Counties, states, countries, continents, or oceans | |
Valdez-Cordova | Census area |
Alaska | state |
United States | country |
North America | continent |
Land | continent |
Map quadrangles, from USGS or Canadian NTS | |
McCarthy C-8 | 1:63,360 Alaska quadrangle |
McCarthy | 1:250,000 Alaska quadrangle |
Watershed boundaries (USGS hydrologic units) | |
Chitina River | hydrologic unit |
190201 | hydrologic accounting unit |
Northwest Alaska | hydrologic subregion |
Alaska | hydrologic region |
Map symbol | Lithology | Unit name |
---|---|---|
Khnl | Sedimentary | Herendeen Formation and similar units |
Qs | Unconsolidated | Unconsolidated surficial deposits, undivided |
Qs | Unconsolidated | Unconsolidated surficial deposits, undivided |
Qs | Unconsolidated | Unconsolidated surficial deposits, undivided |
Trcnk | Sedimentary | Chitistone and Nizina Limestones and Kamishak Formation |
Trn | Igneous - Volcanic | Nikolai and Goon Dip Greenstones and equivalent rocks |
Twv | Igneous - Volcanic | Wrangell Lava |
ID | Data type | Description |
---|---|---|
McCarthy | M-D | McCarthy 11748 line km with spacing 1.60 km over parts of AK |
Mc Carthy | M/R-D | Mc Carthy 1971 line km with spacing 9.60 km over parts of AK |
Tract | Deposit Type | Mineralization age |
---|---|---|
AK-SC05 | Cu-Ag quartz veins | |
AK-SC16 | Kuroko massive sulfide | |
AK-SC23 | Porphyry Cu, BC-Ak type | |
AK-SC33 | Cu (Au) skarn | |
AK-SC21 | Porphyry Cu, BC-Ak type | |
AK-SC28 | Polymetallic vein | |
AK-SC25 | Placer Au | |
AK-SC22 | Porphyry Cu, BC-Ak type | |
AK-SC32 | Cu (Au) skarn | |
AK-SC01 | Basaltic Cu/Kennecott Cu | |
AK-SC18 | Synorogenic-synvolcanic Ni-Cu | |
AK-SC09 | Low-sulfide Au-quartz veins |
Domain | Crust type | Region |
---|---|---|
Wrangellia | Oceanic arc | Alaska |
Record | Type | Comment |
---|---|---|
70AMk60D2 |
Lab ID | Sample medium | Description |
---|---|---|
BAF087 | rock | metamorphic skarn |
BAF088 | rock | igneous granodiorite |
BAF090 | rock | |
BAF093 | rock | |
BAF094 | rock | |
BAF096 | rock | igneous unspecified |
Sample ID | Material | Source |
---|---|---|
C-167989 | Sediment | Stream, Wet |
Sample ID | Date collected | Sample type |
---|---|---|
7002412 | 1978-07-01 | Wet stream sediment sample dried at less than or equal to 100øC and sieved to -100 mesh through stainless steel sieves. |
Sample ID | Date collected | Sample type |
---|---|---|
3002477 | 1978-07-01 | Stream water sample acidified to a pH of less than or equal to 1 with reagent-grade nitric acid. |
Sample ID | Rock type | Rock name |
---|---|---|
BAF087 | metamorphic | skarn |
BAF088 | igneous | granodiorite |
BAF090 | unspecified | |
BAF093 | unspecified | |
BAF094 | unspecified | |
BAF096 | igneous | unspecified |
Site name | Development | Commodities |
---|---|---|
Unnamed (north of Kuskulana Pass) | Occurrence | CU FE |
Site | Status | Commodities |
---|---|---|
Unnamed (north of Kuskulana Pass... | Inactive | Au |
Unnamed (near Peacock Creek) | Inactive | Cu |
Unnamed (north of Kuskulana Pass... | Inactive | Au;Cu |
Sample ID | Sample source | Rock name |
---|---|---|
2819 | Outcrop or artificial surface exposure | Granodiorite |
Sample ID | Sample source | Sample notes |
---|---|---|
C167989 | surface |
Tract name | Deposit type | Geology |
---|---|---|
Yukon-Tanana Upland | porphyry copper | Kluane Arc and Tertiary Kuskokwim Mountains volcanic-plutonic belt (continuation of Canadian Cordilleran continental arc); north of the Denali Fault |
Western Alaska Range | porphyry copper | Cretaceous porphyry prospects along the Kahiltna Basin-Peninsula terrane boundary |
Eastern Alaska Range and Wrangell Mountains | porphyry copper | Cretaceous (115-105Ma) deposits and prospects along the Nutzotin Basin-Wrangellia terrane boundary; south of the Denali Fault |
Skolai Arc - Eastern Alaska | porphyry copper | Late Paleozoic Skolai Arc of the Wrangellia terrane; south of the Denali Fault |
Pacific Margin | porphyry copper | Cretaceous through middle Tertiary volcanic and intrusive rocks representing a series of continental- and island-arc systems accreted and superimposed onto the paleomargin of northeast Asia. |