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  2. Lanzarote - Wikipedia

    en.wikipedia.org/wiki/Lanzarote

    Lanzarote has 213 kilometres (132 miles) of coastline, of which 10 km (6 mi) are sand, 16.5 km (10 + 1 ⁄ 4 mi) are beach, and the remainder is rocky. Its landscape includes the mountain ranges of Famara (671 metres or 2,201 feet) [ 22 ] in the north and Ajaches (608 metres or 1,995 feet) to the south.

  3. Beaches Resorts - Wikipedia

    en.wikipedia.org/wiki/Beaches_Resorts

    Gordon “Butch” Stewart (1941-2021) was the businessperson who founded and owned Beaches Resorts. Adam Stewart (1981-), the son of Gordon “Butch” Stewart, is the Executive Chairman of Sandals Resorts International (SRI).

  4. Siesta Beach - Wikipedia

    en.wikipedia.org/wiki/Siesta_Beach

    Siesta Beach Panorama illustrating the expansive width Roll-out mat aids walking. Siesta Beach (sometimes known as Siesta Key Beach) is a beach located on Siesta Key in the U.S. state of Florida. Unlike beaches elsewhere that are made up mostly of pulverized coral, Siesta Beach's sand is 99% quartz, most of which comes from the Appalachian ...

  5. Seaside resort - Wikipedia

    en.wikipedia.org/wiki/Seaside_resort

    A seaside resort is a city, town, village, or hotel that serves as a vacation resort and is located on a coast. Sometimes the concept includes an aspect of an official accreditation based on the satisfaction of certain requirements such as in the German Seebad. [a] Where a beach is the primary focus for tourists, it may be called a beach resort.

  6. Canary Islands - Wikipedia

    en.wikipedia.org/wiki/Canary_Islands

    North of Lanzarote are the islets of Montaña Clara, Alegranza, Roque del Este and Roque del Oeste, belonging to the Chinijo Archipelago. Northeast of Fuerteventura is the islet of Lobos . There are a series of small adjacent rocks in the Canary Islands: the Roques de Anaga , Garachico and Fasnia in Tenerife, and Salmor and Bonanza in El Hierro.

  7. Geology of the Canary Islands - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Canary_Islands

    Remains of the Famara shield volcano's pile of lava flows at the northern tip of Lanzarote (cliff height: 200–300 m (660–980 ft)) Volcanic activity at Lanzarote started during the Oligocene Epoch at 28 Ma. [50] For about the first 12 million years, the lava pile of a submarine seamount built up from the 2,500 m-deep (8,200 ft) ocean floor. [51]