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Little Chetco River

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The Chetco River is a 56-mile-long (90 km) stream located in the southwestern portion of the U.S. state of Oregon . It drains approximately 352 square miles (912 km ) of Curry County . Flowing through a rugged and isolated coastal region, it descends rapidly from about 3,200 feet (975 m) to sea level at the Pacific Ocean . Except for the lowermost 5 miles (8 km), the river is located entirely within the Rogue River – Siskiyou National Forest . The river rises in the Kalmiopsis Wilderness , northwest of Chetco Peak at the junction of the Oregon Coast Range and the Klamath Mountains . It flows generally north, west, and then southwest, before emptying into the ocean between Brookings and Harbor , approximately 6 miles (10 km) north of the California state line. The Chetco River's watershed remains largely undeveloped, protected by the Rogue River – Siskiyou National Forest and the Kalmiopsis Wilderness. The upper 45 miles (72 km) of the river have been designated Wild and Scenic since 1988.

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65-791: The Little Chetco River is a tributary of the Chetco River in Curry County in the U.S. state of Oregon . Its headwaters lie in the Kalmiopsis Wilderness near the border with Josephine County west of Cave Junction . It flows generally northwest through the Rogue River – Siskiyou National Forest in the Klamath Mountains . The named tributaries of the Little Chetco River are, from source to mouth, Hawk Creek, which enters from

130-626: A log raft consisting of around 1,000 logs. The impact of the raft severely damaged the Hawthorne Bridge , closing it for a year. At 12 feet (3.7 m) above flood stage, the flooding of the Willamette River at Portland in 1964 was second only to the 1948 flood that wiped out Vanport City . At its peak, the water was at the top of Downtown Portland's seawall . Salem Memorial Hospital (now Salem Health ) had to be evacuated after waters from nearby Shelton Ditch and Mill Creek flooded

195-653: A 44.5-mile (71.6 km) stretch of the Chetco River was designated a National Wild and Scenic River , from its headwaters to the boundary of the Rogue River – Siskiyou National Forest. In a court case in 1994, the Chetco was determined to be navigable. In 2002, over 500,000 acres (202,000 ha) of the eastern portion of the watershed and surrounding regions were destroyed in the Biscuit Fire . Originally five separate fires, it

260-568: A massive volcanic arc erupted on the Klamath microcontinent, binding the islands together in a single block. The Klamath microcontinent went through a period of intense tectonic activity known as the Siskiyou orogeny roughly 170 to 165 million years ago. The process was strong enough to force sedimentary rocks deep into the Earth's crust , melting them into large plutons of granite, which rose slowly to

325-584: A tributary of the Rogue River , to the north and east. The Chetco River watershed is covered primarily by temperate coniferous forest , which includes species such as Douglas fir , western hemlock , white fir , Port Orford cedar , California incense cedar , and Sitka spruce . Jeffrey pine , knobcone pine , and golden chinquapin have also been identified. Hardwoods including tanoak , bigleaf maple , red alder , and Pacific madrone are common. Manzanita , hazelnut , vine maple , western skunk cabbage , and multiple species of berries and grasses make up

390-494: Is between 400 and 100 million years old, the oldest rocks in Oregon. The Klamath microcontinent was originally located beneath the ocean near southern California before separating hundreds of millions of years ago. Plate tectonics pushed the microcontinent north, and bits of granite , sea floor sediment, subduction zones , and coral reefs gradually accreted into small islands. Between 212 and 170 million years ago,

455-512: Is collected from rain, and 30 percent from rain on snow. Twenty-five separate wetlands totaling 93 acres (38 ha) have been identified in the watershed. Temperatures average between 32 and 82 °F (0 and 28 °C), although the Brookings effect (or Chetco effect; similar to a foehn wind ) often brings localized hot weather to the Brookings area. The increase in temperature is caused by

