The Island of Rhodes is one of the most popular beach destinations in Europe so the northern coast of the island is full of touristy resorts but the southern coast offers more peaceful beaches and a slower pace of life. While the Island isn’t very big in size, you will still regularly stumble across hidden beaches and fascinating archeological sites.
Finswimmers do not normally use snorkels with a sump valve, as they learn to blast clear the tube on most if not all exhalations, which keeps the water content in the tube to a minimum as the tube can be shaped for lower work of breathing, and elimination of water traps, allowing greater speed and lowering the stress of eventual swallowing of small quantities of water, which would impede their competition performance.
What was once a French colonial resort town in southern Cambodia is now a quiet coastal getaway surrounded by tropical islands. Known for its seafood market, where the fish practically jump from the water to your plate, it’s easy to see why Kep won’t be kept a secret for long. For the time being, you’ll find very few tourists among the locals sampling fresh crab, lobster, shrimp (and pretty much anything that swims) at its popular seafood market — you can go there around sunset and have yourself a five-star meal for less than a few dollars. Travelers visit Kep for its laid-back atmosphere rather than an extensive list of activities. In the past, Kep was primarily limited to expats living in Phnom Penh looking for a quiet weekend getaway, but with a variety of nearby tropical islands like Koh Tonsay — better known as Rabbit Island — it’s no wonder Kep is becoming more difficult for visitors to stay away from.
A third type of volcanic oceanic island is formed over volcanic hotspots. A hotspot is more or less stationary relative to the moving tectonic plate above it, so a chain of islands results as the plate drifts. Over long periods of time, this type of island is eventually "drowned" by isostatic adjustment and eroded, becoming a seamount. Plate movement across a hot-spot produces a line of islands oriented in the direction of the plate movement. An example is the Hawaiian Islands, from Hawaii to Kure, which continue beneath the sea surface in a more northerly direction as the Emperor Seamounts. Another chain with similar orientation is the Tuamotu Archipelago; its older, northerly trend is the Line Islands. The southernmost chain is the Austral Islands, with its northerly trending part the atolls in the nation of Tuvalu. Tristan da Cunha is an example of a hotspot volcano in the Atlantic Ocean. Another hotspot in the Atlantic is the island of Surtsey, which was formed in 1963.
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