[1] The gorge is an indirect product of glaciation; 10,000 years ago, just as the Ice Age was coming to an end, torrential runoff water from melting glaciers eroded a deep, narrow chasm through the limestone barrier.
[1] Although barely 2 kilometres (1 mi) long, this passage is bordered by sheer cliffs up to 50 m (160 ft) high on either side.
Permission to build walking paths along the Gorge was granted in 1887, and the walkway has been open to the public since 1889.
From 1912 until 1956, the Meiringen–Reichenbach–Aareschlucht tramway linked the gorge's western entrance to Meiringen; since 1946 the Meiringen-Innertkirchen railway has also served the same purpose.
For most of its length the path is a wooden construction on a metal frame cantilevered out from the wall of the gorge, with short stretches in tunnel.