FUERTEVENTURA EDITION 27 OUT NOW - CORRALEJO EDITION 37 COMING SOON - BE FEATURED IN OUR CORRALEJO EDITION 37 MAP ➔
Places to surf in Fuerteventura
ADS is also known for the Tide Table that we previously published annually and was popular among surfers, widsurfers and kiters. The Tide Table was distributed free of charge and was present in the main spots of the peninsula and the Canary Islands.
The tides are very long waves that move across our oceans, and they are caused by the gravitational pull from the moon and, to a lesser extent, the sun.
When the highest point of the wave (also known as a crest) reaches a coastline, the coast experiences what we call a high tide. At the lowest point (also known as a trough) reaches the coast, we experience a low tide.
Tidal forces of the moon in the open ocean will form as bulges of water that face the moon, but around land mass and coast lines, the water is able to spread out onto land, which creates the tides.
Earth's tides change based on the gravitational pull of the moon as it orbits us. The gravitational pull of the moon is strongest on whichever side of the Earth is facing it, and gravity pulls the oceans towards the moon, resulting in a high tide.
On the opposite side of Earth, the bulge is caused by inertia. The water moving away from the moon is able to result the gravitational forces trying to pull it in the opposition direction because the gravitational pull is weaker on the far side of Earth. Inertia wins, and this caused the ocean to bulge out and create a high tide.
As the Earth spins, different locations on the planet will face the moon, and this rotation is what allows the tides to cycle around the planet.
CORRALEJO - PLAYA DEL MORO
CORRALEJO - LA ENTUBADERA
CORRALEJO - EL MUELLE
EL COTILLO - PUNTA GORDA
CORRALEJO - EL BURRO
CORRALEJO - BAJO DEL MEDIO
MAJANICHO
EL COTILLO - PIEDRA PLAYA