520-520: Is home to the rare Wolf's Evening Primrose . Notes References Books News articles Websites Other Pacific Northwest flood of 1964 The Christmas flood of 1964 was a major flood in the United States' Pacific Northwest and some of Northern California between December 18, 1964, and January 7, 1965, spanning the Christmas holiday. Considered a 100-year flood , it

585-500: Is located near the south bank of the Chetco at RM 15 (RK 24), about 8 miles (10 km) north of the California border. Trees here are around 300 to 800 years old, 5 to 13 feet (2 to 4 m) in diameter, and some exceed 300 feet (91 m) tall. The redwoods were heavily logged in the early 20th century. Prior to logging, the massive trees created their own microclimate by capturing moisture from fog, and also by

650-447: Is owned by the Bureau of Land Management . Sixteen percent is privately owned, while the remaining one percent is managed by the cities of Brookings and Harbor , Curry County, and the state of Oregon. Approximately 97 percent of the land is used for forestry, 2 percent for agriculture and rural areas, and 1 percent is urban. Gravel and minerals are mined from the lower and upper regions of

715-399: The Klamath Mountains . Steelhead and chinook and coho salmon are the most common anadromous fish that inhabit the Chetco River. Steelhead are abundant and have been spotted in most major and minor streams. Chinook salmon usually travel as far as Boulder Creek, about halfway between the Chetco's headwaters and its mouth. Coho also generally stay in this area, but some have been found in

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780-533: The Lookout Air Raids of 1942. Turning southwest, the river flows through Alfred A. Loeb State Park and collects the North Fork Chetco River on the right at river mile (RM) 5 (or river kilometer (RK) 8). The Chetco becomes an estuary about 1.7 miles (2.7 km) from its mouth. It passes through the communities of Brookings to the north and Harbor to the south, and discharges into

845-543: The National Guard . The hospital was able to reopen five days later after extensive work to repair the flooding damage. The Southern Pacific (SP) rail line between Portland and San Francisco was out of service for eighteen days as crews repaired damage from landslides near the 4,885-foot (1,489 m) Cascade Summit ; and the parallel Willamette Pass highway was blocked for several days. Salt Creek washed out 25 miles (40 km) of Oregon Route 58 and undermined

910-591: The Oregon Coast , downtown Reedsport was flooded with 8 feet (2.4 m) of water, and in Coos Bay , a massive logjam contributed to severe flooding. The ports at Gold Beach and Brookings were destroyed. At Oregon City , Willamette Falls was unrecognizable as a waterfall, and the city was flooded by several feet of water. In Portland , the lower deck of the Steel Bridge was underwater and had also been hit by

975-648: The Siletz Reservation . Oregon—and therefore the Chetco watershed—was jointly occupied by the United Kingdom and the United States after the Treaty of 1818 was signed. The Oregon Treaty was ratified in 1846, giving the United States ownership of Oregon. Soon after, the Oregon Territory was established, and Oregon became a U.S. state on February 14, 1859. The discovery of gold and other precious metals in

1040-645: The United States Department of Agriculture to withdraw the Chetco River from the 1872 Mining Act, thus preventing mineral mining on the river. However, Rutan forfeited his claims by not paying his annual filing fees to the Bureau of Land Management in 2011. The Oregon Department of Environmental Quality (DEQ) has monitored the Chetco River for eight different parameters that affect water quality: temperature, oxygen saturation , pH , nutrients , bacteria , chemical contaminants such as pesticides and metals, turbidity , and alkalinity . Streams that exceed

1105-678: The left ; Ditch and Copper creeks, which enter from the right, and Henry Creek, left. Little Chetco Trail and other connecting trails maintained by the United States Forest Service pass through or near the Little Chetco River watershed. These include the Emily Cabin Trail, the Kalmiopsis Rim Trail, and the Bailey Cabin Trail. Chetco River Native Americans have lived in the Chetco River's watershed for

