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The Cascade mountain system extends from northern California to central British Columbia. In Oregon, it comprises the Cascade Range, which is 260 miles long and, at greatest breadth, 90 miles wide (fig. 1). Oregon's Cascade Range covers roughly 17,000 square miles, or about 17 percent of the state, an area larger than each of the smallest nine of the fifty United States. The range is bounded on the east by U.S. Highways 97 and 197. On the west it reaches nearly to Interstate 5, forming the eastern margin of the Willamette Valley and, farther south, abutting the Coast Ranges.

Along its Oregon segment, the Cascade Range is almost entirely volcanic in origin. The volcanoes and their eroded remnants are the visible magmatic expression of the Cascadia subduction zone, where the offshore Juan de Fuca tectonic plate is subducted beneath North America. Subduction occurs as two lithospheric plates collide, and an underthrusted oceanic plate is commonly dragged into the mantle by the pull of gravity, carrying ocean-bottom rock and sediment down to where heat and pressure expel water. As this water rises, it lowers the melting temperature in the overlying hot mantle rocks, thereby promoting melting. The molten rock supplies the volcanic arcs with heat and magma. Cascade Range volcanoes are part of the Ring of Fire, a popular term for the numerous volcanic arcs that encircle the Pacific Ocean.
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Western Cascades and High Cascades

In Oregon, the Cascade Range is customarily divided into two physiographic subprovinces, the Western Cascades and the High Cascades (fig. 1). The Western Cascades, or Old Cascades in some tourist logs, encompasses volcanic rocks as old as 45 million years. It is a deeply eroded subprovince. West-flowing and northwest-flowing streams have carved canyons as deep as 3,700 feet, measured from adjacent ridgetops to canyon floors.

In contrast, the High Cascades subprovince is little eroded. This distinction arises for two reasons. First, broad uplift of the Western Cascades sometime after 8 million years ago created steep rivers that propelled erosional downcutting. Second, at about that time, volcanism was focused along the axis of the High Cascades, filling old canyons and building up the spine of the range. The Western Cascades subprovince, with only sparse small volcanoes active in the past four million years, was spared the periodic infilling of its canyons by extensive volcanic deposits. Consequently, streams were able to erode unabated, deepening and broadening their courses and continuing to create relief in the Western Cascades.

The High Cascades in Oregon are coincident with the currently active volcanic arc, a nearly continuous band of large, long-lasting volcanic centers and smaller volcanoes, cinder cones, and lava domes. Nearly all of these have been active since four million years ago. To the casual observer, many of the smaller vents and volcanoes are merely bumps on the landscape. Better known are the prominent pinnacles of the glaciated shields or stratocones, such as Three Fingered Jack, Mount Washington, and Mount Thielsen and also the smoother slopes of the less-eroded Mount Bachelor and Mount. McLoughlin.

But the crowning glories of the Oregon Cascades are the major volcanic centers- Mount Hood, Mount Jefferson, the Three Sisters, and Crater Lake, which sits in the caldera created by the eruption of Mount Mazama ( table 1). These major centers are set apart by their longevity and overall size (though not necessarily their present-day height). Volcanic activity at the major centers has persisted for many thousands of years, whereas the lesser volcanoes flare and go extinct more quickly, over spans of many months to centuries (fig. 2). The major centers, with their longer life spans, develop diverse magmatic systems whose eruptive products can span the entire compositional range from basalt to andesite, dacite, and rhyolite. The hot subterranean environment for the long-lived centers is thought to host the major part of Cascade-related geothermal resources.

In terms of morphology (terrain aspects), the Oregon Cascade Range differs from that in Washington State. In Washington, the active volcanic arc is composed chiefly of isolated large volcanoes that have been built on ridgetops of substantially older bedrock, amid deeply eroded canyons. In contrast, the volcanically active part of the Oregon Cascade Range is almost entirely young volcanoes along the entire chain. The major centers in Oregon are embedded in and superimposed on a broad constructional landscape composed of volcanic rocks thousands of feet thick. The Oregon High Cascades presents, overall, a less rugged alpine landscape than its Washington counterpart.
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Numerous glacial episodes have iced over the Oregon Cascade Range during the past two million years. The most recent glacial maximum was about 20,000 years ago, when ice formed a continuous cap from north of Mount Jefferson southward to Mount McLoughlin. At that time, lobes of ice descended into the major river valleys along the west side of the range, reaching as low as 2,000 feet in altitude in the North Santiam and McKenzie River drainages. Glacial ice is dynamic, pulled downslope and down valley by gravity, and rock debris shed from canyon walls is carried along a glacier's margins or transported to its snout. Upon full meltback, ridges of debris outline the past extent of glaciers in the form of lateral and terminal moraines. One consequence is moraine-dammed lakes, such as Crescent, Odell, Cultus, Miller, and Suttle Lakes, all of them popular for fishing, boating, and swimming.

