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Maverick's. Waimea Bay. Pipeline. The names evoke images of the raw beauty of ocean swells exploding on solid reefs, and crowds gathered to watch in awe as expert surfers take on world-class waves. These places are some of the most revered surf spots on Earth, but there's another thing they have in common, something that few people realize: they are all found within national marine sanctuaries. Learn just what makes surfing in your National Marine Sanctuary System so special.
Anatomy of a Wave
- Whitewater: Aerated water that foams and bubbles powerfully as the wave breaks
- Barrel or Tube: The hollow area of a breaking wave
- Peak: The hollow area of a breaking wave
- Lip: The leading edge of the breaking wave
- Face: The smooth, unbroken section of the wave
- Pocket: The steep section of the wave just ahead of the whitewater
- Through: The steep section of the wave just ahead of the whitewater
- Shoulder: The part of the wave that has not yet broken
Riding a Wave
Once the surfer has caught the wave, she can either slow down and tuck into the “barrel”, use her momentum to propel herself back to the shoulder of the wave for more tricks, or continue to leisurely ride the wave.
When tuberiding, surfers ride inside the barrel. Only a small percentage of waves lend themselves to tuberiding, and it is considered one of the more difficult surfing maneuvers.
To tailslide, the surfer slides the tail of her surfboard above and across the wave lip. The key is getting the fins free of the wave by shifting the body’s weight from the back foot to the front foot.
To perform skateboard-inspired aerials, the surfer launches off the crest, flies above the wave, then lands back on the wave face.
If the surfer continues her ride after any maneuver that changes her direction and loses momentum, like a tail slide, she’ll need to re-gain speed by turning back into the direction of the breaking wave.
Evolution of the Surfboard
Surfing has been around for hundreds – perhaps thousands – of years. Through the centuries, surfers have gone in search of the perfect board, trying out different materials and different shapes, each suited to varying ocean conditions.
|Tom Blake||1930s||Hollow Wood|
|Tom Blake||1930s||Hollow Wood|
|Hot Curl||1940s||Hollow Wood|
Parts of a surfboard
Surfboards come in many different shapes and sizes for different conditions and wave types. However, the basics parts of a surfboard remain the same from board to board.
- Deck: The top of the surfboard
- Rocker: The curve of the board from nose to tail
- Fins: Improve stability and control; first added to boards in the 1930s
- Width: Shorter, wider boards are faster and more maneuverable
- Tail: The back of the board
- Rails: The outer edges of the board
- Nose: The front of the board
- Length: Longer boards are slower and more stable
History of Surfing
The history of surfing began in Polynesia, in places like Tahiti, Samoa, Tonga, and Hawai‘i. As our cultures have become more global, so, too, has surfing, with the sport growing across the world.
For hundreds or thousands of years, surfing has been an important part of Polynesian culture, treated as an art more than a sport.
Samoa and Hawai‘i
The particulars of surfing varied around Polynesia: in places like Hawai‘i and Samoa, people surfed on planks and canoes.
Polynesia wasn’t the only place where people rode the waves. In what is now Peru, fishermen rode the surf on small boat-like crafts.
In 1769, during Captain James Cook’s first Pacific expedition, crew members observed native Tahitians surfing “in a manner truely surprising.” Just a few years later, Cook’s crew encountered surfing in Hawai‘i.
In 1885, Hawaiian princes David Kawananakoa, Edward Keli‘iahonui, and Jonah Kuhio Kalaniana‘ole brought surfing to the mainland while students at a military academy in San Mateo, California.
Decades after surfing was largely halted by Christian missionaries, Duke Kahanamoku launched a resurgence of surfing in Hawai‘i and brought the sport to the U.S mainland.
Surfing in the Mainstream
Surfing gained wide attention in the 1950s after TV shows and movies popularized the activity. By the 1960s, surfing exploded into a full-fledged industry and entered the pop culture imagination.
Big wave surfing took off in the 1980s as surfers went in search of ever larger waves around the world. Some of the world’s best waves are found in your national marine sanctuaries.
What Makes a Big Wave
- Winds blow against the surface of the water, transfering energy to the water.
- Small ripples merge into larger waves and build together into sets called “swells.” The wave energy in these swells moves in the direction the wind is blowing.
- As the wave energy moves closer to shore, the upper part of the wave starts to move faster than the bottom part, and creates larger, steeper waves.
- When the wave energy reaches an abrupt change in the ocean floor like a reef, it will create a tubing wave; more gradual changes result in rolling waves.
To make big waves like Maverick’s, this process occurs over thousands of miles of open ocean.