DISCLAIMER This Final Report was prepared with the support of the U.S. Department of Energy (DOE) award number DE-FC-07-01ID14203. However, any opinions, findings, conclusions or recommendations expressed herein are those of the authors and do not necessarily reflect the views of DOE. Neither the United States nor the DOE, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product or process disclosed, or represents that its use would not infringe on privately owned rights. Reference herein to any specific commercial product, process or service by trade name, mark, manufacture, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring, by the United States Government or any agency thereof.

This is 0.55 Quad from NMEI analysis, with possible 0.35 Quad from major new geothermal industrial parks in California, Oregon and Idaho which DSS Industries analyzed and recommended by study a dated March 1978. Note also the above data excludes California,

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This report contains a detailed summary of a methodical and comprehensive assessment of the potential of the Animas Valley, New Mexico geothermal resource leasehold owned by Lightning Dock Geothermal, Inc. Results from the final seismic traverses completed to tie together lithology from gradient and deep exploratory holes, and to develop an integrated resource model are summarized as follows:A seismic traverse oriented in a NW-SE alignment portrays a chaotic subsurface regime that contains numerous dipping structures, and likely folded and compressed structures. Two principle faults appear to bound and create a graben, with the graben strata folded and compressed. An E-W traverse depicts a structural setting in which the mapped surface expression (eroded fault scarp) of the old Animas Valley Fault (a Recent, basin-bounding fault along the eastern margin of the valley) cannot be directly tied to the subsurface structures creating the intense shallow geothermal anomaly.Overall resource assessment is that the potential commercial reservoir contains minimum of 15 MW net to the grid. This compares favorably with the earlier assessment, completed before the drilling and final seismic traverses, that the resource comprised 5 to 15 MW reservoir capacity.