The type specimen was part of a collection compiled by Jay O'Leary, who was then a student of
Harvard College, in 1954 from the west bank of the
Columbia River near
Vantage, Washington. The petrified woods of the area are preserved in an interbed area between the older
Grande Ronde Basalt and the younger
Wanapum basalts, with the interbed overlain by the Ginkgo Flow, the oldest segment of the Frenchman Springs Member of the Wanapum basalts.
K–Ar dating performed on the Grande Ronde Basalts gives an age of 15.6 million years old, and dating of the Frenchman Springs Member gives a date of 15.3 million years old. This places the
vantage woods as from the
Langhian stage of the
Miocene. Mean annual temperature estimates for the vantage paleoclimate were made based on analysis of the fossil wood. Based on a series of wood anatomy characters, a temperature range between . This is distinctly warmer than the modern mean annual temperature of . == Taxonomy ==