Location and Mechanism of Very Long Period Tremor During the 2008 Eruption of Okmok Volcano from Interstation Arrival Times

نویسندگان

  • Matthew M. Haney
  • M. M. Haney
چکیده

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Post-Eruptive Inflation of Okmok Volcano, Alaska, from InSAR, 2008-2014

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Ground surface deformation patterns , magma supply , and magma storage at Okmok volcano , Alaska , from InSAR analysis : 2 . Coeruptive deflation , July – August 2008

[1] A hydrovolcanic eruption near Cone D on the floor of Okmok caldera, Alaska, began on 12 July 2008 and continued until late August 2008. The eruption was preceded by inflation of a magma reservoir located beneath the center of the caldera and ∼3 km below sea level (bsl), which began immediately after Okmok’s previous eruption in 1997. In this paper we use data from several radar satellites a...

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Ground surface deformation patterns , magma supply , and magma storage at Okmok volcano , Alaska , from InSAR analysis : 1 . Intereruption deformation , 1997 – 2008

[1] Starting soon after the 1997 eruption at Okmok volcano and continuing until the start of the 2008 eruption, magma accumulated in a storage zone centered ∼3.5 km beneath the caldera floor at a rate that varied with time. A Mogi‐type point pressure source or finite sphere with a radius of 1 km provides an adequate fit to the deformation field portrayed in time‐sequential interferometric synth...

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Lava volume from the 1997 Eruption of Okmok volcano, Alaska, estimated using spaceborne and airborne interferometric synthetic aperture radar

Interferometric synthetic aperture radar (InSAR) techniques are used to calculate the volume of eruption at Okmok volcano, Alaska by constructing precise digital elevation models (DEMs) that represent volcano topography before and after the eruption. The pre-eruption DEM is generated using TOPSAR data where a three-dimensional multiaffined transformation is used to account for the misalignments...

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تاریخ انتشار 2015