterization of volcanic
environments. A TLS survey of the Vesuvius crater (Somma-Vesuvius volcano, Italy) allows the construction
of an accurate, georeferenced digital model of different sectors of the crater. In each sector, the intensity is
computed for each point as the ratio between the emitted amplitude and the received one, normalized to the
maximum signal, providing the radiometric information. Moreover, the RGB colours of the observed surfaces
can be captured by means of a calibrated camera mounted on the TLS instrument. In this way, multi-band
information is given, since a long range TLS operates in the near infrared band. The reflectance and RGB
data are compared in order to verify if they are independent enough to be complementary for model analysis
and inspection. Results show that the integration of RGB and intensity data can fully characterize this
volcanic environment. The collected data are able to discriminate different volcanic deposits and to detect
their stratigraphic features. In addition, our results shed light on the spatial extension of landslides and on
the dimensions of rock fall/flow deposits affecting the inner walls of the crater. The remotely acquired TLS
information from the Vesuvius crater is compared with that from a sedimentary terrain (coal-shale quarry) to
detect possible similarities/differences between these two geological environments.
Type
article
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Format

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