In November 2008, I made my first trip to Papoose Lake in the Trinity Alps Wilderness. That trip inspired my first blog post which evolved into Field Notes From Plant Explorations. This first post was more about geology than plants because of the unique geologic character of the Papoose Lake Basin.
This month, almost 15 years later, I returned to Papoose Lake to conduct vegetation surveys as part of our Klamath Mountains Vegetation Mapping Project. In many ways the basin is the same but in others changes are afoot. What follows are some reflections on 15 years of blogging through the eyes of a Klamath Mountain lake basin.
In 2010, I first found this tree while backpacking through the Trinity Alps Wilderness in far northern California. Just last week, thirteen years later, my son Sylas and I returned with tools to officially measure and nominate this tree. While points fell just short of the overall champion, it is the second largest foxtail pine known and the largest of the subspecies of the Klamath foxtail pine (Pinus balfouriana subsp. balfouriana).
As a board member of the Whitebark Pine Ecosystem Foundation, I decided to help cook up this project because all is not well with the five-needle pines of western North America.
Five-needle pines along the Pacific Crest Trail include the sugar pine, limber pine, foxtail pine, whitebark pine, and western white pine. Crucial to the mountain ecosystems where they occur, these trees face an uncertain future, and scientists are trying to learn more.
By participating, you will help increase awareness of the changes affecting our world while improving connections to nature. Working together to document what’s happening is a positive step toward recovery.
I have made more posts about foxtail pines than any other trees and it is thus no secret that my favorite conifer is a five-needle pine. There are a lot of thoughts and details about five-needle pines swirling around in my world these days–for better or worse (fires and climate change)–so I figure I’ll add to the story with some updates here.
“Whether old or young, sheltered or exposed to the wildest of gales, this tree is ever found irrepressibly and extravagantly picturesque and offers a richer and more varied series of forms to the artist than any other conifer I know of.”
The following excerpt is from my book Conifer Country. I was inspired to publish it here after a recent trip with my son to visit and measure the Klamath Mountain champion foxtail pine. After this trip, the foxtail pine is his favorite tree species too 🙂
California’s endemic foxtail pines have established two esoteric populations abscinded by nearly 500 miles of rolling mountains and deep valleys. The species was first described by John Jeffrey near Mount Shasta in 1852 , which was most likely a population near Mount Eddy or in the Scott Mountains. Later, this species was discovered in the high elevations (9,000’-12,000’) of the southern Sierra Nevada. The ecological context of Klamath foxtail pines in the Klamath Mountains differs drastically from that in the Sierra Nevada due to the divergence of these populations in the mid-Pleistocene. Though separated over one million years ago, both subspecies exhibit a radiance and individuality for which I honor them as my favorite conifer.
With separation in space and time, divergence—including cone orientation, seed character, crown form, foliage, and even chemistry—has occurred between the two subspecies. Another reason for these variations are genetic bottlenecks that have been promulgated by spatially restricted microsite adaptations, particularly in the Klamath Mountains . Northern foxtail pines (var. balfouriana) are isolated on sky islands—local mountain tops and ridgelines—from 6,500’ to 9,000’ in the eastern half of the Klamath Mountains. By my count there are 16 isolated sub-populations each consisting of one to several isolated mountain-top populations, except in the Trinity Alps where they are locally common in the more contiguous high elevations. On these sites, proper geologic, topographic, and climatic conditions have offered synergistic alliances with shade-tolerant and faster-growing firs and hemlocks.
Mount Linn–also called South Yolla Bolly Mountain–is the highest point in the Coast Range of northern California. It is located to the west of Corning but the area might as well be a world away from the population centers of the state; it is rarely noticed by travelers as they drive Interstate 5. Once off the interstate, scenic forest service roads still take nearly 2 hours to wind to the trailhead. I revisited this fine mountain in July of 2016 to set up a photo-monitoring plot along the Bigfoot Trail and took the time to also map the vegetation on the mountain–particularly the grove of foxtail pines near the summit. This is one of the smallest (12 acres) and most isolated groves for the entire species and one that I am very much concerned about due to climate change. Shasta firs are encroaching upon the trees as snowpack declines and temperatures warm. I was happy to see the trees doing well and many young foxtails sprouting up–just not as many as there are young firs.
