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Notre Dame Academy (Staten Island)

1903 establishments in New York CityAC with 0 elementsCatholic elementary schools in New York CityEducational institutions established in 1903Girls' schools in New York City
Grymes Hill, Staten IslandPrivate elementary schools in Staten IslandPrivate middle schools in Staten IslandRoman Catholic high schools in Staten IslandUse American English from November 2022Use mdy dates from November 2022
Notre Dame School, Staten Island, N.Y. (entrance to main building) (NYPL b15279351 104966)
Notre Dame School, Staten Island, N.Y. (entrance to main building) (NYPL b15279351 104966)

Notre Dame Academy is an American private Catholic girls' school in Staten Island, New York. It is located within the Roman Catholic Archdiocese of New York. As a private school, Notre Dame is not owned by the archdiocese, although it does maintain a close affiliation with the archdiocese. The school is located on a 13-acre (5.3 ha) campus on Grymes Hill in Staten Island, New York. Consisting of an elementary school (PK3 – 8) and high school (9–12), the school serves approximately 700 students.While providing an education in the Catholic tradition, the school is open to girls of all faiths.

Excerpt from the Wikipedia article Notre Dame Academy (Staten Island) (License: CC BY-SA 3.0, Authors, Images).

Notre Dame Academy (Staten Island)
Victory Boulevard, New York Staten Island

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Latitude Longitude
N 40.62875 ° E -74.089305555556 °
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Address

Victory Boulevard 590
10301 New York, Staten Island
New York, United States
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Notre Dame School, Staten Island, N.Y. (entrance to main building) (NYPL b15279351 104966)
Notre Dame School, Staten Island, N.Y. (entrance to main building) (NYPL b15279351 104966)
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Nearby Places

Staten Island Serpentinite

The Staten Island Serpentinite locality is a southward extension of the New England Uplands, adjacent to the Manhattan Prong. It includes Todt Hill on Staten Island, which is the highest point along the Atlantic Seaboard south of Maine, at 410 feet (120 m) above sea level. "Todt" is a Dutch word meaning "dead." This hill perhaps received its name from the Dutch settlers because the hilltops overlooking The Narrows consisted of scattered treeless rocky exposures. The chemical character of the bedrock was, in part, the reason for this. Much of Staten Island is covered by the Harbor Hill moraine, the terminal moraine of the last Wisconsin Stage glacier. However, ledges of bedrock consisting of serpentinite are exposed throughout the upland areas on Staten Island. Grymes Hill, the second highest point on Staten Island and just a few miles from Todt Hill has similar bedrock characteristics. Serpentine, the dominant mineral in serpentinite, is rich in magnesium, an element that most plants cannot tolerate in high concentrations. The enrichment of magnesium in the thin serpentine soil covering the glacier-scoured hilltops is probably responsible for the original barren exposures on Todt Hill. The serpentinite has a bluish to greenish gray color, and consists of serpentine (mostly the variety antigorite), with accessory minerals of chrysotile (a form of asbestos), magnetite, and talc. Serpentinite is derived by the metamorphism of ultramafic rocks (rocks rich in the minerals olivine and pyroxene) in a water-rich environment. The probable original setting for these rocks was within the igneous crust beneath the Iapetus Ocean. The occurrence of serpentinite in the core of Staten Island is an indication that the allochthonous basement rocks consisting of oceanic crustal material were thrust landward onto the eastern margin of the continent during the Taconic orogeny. The occurrence of serpentinite is consistent with the interpretation that Staten Island is east of Cameron's Line. This article incorporates public domain material from Staten Island Serpentinite. United States Geological Survey.