In 1969 Dale Thornburgh and John Sawyer discovered the first subalpine fir in California and also in the Klamath Mountains. This discovery was made in the vicinity of Russian Peak in what is now the Russian Wilderness. Since that time the species has been found in a total of eight locations in California’s Klamath Mountains and twice in Oregon’s Klamath. One of those Oregon locations is near Mt. Ashland and the other was recently discovered by Frank Callahan to the east in the Red Buttes Wilderness. This second location, in an isolated cirque on the north side of Tannen Peak was my destination–with Frank Callahan as my guide.Continue reading “Subalpine Fir in the Red Buttes Wilderness”
Venturing east on Highway 299 from Humboldt Bay, a stark transition–rarely noticed by travelers–occurs at Berry Summit (2900 ft). Leaving the Coast Range and entering the Klamath Mountains the landscape becomes defined by varied, complex rock types. One of these unusual rock types is known as ultramafic rock or more commonly as Serpentine. In North America, serpentine rock appears at the Earth’s surface most frequently in northwest California. The Horse Mountain Botanical Area (HMBA) is a celebration of the rock and climate that interact to create unique high elevation plant communities. In coastal northwest California, spring has arrived. Allison and I did not want winter to pass us by–we were ready for some snow play. Packing our snowshoes and lunch, we drove to the snow of the HMBA in the Klamath Mountains in less than an hour.
High above the headwaters of the Salmon River and Coffee Creek, the remarkable ascension of Packers Peak is surprising next to the seemingly superlative granite of the Alps. The peak is a pedestal on which to perch, understand, and enjoy the complex Trinity Alps Wilderness that surrounds you. It is a steep climb from Big Flat, at the end of Coffee Creek Road, to reach this vantage point; but if you are willing to climb the nearly 3,000 feet in just under 3 miles, you will be rewarded.
Gaining an understanding of geology and fire ecology
I had often pondered a high and extensive ridgeline in the middle of the Trinity Alps Wilderness from other mountain top vantage points on which I stood–at one point or another–in my adventures in the Klamath Mountains. It took me several years to realize this jagged range had its own name and many years more to actually get to this isolated place. Finally, in October, I climbed my way into the high country known as Limestone Ridge. I had read this extensive ridgeline (over 3 miles long) was one of the best examples of Karst topography in western North America. This summer, the spectacular Marble Mountain was my first introduction to Karst limestone landscape in the Klamath so I assiduously pursued a chance to see more. With those distant images and arresting words burned on my brain I was finally climbing–up–up–up–from Hobo Gulch in the Trinity River Canyon.
In the hinterland of northwest California, the Smith River’s crystal blue waters drain abruptly from the Siskiyou Mountains toward the Pacific Ocean—along the way gouging out sparkling canyons through ancient serpentine rock. High levels of precipitation coupled with serpentine geology have fostered unique plant communities in this region. Because the serpentines soils of the Josephine Ophiolite are rich in heavy metals the ecosystem appears infertile. Seemingly sparse red-rock forests endure in stark contrast to the lush redwood forests of the North Coast Range only a few miles away. But upon closer inspection, the red-rock nurtures plant communities that are species rich and teeming with life. Continue reading “Carnivorous Plants of the Smith River Region ~ Stoney Creek Trail”