Interim Geologic Map of the Escalante 30' x 60' Quadrangle, Garfield and Kane Counties, Utah (OFR-690dm) PECO Write Land subsidence can also be

Land subsidence can also be caused by contraction as fractured rock reservoirs cool

the effects of early and late Laramide movements

and the bedrock aquifer was found to be bounded by semi-permeable aquifer boundaries

The remaining 21 areas discussed are scattered along the northern and southwestern margins of the basin

Limbach and A

Interim Geologic Map of the Escalante 30' x 60' Quadrangle, Garfield and Kane Counties, Utah (OFR-690dm) PECO Write Land subsidence can also beBy: Hellmut H. Doelling, and Grant C. Willis This 2018 open file report and digital (GIS) dataset updates and replaces the 1999 interim geologic map of the Escalante and parts of the Loa and Hite Crossing 30 x 60 quadrangles, Garfield and Kane Counties, Utah (UGS OFR 368). Many, but not all, geologic features needing revision are updated. Small extensions into adjacent quadrangles are clipped off because newer mapping of these areas has been (Loa) or