Company

Honey Hole Mines has been in business since 1999 and is registered with Companies of Canada.

HONEY HOLE MINES LTD. was incorporated under the Business Corporations Act in 2011.

The underlying geology of the area is considered part of the Omenica Morphotectonic Belt.

The project area itself is within the Eagle Bay Tectonic assemblage and consists of two primary metamorphic successions.

The dominant group is the upper Proterozoic to Paleozoic Snowshoe Group of rocks, which includes schist, gneiss, schistose quartzite, phyllite, marble, amphibolite, and siltite along with several other lesser units.

This is most likely the dominant group within the claims.

With the advent of the use of modern exploration techniques, Keithley Creek is now poised to become even more important to the mining history of this area.

New discoveries of gold-bearing mesothermal veins, VMS-style mineralization, and placer mineralization has increased in the area and the styles of mineralization are becoming even more diverse.

Significantly, Honey Hole Mines contains all of these elements.

We had spent several years traveling from area to area prospecting and exploring, looking for the lode gold.

In 1997 we came to Keithley Creek and spent a few weeks prospecting, we quickly realized that this property is super high in mineralization, free gold, and ore body.

We initially staked four mineral properties and two placer properties after a few adjustments and making a significant find in 2002 with 300° trend gold ore quartz veins showing the "potential for the mother lode".

We staked what we found to be the best ground and finished staking our remaining property in 2003, we have continued to hold the same ground to date.

Honey Hole Mines Ltd. now owns 26 properties.

• Our CEO

• Vice President / Secretary / Treasurer

• Executives

- Honey Hole Mines Ltd., Holdings -

PROPERTY DESCRIPTION

The property consists of 12 legacy mineral claims and 1 cell mineral claim. There are also 2 legacy placer claims and 11 placer cell claims. The claims are grouped and cover an area of approximately 2,000 acres.

The natural vegetation is predominantly coniferous forest consisting of firs, spruce, cedar, and balsam. Large portions of the property have been logged by clear-cutting and most of these areas have been replanted. Many of the replanted areas contain second-growth trees ranging from two-three meters in height.

A network of logging and skid roads provide good access to all areas of the property, though some upgrading may be required.

The Old Barkerville trail that was used by the stagecoach that transported the gold from the Borland Ranch runs through the center of the properties. This trail is of a fair width and still remains in fairly good condition, this trail may need some repair (clearing of shrubs).

The former old settlement of Keithley Creek was located on the Cariboo Lake.

Portable generating units if required, while water services are plentiful from the numerous creeks and rivers, would supply power for exploration purposes.

PROPERTY LOCATION AND ACCESSIBILITY

The property is located in the Quesnel Highlands of Central British Columbia with elevations ranging from 840 to 1340 meters above sea level.

The property is located approximately 27 km north-northeast of the community of Likely, in the Cariboo Mining Division of British Columbia, Canada, NTS 93A073 centered approximately at latitude 52° 45' N, longitude -121° 25' W.

Access to the property is via an all-weather logging road to Keithley Creek the community of Likely, B.C. Then by Barkerville road which is a logging road on the northeast side of Keithley Creek that leads through the property.

Keithley Creek flows in a southeasterly direction through the mineral property with many creeks such as Donaldson, Honest John, Rabbit, Snowshoe, and Weaver Creeks flowing into Keithley Creek.

CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE, AND PHYSIOGRAPHY

The area receives significant precipitation throughout the year as both rain and snow.

Accumulations of snow may reach three meters or more during the winter months.

Temperatures can vary from -40°C in winter to +38°C in summer.

Our property is situated 95 km northeast of the city of Williams Lake, B.C., the nearest supply center, and 27 km northeast of Likely, B.C., the nearest settlement.

The community of Likely, situated on Quesnel Lake, is reached by a paved highway from a point on Highway 97 about 12 km southeast of the town of Williams Lake.

The distance from Highway 97 to Likely is approximately 90 km.

Williams Lake is a logging and lumber centre serviced by scheduled daily air service from Vancouver. Necessary supplies and equipment as well as local labor and modern communications are readily available.

The community of Likely, is also approximately 148.1 km from the town of Quesnel, B.C. which is also an excellent source of local labor, heavy equipment sales and repairs, and shopping. There is also an airport that has flights that connect with the Williams Lake airport.

Quesnel, B.C. take Highway 97 south 75 km to McKleese Lake, travel east on the Beaver Lake road for approximately 37.2 km then north onto the Likely road for approximately 35.9 km to Likely, B.C.

For access to our properties, you would continue from Likely along Keithley Creek road for approximately 27 km to Keithley Creek.

HISTORY

The Cariboo region of British Columbia is notable for the gold rush that began in 1860.

Doc Keithley made the first discovery of gold and thus Keithley Creek was named after him.

The historic Kitchener Pit located at Keithley Creek produced in 1945 1,100,891 grams, tons unknown. The total amount mined is unknown, production was from 1874 to 1945.

The historic Bullion Pit near Likely produced 175,700 ounces of gold from 200 million tons of gravel and about 1/100th as much platinum. Gold and platinum were reported in similar proportions in placers in the Frank Creek area.

Placer gold was also discovered on Snowshoe, Little Snowshoe, and French Snowshoe Creeks around the same time.

At the historic mines, the strata trend 315°, dip 45° NE and are cut by north-to northeast-trending normal faults dipping 60°E.

The zones of economically important quartz veins are contained in graphite-bearing layers near a contact with carbonate-bearing layers.

In much of the Cariboo district, a layer of distinctive, hard, compact, semi-rigid blue clay sits either on or slightly above bedrock and acts as "false" bedrock. In the placer-gold areas of the Cariboo, large amounts of gold were recovered from gravel resting on this clay. In places, the clay layer was penetrated by the placer miners to reach richer "pay streaks" on true bedrock below.

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