1170-515: The left bank , Tincup Creek on the right bank , and Boulder Creek on the left. It then flows south, gathering the South Fork Chetco River. A few miles farther south, the river passes through a Redwood grove. It flows between Bosley Butte to the north and Mount Emily to the south; the latter is the impact site of one of only four bombs known to have been dropped in the continental United States by an enemy aircraft. This occurred during

1235-407: The moment magnitude scale —caused a tsunami to sweep across California, Oregon, Washington, and British Columbia, reaching Japan the next day. It was produced when the entire Cascadia subduction zone , about 680 miles (1,100 km) long, slipped approximately 66 feet (20 m) in a megathrust event. Another major earthquake occurred in 1873 near present-day Brookings. With a magnitude of 7.3,

1300-542: The tsunami created by the 1964 Alaska earthquake only nine months earlier, also suffered from the floods. Over 22 inches (550 mm) of rain fell on the Eel River basin in a span of two days. By December 23, 752,000 cubic feet per second (21,300 m /s) of water rushed down the Eel River at Scotia (still upstream from the confluence of the Van Duzen River ), 200,000 cubic feet per second (5,660 m /s) more than

1365-578: The understory . Kalmiopsis , a flowering evergreen shrub and the namesake of the Kalmiopsis Wilderness, only grows in the Siskiyou Mountains . Several noxious weeds have also been identified, including gorse , Scotch broom , blackberries , and thistles . The most prevalent species of the extreme southern portion of the watershed is the coastal redwood , one of the tallest types of trees on Earth. The world's northernmost redwood grove

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1430-585: The "hundred year" flood of 1955 in most cases). Sixteen state highway bridges were destroyed in California's 1st congressional district , most of them on Highway 101 , and another ten county bridges were destroyed in Humboldt County. The flood destroyed 37 miles (60 km) of track with multiple stream and river crossings of the Northwestern Pacific Railroad through the Eel River canyon,

1495-465: The 1955 flood, and more than the average discharge of the entire Mississippi River basin. Just under 200,000 cubic feet per second (5,660 m /s) of water flowed down the South Fork Eel River alone, causing severe damage along its entire length. Every stream gauge on the Eel River was destroyed except the one at Fernbridge where the bridge survived the flood. The flood crest at Miranda

1560-587: The 1986 to 1995 results of 94 and 93. Despite the excellent ratings, the Chetco River actually ranks as the second most polluted stream in Curry County, after Floras Creek, a tributary of the New River . Fishing, four-wheel driving, swimming, boating, camping, sightseeing, and picnicking are the primary recreational activities in the watershed. Whitewater kayaking is also popular in the winter months when water levels are high. Several trails are maintained throughout

1625-484: The Chetco River watershed are usually caused by landslides, various forms of erosion, and plugged road culverts. On the Oregon Water Quality Index (OWQI) used by DEQ, water quality scores can vary from 10 (worst) to 100 (ideal). The average for the Chetco River at RM 10.8 (RK 17.4) between 1998 and 2007 was 95 (excellent) in the summer and 90 in the fall, winter, and spring. These scores are comparable to

1690-461: The Chetco for drinking water. Supporting a large population of salmon and trout , the Chetco's water is of very high quality. The watershed is home to many other species, including several that are endemic to the Siskiyou Mountains area. The northernmost grove of Redwoods —the tallest trees on Earth—grow in the southern region of the Chetco's drainage basin. In total, the river is home to over 200 species of animals, and 97 percent of

1755-482: The Chetco region. Various forms of loam comprise its soil. Erosion levels are high due to a combination of high precipitation, steep slopes, and landslides, which can result in earthflows . Humans have lived in the Chetco River watershed since approximately 1,000 to 3,000 years ago. The first inhabitants were perhaps ancestors of the Chetco Indians and other Native American tribes, themselves descendants of

1820-504: The Chetco's total drainage basin. The maximum recorded flow was 85,400 cubic feet per second (2,420 m /s) on December 22, 1964, during the Pacific Northwest flood of 1964 . The minimum flow was 42 cubic feet per second (1.2 m /s) on October 14, 1987. The Chetco River drains 352 square miles (912 km ) of the southern Oregon Coast . About 78 percent is owned by the United States Forest Service , and another 5 percent

