Marble Caves (General Carrera Lake) — show cave
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Marble Caves (General Carrera Lake)

Catedral de Mármol

  • 2 min read
  • 46.646° S 72.609° W

Interesting facts

  • The rock began as limestone and was turned into marble at about 300–400 °C, some 10 to 15 km below the surface.
  • The marble is more than 300 million years old, but the caverns themselves were carved in roughly the last 6,000 years, after the glaciers retreated.
  • Marble dissolves slightly in water, so the rock wears fastest right at the lake surface, where wind-driven waves widen cracks and wash the dissolved stone away.
  • The lake's colour comes from fine glacial silt suspended in the water, which absorbs violet and indigo light and reflects blues and greens.
  • The Marble Chapel is an islet about 25 metres high, eroded so deeply that its base stands on slender columns of stone.
  • The sanctuary was created by a Chilean decree of 22 June 1994 and covers only about 50 hectares.
  • The caverns' layered, cake-like banding records differences in the minerals of the original limestone beds.

Why it is worth it

The Marble Cathedral is a great block of marble standing in the turquoise water of General Carrera Lake in Chilean Patagonia, hollowed through by the lake itself into arches, pillars and vaulted passages. Together with the smaller Marble Chapel and the Marble Caverns cut into the nearby shore, it forms the formations known in Spanish as the Capillas de Mármol, protected as a nature sanctuary since 1994. The rock is Palaeozoic marble, hundreds of millions of years old; the caverns are recent, carved by waves since the glaciers withdrew and left the lake behind.

The colours are what people come for. The marble is mostly white and pale grey, veined and banded with blue and pink, and the smooth, scalloped walls inside the arches pick up the colour of the glacial water beneath them. Depending on the light and the season, the stone shifts from cream to blue to aquamarine, and the ceilings ripple with reflected light. Up close, the surface is sculpted into soft hollows by the water, as if the rock had been poured rather than cut.

General Carrera Lake is itself remarkable: the largest lake in Chile, of glacial origin, around 586 metres deep at its deepest, and shared with Argentina, where its eastern part is called Lake Buenos Aires. Its milky blue-green colour, set against the brown and snow-streaked Andes, makes the approach to the Cathedral half the experience. Boats and kayaks nose between the columns and into the passages, and the best of the formations can only really be understood from water level.

Getting there

Boat and kayak trips leave from Puerto Río Tranquilo, a village on the Carretera Austral (Route 7) on the shore of the lake. Coyhaique, the regional capital, is about 126 km away in a straight line, but by road it is a drive of roughly four hours south along the Carretera Austral. The nearest airport is Balmaceda Airport (BBA), about 108 km away in a straight line, which serves the Coyhaique area; from there the route continues by road.

On these lists

From the encyclopaedia

General Carrera Lake or Lake Buenos Aires is a deep lake located in Patagonia and shared by Argentina and Chile. Both names are internationally accepted, while the autochthonous name of the lake is Chelenko, which means "stormy waters" in Aonikenk. Another historical name is Coluguape from Mapuche, a derivative of this name is applied to Colhué Huapí Lake after Argentine explorer Francisco Moreno reached this lake in 1876 conflating it with Coluguape.

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