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Ore Bin / Oregon Geology magazine / journal - Oregon Department ...

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LEGEND<br />

[',TtJ<br />

_.~C ,<br />

Cascade Volcanic<br />

rocks<br />

UeU<br />

Tyee Formation and<br />

younger marine<br />

sedimentary units<br />

B<br />

Umpqua Group<br />

[(eU:b]<br />

Roseburg Basa t t<br />

[ill]]<br />

Pre-Tertiary<br />

OREGON<br />

CAL I FORN I A<br />

o 10 20 MILES<br />

L . ===::J<br />

20 40 KM<br />

W b---, ~d<br />

Figure 1, Regional geologic map of southwestern <strong>Ore</strong>gon showing Umpqua Group and adjacent<br />

major rock units (modified from Wells and Peck, 1961, and Baldwin, 1976),<br />

Lookingglass Formation: In its type area, southwest<br />

of Roseburg, Baldwin (1974) has subdivided the<br />

Lookingglass Formation into three members: basal conglomerate<br />

and sandstone, middle siltstone and sandstone,<br />

and upper sandstone and conglomerate, Further<br />

south, where the Lookingglass oversteps the pre­<br />

Tertiary, the middle unit becomes coarser; locally, it<br />

pinches out and interfingers with the upper and lower<br />

members. To the north, the Lookingglass, like the Roseburg,<br />

becomes finer grained, and the basal Lookingglass<br />

conglomerate is only locally present, as at<br />

Woodruff Mountain (Figure 2),<br />

Clasts in the Lookingglass conglomerate include a<br />

variety of plutonic and metamorphic rock types apparently<br />

derived from Klamath Mountains terranes, in contrast<br />

to the predominant basalt pebbles in the Roseburg<br />

136<br />

OREGON GEOLOGY, VOL. 42, NO.8, AUGUST 1980

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