| Deposit ID | 10065183 |
|---|---|
| MRDS ID | TC40230 |
| Record type | Site |
| Current site name | Borrow Pit |
| Geographic coordinates: | -111.76212, 34.75616 (WGS84) |
|---|
Political divisions (FIPS codes)
Yavapai(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Sedona(quadrangle 1:24,000 scale)
Sedona(quadrangle 1:100,000 scale)
Holbrook(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Verde(hydrologic unit)
Verde(hydrologic accounting unit)
Salt(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Coconino National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Arizona | Yavapai |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 016N | 006E | 30 | NW4 | Arizona |
| Commodity | Importance |
|---|---|
| Sand and Gravel, Construction | Primary |
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Alluvium |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock |
| (1) | -111.76212, 34.75616 |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC40230 |
USGS, SEDONA 1:24,000 TOPOGRAPHIC MAP.
WEIR, G.W., ULRICH, G.E., AND NEALEY, L.D., 1989, GEOLOGIC MAP OF THE SEDONA 30' X 60' QUADRANGLE, YAVAPAI AND COCONINO COUNTIES, ARIZONA: U.S. GEOLOGICAL SURVEY MAP I-1896, MAP SCALE OF 1:100,000.
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | THE UNCONSOLIDATED MATERIALS EXPLOITED FROM THE BORROW PIT RANGE FROM SILT TO BOULDER GRAVEL IN SIZE. THE GRAVELS ARE COMPOSED MOSTLY OF PALEOZOIC SANDSTONE, CHERT, AND LIMESTONE OF VARIOUS SHADES OF RED, YELLOW, AND WHITE; AND GRAY TERTIARY BASALT THAT APPEAR TO BE IN AN OLDER TERRACE OF THE CREEK IN JACKS CANYON. LOCALLY, THE MATERIAL IS COLLUVIUM FROM THE BEDROCK WHICH IS THE SUPAI FORMATION OF PALEOZOIC AGE. THE COBBLE GRAVEL IS FAIRLY, BUT NOT COMPLETELY, FREE OF COATINGS OF CALCIUM CARBONATE OR CLAY. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1995 | Cox, Leslie | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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