This is just one of 12 giant eruptions reported from the area by the Leicester team, who show that intense hotspot magmatism caused
major crustal subsidence, forming the 100 km - wide Snake River Basin.
The tenement covers 83 square kilometres encompassing approximately 15 kilometres in strike length of the Jenkins Fault Zone,
a major crustal feature that is considered to be a significant influence on the origins and emplacement of the DeGrussa mineralisation.