Geomorphometric monitoring of active slopes and their impact on post-glacier lake in the Tatra Mountains
PBN-AR
Instytucja
Wydział Geodezji Górniczej i Inżynierii Środowiska (Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie)
Książka
Tytuł książki
SGEM2013. GeoConference on Informatics, geoinformatics and remote sensing : 13\textsuperscript{th} international multidisciplinary scientific geoconference : 16–22, June, 2013, Albena, Bulgaria : conference proceedings
Data publikacji
2013
ISBN
978-619-7105-01-8
Wydawca
STEF92 Technology Ltd.
Publikacja
Główny język publikacji
EN
Tytuł rozdziału
Geomorphometric monitoring of active slopes and their impact on post-glacier lake in the Tatra Mountains
Rok publikacji
2013
Strony (od-do)
245--252
Numer rozdziału
Link do pełnego tekstu
Identyfikator DOI
Liczba arkuszy
0.55
Hasło encyklopedyczne
Autorzy
Pozostali autorzy
+ 1
Słowa kluczowe
EN
monitoring
geomorphometry
post-glacial lake
scree
bathymetry
Konferencja
Indeksowana w Scopus
nie
Indeksowana w Web of Science Core Collection
tak
Liczba cytowań z Web of Science Core Collection
Nazwa konferencji (skrócona)
SGEM2013
Nazwa konferencji
GeoConference on Informatics, geoinformatics and remote sensing : 13\textsuperscript{th} international multidisciplinary scientific geoconference
Początek konferencji
2013-06-16
Koniec konferencji
2013-06-22
Lokalizacja konferencji
Albena
Kraj konferencji
BG
Lista innych baz czasopism i abstraktów w których była indeksowana
Streszczenia
Język
EN
Treść
In the natural screes the erosive phenomena occur as a result of physical, chemical or biological factors. These processes are particularly visible in the high mountain environment. They are favored by snow avalanches, heavy rain and naturally occurring large terrain slopes. Their results are the mass movements, which may significantly change the geometry of rock debris and land relief around the scree. Eventually, the consequences of mass movements may also be landslides and rockfalls, which are dangerous to the surrounding area. Therefore, it is important to monitor and clear understand the processes taking place on the slopes. The presented works, performed with the use of terrestrial laser scanning and integrated bathymetric system, were aimed at carrying out an accurate and current bathymetric map of one of the post-glacial lakes in the High Tatras and the depiction of geomorphological phenomena occurring on the surrounding slopes in a uniform spatial reference system. The GNSS observations, referenced to the nationwide CORS (Continuously Operating Reference Station) network, and the additional surveying measurements enabled to create a coherent model of slopes and bottom of the lake in a uniform coordinate system. The authors present a methodology for obtaining the data as well as aspects of measurement accuracy. In addition, the authors present the first detailed bathymetric map of the Czamy Staw Gasienicowy Lake obtained with modem techniques.
Cechy publikacji
chapter-in-a-book
peer-reviewed
Inne
System-identifier
idp:074728