The few glaciers today in the Oregon Cascade Range exist only on high volcanoes such as Mount Hood, Mount Jefferson, and the Three Sisters. For several millennia these glaciers have grown and shrunk in response to climate change. The last episode of growth, referred to as the Little Ice Age, culminated in the late nineteenth century. Its ice advance was limited in extent and did not form a continuous ice cap, but it still left small distinct moraines poised above about 6,800 feet, just a few hundred feet below the toes of still-visible glaciers on the highest Cascade peaks.
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Cascade Range Divides the State

Nothing divides a state like a major mountain range, and the Cascade Range has been a notable barrier. Exemplary of mountain-as-barrier is the contrast of Oregon's wetter west side and drier east side. Moisture-laden air streaming from the Pacific Ocean cools as it ascends the west flank of the Cascades. Cloud formation is a consequence-the well-known orographic effect-commonly leading to rain or snow. West-flank precipitation in the Cascade Range increases upslope to more than 130 inches (3.3 meters) a year at the Cascade crest (fig. 3), whereas the eastern flank and most of the state's east side receive less than 20 inches (0.5 meter) in yearly precipitation. This precipitation gradient persists but is less dramatic in the southern part of the Cascade Range, owing to storm paths but also because the Klamath Mountains (part of the Coast Ranges) expand the breadth and average height of the coastal mountains and wring more moisture from incoming weather systems than the lower and narrower Coast Range farther north.

Vegetation zones follow the precipitation patterns. Climax forest in much of the Western Cascades is western hemlock (fig. 3), a zone that hosts the preponderance of Oregon's Douglas-fir timberlands. In the southern part of the Western Cascades, with less precipitation east of the Klamath Mountains, the same longitudinal zone is characterized by needleleaf-broadleaf forest. Upslope, each of these zones yields to subalpine forests of mountain hemlock, Pacific silver fir, and subalpine fir before passing into rocky alpine zones above the timberline. Downslope on the drier eastern flank, the Cascade Range vegetation is characterized by a forest zone of chiefly ponderosa pine (fig. 3).

River capacity is another response to the orographic effect. For example, streams originating on the west flank of the Cascade Range, in their combined output, transport roughly ten times greater flow than east-flank streams. West-flank streams in the southern part of the Oregon Cascade Range, such as the Rogue, South Umpqua, and North Umpqua Rivers, find their way directly to the ocean by cutting west through the coastal mountain system. Farther north, however, by about the latitude of Eugene, westside Cascade streams begin coalescing into a single major river, the Willamette, which flows north into the Columbia. In many ways the Willamette River is a Cascade Range stream. It gains about 20 percent of its stream flow from Coast Range tributaries, but most of its water comes from Cascade sources: Middle Fork Willamette, McKenzie, South Santiam, North Santiam, and Clackamas Rivers. The Cascade tributaries to the Willamette have about four times the drainage area as Coast Range tributaries.

Eastside streams of the Cascades in Oregon coalesce into the Deschutes and Klamath Rivers. Tributaries to this pair of rivers share a topographic divide just north of Chemult. Streams of the Deschutes river system flow broadly north from there to join the Columbia, whereas the Klamath River flows south and then west to the Pacific. The Klamath River is exceptional for cutting completely across the Cascade Range. It penetrates through the mountains west of Klamath Falls, then winds through northern California to the Pacific Ocean.

