Pregled bibliografske jedinice broj: 701658
Marine erosion and slope movements: SE coast of the Krk Island
Marine erosion and slope movements: SE coast of the Krk Island // Landslide Science for a Safer Geoenvironment, Volume 3: Targeted Landslides / Sassa, Kyoji ; Canuti, Paolo ; Yin, Yueping (ur.).
Peking, Kina: Springer, 2014. str. 563-567 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 701658 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Marine erosion and slope movements: SE coast of the Krk Island
Autori
Benac, Čedomir ; Dugonjić Jovančević, Sanja ; Ružić, Igor ; Vivoda, Martina ; Peranić, Josip
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Landslide Science for a Safer Geoenvironment, Volume 3: Targeted Landslides
/ Sassa, Kyoji ; Canuti, Paolo ; Yin, Yueping - : Springer, 2014, 563-567
ISBN
978-3-319-04995-3
Skup
World Landslide Forum 3
Mjesto i datum
Peking, Kina, 02.06.2014. - 06.06.2014
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
coast; marine erosion; landslide; Adriatic Sea; sea-level
Sažetak
This paper presents the interaction of the marine erosion and slope movements on the south eastern coastal area of the Krk Island. Larger parts of the coastal bedrock are carbonate rocks, and smaller parts are marls and flysch. The bedrock is occasionally covered with Quaternary sediments, which are characterized in terms of engineering soil properties. Complex geological fabric of the coastal area around Stara Baška settlement, in the south western part of the Krk Island, caused different movements on the coast. Due to the different grade of fissuring and karstification, as well as different weathering grade, carbonate and siliciclastic rock mass have wide range of resistance to the sea effects including wave attack. Exposure to the wave attack generated due to winds from the south directions contributes to the decreased resistivity. Additionally, occasional torrent flows and intensive erosion cause sporadic higher slope instability. Effect of the previously registered extremely high tides, as well as the possible hazard increase due to the estimated sea level rise, is also analysed in the paper.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Građevinarstvo
Napomena
DOI: 10.1007/978-3-319-04996-0
POVEZANOST RADA
Ustanove:
Građevinski fakultet, Rijeka
Profili:
Igor Ružić
(autor)
Čedomir Benac
(autor)
Martina Vivoda Prodan
(autor)
Josip Peranić
(autor)
Sanja Dugonjić Jovančević
(autor)