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Fire In The Forests Of Lassen

Burning deadwood to mitigate future fires

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About 70 million years ago, the tectonic plates underlying the Pacific Ocean plunged beneath the North American Plate and began to form the row of volcanoes known as the Cascade Range. Lassen Volcanic National Park crowns the southernmost part of the range in a remote region of northeastern California. The Park is most famous for its spectacular geology, the result of active vulcanism from the ongoing creation of the Cascade Range. The vast majority of the Park’s rock formed within the past three million years as a series of volcanoes rose up and eroded away. Lassen Peak, the Park’s tallest mountain, formed about 27,000 years ago, near the end of the last Ice Age. The Peak hosted the Park’s most recent eruptions from 1914 to 1917. The Park also boasts 17 smaller volcanoes and four mountains remaining along the rim of an enormous eroded volcano. In nine hydrothermal areas, subterranean molten rock heats bodies of water at the Earth’s surface and enriches the soil with otherworldly yellows and reds. The steam and sulfuric stench reminds us that the Park’s history of eruptions is far from over.

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Lassen paintbrush (Castilleja lassenensis) is endemic to montane meadows near Lassen Peak.
Longhorn steer’s-head (Dicentra uniflora)
Sierra bog orchid (Platanthera dilatata var. leucostachys)
Greenleaf manzanita (Arctostaphylos patula)
Seep monkeyflowers (Erythranthe guttata) bloom in the  aftermath of a high-severity burn.
The author (left), fellow sawyer Jake Norman, Turtle (the ax), Thelma (the crosscut saw),  and Pumba (the red fir).
We could see a wall of smoke advancing towards us in Taylorsville after evacuating from Lassen.
A year after the Dixie Fire, I walked through acres of forest that looked just like this: no visible plant life except an occasional flourishing bracken fern (Pteridium aquilinum).
Montane meadows generally flourished in the wake of the Dixie Fire.
Wetlands often stop wildfires at their margins.

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