Most notable of trans-Cascade rivers is the Columbia, which traverses the range at the latitude of Portland. The path it crosses is not coincidence but is an area that has been topographically low many times in the geologic past. For example, voluminous lava flows of the Columbia River Basalt Group, erupted from dikes in northeast and southeast Oregon and southwest Idaho, flooded through low points in the same broad stretch of the Cascade Range between 17 and 12 million years ago. These lava flows buried the area of present-day Portland and the northern Willamette Valley while spreading westward to reach the Pacific Ocean.

Across-Range Traverses

The geology of the Columbia River through the Cascade Range has shaped human history as well. The Columbia was a travel corridor for Native peoples for millennia. It played prominently in oral traditions that predate European contact, carving the broad gorge between Cascade volcanoes Mount Hood and Mount St. Helens. In the early 1800s, Meriwether Lewis and William Clark followed the river westward on their journey of discovery. Since then, the Columbia River has been the chief corridor for people and goods traveling across Oregon by road, rail, or barge, owing to the comparatively easy transect provided by the river's valley.

But the free-flowing Columbia River of the past, with its narrow gorge and hazardous rapids, was a challenging route across the Cascade Range. Native American trails and then stage and wagon roads provided crossings farther south, such as the Barlow Road, Santiam Pass, and Willamette Pass. Seven of those roads were well traveled by 1890, and two trans-Cascade highways were surfaced by 1930-the Columbia River Highway and the road to Crater Lake (fig. 4). The Crater Lake road, more or less along today's Oregon Highway 62, traversed the upper Rogue River valley, crossed the summit south of the lake, and continued east to Fort Klamath. By 1950, the paved-road system of highways across the Cascade Range looked much as it does today. As might be expected, Oregon's greatest across-Cascade average daily vehicle traffic now crosses on Interstate 84, constructed in the 1970s through the Columbia River Gorge.

Railroads first crossed the Cascade Range in 1882 along a path down the Oregon side of the Columbia River from The Dalles to Portland. Five years later, the first Oregon-California railroad was completed west of the Cascade Range, over Siskiyou summit (similar to the route of Interstate 5). But not until 1926 was the second of Oregon's across-Cascade rail lines finished, the route from Eugene to Klamath Falls (fig. 4). This trackage follows the Middle Fork of the Willamette River from Eugene to Oakridge, a route paralleled today by Oregon Highway 58.

Continuing southeast from Oakridge, the rail line makes two large hairpin turns while ascending to about 4,800 feet altitude, where trains slip into a 3,700-foot-long tunnel. Few hikers on the Pacific Crest National Scenic Trail are aware that diesel locomotives rumble 100 feet beneath them at the mountain crest just south of Willamette Pass. The tunnel daylights east of the crest on the south side of Odell Lake, at the old Cascade Summit siding. Although used mainly by freight trains, the route is also used by Amtrak's Coast Starlight, which carries passengers along the Eugene-Klamath Falls alignment across the Cascade Range.
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Natural Resources

The main economic resource extracted from the Cascade Range has been timber from privately held tree farms and federal forestlands (fig. 4). The expansion of population and transportation routes southward through the Willamette Valley and beyond during the early to mid-1900s spurred the growth of mill towns in valleys along the Cascade Range. Timber harvests peaked in the 1970s to mid-1980s, but management decisions thereafter reduced the availability of land for timber production from federally managed sources. Consequently, Cascade Range timber harvests, which were taken largely from national forests, plunged dramatically, with a devastating effect on many timber towns. Enhanced tourism and recreation have never come close to matching the economic value once created by the timber harvests of the twentieth century.

The Cascade Range provides opportunities for sightseeing, hiking, camping, fishing, boating, hunting, skiing, and snow play. Visitation at Oregon's sole national park, Crater Lake, averages about a half-million people per year. National forest visits, which occur across a much larger area, are ten times more numerous, with annual visitation in the period around 2012 at about 5.3 million for the Oregon Cascade Range national forests combined. Nearly one-third of those visits were for winter skiing at resorts near Mount Hood and Mount Bachelor. Oregon residents make the greatest use, by far, of recreational opportunities in the Oregon Cascade Range. After accounting for visitors from southernmost Washington or northern California, only 15 to 20 percent of forest visits originate from other states, and foreign visitors are only one percent or so.

