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<br />pressure again <br /> <br />. <br /> <br />forced <br /> <br />. <br /> <br /> <br />salt flow from the Meeker well into the river. <br /> <br />From the time that the flow was terminated at the Marland well until <br /> <br />1968. the upper portion of the cased well was dry. according to <br /> <br />local sources. After the Meeker well was plugged, water again rose <br /> <br />in the casing of the Marland well. There is no measurable flow at <br /> <br />the well head. although water seeps from the rusted casing in many <br /> <br />places. <br /> <br />3. In 1945, the Stanolind Oil and Gas Company drilled the Scott <br /> <br />#1 oil test by rotary methods to a depth of 6.645 feet for a test <br /> <br />of the Leadville or Madison limestone. The Weber sandstone zone <br /> <br />was adequately cased off and no leakage has been noted. The well <br /> <br />was plugged following completion as a dry hole. The well was drilled <br /> <br />tr) <br />(Q <br />Cl') <br />Q <br /> <br />about 450 feet southwest of the Marland well and located in the <br /> <br />NE~. SW~. Sec. 20. T€I 1 N<J' RI) 93 Wj (, fl~ <br /> <br />4. From 1957 to 1960. an operator by the name of Nick Kritsas <br />one and one-half <br />drilled two test wells aboullx~ miles north of the foregoing well. <br /> <br />Cable tool methods were used but could not cope with salt water <br /> <br />problems and subsequent XR~ lack of funds. The Kritsas #1 was <br /> <br />drilled to a depth of 1.665 feet into the Entrada sandstone and was <br />f.PI1. <br />located in the HEk~xNt NE~. NW~. Sec. 17, T(;) 1 N"J. Rc;::; 93 WJJ The <br /> <br />t" <br />o <br />0.3 <br />N <br /> <br />southwest in the Sw~. NW~, Sec. 17. T0 1 N~, R~ 93 <br /> <br />mile to the <br />(; P1'1; <br />W0.1\ to a depth of <br /> <br />Xixix Kritsas #2 was drilled about one-fourth of a <br /> <br />1,130 feet in the Morrison formation. Appearance of salt water in <br /> <br />these wells in formations higher in the geologic section by several <br /> <br />hundreds of feet is evidence of vertical and lateral migration of <br /> <br />-2- <br />