E-SCAN 3D survey equipment is designed and tested
for operation at -40 degrees (including batteries).

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The E-SCAN crew prepares to lay grid wire on cut lines in dense bush, in the Athabasca Basin of Northern Saskatchewan (2001).

Seen in the distance, a small lake will require winter lake tools to maintain the uniformly spaced grid of survey electrodes across the entire survey area. Projects that are mainly on land can be done in winter or summer. Where there are extensive open-water lake or swamp areas, the decision to operate in summer or in winter will depend upon local conditions and client timing requirements. Both can be done cost-effectively by using the corresponding set of specialized lake survey equipment. Northern lake projects may benefit from using the winter ice as an easily-traveled, stable platform for the 3D E-SCAN survey, using holes drilled in the ice to place lake-bottom electrodes. Where timing doesn't permit waiting for winter, or where a lake will not freeze sufficiently to safely support work crews, different equipment gets the job done on the open water. See "... in any terrain - lakes" in a tab further down the Home Page.

The target in the Athabasca Basin is deep unconformity uranium, here estimated at about 500 metres below surface. Anomalies are conductive features in a resistive host, an ideal geophysical target setting whose interpretation here is routinely compromised (for non-3D methods) by irregular, alternating conductive-resistive (swamp-esker) surface conditions.

Special equipment: Disc-brake damping on the wire spoolers mounted on the back of snowmobiles can spit out grid wire at up to 40 km/hour across lake ice and snow. Gas-powered wire winders make the subsequent wire recovery even faster.
This gas-powered ice auger can penetrate up to 2 metres of ice in 60 seconds, giving access to the lake-bottom for a brief period before the hole freezes over. In a typical through-ice survey, several hundred survey electrodes are placed in the conductive mud on the lake bottom, establishing electrical contact with the rocks below. The depth-to-bottom is measured as each electrode is lowered from the ice surface, generating a full 3D record of electrode locations for accurate 3D imaging of the earth geo-electric model. GPS position records allow later recovery of the wire and electrodes even when snow has drifted over the stations.

Special equipment: At -40 degrees, the ground can be frozen deep and hard, even below an insulating blanket of snow. Above, a Pionjar "plugger" is adapted to drive the 1/2 inch and 5/8 inch (13, 16 mm) stainless steel electrodes into the hard ground. All small tools have colorful tethers so that they remain easy to locate in the snow.