Easter Island is a Polynesian
island in the southeastern Pacific Ocean, at the southeastern most point
of the Polynesian triangle. The island is a special territory of Chile.
Easter Island is famous for its monumental statues, called moai created
by the Rapa Nui people. It is a world heritage site with much of the
island protected within the Rapa Nui National Park.
The name “Easter Island” was given by the island’s first recorded
European visitor, the Dutch explorer Jacob Roggeveen, who encountered it
on Easter Sunday 1722, while searching for Davis or David’s island. The
island’s official Spanish name, Isla de Pascua, is Spanish for “Easter Island”.

The current Polynesian name of the island, “Rapa Nui” or “Big Rapa”, was
coined by labor immigrants from Rapa in the Bass Islands, who likened
it to their home island in the aftermath of the Peruvian slave
deportations in the 1870s. However, Thor Heyerdahl has claimed that the
naming would have been the opposite, Rapa being the original name of Easter Island, and Rapa Iti was named by its refugees.
There are several hypotheses about the “original” Polynesian name for Easter Island,
including Te pito o te henua, or “The Navel of the World” due to its
isolation. Legends claim that the island was first named as Te pito o te
kainga a Hau Maka, or the “Little piece of land of Hau Maka”. Another
name, Mata-ki-Te-rangi, means “Eyes that talk to the sky.”
Easter Island is a volcanic high island, consisting mainly of three
extinct volcanoes: Terevaka forms the bulk of the island. Two other
volcanoes, Poike and Rano Kau, form the eastern and southern headlands
and give the island its approximately triangular shape. There are
numerous lesser cones and other volcanic features, including the crater
Rano Raraku, the cinder cone Puna Pau and many volcanic caves including
lava tubes. Poike used to be an island until volcanic material from
Terevaka united it to Easter Island. The island is dominated by hawaiite
and basalt flows which are rich in iron and shows affinity with igneous
rocks found in Galapagos Islands.

Easter Island and surrounding islets such as Motu Nui, Motu Iti are the
summit of a large volcanic mountain which rises over two thousand metres
from the sea bed. It is part of the Sala y Gómez Ridge, a mountain
range with dozens of seamounts starting with Pukao and then Moai, two
seamounts to the west of Easter Island, and extending 2,700 km (1,700 mi) east to the Nazca Seamount.
Pukao, Moai and Easter Island were formed in the last 750,000 years,
with the most recent eruption a little over a hundred thousand years
ago. They are the youngest mountains of the Sala y Gómez Ridge, which
has been formed by the Nazca Plate floating over the Easter hotspot.
Only at Easter Island, its surrounding islets and Sala y Gómez does the Sala y Gómez Ridge form dry land.
In the first half of the 20th century, steam came out of the Rano Kau
crater wall. This was photographed by the island’s manager, Mr Edmunds.
Trees are sparse on modern Easter Island, rarely forming small groves.
The island once had a forest of palms, and it has been argued that
native Easter Islanders deforested the island in the process of erecting
their statues. Experimental archaeology has demonstrated that some
statues certainly could have been placed on “Y” shaped wooden frames
called miro manga erua and then pulled to their final destinations on
ceremonial sites. Other theories involve the use of “ladders” (parallel
wooden rails) over which the statues could have been dragged. Rapanui
traditions metaphorically refer to spiritual power (mana) as the means
by which the moai were “walked” from the quarry. But, given the island’s
southern latitude, the climatic effects of the Little Ice Age may have
contributed to deforestation and other changes, though such speculation
is unproven.

Jared Diamond dismisses past climate change as a dominant factor on the
Island’s deforestation in his book Collapse which presents an extensive
look into the collapse of the ancient Easter Islanders. Diamond argues
that the disappearance of the island’s trees seems to coincide with a
decline of its civilization around the 17th and 18th century. Midden
contents show a sudden drop in quantities of fish and bird bones as the
islanders lost the means to construct fishing vessels and the birds lost
their nesting sites. Soil erosion due to lack of trees is apparent in
some places. Sediment samples document that up to half of the native
plants had become extinct and that the vegetation of the island was
drastically altered. Chickens and rats became leading items of diet and
there are contested hints that cannibalism occurred, based on human
remains associated with cooking sites, especially in caves.
The large stone statues, or moai, for which Easter Island is world-famous, were carved during a relatively short and intense burst of creative
and productive megalithic activity. A total of 887 monolithic stone
statues have been inventoried on the island and in museum collections.
Although often identified as “Easter Island heads”, the statues are
actually complete torsos, the figures kneeling on bent knees with their
hands over their stomach. Some upright moai have become buried up to
their necks by shifting soils.
The period when the statues were produced remains disputed, with estimates
ranging from 400 CE to 1500–1700 CE. Almost all (95%) moais were carved
out of distinctive, compressed, easily worked volcanic ash or tuff
found at a single site inside
the extinct volcano Rano Raraku. The native islanders who carved them
used only stone hand chisels, mainly basalt toki, which still lie in
place all over the quarry. The stone chisels were re-sharpened by
chipping off a new edge when dulled. The volcanic stone the moai were
carved from was first wetted to soften it before sculpting began, then
again periodically during the process. While many teams worked on
different statues at the same time, a single moai would take a team of
five or six men approximately one year to complete. Each statue
represents a deceased long-ear chief or important person, their body
interred within the ahu, or coastal platforms, the moai stand upon.
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