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Puerto Peñasco is often called "Rocky Point" in English, and has been nicknamed "Arizona’s Beach" as it is the closest beach to cities such as Phoenix and Tucson. The warm sea surface temperatures of the northern end of the gulf cause Puerto Peñasco to have a much warmer climate than coastal cities on the Pacific both in the Mexican and ...
The lighthouse is operated in a semi-automatic way, receiving periodic visits from technicians from the maritime signals team of the Port Authority of Las Palmas. [5] It is registered under the international Admiralty number D2807.5 and has the NGA identifier of 113–23990. [4] [6]
Las Palmas is located in the northeastern part of the island of Gran Canaria, about 150 km (93 mi) west of the Moroccan coast [12] in the Atlantic Ocean. Las Palmas experiences a hot desert climate, [note 1] offset by the local cooler Canary Current, with warm temperatures throughout the year. It has an average annual temperature of 21.2 °C ...
La Isleta Lighthouse (Spanish: Faro de La Isleta) is an active 19th century lighthouse on the Spanish island of Gran Canaria in the Canary islands.The lighthouse has been constructed on the rocky peninsula of La Isleta, which overlooks the Port of Las Palmas to the north of the city of Las Palmas, the capital of Gran Canaria. [1]
The lighthouse is the second to be constructed on the rocky headland of Punta Sardina (Sardine Point), which overlooks the Atlantic Ocean. The first was completed in 1891, as part of the first maritime lighting plan for the Canaries. It remained in service until it was demolished in the 1980s to make way for the new modern tower. [3]
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Las Palmas de Gran Canaria : Caja Insular de Ahorros de Canarias. Barrera Artiles, José (1995). Las Canteras (1900–2000) (in Spanish). Las Palmas de Gran Canaria : Ayuntamiento de Las Palmas de Gran Canaria, Concejalía de Playas. ISBN 84-88979-13-4. González Jiménez, José F. (1998). Peces de Canarias : guía submarina (in Spanish). La ...
Pico Viejo (left) and Teide (right) in Las Cañadas caldera. The rejuvenation stage of Tenerife (after a long erosive gap in activity at the centre of Tenerife) started at about 4 Ma and continues to the present day. Between 4.0 and 0.2 Ma, a large stratovolcano (Las Cañadas volcano) formed, centred in the central part of Tenerife.