. The Cascade Range and Ashland forest reserves and adjacent regions. 392 FOREST RESERVESo moderatel}^ uniform, heavy forest stand, in which yeUow pine largely predominates. The mill timber is of good dimensions and qualit}'-. The forest is fire marked throughout. The sugar pine in the township has been badly culled by shake makers. Agricultural claims have been entered in the heavy timber, the sugar pine fit for shakes cut off, and the entry abandoned. Great quantities of large sugar pine lie rotting on the ground—cut down found to split hard, and rejected. Almost every sugar pine of any cons
. The Cascade Range and Ashland forest reserves and adjacent regions. 392 FOREST RESERVESo moderatel}^ uniform, heavy forest stand, in which yeUow pine largely predominates. The mill timber is of good dimensions and qualit}'-. The forest is fire marked throughout. The sugar pine in the township has been badly culled by shake makers. Agricultural claims have been entered in the heavy timber, the sugar pine fit for shakes cut off, and the entry abandoned. Great quantities of large sugar pine lie rotting on the ground—cut down found to split hard, and rejected. Almost every sugar pine of any considerable size in the township is ax marked, to try its splitting qualities. Forested and other areas in 2\ 35 S., R. 3 E., Oregon. Acres. Forested area 20, 040 Nonforested area (glades and meadow, 1,500; burned, 1,500) 3, 000 Badly burned area 500 Logged area (the sugar pine culled 10 per cent) 12, 000 Total stand of timber vi T. 35 S., B. 3 E., Conqxjsitlon of forest in, T. 35 S., R. 3 E., Oregon, including trees of all species irith hascd diameters of 4 Inches and ujnvard. Per cent. Yellow pine _ 70 Sugar pine 3 Red fir , 20 White fir '. 5 Incense cedar 5 Oaks, etc ... J Township 35 South, Range -i East. This township lies well over on the western slopes of the main range of the Cascades, owing to a curve in the crest line toward the east after leaving Mount Pitt. The western portion of the township consists of a series of low, nar- row terraces parallel to the crest of the range, each terrace appearing to mark the outer rim of successive lava flows. The central and east- ern areas comprise bowlder-strewn slopes rising with an easy gradient toward the Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Leiberg, John B. , 1853-. Washington : Gov't Print. Off.
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