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Three orogenies produced the Appalachians: the Ordovician Taconic orogeny, which involved arc accretion; the Acadian–Neoacadian orogeny, which involved north-to-south, transpressional, zippered, Late Devonian–early Mississippian collision of the Carolina superterrane in the southern central Appalachians, the Avalon and Gander superterranes in the New England Appalachians, and Silurian collision in the Maritime Appalachians and Newfoundland; and the Alleghanian orogeny, which involved late Mississippian to Permian collision of all previously formed Appalachian crust with Gondwana to form supercontinent Pangea.
The Alleghanian orogeny also involved zippered, north-to-south, transpressional, then head-on collision. Similar coeval orogenies affected western and central Europe (Variscan events), eastern Europe and western Siberia (Uralian events), and southern Britain and Ireland; only the Caledonide (Grampian–Finnmarkian; Caledonian–Scandian) events affected the rest of Britain and the Scandinavian Caledonides.
Missoula is dubbed the Garden City for its mild winters relative to the rest of Montana.