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- W2076169710 abstract "Ground Penetrating Radar (GPR) and Airborne Synthetic Aperture Radar (AIRSAR) data allow detection of lava flows with different backscatter characteristics and dielectric properties. The backscattering and penetration depth of the GPR and AIRSAR signals depend on the frequency of the instrument, the surface roughness, moisture content and dielectric properties of surface and near surface materials. Preliminary GPR surveys in Craters of the Moon (COM) National Monument with a 100-MHz, bi-static antenna obtained penetration depths up to 50 meters in a section of the Great Rift and allowed the identification of lava flows of different ages. Lava flow ages and the location of source vents for older eruptive periods (~15,000 yrs) are either speculative or unknown, due to the changing orientation of the rift and burial of older flows." @default.
- W2076169710 created "2016-06-24" @default.
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- W2076169710 date "2005-01-01" @default.
- W2076169710 modified "2023-09-25" @default.
- W2076169710 title "Identifying subsurface stratigraphy and source vents with AIRSAR and ground penetrating adar in craters of the moon national monument, Idaho" @default.
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- W2076169710 doi "https://doi.org/10.1190/1.2147898" @default.
- W2076169710 hasPublicationYear "2005" @default.
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