Editing Surfing (section)

=== Surf breaks ===
A [[surf break]] is an area with an obstruction or an object that causes a wave to break. Surf breaks entail multiple scale phenomena. Wave section creation has microscale factors of peel angle and wave breaking intensity. The micro-scale components influence wave height and variations on wave crests. The mesoscale components of surf breaks are the ramp, platform, wedge, or ledge that may be present at a surf break. Macro-scale processes are the global winds that initially produce offshore waves. Types of surf breaks are headlands (point break), beach break, river/estuary entrance bar, reef breaks, and ledge breaks.<ref name=Scarfe2009 />

==== Headland (point break) ====
A [[headland]] or point break interacts with the water by causing refraction around the point or headland. The point absorbs the high-frequency waves and long-period waves persist, which are easier to surf. Examples of locations that have headland or point break-induced surf breaks are Dunedin (New Zealand), Raglan (New Zealand), Malibu (California), Rincon (California), and Kirra (Australia).<ref name=Scarfe2009 />

==== Beach break ====
A beach break is an area of open coastline where the waves break over a sand-bottom. They are the most common, yet also the most volatile of surf breaks. Wave breaks happen successively at beach breaks, as in there are multiple peaks to surf at a single beach break location. Example locations are Tairua and Aramoana Beach (New Zealand) and the Gold Coast (Australia).<ref name=Scarfe2009 />
<gallery>
JunoBeachBeachBreak.jpg|A group of surfers surfing a beach break in [[Juno Beach, Florida]].
</gallery>

==== River or estuary entrance bar ====
A river or estuary entrance bar creates waves from the ebb-tidal delta, sediment outflow, and tidal currents. An ideal estuary entrance bar exists in Whangamata Bar, New Zealand.<ref name=Scarfe2009 />

==== Reef break ====
A reef break is conducive to surfing because large waves consistently break over the reef. The reef is usually made of coral, and because of this, many injuries occur while surfing reef breaks. However, the waves that are produced by reef breaks are some of the best in the world. Famous reef breaks are present in Padang Padang (Indonesia), Pipeline (Hawaii), Uluwatu (Bali), and Teahupo'o (Tahiti).<ref name=Scarfe2009 /><ref>{{cite web|last1=Hurt|first1=Garek|title=The differences between beach breaks, point breaks, and reef breaks |url=https://www.degree33surfboards.com/blogs/gettin-pitted/14071029-the-differences-between-beach-breaks-point-breaks-and-reef-breaks|website=Degree 33 Surfboards|access-date=26 November 2017}}</ref>

==== Ledge break ====
A ledge break is formed by steep rocks ledges that make intense waves because the waves travel through deeper water then abruptly reach shallower water at the ledge. Shark Island, Australia is a location with a ledge break. Ledge breaks create difficult surfing conditions, sometimes only allowing body surfing as the only feasible way to confront the waves.<ref name=Scarfe2009 />