Geologic resources have seen only miniscule extraction from Cascade Range areas. The industrial products, chiefly sand and gravel, are located too far from population centers to warrant production for more than local use. Precious metals (e.g., gold, silver) and base metals (copper, molybdenum, lead, zinc) were mined in the late 1800s and early 1900s at a few Western Cascades localities where small igneous intrusions, all older than about eight million years, led to localized hydrothermal enrichment of ore in quartz vein deposits. These intrusions are probably the ancient roots of large volcanic systems, exposed today by the uplift and deep erosion of the Western Cascades. At several sites, the economically viable part of the deposits has been mined out, although changing technology leads to sporadically renewed interest where mineral resource potential still exists. Erosion and stream sedimentation have stripped and redeposited some ores in stream-terrace deposits downstream from the host sites. The resulting placers are also mined, but mainly as recreational activity.

Geothermal resources became an attractive promise in the western U.S. following the oil embargoes of the 1970s. Although the active volcanic systems of the Cascade Range have always been targets, assessing their geothermal resource potential has proven difficult. Abundant precipitation along the range crest plays havoc on the distribution of surface heat flow from magmatism in the High Cascades. Despite focused volcanism in the High Cascades, hot springs are found almost exclusively in the Western Cascades. Paradoxically, heat flow is substantially higher in the High Cascades than in the Western Cascades, but the deluge of precipitation literally washes magmatic heat down through the permeable lava of the young volcanic rocks. Heated water is shunted in aquifers to a few springs in the Western Cascades, such as Austin, Breitenbush, McCredie, Kitson, and Umpqua hot springs. These springs form a crude north-south lineament, as if aligned along some fundamental Earth structure. But their locations all lie at altitudes between about 2,500 and 3,500 feet on floors of major valleys, where deep canyons have cut into groundwater aquifers sourced in or near the High Cascades. From year to year, geothermal energy exploration is moderated by the cost of energy produced by other methods.

Surface water resources of the Cascade Range are managed for flood control, hydropower, irrigation, and recreation. Segments of the Willamette River's main tributaries were dammed during the mid-twentieth century by the U.S. Army Corps of Engineers, chiefly for flood control. Reservoirs behind eight of those dams have hydropower-generating capacity, with additional hydropower from commercial operations on reservoirs, forebays, penstocks, and powerhouses on the Clackamas, North Umpqua, Rogue, Klamath, and Deschutes Rivers. Together, these systems have a capacity of about 1.48 gigawatts (GW), similar to single Columbia River dams at The Dalles (1.8 GW) or Bonneville (1.1 GW). Just over 30 percent of the Cascades-based capacity is from the three dams in the Deschutes River hydropower system.

Throughout the Cascade Range, the number of dams may decrease in the future, especially where dams were built as part of federally issued long-term leases. Each lease renewal requires dam improvements for enhanced fish passage and other river-management aspects, the modifications for which often exceed the expected investment returned from power generation. Although the Marmot and Little Sandy dams of the Sandy River hydropower system were removed in 2007-2008, several dams were relicensed recently, and diminished future snowpacks as a likely consequence of climate change may increase the importance of dams for water storage.

Watersheds in the Cascade Range produce high-quality drinking water. Famous among them is the Bull Run watershed on Mount Hood, which once supplied all of Portland's water needs (the Columbia well field now augments Portland's water supply in low-flow months). Water from Bull Run is low in dissolved minerals and meets or exceeds all drinking water-quality standards as measured at the entry point to the distribution system. Quality is so high that the city does not filter the water but disinfects it to remove naturally occurring microorganisms.

Rugged, diverse, and dynamic, the Oregon Cascade Range provides a fitting backdrop for forest production, recreational activities, and surface and groundwater resources that serve Oregon and the nation.
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The Cascade mountain system extends from northern California to central British Columbia. In Oregon, it comprises the Cascade Range, which is 260 miles long an...

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This includes climate, geology, wildlife and plants.

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Cascade Range

Geology

Topography

The Cascade Range lies in the United States with sections extending into Canada. The mountains are 1,100 km long and begin at British Columbia in Canada, stretch through Washington (see Washington hikes) and Oregon, and reach an end in Northern California.

The small section of the range that lies within Canada is known as the Canadian Cascades.

The Cascades contain many volcanoes, the tallest ones are known as the High Cascades with most of them towering over the surrounding mountains.

