Conifers Archives - Page 6 of 18

June 2, 2019June 3, 2019

Residual Old Growth

Big Trees of the Freshwater Creek Drainage, Humboldt County

Image from Save the Redwoods League Conservation Report (2018).

Old-growth forests are forests that have developed over long periods of time, without experiencing severe, stand-replacing disturbance—a fire, windstorm, or logging. Within the redwood forest belt, of the estimated 1.6 million acres of redwood forest remaining, only 7% is old growth. The remaining 93% is considered some level of second growth. Around Humboldt Bay where we live that number is approaching 99%. The old-growth trees that do remain are often mixed within the second growth forests. Most often, an old tree was left behind by loggers because of imperfections like broken tops or less than optimal heartwood. This post explores some of the residual old growth in my neighborhood.

August 7, 2018August 23, 2020

Klamath National Forest Whitebark Pine

Mapping and monitoring Pinus albicaulis

For the better part of July I was contracted by the Forest Service Region 5, in a partnership with the CNPS Vegetation Program, to follow up with our 2013 work mapping and monitoring whitebark pine in the north state. I visited numerous sites where I predicted Pinus albicaulis might occur to conduct surveys and improve our state-wide range map for the species. Overall, the health of the species in northern California is in slow decline due to a variety of factors including mountain pine beetle, white pine blister rust, global climate change, and recent high intensity fires. In an earlier post, I shared some highlights from the Modoc National Forest, this post shares images and highlights from Klamath National Forest whitebark pine work.

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July 19, 2018

Warner Mountains — whitebark pines and beyond

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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August 25, 2017

Mill Creek Wilderness

The main event has been on the calendar for the past eight years. I have heard stories from friends who have actually traveled around the world to see the phenomenon–and from that alone I knew if there was and eclipse practically in our backyard, we needed to go. We selected a spot in the heart of the Ochoco National Forest and literally on the edge of the Mill Creek Wilderness in a meadow complex. The Mill Creek Wilderness Twin Pillars Trail was our hiking destination the day before the eclipse event. The wilderness protects a harsh environment typified by ancient lava flows, fire-prone conifer forests, and the Mill Creek Drainage itself. We found wonderful views across central Oregon and a fire-scared landscape on our way to the Twin Pillars. In addition, western larch (Larix occidentalis), was the conifer highlight on this adventure.

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April 16, 2017January 9, 2019

Torrey Pine Forest

Santa Rosa Island Torrey pine (Pinus torreyana ssp. insularis)

Torrey pine range map from *Conifers of the Pacific Slope*.

The first time Santa Rosa Island landed on my plant exploring radar screen was when I learned about the Torrey pine some time in the early 2000s. I had never even seen this tree until I took a trip to Torrey Pines State Reserve north of San Diego in early 2012. It is the rarest pine in North America with several thousand “mature” trees on both the mainland and island. My bucket list for understanding the ecology of this species is complete now that I have visited the island.

As mentioned in an early post, pigs were first introduced on Santa Rosa in the mid 1800s. By 1888 it is estimated, based on historical records, that there were only 100 Torrey pines on the island. Today, all herbivorous megafauna have been removed (minus 5 sterile horses from the old ranch) and the Torrey pine are thriving–with an estimated 12,300 trees–one-quarter of which are saplings!

Researchers debate the arrival time of the Santa Rosa Torrey pine, estimating anywhere from 6,000 to over 1 million years. Disagreement also exists as to whether these two population represent subspecies or varieties of each other. Some argue the two populations are genetically different enough to be considered a subspecies, others prefer distinction at the variety level. Regardless, it is a beautiful species and well worth seeing in the wild.

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