1885-464: The Granite and Carter Creek area, about 12 miles (19 km) above Boulder Creek. Coastal cutthroat trout can be found all around the watershed; some migrate to the ocean, while others live in the river and its tributaries year round. Pacific lamprey , three-spined stickleback , and various sculpins have also been observed. The Chetco River flows through the ancient Klamath Mountain terrane , which

1950-623: The Kalmiopsis Wilderness and surrounding regions. As of the 2010 census , the city of Brookings had a population of 6,336, while nearby Harbor had 2,391. In total, over 14,000 residents of the Brookings–Harbor area depend on the Chetco River for drinking water. Nearby watersheds include the Winchuck and Smith rivers to the south, the Pistol River to the north, and the Illinois River ,

2015-669: The Kalmiopsis Wilderness, and ending 24 miles (39 km) downstream. Despite environmentalists' concerns, he proposed mining the Chetco riverbed for gold and minerals via commercial suction dredges , permitted by the General Mining Act of 1872 . In 2010, the Chetco River was identified as the seventh most endangered river in America by advocacy organization American Rivers , facing a threat of "motorized instream mining". Oregon's governor, Ted Kulongoski , two senators, Ron Wyden and Jeff Merkley , and congressman Peter DeFazio all asked

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2080-430: The Kalmiopsis Wilderness, as well as other regions in the watershed. Eight boat launches are located on the river between its confluence with the south fork and its mouth. Alfred A. Loeb State Park , located on the banks of the Chetco, has three cabins and 48 camping sites. Several large parks are located in Brookings. The 33-acre (13 ha) Azalea Park in Brookings features five species of wild azaleas . The park

2145-455: The Pacific Ocean. The United States Geological Survey monitors the flow of the Chetco River at a stream gauge at RM 10.7 (RK 17.2), which is 6.8 miles (11 km) northeast of Brookings. It opened in 1969, and continues to operate. The average flow was 2,263 cubic feet per second (64.08 m /s) from a drainage area of 271 square miles (702 km ), about 77 percent of

2210-590: The SP viaduct footings. Landslides covered 700 feet (210 m) of SP track near Oakridge , and swept away 130 feet (40 m) of the Noisy Creek bridge 20 miles (32 km) north of Crescent Lake . The Willamette River washed out 300 feet (91 m) of SP track between Portland and Albany . Starting on December 21, intense downpours across Northern California caused numerous streams to flood, many to record-breaking levels. California Governor Brown declared 34 counties in

2275-472: The average normal December rainfall is 12 inches (300 mm), there was over 38 inches (970 mm) of rain. As rivers and streams overflowed and the soil became saturated, mudslides occurred, roads closed, and reservoirs overflowed. Many towns were isolated. By the end of the flood, every river in Oregon was above flood stage, and more than 30 major bridges were impassable. Heavy warm rain and melting snow caused more flooding in late January 1965, after

2340-465: The first humans who traveled across the Bering land bridge from Siberia over 10,000 years ago. At least nine separate villages were constructed along the Chetco River, including two on either side of its mouth. The Native Americans named the river "chit taa-ghii~-li~'". The first European American to visit the area may have been Sir Francis Drake on June 5, 1579, during his circumnavigation of

2405-881: The flood as the fifth most destructive weather event in Oregon in the 20th century. California Governor Pat Brown was quoted as saying that a flood of similar proportions could "happen only once in 1,000 years," and it was often referred to later as the Thousand Year Flood. The flood killed 19 people, heavily damaged or completely devastated at least 10 towns, destroyed all or portions of more than 20 major highway and county bridges, carried away millions of board feet of lumber and logs from mill sites, devastated thousands of acres of agricultural land, killed 4,000 head of livestock, and caused $ 100 million in damage in Humboldt County, California , alone. An atypical cold spell began in Oregon on December 13, 1964, that froze

