Cadair Idris is formed from a complexly fractured and
folded pile of both
sedimentary rocks and
igneous rocks of
Ordovician age. They comprise the
mudstones and
siltstones of the Ceiswyn Formation which form much of the southern part of the mountain, together with the varied rocks of the underlying
Aran Volcanic Group. The steep cliffs rising above Llyn Cau to the north are formed from hard-wearing
basalts and
tuffs of the Pen y Gadair Volcanic Formation whilst those on the south side are acid tuffs of the Craig Cau Formation. The imposing cliffs which characterise the north side of the mountain are formed from a micro
granite intruded into the Ty'r Gawen mudstones. In common with the rest of Snowdonia, the faulting and folding of this rock succession took place during the
Caledonian Orogeny. '' by
Richard Wilson, 1774 The crater-like shape of Cwm Cau has given rise to the occasional mistaken claim that Cadair Idris is an
extinct volcano (though as noted above, some of its bedrock is volcanic in origin). This theory was discounted as early as 1872, when
Charles Kingsley commented in his book
Town Geology: The natural bowl-shaped depression to which the name of
chair has been attached, was formed by a
cirque glacier during multiple
ice ages when snow and ice accumulated on these slopes partly through
avalanching. The glacier was up to a square kilometre in size surrounded on three sides by steep cliffs the highest being the headwall. The
chair of Cadair Idris is this bowl-shaped hollow in the bedrock formed by the movement of glacial ice across the floor of the hollow,
abrading it and the lip over which it then flowed. near
Llyn Cau. The direction of the
glacial movement was from left to right. There are several tear-drop shaped knolls above the edge of Llyn Cau, each of which is a
roche moutonnée formed by the abrasive action of the moving ice. The two highest lakes are Llyn Cau and Llyn y Gader; the latter is thought to have a maximum depth of about . Much of the area around Cadair Idris was designated a
National Nature Reserve in 1957, and is home to
Arctic–alpine plants such as
purple saxifrage and
dwarf willow. ==Myths, legends and popular culture==