Vertical Crustal Movement in Iceland View Full Text


Ontology type: schema:Chapter     


Chapter Info

DATE

1974

AUTHORS

Eysteinn Tryggvason

ABSTRACT

The rift zones of Iceland are subsiding at relatively constant rate. The absolute subsidence has not been determined but the rate of tilt of the flanks of the rift zones is 0.2 to 0.7 microradians per year and the width of the zone that is being tilted appears to be more than 40 kilometers. It is estimated that the central part of the rift zone is subsiding 0.5 to 1.0 centimeter per year relative to surrounding areas. The ground deformation associated with this subsidence is characterized by gentle bending of the earth’s crust with no measureable fault displacement except during earthquakes and possibly during a period of one or two years after earthquakes. More... »

PAGES

241-262

References to SciGraph publications

  • 1967-02. Some problems of volcanism in Iceland in INTERNATIONAL JOURNAL OF EARTH SCIENCES
  • Book

    TITLE

    Geodynamics of Iceland and the North Atlantic Area

    ISBN

    978-94-010-2273-6
    978-94-010-2271-2

    Author Affiliations

    Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1007/978-94-010-2271-2_17

    DOI

    http://dx.doi.org/10.1007/978-94-010-2271-2_17

    DIMENSIONS

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