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Casa Belvedere

2008 establishments in New York CityGrymes Hill, Staten IslandHouses completed in 1908Houses on the National Register of Historic Places in Staten IslandItalian-American culture in New York City
Italian-American museumsMuseums established in 2008Museums in Staten IslandNew York City Designated Landmarks in Staten IslandNew York City Registered Historic Place stubsRenaissance Revival architecture in New York CityStaten Island geography stubsUse American English from June 2022Use mdy dates from June 2022
LOUIS A AND LAURA STIRN HOUSE, STAPLETON, RICHMOND COUNTY, NY
LOUIS A AND LAURA STIRN HOUSE, STAPLETON, RICHMOND COUNTY, NY

Casa Belvedere is a cultural center devoted to Italian studies, located at 79 Howard Avenue, Grymes Hill, Staten Island, New York City. The mansion was constructed in 1908, and is an Italian Renaissance style building with Arts and Crafts detailing. It is a 2+1⁄2-story, stuccoed masonry structure with a 2+1⁄2-story service wing and attached conservatory. It features an overhanging clay tile hipped roof with bracketed eaves and a portico with Ionic order columns and Doric order corner piers. Also on the property is a contributing former garage.: 5, 9 Over the years it housed a number of different families, including for several years being the official residence of the President of Wagner College. It was declared a New York City Landmark in 2006 and listed on the National Register of Historic Places in 2010 as the Louis A. and Laura Stirn House. In 2008 it was purchased by Gina Biancardi and Luciano Rammaironi, and turned into a cultural center. In this role it hosts Italian language classes for both adults and children, wine tastings, lectures, films, cooking lessons, book signings, displays of Italian-made motor vehicles (e.g. Alfa Romeo, Lamborghini, and Vespa), and art exhibits, all with an Italian orientation.: 16 

Excerpt from the Wikipedia article Casa Belvedere (License: CC BY-SA 3.0, Authors, Images).

Casa Belvedere
Howard Avenue, New York Staten Island

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Latitude Longitude
N 40.628333333333 ° E -74.088333333333 °
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Address

Howard Avenue 79
10304 New York, Staten Island
New York, United States
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LOUIS A AND LAURA STIRN HOUSE, STAPLETON, RICHMOND COUNTY, NY
LOUIS A AND LAURA STIRN HOUSE, STAPLETON, RICHMOND COUNTY, NY
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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.