This part of the House Range is chiefly made up of a passive margin sequence of Cambrian to Ordovician carbonate rocks.
 The top of the range is the type section for the aptly named Notch Peak Dolomite.
 At the base of the range is the pink/orange Notch Peak granite and monzonite, which is Jurassic in age (143 to 169 million years old).
 Around Notch Peak, especially from the west side (Tule Valley side), white Lake Bonneville fossiliferous marls occur.

Because of the intrusion, a hike up the canyon below the notch can clearly show a well-developed metamorphic aureole and even inter-fingering textures between the intrusion and the bedrock.
 Also, small quantities of tungsten and placer gold have been found around the Notch Peak area.
This part of the House Range is chiefly made up of a passive margin sequence of Cambrian to Ordovician carbonate rocks.  The top of the range is the type section for the aptly named Notch Peak Dolomite.  At the base of the range is the pink/orange Notch Peak granite and monzonite, which is Jurassic in age (143 to 169 million years old).  Around Notch Peak, especially from the west side (Tule Valley side), white Lake Bonneville fossiliferous marls occur.
Because of the intrusion, a hike up the canyon below the notch can clearly show a well-developed metamorphic aureole and even inter-fingering textures between the intrusion and the bedrock.  Also, small quantities of tungsten and placer gold have been found around the Notch Peak area.
Notch Peak