Schuylkill River at Penrose Ferry Bridge, Philadelphia, Philadelphia Co., Pennsylvania, USAi
Regional Level Types | |
---|---|
Schuylkill River at Penrose Ferry Bridge | Bridge |
Philadelphia | City |
Philadelphia Co. | County |
Pennsylvania | State |
USA | Country |
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Latitude & Longitude (WGS84):
39° 53' 52'' North , 75° 12' 41'' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Colwyn | 2,553 (2017) | 3.9km |
National Park | 2,999 (2017) | 4.5km |
Darby | 10,687 (2017) | 4.7km |
Sharon Hill | 5,702 (2017) | 5.2km |
Whitman | 49,732 (2018) | 5.2km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Delaware Valley Paleontological Society | Philadelphia, Pennsylvania | 7km |
Philadelphia Mineralogical Society | Philadelphia, Pennsylvania | 7km |
Delaware Valley Earth Science Society | Woodbury, New Jersey | 8km |
Tuscarora Lapidary Society | Brookhaven, Pennsylvania | 15km |
Delaware Mineralogical Society, Inc. | Wilmington, Delaware | 33km |
The Penrose Ferry Bridge spanned the Schuylkill River in the South Philadelphia neighborhood from 1860 to 1876 and again from 1878 to 1949, but now no longer exists. It was replaced by the Platt Bridge a short distance to the north.
The deposit of clay underneath the city of Philadelphia, ten miles square with an average depth of fifteen feet containing a diffusion of gold. The weight of one hundred and thirty grammes of clay, duly dried and treated, yielded one eighth of a milligram of gold, a very decided quantity on a fine assay balance. Experiments were repeated upon clay taken from the cellar of a new market-house in Market Street, near Eleventh Street, at the depth of fourteen feet where it could not have been an artificial deposit, and from a brickyard in the suburbs of the city with nearly the same result. The assays gave seven-tenths of a grainsay, or three cents worth of gold to the cubic foot. Assuming the data already given, we get four thousand one hundred and eighty million cubic feet of clay under the streets and houses. Although void of value, the corporate limits of the city would afford eight times this bulk of clay, amounting to more gold than has yet been brought to market, according to the Statistics from California and Australia (1861).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsGallery:
List of minerals arranged by Strunz 10th Edition classification
Unclassified Minerals, Rocks, etc. | |||
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ⓘ | 'Clays' | - |
List of minerals for each chemical element
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A) In-text Citation No.Dubois and Eckfeldt (Messrs.), Natural Dissemination of Gold, Proceedings of the American Philosophical Society: VIII: 273.
Genth, F. A. (1875), Preliminary Report of The Mineralogy of Pennsylvania, 2nd Geological Survey of Pennsylvania, B2.
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Carolinia DomainDomain
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Schuylkill River at Penrose Ferry Bridge, Philadelphia, Philadelphia Co., Pennsylvania, USA