Predictive model of the vertical movements of the earth's surface: implications for the land use of the Lithuanian coastal area

Šliaupa, Saulius; Bitinas, Albertas; Zakarevičius, Algimantas

Use this url to cite publication: https://hdl.handle.net/20.500.14911/138376

Predictive model of the vertical movements of the earth's surface: implications for the land use of the Lithuanian coastal area

Details

Publication Type (CRIS)

Straipsnis recenzuojamoje užsienio tarptautinės konferencijos medžiagoje / Article in peer-reviewed foreign international conference proceedings (P1d)

Publication Type (eLABa)

Straipsnis recenzuotame konferencijos darbų leidinyje / Article published in peer-reviewed conference proceedings (P1d)

Author(s)

Author	Affiliation
Šliaupa, Saulius	Geologijos ir geografijos institutas
Bitinas, Albertas	Lietuvos geologijos tarnyba prie Aplinkos ministerijos
Zakarevičius, Algimantas	Aviacijos technologijų katedra / Department of Aviation Technologies (0838)

Title

Predictive model of the vertical movements of the earth's surface: implications for the land use of the Lithuanian coastal area

[en]

Saulius Šliaupa, Albertas Bitinas, Algimantas Zakarevičius

Is part of

33e Symposium International FESF Strasbourg : Recent Developments in Environmental Protection. Vol. 40, Social Strategies

Published In

Year	Start Page	End Page
2005	221	235

Publisher

Bern : Peter Lang, 2005

Extent

p. 221-235

URI

URI
https://hdl.handle.net/20.500.14911/138376

Cited references

Science / Art Area

Technologijos mokslai / Technological sciences (T)

Field of Science / Art

Matavimų inžinerija / Measurement engineering (T010)

Geologija / Geology (N005)

Keywords (en)

Abstract (en)

The coastal areas are sensitive to the vertical movements of the earth's surface as it leads to either drowning of the mainland territories that are often densely populated, or conversely to shallowing of the harbor areas. The latter phenomenon is well known in the Scandinavian coastal area of the Baltic Sea that is accounted to the isostatic rebound of the lithosphere after the glaciation. [...].