Exhibit 99.2
2008 Fieldwork Summary Report
Key 1-4 Mineral Claims
SE Cuprite Hills Area
Esmeralda County
Nevada, USA
Prepared by: James W. McLeod, P. Geo.
For: Ameriwest Minerals Corp.
Dated: July 16, 2008
Table of Contents
Page
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Contents 2
Illustrations 2
Summary 3
Interpretation and Conclusions 3
Recommendations 5
Appendix 1 - Mobile Metal Ion (MMI) Soil Sample Data After page
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Illustrations
After page
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Figure 1. Location Map - As Shown 3
Figure 2. Claim Area Map, Scale - 1: 24,000 4
Figure 5. Sample Location Map - 1: 6,000 5
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Summary
This report summarizes the fieldwork program conducted on behalf of Ameriwest
Minerals Corp. on their 100% owned Key 1-4 mineral claims situated in the SE
Cuprite Hills Area 15 airmiles south of the Town of Goldfield, Nevada. The
property is road accessible by traveling south of Goldfield, NV on Highway 95
for 15 miles to Nevada Highway 266 that is taken to the west for 0.2 of a mile
and then traveling north-northwest for 1 mile to the property.
The work program was conducted during April 2008 at the request of the Board of
Directors of the Company.
The Key property consists of four contiguous, located, lode mineral claims that
comprise a total of 82.64 acres.
Some apparently anomalous gold exploration suite (GES) composed of the elements
cobalt, gold, nickel, palladium and silver were encountered on the Company's
property during the Phase 1 exploration program.
Interpretation and Conclusions
The property does not appear in the historical record as having undergone
specific mineral exploration work, but it is likely that the general area has
received some attention (prospecting) in the past because of its' location and
geological setting.
The possibility of underlying metamorphosed sediments and volcanic rock units
are suggested by examination of the surface veneer throughout the mineral
claims.
All of the mineral claim area is overburden covered with a fine, slightly sandy
loess (wind deposition of the fine silt) and offers exploration potential. Some
hydrothermal solutions caused by underlying intrusive activity and possibly
related to the volcanic rock units appear to have affected the central portion
of the property or in close proximity to occur as quartz vein particles of
various sizes and angularity that are observed to be present in varying amounts
that could be the host of the GES values.
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Figure 1. Location Map - As Shown
The object of our initial exploration undertaking was to assess areas that may
require more detailed investigations to assist in determining their economic
significance. The MMI data obtained from the initial exploration work on the Key
1-4 mineral claims exhibit some anomalous results. It is the opinion of the
author that follow-up work could be done. The initial MMI data indicates some
coincident, anomalous behavior in the Gold Exploration Suite (GES). Some fill-in
MMI soil sampling is recommended and to be contingent upon positive results
being obtained prior to embarking on the Phase 2 exploration program.
The analytical results were subjected to a statistical analysis. The statistical
results obtained from the data allowed representation in the form of percentage
distribution histograms for a variety of elements and particularly groups or
suites of elements that are often found to occur together in ore situations and
may be coincident in a variety of mineralogical settings. The table summarizes
the results for the Gold Exploration Suite (GES) comprised of cobalt, gold,
nickel, palladium and silver as this is the suite that exhibited anomalous data
from the exploration program. These results are summarized as follows:
Element Anomalous Sample Number
- ------- --------- -------------
(ppb)
Cobalt (greater than or equal to) 35 24, 27, (40)
Gold (greater than or equal to) 0.75 6, (21), 26, 27
Nickel (greater than or equal to) 149 22, (24), 27
Palladium (greater than or equal to) 0.4 Nil
Silver (greater than or equal to) 32 (15), 24, 27
(-) refers to a sample value that is very close to being anomalous.
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Figure 2. Claim Area Map, Scale - 1: 24,000
Recommendations
The MMI soil data results of the GES are in some instances coincident and
therefore it may be stated that there is a possibility of encountering an
underlying occurrence of in-place mineralization. The final decision to conduct
further exploration as fill-in MMI sampling around the anomalous areas of
interest must be left to the Company.
Respectfully submitted,
/s/ James W. McLeod, P. Geo.
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James W. McLeod, P. Geo.
Consulting Geologist
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Figure 5. Sample Location Map - 1: 6,000
Appendix 1: Mobile Metal Ion (MMI-M) Geochemical Soil Data.
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