Part two of whitebark pine negative reports in the Trinity Alps Wilderness
As mentioned in my last post, part of last summer’s whitebark pine conservation assessment and mapping project involved predicting location where the species might occur but was not yet documented. While I found success with some predictions, others turned into negative reports with “ground-truthing.” One negative report was in the Trinity Alps Wilderness around Stonewall Pass, another was in the Foster and Lion lakes region where I based my prediction on the significant landmass above 7,500′.
Part of last summer’s whitebark pine conservation assessment and mapping project involved predicting location where the species might occur but had not yet been documented. While I found success with some predictions, others turned into negative reports with “ground-truthing.” One of these areas was in the Trinity Alps Wilderness around Stonewall Pass where I predicted WBP would occur because there is significant landmass above 7,500′.
The geology of the Stonewall Pass region is built from a majority of mafic and ultramafic rocks. Granite and Gibson peaks are themselves granite, but the remainder of the landscape is composed of serpentine, which makes survival difficult for many species. Interestingly, whitebark pine are found on the serpentine of the Scott-Trinity Mountains around China Peak and Mount Eddy, but it turns out they are absent from the Stonewall Pass serpentines. Whitebark’s absence on the granite of Gibson and Granite peak is most likely due to the size of the inhabitable area offered by the small granite plutons here as well as the increased competition from granite-loving species like mountain hemlock and Shasta fir.
Ecological amplitude is the range of habitats, often dependent on and defined by elevation, within which a certain species has the ability to survive. In the Klamath Mountains there are two species of pines that define the highest elevations–growing at or near the summits of peaks from ~7500′ to 9000′ (The Klamath Mountains get no higher). Foxtail pine (Pinus balfouriana) and whitebark pine (Pinus albicaulis) inhabit our sky islands where they are the crowning jewels of this coniferous wonderland.
Box Camp Mountain is interesting for several reasons. The first is that its summit is only 7,267′ yet both species of said pines live in this fringe habitat. This is generally on south-facing slopes where lack of competition from firs and hemlocks (which thrive on north-facing slopes) is minimal. When approaching the summit I began to doubt the reports of these pines being here; but in the last few hundred feet they began to appear. Throughout Holocene warming, these two species (and others) have slowly been retreating up regional mountains. Now, after thousands of years, they have reached their ecological climax on Box Camp–there is no more up on which to grow. This mountain holds the most formidably presumptive story I have attempted to read in a high elevation Klamath landscape–and what I read does not appears to have a happy ending.
Sequoia National Park & Monument • Original Publication DATE: 6/10/2011
Sequoia National Monument – In search of giant sequoia (Sequoiadendron gigantium)
A slow return north from Mexico found me revisiting old stomping grounds in the southern Sierra Nevada. I first drove from Kernville to Springville to fully enjoy the Giant Sequoia National Monument. When I first ventured out on my own after college I lived near Springville and taught environmental education at SCICON. On weekends I would often attend church in the Freeman Creek grove, disappearing for hours on end in one of the largest stands of sequoias outside the national parks. I returned to this grove to re-explore 15 years after my first visits–I think the trees have gotten bigger.
Mount Linn–also called South Yolla Bolly Mountain–is the highest point in the Coast Range of northern California. It is located to the west of Corning but the area might as well be a world away from the population centers of the state; it is rarely noticed by travelers as they drive Interstate 5. Once off the interstate, scenic forest service roads still take nearly 2 hours to wind to the trailhead. Although this place has always been on my list of places to visit–the impetus for this visit was to collect some samples of the rare Sierra juniper (Juniperus grandis) for Robert Adams of Baylor University so that, through DNA testing, he might find out if these trees truly are what we think they are (see previous blog). After a 25 mile sojourn deep into the wilderness to collect those specimens it was time to search for the southern most stand of foxtail pine in northwest California–on Mount Linn.