Henryton, Carroll Co., Maryland, USA
|Latitude & Longitude (WGS84):||39° 21' 4'' North , 76° 54' 48'' West|
|Latitude & Longitude (decimal):||39.35111,-76.91333|
|Köppen climate type:||Cfa : Humid subtropical climate|
A populated place. The area contains a large pegmatite body that was mined for feldspar and other minerals. Quarry sites and outcrops are currently (2016)within Patapsco State Park.
Commodity ListThis is a list of exploitable or exploited mineral commodities recorded from this region.
Mineral ListMineral list contains entries from the region specified including sub-localities
6 valid minerals.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
Select Rock List TypeAlphabetical List Tree Diagram
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
541 - 2500 Ma
|Wissahickon Formation; Lower Pelitic Schist|
Age: Proterozoic (541 - 2500 Ma)
Stratigraphic Name: Wissahickon Formation
Description: (Formerly mapped as oligoclase facies of Wissahickon Formation.) Medium- to coarse-grained biotite-oligoclase-muscovite-quartz schist with garnet, staurolite, and kyanite; fine- to medium-grained semipelitic schist; and fine-grained granular to weakly schistose psammitic granulite; psammitic beds increase upward; apparent thickness 5,500 feet or more.
Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052.