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Goran VLASTELICA 1 , Kristina PIKELJ 2 , Branko KORDIĆ 3 1 Facultyof Civil Engineering, Architecture and Geodesy, University of Split, Croatia 2 Faculty of Science, Department of Geology, University of Zagreb 3 Croatian Geological Survey, Zagreb, Croatia

Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

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Page 1: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Goran VLASTELICA1, Kristina PIKELJ2, Branko KORDIĆ3

1Facultyof Civil Engineering, Architecture and Geodesy, University of Split, Croatia

2Faculty of Science, Department of Geology, University of Zagreb 3Croatian Geological Survey, Zagreb, Croatia

Page 2: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Rationale

cliffs in soft rocks – rare coastal

forms in Croatia

Croatian Adriatic coast is mostly

built in carbonates (> 90%)

flysch* is less present coastal rock

(~6%)

flysch cliff in Split urban zone

occupied since 1980-ies

tourism, urbanization

cliff stability? cliff erosion?

*flysch → marl - siltstone - sandstone -

breccia assemblage

Political and simplified lithological map of the

Eastern Adriatic coast (modified after Pikelj &

Juračić, 2013)

Page 3: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Study area and aims

to recognize cliff erosion driving mechanisms

to assess the erosional rate

Split cliff developed in

flysch

(slobodnadalmacija.hr)

Page 4: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Methodology

cliff-face morphology was scanned

11 times over 6 years (2012-2018)

by terestrial laser scanner

overlapped point clouds

4 representative profiles were

chosen and compared

cliff-top, cliff face and shore

platform were examined 15 times

during various various

seasons/weather conditions

Cliff face during scanning process (above) and

examination during cold season (below)

Page 5: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

cliff retreat rates: 3-18 cm/y

extreme erosion (up to 34 cm/y)

during 2014/2015 and 2017/2018 –

higher precipitation

occurence of landslides 2018 –

due to intensive rain

water related denudation

processes:

gullies formation,

groundwater seepage

sapping

slaking

removal of material by waves

Results

Position of chosen profiles (above) and example

of compared profiles on the steepest part of the cliff

Spring 2012

Spring 2014

Autumn 2014

Spring 2015

Autumn 2015

Spring 2016

Autumn 2016

Spring 2017

Page 6: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Re-occurence in 2018 – due to intensive rain

Initial landslide in 2010

Results

2010. 2015.

2019. 2018.

Page 7: Goran VLASTELICA , Kristina PIKELJ Branko KORDIĆ · seasons/weather conditions Cliff face during scanning process (above) and examination during cold season (below) ... PowerPoint

Conclusions

erosion of soft flysch cliff in the urban zone

stronger erosion occurs during cold/wet season - slaking

denudational processes related to intensive rain and higher precipitation

rates

flysch lithology – the main precondition of the enhanced weathering

highly needed management of erosion

This research was supported mostly by the project entitled

Risk Identification and Land-Use Planning for Disaster Mitigation of Landslides,

sponsored by Japan Science

and Technology Agency - JST, Japan International Cooperation Agency - JICA and

Ministry of Science, Education and Sport of Republic of Croatia