Geologic Trip, Rogue Valley Roxy Ann Peak |
Diabase Dike |
Roxy
Fm |
Payne
Cliffs Fm |
Roxy
Anne Peak (3,576’) is a distinctive landmark on the east side of Medford that
can be seen for many miles in the Rogue Valley area. Although the peak may
look like a volcano, it is not a volcano. The top of the peak is formed from
a thick diabase dike that has intruded the older sedimentary and volcanic
rocks of the Roxy and Payne Cliffs Formations that make up the middle and
lower slopes of the mountain. If Roxy Ann Peak were a volcano, the entire
peak would have been formed from volcanic rocks. The
photograph, right, looks down the southeast ridge of Roxy Ann Peak toward the
rock quarry in the left center of the photograph. The large fractured rocks
in the foreground are from an outcrop of the diabase intrusive at the top of
Roxy Ann Peak. The
diabase is massive, hard, and breaks into large blocks that have resisted
erosion. This hard cap of diabase protects the underlying rocks from erosion
and gives the peak its steep distinctive top. Diabase
and basalt have the same composition, but diabase forms from magma that does
not reach the surface of the earth whereas basalt forms from magma that
reaches the surface, generally as lava flows. The diabase at Roxy Ann Peak
has a K-Ar age-date of 30.8 ± 2 Ma. Roxy
Ann Peak lies within Prescott Park, which is owned by the City of Medford.
The park has a number of trails that offer good access to the peak. The
parking area for Prescott Park is at the gate on Roxy Ann Road, 1.4 miles
north of Hillcrest Rd. (42° 20’ 44’’ N, 122° 47’ 10’’
W). The
Payne Cliffs Formation consists of non-marine sandstone, shale and
conglomerate of Oligocene age. The Roxy Formation consists of volcaniclastic
sedimentary rocks, tuffs, and basalt and andesite lava flows. These rocks
represent the earliest volcanic activity of the Western Cascades in this
area. External Websites City
of Medford:
Prescott Park Brochure ODGM:
Geologic Map, Bear Creek Valley Wikipedia:
Roxy Ann Peak Return to:
Rogue Valley |