The northern reaches of the range are more rugged and support glaciers. While the mountains don't reach extreme heights in this section of the Cascade Range, the valleys are quite low and deep, resulting in excellent relief.

There is only one major break in the Cascade Mountains outside of Canada: the Columbia River Gorge. The Columbia River cut through the mountains over millions of years, thereby creating the gorge and exposing the distorted layers of basalt that were uplifted from the Earth's crust.

Climate

Wildlife and Plants

Regions In Cascade Mountain Range

North Cascades

High Cascades

The High Cascades make up the rest of the Cascade Range all the way from Mount Rainer, in Washington, through the state of Oregon, until Lassen Peak in Northern California.

The mountains in this region are of volcanic origin, having built up from lava and volcanic debris over many years.

A chain of lava domes, long-lasting volcanoes and cinder cones make up the High Cascades. Sitting on the Pacific Ring of Fire, this region of the Cascade Range has been volcanically active for several million years.

Mount Rainier

Mount Baker

Mount St. Helens

Mount St. Helens is another active stratovolcano in Washington and has an elevation of 2,549 meters. It has the most thermal activity out of all the volcanoes in the Cascade Range and is famous for its pyroclastic flows and ash explosions.

Mount Hood

Mount Hood is a stratovolcano that is considered to be potentially active. Its height has varied over the years due to the amount of snow on its peak. The most recent estimation puts the mountain at a height of 3,429 meters.

It is the highest peak in Oregon and although it is thought to be the volcano most likely to erupt in the state, the chances are very slim so it is generally considered to be dormant. Mount Hood supports a dozen named snow fields and glaciers, the majority of which are over the 1,800 meter level.

For one of the best views of Mount Hood head on one of the hikes near Portland.

Mount Adams

Notable Hikes in the Cascades

The Cascade Range is home to many hiking trails and national parks to explore along its vast lengths. From forested walks around the lower slopes to steep trails leading to glaciers in the higher reaches of the mountains, there is a trail for everyone to enjoy.

See more hikes in San Diego and Southern California hikes.

Here are some notable hikes in the Cascade Range.

Palmer Glacier Hike

Easy Pass Hike

Although its name might suggest otherwise, the hike to Easy Pass is quite a strenuous journey.

It is a 7.4 mile round trip hike that leads you up a short, but steep trail across rocky meadows and talus slopes until you get to Easy Pass.

The hike to the pass offers hikers the chance to see stunning views over Fisher Basin and to the Black and Fisher Peaks towering over the land.

Copper Ridge Loop

Cascade Pass Hike

The hike to Cascade Pass is a great 12 mile long day hike that is only open in the summer months.

This is one of the most popular trails in the North Cascade National Park.

It's quite a steep hike with an elevation gain of 4,000 feet. The Cascade Pass trail is also great for wildlife viewing.

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Cascade Range - The Pacific Ring Of Fire Volcanoes

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Cascade Range is a mountain range along the Pacific Ring of Fire, running from British Columbia to California with multiple volcanoes.

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Lots of animals live in the natural areas surrounding the Cascade Loop. What you see during your trip will depend on the season, time of day, weather, and how far from the roadway you explore. Animal behavior varies. Watch for signs of wildlife: tracks, scat, signs of feeding, burrowing and in some cases, rubbings on trees.

Enjoy looking for and photographing wildlife but be alert and safe! Do your research before heading out. Keep a safe distance from all wildlife, do not attempt selfies with critters, and do not offer them your food.

A few animals/mammals tend to generate the most questions and interest among Cascade Loop travelers. Take a peak at the links below for some additional info:

Sources: Wildlife of the Pacific Northwest-David Moskowitz, National Wildlife Federation, Methow Subbasin Wildlife Assessment and Inventory-Northwest Council, 2004, Washington Department of Fish and Wildlife

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Lots of animals live in the natural areas surrounding the Cascade Loop. What you see during your trip will depend on the season, time of day, weather, and how far

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Learn about the species that live inCascade Range!

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Safety - North Cascades National Park (U.S. National Park Service)

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Wildlife Hazards

North Cascades National Park Service Complex contains a wide variety of wildlife species, as well as the opportunity to view animals in their natural setting. Always enjoy wildlife from the safety of your car or from a safe distance. Do not approach wildlife.

