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We feel it is important to be able to get your message across to as many people as possible. If you have an idea for an article why not put pen to paper (sort of!) and let people know your thoughts and feelings on matters that affect you as a surfer in Cornwall. When you get that burning desire to write an article on an issue which you feel strongly about, please submit the article to cornwallsurfpoint snail mindator dot net
Surfing originated from Tahiti and Hawaii and is it generally thought that it was the Polynesians that first took to the waves. Originally surfing on large wooden boards crafted by the elders. It is thought that many royals in the communities took great satisfaction in surfing and proved themselves to be great leaders by riding the largest waves possible. One leader even went so far as to never go out in the waves unless everyone else was to afraid to!
The first Westerner to come across surfing was Captain James Cook who recognized surfing in the early 1770’s. Westerners declared that surfing was an unholy pursuit and eradicated it from the local way of life.
Surfing was brought to the America and Australia in 1915 by Duke Kahanamoku, a Hawaiian Olympic champion. The American people embraced the sport and surfing took off on the course of history. It was only in the 1960’s that surfing was introduced to Cornwall, UK by lifeguards from Australia. Surfing in Cornwall soon took off and seemed to fit nicely with the hippy revolution of the time.
Cornwall holds some world class surfing waves, notably Fistral beach Newquay, but also more locally know is Porthleven which holds a powerful wave indeed. Newquay has been internationally renowned on the competitive circuit for some time now and goes from strength to strength with talk of a new artificial reef being implemented.
Surfing has for many people become an absolute life culture. Cornwall holds some of the worlds most beautiful landscapes and it is a pleasure to be involved with nature in the way that surfing allows you to.
Originally developed by Hawaiian islanders (see Ngaru), before the 15th century, "he'e nalu" spread in the early 20th century to the mainland USA and Australia, where heavy timber "plank" boards were ridden directly towards beaches.
The sport exploded in popularity in the 1950s and 1960s, when cheaper, more manoeuvrable, and lighter boards made of fibreglass and foam became available and the teenaged baby boomers headed to the beach in droves to enjoy the manoeuvrability and stunts made possible by the new boards. Surfing in Cornwall didn't kick off till much later! The sport has spread to most places where waves of sufficient size and shape appear, including Brazil, Costa Rica, France, Ireland, México, New Zealand, Norway, South Africa, and many island states including Barbados in the Caribbean and Tahiti in the Pacific. Long Island is also a very popular spot for surfing.
Equipment used in surfing includes a leash (to keep a surfer's board from washing to shore after a 'wipeout', and to prevent it from hitting other surfers), surf wax and/or traction pads (to keep a surfers feet from slipping off the deck of the board), and "skegs" (also known as fins) which can either be permanently attached ("glassed-on") or interchangeable. Check out other sections of this site fo find certain suppliers of surfing equipment in Cornwall. In warmer climates swimsuits, surf trunks or boardshorts are worn; in cold water surfers can opt to wear wetsuits, booties, hoods, and gloves to protect them against lower water temperatures.
Surfing's appeal probably derives from an unusual confluence of elements: adrenaline, skill, and high paced manoeuvring are set against a naturally unpredictable backdrop—an organic environment that is, by turns, graceful and serene, violent and formidable. Surfers' skills are tested not only in their ability to control their board in challenging conditions, but by their ability to execute various manoeuvres such as the 'cutback' (turning back toward the breaking part of the wave), the 'floater' (riding on the top of the breaking curl of the wave), 'off the lip' (banking off the top of the wave), the 'aerial' (arcing through the air above the wave) and, if the surf conditions allow it, tube riding. This is the holy grail of surfing, where the surfer manoeuvres into a position where the wave curls over the top of them, forming a "tube" (or "barrel"), with the rider inside the cylindrical portion of the wave. However, such situations do not exist if the waves 'dump' or 'close-out', meaning that they break in large parts at a time.
The drama of surfing obscures the sport's mundane aspects. Most people only see the pros riding and miss (when televised) or ignore the time-consuming paddling out and waiting required to get a surfer into position. In recent times national media has portrayed surfing in Cornwall in a very lame way! Either boogie boarders, or "Newquay, Newquay, Newquay"!!
Competitive surfing is a comparison sport. Riders, competing in pairs or small groups, are allocated a certain amount of time to ride waves and display their prowess and mastery of the craft. Competitors are then judged according to how competently the wave is ridden, including the level of difficulty, as well as frequency, of manoeuvres. There is a professional surfing world championship series held annually at surf beaches around the world.
Although competitive surfing has become an extremely popular and lucrative activity, both for its participants and its sponsors, the sport does not have its origins as a competitive pursuit. It is common to hear debate rage between purists of the sport, who still maintain the ideal of 'soul surfing', and surfers who engage in the competitive and, consequently, commercial side of the activity.
A non-competitive adventure activity involving riding the biggest waves possible (known as "rhino hunting") is also popular with some surfers. A practice popularised in the 1990s has seen big wave surfing revolutionised, as surfers use jet skis to tow them out to a position where they can catch previously unrideable waves (See also: tow-in surfing). These waves were previously unrideable due to the speed at which they travel. Some waves reach speeds of over 60 km/h; jetskis enable surfers to reach the speed of the wave thereby making them rideable. Jetskis not only allow surfers to ride these waves but allow them to survive 'wipeouts'. In many instances surfers would not survive the battering of the 'sets' (groups of waves together) without drowning. This spectacular activity is extremely popular with television crews, but because such waves rarely occur in heavily populated regions, and usually only a very long way out to sea on outer reefs, few spectators see such events directly.
Surfing conditions at a particular location or "break" that is known for surfing (see below) are almost never ideal. Wind blown consistently over a large area of fetch, or open water, causing swell in Cornwall. To learn more about surf meteorology, see StormSurf's Tutorials. As waves near their ultimate destination (Cornwall!), the bottom of the wave begins to run aground as the water becomes more shallow.
There are two primary factors that contribute to the general characteristics of waves at a particular break: (1) the "swell window" or the exposure of the location to wave-generating areas of fetch, and (2) the structure of the ocean floor (composition, shape).
The swell window determines the potential of a break to receive waves. In general, the western coast of any continent usually has better breaks since winds (and, therefore, waves) tend to travel from west to east. Coastlines that face east or south (in the Northern Hemisphere) or north (in the Southern Hemisphere) that are exposed to tropical storms and hurricanes can also be surfable on a consistent basis. When waves break along a section of coastline at an angle almost perpendicular to the land, these special locations, known as point breaks, can produce very long-lasting waves that can be surfed for several hundred meters. The two main types of waves for surfing apart from the pointbreak are the reef break (waves breaking over a coral reef or rockbed) and the beach break (waves breaking onto sand bars). To learn more about the types of waves for surfing see Surfing-Waves.com Wave information.
The structure of the ocean floor is the biggest factor that determines the broad characteristics of waves at a particular break. For instance, there are beach breaks (soft sand bottom) that generate slower, mushy waves and reef breaks (coral reef or rock bottom) that tend to generate faster, more powerful waves. Based on the structure of the ocean floor, a location may break better on a particular tide, say, an incoming high tide or a low-low tide.
Local wind conditions, water temperature, solar radiation, the crowd factor, hazardous aquatic life, water pollution, and aggression of local surfers are other factors that can have impact on the experience one might have surfing at a particular break.
The availability of free model data from the NOAA has allowed the creation of several Surf forecasting websites. These automatically combine the above variables into a presentation of how good the surf will be.