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Isostasy - Geodesy
Royal Institute of Technology, Stockholm, Sweden.
University of Gävle, Faculty of Engineering and Sustainable Development, Department of Industrial Development, IT and Land Management, Land management, GIS. Royal Institute of Technology, Stockholm, Sweden. (Geospatial information science)
2016 (English)In: Encyclopedia of Geodesy / [ed] Grafarend, Erik, Springer , 2016Chapter in book (Other academic)
Abstract [en]

Isostasy (Greek isos “equal,” stasis “stand still”) is a term in geology, geophysics, and geodesy to describe the state of mass balance (equilibrium) between the Earth’s crust and upper mantle. It describes a condition to which the mantle tends to balance the mass of the crust in the absence of external forces.

Place, publisher, year, edition, pages
Springer , 2016.
Series
Encyclopedia of Earth Sciences Series, ISSN 1388-4360
National Category
Other Earth and Related Environmental Sciences
Identifiers
URN: urn:nbn:se:hig:diva-22751DOI: 10.1007/978-3-319-02370-0_111-1ISBN: 978-3-319-01870-6 (print)ISBN: 978-3-319-01869-0 (print)ISBN: 978-3-319-01868-3 (print)OAI: oai:DiVA.org:hig-22751DiVA: diva2:1046304
Available from: 2016-11-13 Created: 2016-11-13 Last updated: 2016-11-24Bibliographically approved

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