Feeding, harassing, or molesting wildlife is strictly prohibited and subject to fine. Bears, mountain lions, mountain goats, or any other species of wildlife can present a real and painful threat, especially females with young.

You must stay at least 100 yards (91 m) away from bears and wolves and at least 25 yards (23 m) away from all other large animals, including elk, mountain goat, deer, moose, and coyotes.

Learn more about bear safety.

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Wildlife Safety - North Cascades National Park (U.S. National Park Service)

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Learning about wildlife hazards before your visit can help you have a safer and more enjoyable experience.

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Backcountry safety for hikers and backpackers in the Pacific Northwest

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Cascade Range, segment of the Pacific mountain system of western North America. The Cascades extend northward for more than 700 miles (1,100 km) from Lassen Peak, in northern California, U.S., through Oregon and Washington to the Fraser River in southern British Columbia, Canada. Many peaks exceed 10,000 feet (3,000 metres), including Mount Hood (11,235 feet [3,424 metres], highest point in Oregon) and Mount Rainier (14,410 feet [4,392 metres], highest in Washington and in the Cascade Range). Most of the summits are extinct volcanoes, but Lassen Peak (10,457 feet [3,187 metres]) and several others have erupted in the recent past. Mount Baker (10,778 feet [3,285 metres]) steamed heavily in 1975, and Mount St. Helens (8,365 feet [2,550 metres]) erupted in 1980 and again in 1981. The mountains lie 100 to 150 miles (160 to 240 km) inland from the Pacific Ocean and east of the broad depressions known as the Puget Sound Lowland and the Willamette Valley, which separate the moist coastal region from the arid interior. They are continued by the Coast Mountains of British Columbia to the north and the Sierra Nevada to the south.

Marked by glaciation (which has formed many lakes) and stream dissection, the mountains are a headstream region for the Willamette River. Except for the peaks lying above the timberline, the entire range is heavily wooded and is within conservation areas and national forests. The western slope, fed by up to 100 inches (2,500 mm) of precipitation yearly, has dense stands of Douglas fir trees. North Cascades, Mount Rainier, Crater Lake, and Lassen Volcanic national parks, as well as Lava Beds National Monument and Manning Provincial Park (Canada), offer unusual natural formations and magnificent scenery. Tourism, outdoor recreation, and water for hydroelectric power, irrigation, and industry are the main activities and assets of the range.

The English navigators George Vancouver and William R. Broughton saw the Cascades in 1792. The American explorers Meriwether Lewis and William Clark, on their expedition to the northwest in 1806, passed through the range in the 4,000-foot- (1,219-metre-) deep Columbia River Gorge on the Washington-Oregon border. The range was named for the great cascades found near the gorge.

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Cascade Range | mountains, United States

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Cascade Range, segment of the Pacific mountain system of western North America. The Cascades extend northward for more than 700 miles (1,100 km) from Lassen Peak, in northern California, U.S., through Oregon and Washington to the Fraser River in southern British Columbia, Canada.

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Cascade Range is a 1,130 kilometers long mountain range running from Canada's British Columbia through the U.S. states of Washington and Oregon to Northern California. It is a major mountain range of Western North America.

Mount Rainier is the highest peak in this mountain range. Many peaks in the range exceed 3,000 meters in height. Most of the summits are extinct volcanoes. They are part of the Pacific Ring of Fire. The small part of the range in British Columbia is called the Canadian Cascades or Cascade Mountain.
Quick Facts: -

The English navigators George Vancouver and William R. Broughton were the first to see the Cascades in 1792.

The Cascade Range has had a major influence on the climate, agriculture, population, economy etc.

Alexander Ross was the first European explorer to cross the North Cascade's peaks while looking for a trade route.

In North Cascades, there are more than 300 glaciers. It is equal to one-third of all glaciers found in lower 48 states in the US.

The tallest volcanoes of the Cascades are called the High Cascades and dominate their surroundings.

This mountain range is best known for its tall volcanoes and dense evergreen forests.

The Cascade Range is a part of the American Cordillera. It is a chain of mountain ranges.

There are many lakes in the mountain range but Crater Lake is the most famous one.

Precipitation is substantial because of the proximity of this mountain range to the Pacific Ocean.

