Parc des Buttes-Chaumont
| Parc des Buttes-Chaumont | |||
|---|---|---|---|
| Type | Urban park | ||
| Location | 19th arrondissement, Paris | ||
| Coordinates | 48°52′49″N 2°22′58″E / 48.88028°N 2.38278°ECoordinates: 48°52′49″N 2°22′58″E / 48.88028°N 2.38278°E | ||
| Area | 61 acres (25 ha) | ||
| Created | 1867 | ||
| Operated by | Direction des Espaces Verts et de l’Environnement (DEVE) | ||
| Status | Open all year | ||
| Public transit access |
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The Parc des Buttes-Chaumont (pronounced [paʁk de byt ʃomɔ̃]) is a public park situated in northeastern Paris, in the 19th arrondissement. Occupying 24.7 hectares (61 acres), it is the fifth-largest park in Paris, after the Bois de Vincennes, the Bois de Boulogne, the Parc de la Villette, and the Tuileries Garden. It was opened in 1867, late in the regime of Emperor Napoleon III, and was built by Jean-Charles Alphand, who created all the major parks of Napoleon III. The park has 5.5 kilometres (3.4 miles) of roads and 2.2 kilometres (1.4 miles) of paths. The most famous feature of the park is the Temple de la Sibylle, inspired by the Temple of Vesta in Tivoli, Italy, perched at the top of a cliff fifty metres above the waters of the artificial lake.
Map of the Parc des Buttes-Chaumont.
A view of the park and the Temple de la Sibylle.
The park on a sunny afternoon.
The sloping lawns of the Parc are a popular gathering place on weekends.
The main promenade within the park.
A pathway through the park.
Temple Sybille from the lake shore
The park took its name from the bleak hill which occupied the site, which, because of the chemical composition of its soil, was almost bare of vegetation- it was called Chauve-mont, or bare hill. The area, just outside the limits of Paris until the mid-19th century, had a sinister reputation; it was close to the site of the Gibbet of Montfaucon, the notorious place where the bodies of hanged criminals were displayed after their executions from the 13th century until 1760. After the 1789 Revolution, it became a refuse dump, and then a place for cutting up horse carcasses and a depository for sewage. The director of public works of Paris and builder of the Park, Jean-Charles Alphand, reported that "the site spread infectious emanations not only to the neighboring areas, but, following the direction of the wind, over the entire city." Another part of the site was a former gypsum and limestone quarry mined for the construction of buildings in Paris and in the United States. That quarry also yielded Eocene mammal fossils, including Palaeotherium, which were studied by Georges Cuvier. This not-very-promising site was chosen by Baron Haussmann, the Prefet of Paris, for the site of a new public park for the recreation and pleasure of the rapidly growing population of the new 19th and 20th arrondissements of Paris, which had been annexed to the city in 1860.
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