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Hinchcliffe Stadium, Paterson, Passaic Co., New Jersey, USA

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Latitude & Longitude (WGS84): 40° 55' 5'' North , 74° 10' 51'' West
Latitude & Longitude (decimal): 40.91833,-74.18111
GeoHash:G#: dr70zbyyw
Köppen climate type:Cfa : Humid subtropical climate


Hinchliffe Stadium is a historic, 10,000 seat municipal stadium that was built in Paterson, NJ in 1931-32. The stadium was built above Paterson's Great Falls and is surrounded by the city's National Landmark Historic District. Named after Mayor John Hinchcliffe, the stadium is a large concrete oval fashioned in the classical amphitheater design. The stadium had major renovations done in 1963 and 1983. Digging done during the initial excavations yielded documented creme and light brown stilbite, mass & bladed barite with a bluish hue, fibrous white pectolite,and green prehnite. A single specimen of barite had tiny crystals of harmotome, a member of the phillipsite group.


Mineral List


7 valid minerals. 1 erroneous literature entry.

Regional Geology

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

Early Jurassic
174.1 - 201.3 Ma



ID: 2821781
Orange Mountain Basalt

Age: Early Jurassic (174.1 - 201.3 Ma)

Stratigraphic Name: Orange Mountain Basalt

Description: (Olsen, 1980) - Dark-greenish-gray to greenish-black basalt composed mostly of calcic plagioclase (typically An65) and clinopyroxene (augite and pigeonite); crystals are generally less than 1 mm (0.04 in) long. Consists of three major flows. The flows are separated in places by a weathered zone or by a thin, up to 3-m- (10-ft-) thick bed of red siltstone (not shown on map) or volcaniclastic rock. Lowest flow is generally massive and has widely spaced curvilinear joints; columnar joints in lowest flow become more common toward the northeast. Middle flow is massive or has columnar jointing. Lower part of the uppermost flow has pillow structures; upper part has pahoehoe flow structures. Tops and bottoms of flow layers are vesicular. Maximum thickness is about 182 m (597 ft).

Comments: Newark Supergroup, Brunswick Group (Lyttle and Epstein, 1987).

Lithology: Major:{basalt}, Minor:{siltstone}

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. [133]

Triassic
201.3 - 252.17 Ma



ID: 3187774
Mesozoic intrusive rocks

Age: Triassic (201.3 - 252.17 Ma)

Comments: Newark Graben System; Newark-Delaware Basin

Lithology: Intrusive igneous rocks

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Peters, J.J. and T.A. (1978) Famous Mineral Localities: Paterson New Jersey. Mineralogical Record, 9, 162.

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