Gopher Gold Deposit

Gopher Gold Deposit

Gopher Gold Depository
Gopher Gold Deposit

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During the COVID-19 pandemic the DSB is accepting payments remotely via Gopher Gold only.
Directions how to deposit to gopher gold to use your U card to pay for prints and other campus services:
https://ucard.umn.edu/umtc/deposit
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DSB ARTS Student Price ListPaper TypeLusterMatteYour Own Paper
Sheet Size
8.5x11$2.50$2.00$1.50
11.7x16.5$4.00$3.00$2.00
13x19$5.00$4.00$3.00
17x22$6.50$5.50$4.00
Roll Size
24' Wide$0.40 / linear inch$0.35 / linear inch$0.25 linear inch
44' Wide$0.460 / linear inch$0.55 / linear inch$0.40 / linear inch
8.5x11' Transparency Film: $2.50 per sheet
24' Wide Transparency Film: $0.45 / linear inch
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DSB Prices for Non-ARTS University Students, Faculty, & StaffPaper TypeLusterMatteYour Own Paper
Sheet Size
8.5x11$3.50$3.00$2.50
11.7x16.5$5.00$4.00$3.00
13x19$6.50$5.00$4.00
17x22$8.00$6.50$5.00
No deposit slots lv. Roll Size
24' Wide$0.55 / linear inch$0.50 / linear inch$0.40 / linear inch
44' Wide$0.75 / linear inch$0.70 / linear inch$0.55 / linear inch
Gopher Gold Depository8.5x11 Transparency Film: $3.50 per sheet
24' Wide Transparency Film: $0.65 / linear inch
Directions how to deposit to gopher gold to use your U card to pay for prints and other campus services:
https://ucard.umn.edu/umtc/deposit
Gopher Gold DepositGeologic descriptionWillow Creek drains across the contact between Mesozoic slate and graywacke (KJs) and Tertiary strata of the Sterling (?) (Tcp) and Tyonek (?) (Tts) Formations of the Kenai Group (Reed and Nelson, 1980). The placer gold deposits within Willow Creek and the headwater drainages, Gopher and Ruby Gulches, are hosted in Pleistocene stream gravels. At the head of Gopher Gulch, highly argillaceous white quartz congomerate contained about 1500 ounces of angular gold in a 320 by 660 foot cut (C.C. Hawley and Associates, Inc., 1978). Gold is concentrated mainly on bedrock (Cobb and Reed, 1980). Mertie (1919) describes intricately intergrown gold and lead in one specimen from this locality. Mining was conducted on Gopher Gulch as early as 1917 (Garrett, 1998).
The white quartz conglomerate placers (e.g. Willow Creek, Thunder Creek, TL032, TL058, Dollar Creek, TL031) represent the oldest placers in the Cache Creek area. Capps (1925) describes the white quartz conglomerate as the basal unit of the Tertiary Kenai Formation. However Clark and Hawley (1968) suggest that the white quartz conglomerate is older and that the Kenai Group was deposited on it. They believe the auriferous conglomerate is near its original source in part because the characteristics of the gold show a common source that has not moved far or has not been reworked. Further, they indicate that the conglomerate is a product of shearing and weathering in situ of argillic altered, auriferous Tertiary quartz porphyry intrusive rocks and associated quartz veins that were emplaced along northeast, high angle normal faults. The lineaments in Dutch and Cache Creeks represent two of these faults.
Tributaries to Willow Creek which have been mined include: Ruby Creek (TL041), Willow Creek (TL042); Falls Gulch, Rocky Gulch, Slate Gulch, and Snow Gulch. See also Peters Creek (TL045).
Geologic map unit(-150.868288377309, 62.5774810631695)
Mineral deposit modelPlacer Au-PGE (Cox and Singer, 1986; model 39a).
Mineral deposit model number39a
Age of mineralizationTertiary and Pleistocene (Clark and Hawley, 1968).
Alteration of depositC.C. Hawley and Associates, Inc. (1978) describe argillic alteration of the Tertiary quartz porphyry intrusive rocks.

Paper Type	Luster	Matte	Your Own Paper
Sheet Size
8.5x11	$2.50	$2.00	$1.50
11.7x16.5	$4.00	$3.00	$2.00
13x19	$5.00	$4.00	$3.00
17x22	$6.50	$5.50	$4.00
Roll Size
24' Wide	$0.40 / linear inch	$0.35 / linear inch	$0.25 linear inch
44' Wide	$0.460 / linear inch	$0.55 / linear inch	$0.40 / linear inch

Geologic description Willow Creek drains across the contact between Mesozoic slate and graywacke (KJs) and Tertiary strata of the Sterling (?) (Tcp) and Tyonek (?) (Tts) Formations of the Kenai Group (Reed and Nelson, 1980). The placer gold deposits within Willow Creek and the headwater drainages, Gopher and Ruby Gulches, are hosted in Pleistocene stream gravels. At the head of Gopher Gulch, highly argillaceous white quartz congomerate contained about 1500 ounces of angular gold in a 320 by 660 foot cut (C.C. Hawley and Associates, Inc., 1978). Gold is concentrated mainly on bedrock (Cobb and Reed, 1980). Mertie (1919) describes intricately intergrown gold and lead in one specimen from this locality. Mining was conducted on Gopher Gulch as early as 1917 (Garrett, 1998). The white quartz conglomerate placers (e.g. Willow Creek, Thunder Creek, TL032, TL058, Dollar Creek, TL031) represent the oldest placers in the Cache Creek area. Capps (1925) describes the white quartz conglomerate as the basal unit of the Tertiary Kenai Formation. However Clark and Hawley (1968) suggest that the white quartz conglomerate is older and that the Kenai Group was deposited on it. They believe the auriferous conglomerate is near its original source in part because the characteristics of the gold show a common source that has not moved far or has not been reworked. Further, they indicate that the conglomerate is a product of shearing and weathering in situ of argillic altered, auriferous Tertiary quartz porphyry intrusive rocks and associated quartz veins that were emplaced along northeast, high angle normal faults. The lineaments in Dutch and Cache Creeks represent two of these faults. Tributaries to Willow Creek which have been mined include: Ruby Creek (TL041), Willow Creek (TL042); Falls Gulch, Rocky Gulch, Slate Gulch, and Snow Gulch. See also Peters Creek (TL045).
Geologic map unit	(-150.868288377309, 62.5774810631695)
Mineral deposit model	Placer Au-PGE (Cox and Singer, 1986; model 39a).
Mineral deposit model number	39a
Age of mineralization	Tertiary and Pleistocene (Clark and Hawley, 1968).
Alteration of deposit	C.C. Hawley and Associates, Inc. (1978) describe argillic alteration of the Tertiary quartz porphyry intrusive rocks.