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Fun Facts for Kids about Cascade Mountain Range

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Cascade Range is a 1,130 kilometres long mountain range running from Canada's British Columbia through the U.S. states of Washington.

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A Field Guide To Edible and Medicinal Mushrooms of the Pacific Northwest · iNaturalist

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A guide to the wild edible fungi and medicinal mushrooms found in the Pacific Northwest region of North America: British Columbia, Washington, Oregon and Northern California.

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Top 20 Most Common Toxic or Poisonous Mushrooms in Oregon - Picture Mushroom

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Gather round, fungi enthusiasts! Nestled amidst the United States' Pacific Northwest, Oregon is known for its lush, cool climate and diverse terrain, creating an ideal habitat for mushroom propagation. Our guide, 'Top 20 most common poisonous mushrooms in Oregon,' focuses on teaching you to safely forage while steering clear of the toxic species commonly encountered in this region.

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In recent years - and 2020 is no exception - parts of the Pacific Northwest that are typically too wet to burn are experiencing more frequent, severe and larger wildfires due to changes in climate. New research from Portland State University found that while the increased wildfire activity is causing widespread changes in the structure and composition of these mid-to-high elevation forests, the new landscapes are likely to be more resilient to projected upward trends in future fire activity and climate conditions.

The study, led by PSU graduate student Sebastian Busby, examined temperate forests that burned expansively, severely and repeatedly between 2003 and 2015 in the central Cascade Range of Oregon and Washington. On Mt. Adams, these wildfires included the 2008 Cold Springs, 2012 Cascade Creek and 2015 Cougar Creek fires. On Mt. Jefferson, the wildfires included the 2003 Booth and Bear Butte Complex, 2007 Warm Springs Area Lightning Complex and 2014 Bear Butte 2 fires. Some areas Busby studied have burned again this summer as part of the Lionshead fire in the Mt. Jefferson area.

Busby said that historically, wet and cool climate limited fire events in these humid forest environments to an interval of 50 to 200-plus years. But climate change has led to warmer winters, reduced mountain snowpack and longer, drier summers and fire seasons. The time between repeated wildfire events in this study was less than 12 years.

"These forests are drying out earlier in the year, making them more vulnerable to frequent, severe and larger wildfires," Busby said. "Because these forests have not historically burned very often, they're composed of high densities of tree species that are not well-adapted to frequent and very large severe fires."

True firs were the dominant conifer tree species across the study areas, but post-fire tree regeneration was generally very poor due to a lack of live mature trees remaining after the fires to reseed the forest.

The burned areas, however, did support the establishment of pines at a low density, which are functionally better adapted to fire. The findings suggest that in the near term, these forests may transition from a dense fir-dominated conifer forest into a patchy, low-density, pine-dominated forest that will likely lack the fuel connectivity conducive to crown fires. Busby said that while widespread forest composition change and forest cover loss may be alarming, the results indicate that the altered structure and composition are likely to be more resilient in the face of future fire and climate conditions, such as drought and heatwave events.

"From an ecological point of view, these reburned forests are going to have a greater abundance of tree species that are better adapted to fire and potentially have less flammable forest structure overall," he said. "Now, in these post-reburned forests that are growing in a warmer and drier world, it will be up to us to decide whether we let future fires burn or not."

If forest managers and other stakeholders choose to suppress them, they risk returning these forests to their historical dense structures, which thrived in cool and wet climates. However, under ongoing warming conditions, this alternative might increase the likelihood of severe and expansive fires in the future, negatively impacting human life, property, and natural resources.

"Wildfires are a natural ecological process on these landscapes and have been for thousands of years," Busby said. "Wildfire can be a great catalyst for change, but that change doesn't have to be entirely negative. We must learn to co-exist with wildfires, use them effectively, and embrace the positive elements they bring to our regional forests and ecosystems."

The findings are published in the journal Ecosphere. Busby's co-authors are Andrés Holz, associate professor of geography at PSU, and Kevan Moffett, assistant professor of environmental hydrology at Washington State University-Vancouver.

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Driven by climate, more frequent, severe wildfires in Cascade Range reshape forests

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In recent years - and 2020 is no exception - parts of the Pacific Northwest that are typically too wet to burn are experiencing more frequent, severe and larger wildfires due to changes in climate.