You'd be wrong to think that just because your old Toyota has a quite a few miles on it exactly means it's lost its value. When you're trying to find the ideal Toyota in for you, you can trust the qualified and experienced representatives at your nearby Toyota dealership to find the right fit for you. 20 years of change on Cooper Spur… and the future?Ĭategories Categories WyEast Words arrowleaf balsamroot Bennett Pass Camp Creek CCC Celilo Falls Clackamas River Climate Change Cloud Cap Columbia Gorge Columbia River Columbia River Gorge Columbia River Gorge National Scenic Area Cooper Spur Dollar Lake Fire Eagle Creek Eagle Creek Fire East Fork Hood River Eliot Glacier Elk Cove FHWA Forest Service Government Camp Highway 26 Highway 35 Historic Columbia River Highway Historic Columbia River Highway State Trail Hole-in-the-Wall Falls Hood River Hood River County Hood River Valley Latourell Falls Laurel Hill logging Lolo Pass Lookout Mountain Metlako Falls Mirror Lake Mount Hood Mount Hood Highway Mount Hood Loop Highway Mount Hood National Forest Mount Hood National Park Campaign Mount Hood National Recreation Area ODOT Old Vista Ridge Trail Oneonta Gorge Oregon State Parks Owl Point Pacific Crest Trail parking poison oak Punch Bowl Falls Rhododendron Salmon River Samuel Lancaster Shepperd's Dell Surveyors Ridge Tamanawas Falls Timberline Lodge Timberline Trail TKO Trailkeepers of Oregon U.S.Know you can trust your local Toyota dealers to give you the quality and professionalism you know you can.Until that day, the area can be explored off-trail, with access from adjacent forest roads. In the long term, the Mount Hood National Park Campaign envisions bringing the L-shaped piece of private land into public ownership, and providing recreational and interpretive access to the area. So for now, this is yet another unique natural feature at risk of development. While this private land is already inside the Mount Hood National Forest jurisdictional boundary, the agency rarely acquires land thanks to lack of dedicated funding or a clear mission on which lands ought to be acquired. Part of the lava flow, along the northeast corner (see map), is on private land. This is where the Parkdale Lava Flow stands today. The Forest Service has designated 854 acres of the Parkdale Lava Flow as a geologic “Special Interest Area” for the stated purpose of “public recreation use, study and enjoyment.” In its forest plan, the agency has committed to managing such areas in a natural condition, pending a detailed implementation plan for each area. Through sheer luck, the flow was never mined for aggregate, despite its proximity to huge construction projects, such as the dams and highways in the nearby Columbia River Gorge. As might be expected, the flow is also home to small wildlife that thrive in the shelter that the jumbled rock provides. Since the eruption 7,000 years ago, a few trees have pioneered the lava flow, mostly along shaded side slopes, but it mostly looks like it erupted very recently. This puts both events within the period when the first Native Americans were living in the region, and we can only imagine how the ensuing chaos must have impacted these early residents. Geologists note that the Parkdale flow overlays traces of Crater Lake ash deposited in the Mount Hood area, suggesting that the lava flowed just after the destruction of Mount Mazama.
The Parkdale Lava Flow falls partly into private ownership That’s 4 million dump truck loads of lava, and when the lava cooled, it covered nearly 3,000 acres to depths as much as 300 feet.
By the time the eruption was over, the lava had traveled more than four miles, and poured more than 390 million cubic yards of molten rock on the surface. Flowing north from a deep fissure at the foot of Mount Hood, the lava first poured down the valley in a single, broad stream, pushing the Middle Fork of the Hood River from its channel.Īs the river of molten rock reached the flats of the upper Hood River Valley, the lava began to spread out from the river channel, with great lobes spilling sideways from the main flow onto the valley floor. But viewed from above, the formation takes on a more recognizable form. the lava flow looks like a ridge of jumbled boulders, with the occasional Douglas fir or ponderosa pine poking out of the chaos. This Google Earth view looks south, from the toe of the Parkdale Lava Flow, toward its origin, at the foot of Mount Hoodįrom the farms near Parkdale.
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