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Ponce Limestone includes beds of brown clay and has a maximum estimated thickness of 850 meters. [4] It consists mostly of yellowish-orange, soft to moderately hard, fossiliferous limestone and appears almost continuously as a narrow band extending from Bahía Montalva in Patillas to Río Pastillo, in Barrio Canas.
Ponce Limestone: Early Miocene-Early Pliocene [122] Aymamón Limestone: Mid-Late Miocene [123] Aguada Limestone: Early-Late Miocene [124] Quebradillas Limestone: Middle Miocene [125] Cibao Formation: Aquitanian-Burdigalian [126] Lares Limestone: Late Oligocene-Early Miocene [127] Guayanilla Formation: Late Oligocene [128] Guatemala Group: Cibao ...
The Parque Nacional de las Cavernas del Río Camuy (English: Camuy River Cave National Park) is a cave system in Puerto Rico. It is located between the municipalities of Camuy, Hatillo, and Lares in northwestern Puerto Rico, but the main entrance to the park is located in Quebrada, Camuy.
Carboniferous Limestone – Limestone deposited during the Dinantian Epoch of the Carboniferous Period; Coquina – Sedimentary rock that is composed mostly of fragments of shells; Coral rag – Limestone composed of ancient coral reef material; Chalk – Soft carbonate rock; Fossiliferous limestone – Limestone containing fossils
The historic zone is located in what is commonly called Ponce Pueblo – the central downtown and oldest area of the city. While there are several roads that lead to it, the most common point of entry is via PR-1, which becomes the Miguel Pou Boulevard, and then into the one-way Isabel Street, leading to the center of Ponce at the Plaza Las Delicias.
Ponce (US: / ˈ p ɔː n s eɪ, ˈ p oʊ n-/ PAWN-say, POHN-, UK: / ˈ p ɒ n-/ PON-, Spanish: ⓘ) is a city and a municipality on the southern coast of Puerto Rico. [25] The most populated city outside the San Juan metropolitan area, Ponce was founded on August 12, 1692 [note 1] [26] [20] [27] [17] and is named after Juan Ponce de León y Loayza, [28] the great-grandson of Spanish ...
The limestone caves in the park have stalagmites, stalactites, and flowstones formed by the erosion of bedrock. Other formations are above ground, including rivers and springs. [1] Florida Caverns State Park and the neighboring golf course were constructed by the Civilian Conservation Corps as part of the New Deal. The park opened in 1942.
Museo Parque de Bombas [3] (Parque de Bombas Museum) is a museum located inside the historic Parque de Bombas in the Ponce Historic Zone in Ponce, Puerto Rico. This museum is located at the Plaza Las Delicias town square, directly behind the Ponce Cathedral. It is housed in a building that once housed the city's main (and, initially, its only ...