22) Tusse de Remuñé

The Tusse de Remuñé was a southwest-facing glacier at the base of the Pico de la Tusse de Remuñé (3,041 m). Before splitting off as an independent glacier, it formed part of the easternmost end of the 23) Literola Glacier, which is why its characteristics and extent are described together with the aforementioned glacier. The ice of the former ice shelf was almost always hidden under a snowpack. It became extinct in 2006, leaving as proof of its existence a small lake, some moraine lobes and a consistent frontal moraine that belonged to the Literola Glacier.

Este aparato glaciar pertenece al siguiente macizo:

C) Perdiguero Massif

Aragón
20 glaciers

Galería de imágenes

The location of the extinct AG de Tusse de Remuñé (22) under the summit of the same name (6), and of Literola (23) at the base of the Crabioules (7). The Ibones Blancos de Literola (19) are very well camouflaged behind the front moraine of the PEH (18). The Ibón de Literola (20) is the product of over-excavation of the ice in previous glacial periods (Jordi Camins - 2017).

The extinct glacier de la Tusse de Remuñé (22) under the summit of the same name (6) in 2012. Pico Maupás (5) and location of the old glacier of Literola (23) with the Ibón Blanco de Literola, its two younger brothers and the LIA moraine (18) from Pico Royo (Jordi Camins).

The Tusse de Remuñé icefield in 1976 (Camil José Guiu – AFCEC).

The small mountain lake occupying the position of the extinct Tusse de Remuñé glacier and the moraine lobes (Jordi Camins - 2012).

The always attractive Ibón de Literola (no. 20 in photo 132). The magnificent moraine of the Literola Glacier and the small Ibón, in the sector occupied by the Tusse de Remuñé Ice-house (Jordi Camins - 2023).