2470-523: The geography of the region; cool air funnels down the Chetco River valley from the Siskiyou and Coast ranges, gradually heating up before eventually reaching Brookings as a warm wind. The mountains also shield the area from cool marine layers . Partially as a result of this phenomenon, Brookings recorded its highest temperature ever, 108 °F (42 °C), on July 8, 2008. Earthquakes are common, and large-scale ones occur around every 300 years. The Cascadia earthquake of 1700 —estimated at 8.7–9.2 on

2535-495: The hospital's basement. Hospital staff, parks department employees, and inmates from the Oregon State Penitentiary placed sandbags around the hospital to prevent floodwaters from coming in. Eventually, the flooding coupled with a loss of power led to the decision to evacuate patients to Salem General Hospital on Center Street. 121 patients were evacuated from Salem Memorial by hospital staff, doctors, ambulance crews, and

2600-430: The immense amount of shade they produced. The redwoods region is less mountainous than the rest of the watershed, and meandering streams are much more common. Over 200 species of animals inhabit the river and its tributaries. Birds such as loons , grebes , ducks, kingfishers , and bald eagles are known to live around streams and other regions of the watershed. Auks , gulls , and terns have been spotted around

2665-556: The last one to three thousand years. Several explorers, including Sir Francis Drake , George Vancouver , and Jedediah Smith , visited the region between the 16th and 19th centuries, and found the Chetco people inhabiting the area. Non- indigenous settlers arrived soon after gold and other precious metals were discovered in the 1840s and 1850s. The town of Brookings was founded in the early 20th century, and incorporated in 1951. Fourteen thousand residents of Brookings and Harbor rely on

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2730-743: The late 1870s", according to the National Weather Service office in Portland. Some of the worst mudslides occurred in the Mount Hood Corridor , and one man died in a mud and debris avalanche near Rhododendron that destroyed 15 houses. Other deaths occurred from drowning and electrocution, and one man died when the new John Day bridge collapsed. Yamhill County was severely affected. The Highway 219 bridge between Newberg and St. Paul , and Wilsonville Road between Newberg and Wilsonville were closed, trapping hundreds of people. On

2795-463: The microcontinent collided with the much larger North American continent. The process uplifted the complex and exotic terranes of the microcontinent to form the Klamath Mountains. Many glaciers carved U-shaped valleys and cirques during the last ice age , and several alpine lakes still exist today. Today, sandstone , shale , granite , and serpentine are the primary rock types in

2860-489: The north, connecting the region to the rest of the Oregon coast. In 1917, a 1,200-foot-long (366 m) wharf was built at the mouth of the river. Jetties were constructed on either side of its mouth by the United States Army Corps of Engineers in 1957. The Siskiyou National Forest was created on October 5, 1906, protecting the entire upper portion of the Chetco watershed. The nearby Rogue River National Forest

2925-560: The quake was felt from Seattle to San Francisco . Wind is also a factor in the region; storms can sometimes reach over 100 miles per hour (160 km/h). The Columbus Day Storm of 1962 brought devastating winds to nearly all of Oregon; nearby Port Orford recorded gusts exceeding 190 miles per hour (310 km/h). The storm killed 38 people across the state and caused over $ 200 million worth of damage. The watershed often experiences wildfires, some of them major. The Biscuit Fire of 2002 burned over 500,000 acres (200,000 ha) of

2990-515: The region disaster areas . Together, Del Norte , Humboldt , Mendocino , Siskiyou , Trinity , and Sonoma counties sustained more damage than the other 28 counties combined. Twenty-six U.S. Geological Survey (USGS) stream gauges were destroyed. The Eel , Smith , Klamath , Trinity , Salmon , and Mad rivers, as well as other rivers and large streams, all went well beyond flood stage and peaked nearly simultaneously around December 21 and 22, breaking previous records (notably those set in

