river grow to an enormous size: two hundred and fifty feet in height—and from fifteen to more than fifty feet in circumference;[59] the cones or seed vessels are in the form of an egg, and oftentimes more than a foot in length; the seeds are as large as the castor bean. Farther south is another stream, which joins the ocean twenty-three miles from the outlet of the Umpqua. At its mouth are many bays; and the surrounding country is less broken than the valley of the Umpqua.[60]
{246} Farther south still, is another stream called the Klamet. It rises, as is said, in the plain east of Mount Madison, and running a westerly course of one hundred and fifty miles, enters the ocean forty or fifty miles south of the Umpqua. The pine and cedar disappear upon this stream; and instead of them are found a myrtaceous tree of small size, which, when shaken by the least breeze, diffuses a delicious fragrance through the groves. The face of the valley is gently undulating, and in every respect desirable for cultivation and grazing.
The Willamette rises in the President's range, near the sources of the Klamet. Its general course is north north-*west. Its length is something more than two hundred miles. It falls into the Columbia by two mouths; the one eighty-five, and the other seventy miles from the sea. The arable portion of the valley of this river is about one hundred and fifty miles long, by sixty in width. It is bounded on the west by low wooded hills of the coast range; on the south by the highlands around the upper waters of the Umpqua; on the east by the President's
