Letter from Jane Bartley to Medibel (Meddie) Bartley, dated March 23, 1960, in which she writes about her disappointment with her grades and her upcoming participation in the Cherry Blossom Parade. It includes an envelope, postmarked March 24, 1960.

From abstract: The Piedmont Upland in Maryland, Pennsylvania, and Delaware is about 160 miles long and at the most 50 miles wide. Rocks that underlie the province are the Baltimore gneiss of Precambrian age and quartzite, gneiss, schist, marble, phyllite, and greenstone, which make up the Glenarm series of early Paleozoic(?) age. These are intruded by granitic, gabbroic, and ultramafic igneous rocks. Most of the ultramafic rocks, originally peridotite, pyroxenite, and dunite, have been partly or completely altered to serpentine and talc; they are all designated by the general term serpentine. The bodies of serpentine are commonly elongate and conformable with the enclosing rocks.

Letter from W. H. Louviere to John N. Curlett discussing the need to reduce their money contributions.