The Maple Dell Ne Workings is a mine located in Utah county, Utah at an elevation of 5,699 feet.
About the MRDS Data:
All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.
Mine Info
Elevation: 5,699 Feet (1,737 Meters)
Commodity:
Lat, Long: 39.97417, -111.68972
Map: View on Google Maps
Satelite View
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
Maple Dell Ne Workings MRDS details
Site Name
Primary: Maple Dell Ne Workings
Commodity
Tertiary: Iron
Location
State: Utah
County: Utah
District: Santaquin District
Land Status
Land ownership: National Forest
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.
Holdings
Not available
Workings
Type: Underground
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Physiographic Detail: Wasatch Mountains
Mineral Deposit Model
Not available
Orebody
Form: TABULAR
Structure
Type: R
Description: Wasatch Fault
Type: L
Description: Bear Canyon Thrust Fault To North, Payson Canyon Wrench Fault To West
Alterations
Not available
Rocks
Name: Dolomite
Role: Host
Age Type: Host Rock
Age Young: Mississippian
Analytical Data
Not available
Materials
Gangue: Calcite
Gangue: Limonite
Comments
Comment (Workings): ADIT IS MAIN WORKING, IT TRENDS N84E AND IS COLLAPSED 47 FT INSIDE THE PORTAL; SHAFT IS ACTUALLY SHORT ADIT WITH DEEP WINZE, A DRIFT 15 FT. DOWN THE WINZE HEADS THE SAME DRIRECTION AS THE SHORT ADIT
Comment (Location): INFO FROM LAND.ST :(1975)
References
Reference (Deposit): TRIPP, B.T., 1981, ON SITE INVESTIGATION: UGMS.
Reference (Deposit): PETERSON, D.J., 1956, STRAT. AND STRUCT. OF THE WEST LOAFER MTN.-UPPER PAYSON CANYON AREA, UTAH CO., UTAH: BRIGHAM YOUNG UNIVERSITY RESEARCH STUDIES, VOL. 3, NO. 4.
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