Klamath Mountain Peat Bog

Isinglass Lake

On a recent trip into the Marble Mountain Wilderness to map and monitor whitebark pine (Pinus albicaulis) on the Klamath National Forest, I found myself near Isinglass Lake. I had read that the only population of great sundew (Drosera anglica) in the Klamath Mountains was documented here in 1972. I knew there was a Klamath Mountain peat bog to be found.

Klamath Mountain Peat Bog
Isinglass Lake is surrounded by an accumulation of peat, know as a peat bog.
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Warner Mountains — whitebark pines and beyond

Warner Mountains
Conifers of the Warner Mountains. Maps from Conifers of the Pacific Slope.

The Warner Mountains are a north-south trending fault block range in the northeastern corner of California, extending northward into Oregon. The length of the range is approximately 90 miles, with the northern California portion bounded by Goose Lake on the west and Surprise Valley on the east. In California, elevations range between 5,000-9,897 feet (on Eagle Peak). In the High Grade district, which is the extreme northern limits of the Warners in California, the range has a fairly even crest of 7500 feet, reaching an elevation of 8290 feet on Mount Bidwell. This is the area where I spent four days mapping and monitoring whitebark pine (Pinus albicaulis) for the US Forest Service.

The geology of the region is complex and compelled me to understand it better. Bedrock consists of sedimentary rocks of the Oligocene overlain by rhyolitic to basaltic volcanic rocks of the Miocene. The basal andesite is overlain by rhyolite and glassy rhyolite, which are in turn overlain by basalt flows. There are valuable minerals and gems found in this area that have justified a long-standing history of mining. Gold was the first and major extracted mineral soon followed by opals, petrified wood, and even obsidian. The range is a complex assemblage of interesting rocks for sure which help sculpt the regional ecology.

The northern Warner Mountains have a long history of mining.

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Post Eclipse Complex

Siskiyou Wilderness

Eclipse Complex
From InciWeb

It is no secret that the Siskiyous are my favorite place in the Klamath Mountains. I have spent many days and hiked numerous miles across this region. The Bigfoot Trail travels the entire crest of the range as well.

In early August 2017, lightning ignited a series of fires first named Oak, Cedar, Clear, and Prescott. These fires later grew together and were combined into the Eclipse Complex. Over the next month, approximately 100,000 acres burned in and around the Siskiyou Wilderness. Between last October and now I have had reason to visit much of this area for work and play. What follows are some of the pictures I have taken.

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Coastal Lowland Forests

The Klamath Mountains

Coastal lowland forests of the Klamath Mountains. From the future book, The Klamath Mountains: A Natural History.

The coastal lowland forests receive the most annual rainfall of anywhere else in the Klamath Mountains. From the north in Oregon the Coquille, Rogue, and Illinois rivers drain southwest Oregon and the Smith River country is California’s only temperate rainforest. The rich soils, temperate year-round growing season, and high rainfall (often over 100 inches) nurture these impressive forests.

Klamath coastal lowland forests are typified by dense, closed canopies on well-developed soils (sometimes serpentines). The dominant tree species have high colonizing abilities, long life, and a wide ecological tolerances to environmental conditions, including dry summers with occasional persistent fog. These forest thrive below the snow belt on the extreme western slopes of the Siskiyou Mountains. Species like Douglas-fir (Pseudotsuga menziesii) and Port Orford-cedar (Chamaecyparis lawsoniana) secure the highest place in the canopy, often approaching 300’. A second canopy forms one hundred feet below and includes species like tanoak (Notholithocarpus densiflorus) and madrone (Arbutus menziesii) where they share an understory with coastal specialists like salal (Gaultheria shallon) and evergreen huckleberry (Vaccinium ovatum). With the high volumes of rain that falls each winter, banks of coastal rivers and streams are frequently disturbed and then repeatedly pioneered by red alder (Alnus rubra).

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Hell Gate

Botanizing the South Fork National Recreation Trail – Trinity County

Hiking Hell Gate

Hell Gate highlights the lowland interior forest of the southern Klamath Mountains along the Trinity River on the Shasta-Trinity National Forest. The Trinity is surely one of the most spectacular rivers in the state and this hike is along a roadless stretch in the upper reaches of the south fork. The old-growth Douglas-fir/mixed evergreen forest is top-notch, especially along the north-facing sections of trail. Oak woodlands are on benches above the river, with Oregon white oak mixing with picturesque grasslands–though the lack of fire is allowing extensive conifer encroachment. Some of the largest Pacific yew I have ever seen can be found along the trail as well.

The area is dotted with private in-holdings and these beautiful old homes appear at random intervals along the trail. The trail is open to biking and—for these home-owners—OHVs. Swimming opportunities abound and solitude can be easily found, especially in the winter (there are bridges on all major stream crossings). The hike, as written and drawn in Conifer Country, is 7 miles to Smokey Creek but the National Recreation Trail extends the length of this roadless stretch of river—for a total of 15 miles from Hells Gate to Wild Mad Road. The upper reaches of this trail is part of the Bigfoot Trail.

I am highlighting three species below that I found on our hike. One that is a regional endemic, one that reaches it coastal range extension here, and a third that is found across the northern hemisphere. These selections highlight the regional diversity with a biogeographical perspective.

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