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How Raglan (Manu Bay) Works

Waikato, New Zealand · part of the Raglan (Manu Bay) spot guide

Manu Bay is the best-known section of the Raglan point system — a two-kilometre chain of linked left-hand points on a single rock headland on New Zealand’s west coast, and one of the longest left-hand walls on Earth, immortalised in the 1966 film "The Endless Summer." A clean southwest groundswell peels in sequence through Indicators, Whale Bay and Manu Bay.

sea surfaceocean side→ shoreOuter approach / Indicators takeoff12–20 ftPoint shoulder / walling reef6–12 ftManu Bay takeoff ledge4–8 ftInside / boat-ramp end2–6 ft
Illustrative cross-section of the seabed at Raglan (Manu Bay) — depths are approximate research figures, not survey data; horizontal distances not to scale.
ZoneApprox. depthWhat happens here
Outer approach / Indicators takeoff12–20 ftWhere wrapping SW groundswell first feels the point and begins to bend; longer-period sets stand up here first
Point shoulder / walling reef6–12 ftThe boulder reef along the headland that holds the long peeling wall
Manu Bay takeoff ledge4–8 ftA ledgy rock step that jacks the wave — hollow on lower tide, fuller on high
Inside / boat-ramp end2–6 ftA shallow boulder shelf where the ride tapers, with exposed rock at low tide

The headland points southwest into the incoming Tasman and Southern Ocean swell. Long-period southwest groundswell refracts around the rock point, bending its crest to follow the shoreline, which converts open-ocean energy into a slow, ordered, downcoast-peeling left rather than a closeout — the mechanism behind Raglan’s reputation. On an aligned day a surfer can connect Indicators through Manu to Whale Bay in one ride of 800 metres and more. The bottom is volcanic rock and rounded boulders, so booties are standard and it is an intermediate-to-expert wave largely because of the rock.

There is no local buoy — the nearest is thousands of km away — so Raglan is forecast off models. Because the swell wraps the point, the breaking face is typically smaller than the raw open-ocean height but far more organised and longer: the point trades height for length and holds size where beaches close out.

Satellite view of Manu Bay and the Raglan point system, Waikato, New Zealand

Raglan (Manu Bay) wave mechanics — FAQ

Why is Raglan called the world’s longest left?

Manu Bay is one of three linked left-hand points on a single southwest-facing rock headland. Long-period southwest groundswell wraps around the point and peels in order through Indicators, Whale Bay and Manu Bay, so on an aligned day you can ride 300-to-500 metres at Manu alone, or 800 metres and more connecting all three. It was immortalised in the 1966 film "The Endless Summer."

What’s the ideal setup?

A southwest-to-west-southwest groundswell from about 225–250° with a long period around 14-to-16 seconds, open-ocean height around one-and-a-half to two-and-a-half metres, and a light east or southeast offshore wind. Mid tide is the safe all-round choice; drop lower for barrels, go higher for size and to connect the full point.

Is the size number the wave I’ll surf?

No — forecast height is the open-ocean swell height, not the breaking face. Because the swell wraps the point, the face you surf is usually smaller than the model height but much longer and more organised. The point holds up to about 12 feet and keeps producing makeable walls when open beaches close out.

Researched from published surf journalism, oceanographic references and chart data; figures are approximate and confidence-checked. Updated 2026-07-06.