Land subsidence in southwest Utah from 1993 to 1998 measured with Interferometric Synthetic Aperture Radar (InSAR) (MP 06-5) Media Type:CD Lake Bonneville finally regressed about

Lake Bonneville finally regressed about 10

000-foot Brian Head Peak

and Wellington are in the lowlands

the significance of different stone materials

Land subsidence in southwest Utah from 1993 to 1998 measured with Interferometric Synthetic Aperture Radar (InSAR) (MP 06-5) Media Type:CD Lake Bonneville finally regressed aboutBy: R. R. Forster The objective of this study is to measure land surface subsidence in southwest Utah using Interferometric Synthetic Aperture Radar (InSAR). During the winter of 2004 2005 the Utah Geological Survey documented earth fissures near Beryl Junction in Iron County, Utah. The UGS concluded that these fissures formed due to groundwater withdrawal in the area, which has caused compaction in the Escalante Valley aquifer and ground subsidence