| Deposit ID | 10013978 |
|---|---|
| MRDS ID | D010558 |
| Record type | Site |
| Current site name | Iron Dike |
| Geographic coordinates: | -105.6956, 40.39359 (WGS84) |
|---|---|
| Elevation | 3487 |
| Location accuracy | 500(meters) |
| Relative position | 10 MILES N83W FROM ESTES PARK |
Political divisions (FIPS codes)
Larimer(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Trail Ridge(quadrangle 1:24,000 scale)
Estes Park(quadrangle 1:100,000 scale)
Greeley(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Big Thompson(hydrologic unit)
South Platte(hydrologic accounting unit)
South Platte(hydrologic subregion)
Missouri(hydrologic region)
Federal lands
Rocky Mountain National Park(National Park)
National Park NPS(Type of land area)
NPS(Federal land areas administered by NPS)
| Country | State | County |
|---|---|---|
| United States | Colorado | Larimer |
| United States | Colorado | Boulder |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 006N;005N;004N;004N | 075W;074W;074W;073W | 10,14,15,23,25,26,36;05,06,08,16,21,22,25,26,27,36;01;21,28,34 | Colorado |
| Commodity | Importance |
|---|---|
| Iron | Tertiary |
| Titanium, Metal Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Apatite | Gangue |
| Augite | Gangue |
| Biotite | Gangue |
| Labradorite | Gangue |
| Limonite | Gangue |
| Quartz | Gangue |
| Sillimanite | Gangue |
| Result | ANALYSIS OF AUGITE FROM TRAIL RIDGE EXPOSURE SHOWED 49.23% SIO2, 0 .35% TIO2, 5.73% AL203, 1.02% FE203, 14.70% FEO, 0.30% MNO, 11.90% MGO , 14.89% CAO, 0.92% NA20, 0.66% K20, 0.19% P205. ANALYSIS OF FRESH DIA BASE AT CONTACT WITH GRANITE SHOWED 48.71% SIO2, 0.74% TIO2, 16.47% AL 203, 2.90% FE203, 12.01% FEO, 0.19% MNO, 4.47% MGO, 7.85% CAO, 4.60% N A20, 1.17% K20, 0.53% P205, 0.78% H20. |
|---|
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite > Diabase | ||||
| Rock unit name | Diabase Dike;Silver Plume Granite | ||||
| Rock description | Diabase Dike;Silver Plume Granite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite > Diabase |
| Rock unit name | Diabase Dike;Metasedimentary Rocks Undivided |
| Rock description | Diabase Dike;Metasedimentary Rocks Undivided |
| (1) | -105.6956, 40.39359 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Front Range Uplift, Silver Plume Batholith, Boulder Creek Batholith |
| Type of structure | Local |
| Structure description | Nw-Trending Faults |
| General form | TABULAR |
|---|---|
| Thickness | 30.48M |
| Length | 61153.4M |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Trail Ridge Area |
|---|
| Ownership category | National Park |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D010558 |
BOOS, M.F., AND BOOS, C.M., 1933, IRON DIKE (ABS.): GSA BULL., V. 4 4, P. 73.
CRAWFORD, R.D., 1908, GEOLOGY AND PETROLOGY OF THE SUGARLOAF DISTRI CT: UNIV. COLORADO STUDIES, V. 6, P. 97-131.
| Subject category | Comment text |
|---|---|
| Deposit | DIABASE DIKE CONTAINING FE-RICH MINERALS AND LIMONITE-STAINED WEA THERING PRODUCTS TRENDS GENERALLY N30W, 60 TO 80 SW, PARALLEL TO ARE A BRECCIA REEFS, CHARACTERISTICALLY 50 TO 100 FT WIDE BUT IN PLACES ONL Y A FEW FEET OR INCHES, INTERSECTED AND OFFSET BY NUMEROUS EAST-WEST-T RENDING FAULTS, SOME OF WHICH HAVE LOCALIZED W MINERALS AND TELLURIDES SUCH AS IN BOULDER CO. GRAIN SIZE INCREASES INWARD FROM CHILLED WALL R OCK CONTACTS. AVERAGE MODAL COMPOSITION (VOL%): 49.8% LABRADORITE, 38. 4% AUGITE, 8.5% TITANIFEROUS MAGNETITE, 2.3% QUARTZ, 1.0% ORTHO CLASE. TITANIFEROUS MAGNETITE OCCURS AS EQUANT CRYSTALS, PLATES, SKELETAL DE NDRITIC CRYSTALS AND IN VEINS FILLING FRACTURES IN PYROXENE AND PLAGIO CLASE. DIKE PREVIOUSLY THOUGHT TO BE LARAMIDE IN AGE AND CORRELATED WI TH OTHER MAFIC INTRUSIVES IN AREA, BUT WAHLSTROM'S CHEMICAL ANALYSES S HOWED DIFFERENCES THAT SUGGEST IT FORMED SEPARATELY; STATE GEOLOGIC MA P SHOWS DIKE TO BE PREC Y AGE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1983 | Schwochow, Stephen D. | Colorado Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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