3055-899: The region's only major railroad. Many communities of Del Norte and Humboldt counties suffered extensive power outages and were left isolated or cut off from the rest of the state for a period, including the region's larger populated areas around Humboldt Bay , such as Eureka and Arcata , despite the fact that those cities were located on higher ground and not in the path of raging rivers. Riverside communities like Klamath , Orleans , Myers Flat , Weott , South Fork , Shively , Pepperwood , Stafford , and Ti-Bar were completely destroyed by flood waters; some of them were never rebuilt and none regained their former status. Metropolitan , Rio Dell , and Scotia were significantly damaged. The Pacific Lumber Company sawmill at Scotia lost 40 million board feet (94,000  m ) of logs and lumber washed downstream. Crescent City , still recovering from

3120-446: The region. He opened a gold mining camp on the site in 2007, flying in customers by helicopter. Curry County officials soon stated that the camp violated zoning and sanitation laws, but inspections were stymied because of the area's inaccessibility. Rutan bought several more claims in the Wild and Scenic section of the Chetco River in the following years, beginning 6 miles (10 km) inside

3185-726: The river at Hoopa . Between December 20 and December 26, 10,390,000 acre-feet (12.82 km ) of water flowed into the Pacific Ocean from the combined rivers and streams on the North Coast (of California). In the California Central Valley , the Yosemite Valley was flooded, and residents of Yuba City were evacuated. Many streams reached record flood stages, including the Feather River , Yuba River , American River , Cottonwood Creek , and Butte Creek . The flood caused

3250-453: The river's mouth, and black-legged kittiwakes nest in the area during the winter. The wildlife in the Kalmiopsis region of the Chetco watershed is more diverse than that of any other region in Oregon. Mammals such as American black bears , black-tailed deer , bobcats , ring-tailed cats , and gray foxes are common inhabitants of this region. The rare Siskiyou chipmunk is endemic to

3315-612: The soil, and it was followed by unusually heavy snow. Subsequently, an atmospheric river brought persistent, heavy, warm rain. The temperature increased by 30 to 40 °F (17 to 22 °C). This melted the snow, but left the soil frozen and impermeable. Some places received the equivalent of a year's rain in just a few days. Albany received 13 inches (330 mm) of rain in December, almost double its average December rainfall of 7 inches (200 mm). Detroit recorded an extra 18 inches (460 mm) of rain, and at Crater Lake , where

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3380-473: The southern Oregon coast region. The company constructed a sawmill in 1914, and founded the town of Brookings. Brookings was not incorporated until 1951. The region remained relatively isolated due to its mountainous terrain until 1924, when Highway 101 was extended from Crescent City, California , to Brookings. In 1932, the Isaac Lee Patterson Bridge was completed over the Rogue River to

3445-639: The standard level are then placed on the DEQ 303d list in accordance with the Clean Water Act . The Chetco from Box Canyon Creek to its mouth exceeded the standard level for temperature and turbidity. The North Fork, South Fork, and other tributaries were also listed for temperature and turbidity. All tributaries of the Chetco usually exceed the 64 °F (18 °C) temperature standard. Water temperatures range from 62.6 °F (17.0 °C) at Bosley Creek to 76 °F (24 °C) at Willow Bar. High turbidity levels in

3510-484: The surface. Shortly after, a large portion of sea floor was thrust over the older Klamath terranes; much of it is still visible atop Vulcan and Chetco peaks. This region is known as the Josephine Ophiolite , and contains a rare type of rock called peridotite , originating from the Earth's mantle . The mountainous terrain of the Chetco River watershed was created approximately 130 million years ago when

3575-452: The town of Klamath under 15 feet (4.6 m) of water. The Trinity River , one of the Klamath's largest tributaries , also flooded and wrought destruction along its length. The Trinity, however, did not break the 1955 flood's records because of the newly constructed Trinity Dam , which stored 372,200 acre-feet (459,100,000 m ) of runoff from the storm. Nonetheless, 231,000 cubic feet per second (6,540 m /s) of water rushed down

