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fujisoft.tw

Show text Show cached source Open source URL	Dodatno ležište
Compare text pages Compare HTM pages Open source URL Open target URL Define rooms-silak.com as primary domain	Additional bed
Compare text pages Compare HTM pages Open source URL Open target URL Define rooms-silak.com as primary domain	Lit supplémentaire
Compare text pages Compare HTM pages Open source URL Open target URL Define rooms-silak.com as primary domain	Zusatzbett
Compare text pages Compare HTM pages Open source URL Open target URL Define rooms-silak.com as primary domain	Posto letto supplementare
Compare text pages Compare HTM pages Open source URL Open target URL Define rooms-silak.com as primary domain	Dodatno ležišče

madrid.ticketbar.eu

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Duž dijela jugozapadne obale otoka ističe se strmac koji doseže visinu višu od 160 m iznad morske razine na lokaciji Grpašćak, ali proteže se i ispod morske razine do dubine od 85 m te predstavlja najveći strmac na Jadranu. Značajnu ulogu u formiranju strmca imali su pokreti duž Dugootočkog rasjeda, a dodatno je oblikovan abrazijskim procesima zbog obale okrenute otvorenom moru.

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Today’s relief is the result of geological characteristics of the area and the post-Pliocene ingression of sea when the global sea level rose 100 m. The rising of global sea level made changes to the area of Telašćica. Telašćica Bay used to be a dry field divided into three sections – three karst sinkholes with occasional flows of streams. During this period, the relief above sea level was exposed to processes of erosion and corrosion, and abrasion along the coastline. The peaks of mountain chains that stretched in the northwest-southeast direction in several parallel lines are now islands. The most prominent feature of one part of the southwestern coast is a steep slope reaching up to a height of 160 m above sea level at the location of Grpašćak, and stretching down to a depth of 85 m under sea level, presenting one of the greatest steep slopes of the Adriatic. Movements along the fault of Dugi Otok had played a significant role in the formation of the steep slope, and it was further shaped by processes of abrasion because of the coast facing in the direction of the open sea. The entire area of Dugi Otok is located on a seismically active zone with folding, faulting and pulling of the Earth’s crust.

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