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Easter Island / Rapa Nui

Easter Island Bark EUROPA Rapa Nui by Jordi Plana Morales

The most remote landfall in the Pacific

Easter Island — Rapa Nui — lies in the southeastern Pacific Ocean at approximately 27° south, 109° west. It is one of the most remote inhabited places on Earth, with no significant landmass nearby in any direction. The island was formed by three extinct volcanoes and covers roughly 163 square kilometres. In 1995, UNESCO named Easter Island a World Heritage Site, with much of the island protected within Rapa Nui National Park. For those arriving by sailing ship after weeks on the open Pacific, it is among the most striking landfalls in the world.

Rapa Nui — The Island

The only town and harbour on the island is Hanga Roa, a small, unhurried place where Rapa Nui culture continues to live in language, ceremony, and daily life. The island is a special territory of Chile, but it feels like neither — it belongs to its own history, its own ocean, its own silence.

Between the 10th and 16th centuries, a society of Polynesian origin built shrines and erected enormous stone figures across this island in total isolation from the rest of the world. These are the moai — monolithic ancestor figures carved from volcanic tuff at the quarry of Rano Raraku, transported across rugged terrain, and raised on ceremonial stone platforms called ahu around the island's perimeter. Around 900 moai have been documented, alongside more than 300 ahu. Nearly half of the statues remain at Rano Raraku, some finished, many not, left in the hillside as though work stopped mid-morning and no one came back.

Almost all moai face inland, across the clan lands they were built to protect, with their backs to the sea. They are not decorative. The Rapa Nui people believed the moai held the spirits of their ancestors — that by raising these figures in stone, the protection and guidance of the dead could remain among the living.

The quarry at Rano Raraku, the fifteen-moai platform of Ahu Tongariki, and the ceremonial village of Orongo on the rim of the Rano Kau crater are among the most significant sites. Visits to most areas of the national park require a local guide — a measure introduced to protect what remains of a landscape that took centuries to build and is not replaceable.

Easter Island Bark EUROPA Rapa Nui by Jordi Plana Morales

Arriving by sail

There is no view of Rapa Nui from a runway. Flying in, the island simply appears through a porthole window — there, and then landed.

Arriving by sailing ship is a different experience entirely. From the Galápagos, the course is set southwest. The southeast trade winds carry the ship across the eastern Pacific, the equator passes beneath the keel in the early days, and then there is nothing — no land, no shipping lanes, no other lights at night — for the better part of three weeks. The crossing covers close to 1,940 nautical miles.

As Rapa Nui draws near, the ocean changes. The swell lengthens. The air cools. The island's volcanic cliffs rise from the horizon as a dark line, then slowly take shape — the crater of Terevaka, the coastal terraces, and finally the anchorage at Hanga Roa. It is the kind of arrival that earns its meaning through the days of ocean that came before it.

Rapa Nui was first settled by Polynesian navigators who crossed this same ocean on vessels guided by stars, currents, and the flight of seabirds. Arriving under sail connects you, however distantly, to that tradition of purposeful ocean crossing — to the understanding that distance is not an obstacle to cross quickly, but a passage to be made with care.

Sailing to Rapa Nui in July

Bark EUROPA arrives at Easter Island in July, during the Southern Hemisphere winter. The conditions on both the crossing and the island itself are worth knowing before you sail.

On the passage from the Galápagos

The eastern South Pacific is governed by a large, stable high-pressure system whose centre typically sits close to Easter Island itself. This makes the westward crossing a largely downwind passage once the equatorial light-wind zone is cleared in the first days.

The trade winds on this passage follow a diurnal pattern — tending to strengthen around sunset, blow steadily overnight, and ease at daybreak before building again through the day. Overall conditions are generally settled, with typical sustained winds in the range of 15 to 20 knots.

Nights on this crossing are exceptional. Far from any light pollution, the Milky Way is visible to the horizon on clear nights. The Southern Cross climbs a little higher each night as the ship moves south.

On the island in July

  • Average daytime temperatures around 21°C, dropping to approximately 15°C overnight. Layers are useful, particularly for evenings ashore.
  • July falls within the island's winter rainy season. Showers are possible, though they rarely last all day.
  • Winds on the island are predominantly from the north and northwest in winter, and can be felt strongly at exposed sites such as the Rano Kau crater rim.
  • Easter Island sits outside the cyclone belt and is not affected by tropical storms at any time of year.
  • July is outside the peak tourist season. Visitor numbers at archaeological sites are lower and the island feels quieter.

Conditions on ocean passages can vary. The permanent crew monitors weather continuously and adjusts the route accordingly.