3640-457: The waters had begun to recede from the December flood. More mudslides occurred in places that had withstood the December flooding, and there were more deaths. Many streams in the northern San Joaquin Valley reached higher flows than they had in December. The Christmas flood of 1964 was "the most severe rainstorm to ever occur over central Oregon, and among the most severe over western Oregon since

3705-611: The watershed brought settlers to the region in the 1840s and 1850s. Nickel , cobalt , and chromium were also mined. The town of Harbor was founded on the south bank of the Chetco River in 1891, and a ferry service across the river opened in 1904. It was shut down in 1915 when the Chetco Bridge opened. In 1912, the Brookings Lumber & Box Company moved north from the San Bernardino Mountains in southern California to

3770-463: The watershed is forested. The Chetco River begins about 4 miles (6 km) east of Chetco Peak, approximately 3,201 feet (975.7 m) above sea level. It flows north, gathering small tributaries such as the Little Chetco River and Babyfoot Creek. The river turns west near the 5,098-foot-tall (1,554 m) Pearsoll Peak , the highest point in the watershed. It receives Box Canyon Creek on

3835-400: The watershed, respectively. The region is mostly mountainous, characterized by steep river valleys. Elevations in the Chetco River watershed range from sea level to 5,098 feet (1,554 m) at the summit of Pearsoll Peak. Precipitation averages between 45 and 140 inches (1,143 and 3,556 mm) per year, with October through June being the wettest months. Seventy percent of surface runoff

3900-432: The world. The Vancouver Expedition also explored the area in 1792. In June 1828 Jedediah Smith and his company of fur traders camped on the south bank of the river near a Native American village. Between 1853 and 1855, many Native Americans were killed and their villages destroyed in skirmishes occurring around the same time as the nearby Rogue River Wars . On July 9, 1856, the remaining Chetco were marched north to

3965-672: Was 46 feet (14 m). Signs were later placed on top of tall poles to mark the unusual height of the water. The Smith River, located in Del Norte County near the Oregon border, reached flows of 228,000 cubic feet per second (6,460 m /s) at Hiouchi , easily surpassing the 1955 flood's previous record of 165,000 cubic feet per second (4,670 m /s). The town of Gasquet received 26.6 inches (676 mm) of rain over an eight-day period, and Crescent City received 9.2 inches (230 mm). The Klamath River reached flows of 557,000 cubic feet per second (15,800 m /s), submerging

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4030-458: Was caused by several lightning strikes between July 12 and 15. By August 17, all five had burned together, creating one massive fire. It burned for over five months and was not fully extinguished until December 31. In 2002, 45 acres (18 ha) of land on the Little Chetco River were sold to Washington real estate developer David Rutan, only several months after the Biscuit Fire tore through

4095-506: Was combined with it in 2004, creating the nearly 1,800,000-acre (728,000 ha) Rogue River – Siskiyou National Forest. In 1964, the United States Congress set aside over 80,000 acres (32,000 ha) of the eastern Chetco River watershed and surrounding regions to create the Kalmiopsis Wilderness. The wilderness was expanded several times in the 1970s, and now encompasses over 180,000 acres (72,800 ha). On October 28, 1988,

4160-577: Was designated an Oregon State Park in 1939, but was given to Brookings in 1993. It hosts the American Music Festival from June until September. The Nature's Coastal Holiday light show is displayed in Azalea Park every December. Chetco Point Park, located near the wharf, has several fire rings and picnic tables , as well as views of the river, the Pacific Ocean, and the Port of Brookings Harbor . It

4225-644: Was the worst flood in recorded history on nearly every major stream and river in coastal Northern California and one of the worst to affect the Willamette River in Oregon . It also affected parts of southwest Washington , Idaho , and Nevada . In Oregon, 17 or 18 people died as a result of the disaster, and it caused hundreds of millions of dollars in damage. The flooding on the Willamette covered 152,789 acres (61,831.5 ha). The National Weather Service rated

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