2011-09-28_PERMIT FILE - X201123500

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Hydrology & Water Use The Little Snake River is a perennial stream that supplies water for irrigation and recreation in the region. The proposed exploration permit area is south of the Little Snake River and the closest proposed hole (Hole 10) is over a 1/4 mile away from the Little Snake River. The exploration area is dissected by numerous creeks that drain into the Little Snake River. The most significant creeks include Timberlake and Fourmile. Pole Gulch also occurs but is less significant. These streams are intermittent and flow primarily during the spring snowmelt and occasionally after a significant rainstorm. Linc Energy will take every precaution to contain drilling fluids at the site from entering any drainage in the proposed exploration permit area. A source of water for drilling will be approved prior to project startup. Geology The Little Snake River exploration permit area resides in the Sand Wash Basin, a basin principally restricted to northwest Colorado. A west to east trending structural high referred to as the Cherokee Ridge occurs along the Wyoming and Colorado border and separates the Sand Wash Basin on the south from the Washakie Basin in Wyoming to the north. The regional stratigraphy of the area consists of Tertiary and Cretaceous units containing from bottom to top as the Upper Cretaceous Lance Formation, the Paleocene Fort Union Formation and the Eocene Wasatch Formation. The surface consists mainly of the Wasatch Formation with minor exposures of the Fort Union in the northernmost part of the exploration application area. These Tertiary formations are locally overlain by modern Quaternary alluvium deposits confined to drainages of Little Snake, Timberlake Creek and Fourmile Creek. These modern alluvium deposits consist of the Piney Creek Alluvium and younger deposits. Within the Little Snake River area the Wasatch Formation ranges in thickness from 900 to 3,000 feet and averages about 1,500 feet thick. It consists of claystone, shale and sandstone. The contact with the underlying Fort Union Formation is believed to be unconformable. The Fort Union Formation unconformably overlies the Lance Formation and ranges about 300 to 3,000 feet thick averaging 1,300 feet thick. The Fort Union Formation contains relatively thick coal seams which are of interest to Linc Energy for potential UCG applications. The Fort Union Formation consists of shale, mudstone, siltstone, sandstone and coal. The coal is considered subbituminous. Oil and gas logs within the area of interest were used to located and correlate individual coal seams. The structure is relatively gentle with a southwestward dip ranging from about 1 to 5 degrees. No major faults were identified in the exploration area being considered. However, immediately south, faulting has been identified as well as the occurrence of Upper Tertiary intrusive intermediate to felsic dikes. Wildlife and Vegetation The area has diverse fauna and flora. A Threatened and Endangered third party report will be provided to the Division. This survey is planned to be completed this Fall. A cultural study will also be conducted in the vicinity of the proposed drill sites.