Gemstone Beach, Orepuki

BY NICK MORTIMER (GNS)
Accessibility: EASY
Gemstone Beach pebbles. J.Thomson / GNS Science
Gemstone Beach is so named because of the variety of semi-precious stones that can be found as pebbles on the beach there. The sand level varies by the month, year and decade. Sometimes there are lots of pebbles exposed just north of Taunoa Stream mouth, sometimes very few. The pebbels are not eroded out of the cliffs but have travelled down the Waiau River from Fiordland and been transported east along Te Waewae Bay.
The most prized stone on the beach is a mineral called hydrogrossular. It occurs as rare, hard, translucent, waxy-whitish green pebbles 1-10cm in size. Hydrogrossular is a calcium aluminum garnet with water in its mineral structure (most garnets have no water). As they are loose pebbles on a beach, it's clear that the hydrogrossulars have come from somewhere else. That somewhere is the Countess Range where the garnets form in rocks called rodingites in the Dun Mountain Ophiolite Belt. They have been tumbled and polished in a 150 km journey down the Eglinton and Waiau valleys.
The smooth and wet pebbles reveal a variety of rich colours and textures. There are many different kinds of rock.

(1) hydrogrossular (waxy whitish green)

(2) epidosite (apple or pistachio green)

(3) jasper chert (hard, deep red)

(4) rhyolite porphyry (pale red, scattered feldspar crystals)

(5) granite (grey, interlocking crystals)

(6) quartz (white, milky)

The sand on the beach is different again in composition. There are concentrated pockets of black sand and tracks and traces of reddish sand. The black sand grains are magnetite and the red ones almandine garnet. These, too have come from Fiordland.
Directions/Advisory

Gemstone Beach is signposted off State Highway 99, about 500m north of Orepuki. There is a small carpark at the end of Mullans Road West.

Watch for waves. Avoid high tide.

Google Directions

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Accessibility: EASY

A short scramble down to the beach. You may get wet feet crossing Taunoa Stream. The pebbles are only visible at low and mid tide.

Features
Metamorphic Geothermal
Geological Age
Holocene
Zealandia Evolution Sequence
Pākihi Supergoup: 5 million years ago – present