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Northern Oregon Coast Range

Coordinates: 45°39′53″N 123°32′53″W / 45.66472°N 123.54806°W / 45.66472; -123.54806
From Wikipedia, the free encyclopedia
Northern Oregon Coast Range
The Northern Coast Range, seen from Saddle Mountain in Clatsop County
Highest point
PeakRogers Peak
Elevation3,706 ft (1,130 m)
Coordinates45°39′53″N 123°32′53″W / 45.66472°N 123.54806°W / 45.66472; -123.54806
Dimensions
Length100 mi (160 km) north–south
Geography
CountryUnited States
StateOregon
SubdivisionsTualatin Mountains
Parent rangeOregon Coast Range, Pacific Coast Ranges
Borders onCentral Oregon Coast Range
Geology
OrogenyGeologic fault, basalt flows
Age of rockPaleocene and Eocene
Type of rockvolcanic and forearc basin

The Northern Oregon Coast Range is the northern section of the Oregon Coast Range, in the Pacific Coast Ranges physiographic region, located in the northwest portion of the state of Oregon, United States. This section of the mountain range, part of the Pacific Coast Ranges, contains peaks as high as 3,710 feet (1,131 m) for Rogers Peak.[1] Forests in these mountains are considered to be some of the most productive timber land in the world.[2] The Central Oregon Coast Range is directly south of this section with the Southern Oregon Coast Range beyond the central range.

Geology

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The origins of these mountains began approximately 40 million years ago during the Eocene age. During this time-period, sandstone and siltstone formed in the area. Additionally, igneous rocks and basalt flows combined with basaltic sandstone to create many of the mountainous formations. Other sedimentary rock in the area formed more recently, around 20 million years ago. It is hypothesized that portions of the northern section of the range were islands during parts of the Eocene era.[3] Other portions of the mountains consist of marine sedimentary rock.[4] The entire coast range sits on a convergent tectonic margin interacting with the Juan de Fuca Plate that is subducting beneath North America tectonic plate.[5] Also, weathering and erosion of the region is a major factor in shaping the landscape. Heavy rainfall and landslides have worked to alter the mountains.[4]

The range is part of a broad, plunging structural arch of sedimentary and Tertiary volcanic strata that is being uplifted. Eocene and Miocene sections form the flanks of the uplifted sections. Some of the oldest rocks are submarine tholeiitic basalts from the Eocene era. The basalt came from the basalt flows that covered much of Oregon and originated from volcanoes in the central portion of the state. Other rocks include sandstone, mudstone, and siltstone. It was during the middle Miocene period that the range was uplifted in the broad, northeast-plunging arch.[6]

Flora and fauna

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Logging in the mountains
Fallen logs over the outflow from Soapstone Lake.

Portions of the range are in the Siuslaw National Forest and Tillamook State Forest, and large sections of the range were burned in forest fires during the 1930s and 1940s as part of the Tillamook Burn. In the forested areas trees include Sitka spruce, western redcedar, Douglas fir, and western hemlock.[7] Other plants that grow in the region are huckleberry, salmonberry, thimbleberry, salal, vine maple, sword and bracken ferns and Oregon grape to name a few.[7][8]

Arthropods and molluscs found include collembolans, spiders, beetles, slugs, millipedes, weevils, and various centipedes.[7][8] Animals that inhabit the Northern Coast range are the rough-skinned newt, chipmunks, bears, rabbits, white-footed deer mice, Columbian black tail deer and others.[8] Birds include chickadees, red-breasted nuthatches, kinglets, Western pileated woodpeckers, Oregon Canada jays, California creepers, and Sitka red crossbills among others.[8]

Location and climate

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The range begins at the Columbia River, with some mountainous features on the north side of the river, and continues south roughly 100 miles (160 km) to the Salmon River where Oregon Route 18 traverses the range from the Willamette Valley to the Oregon Coast. The width of the range varies but is roughly 35 miles (56 km).[2]

The climate of the range is moderate because of marine influences, and annual precipitation is heavy, varying from 60 to 180 inches (1,500 to 4,600 mm).[9]

Peaks

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Fog covering the mountains near Balm Grove
Youngs River, Saddle Mountain and the Northern Oregon Coast Range from the Astoria Column

All mountains over 3,000 feet (910 m) in elevation in the Northern Coast Range.

Mountain Name Elevation County
feet metres
Rogers Peak 3,706 1,130 Tillamook
South Saddle Mountain 3,465 1,056 Washington
Larch Mountain 3,452 1,052 Washington
Trask Mountain 3,426 1,044 Yamhill
Saddle Mountain 3,288 1,002 Clatsop
Triangulation Point 3,235 986 Tillamook
Kings Mountain 3,226 983 Tillamook
Mount Hebo 3,154 961 Yamhill
Edwards Butte 3,136 956 Tillamook
Buck Mountain 3,097 944 Tillamook
Sheridan Peak 3,091 942 Yamhill
Woods Point 3,084 940 Tillamook
Gobblers Knob 3,058 932 Tillamook
Onion Peak 3,057 932 Clatsop

Other peaks

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Rivers

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Map of the region with major rivers in blue. Orange line shows divide between watersheds flowing to the east and those flowing north or west.

The following rivers have their headwaters in the Northern Oregon Coast Range:

References

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  1. ^ Rogers Peak. Peakbagger.com. Retrieved February 29, 2008.
  2. ^ a b Northern Coast Range Adaptive Management Area; Chapter 2: Physical and Biological Environment. Oregon State University. Retrieved February 29, 2008.
  3. ^ Upper Nehalem Watershed Analysis. (PDF) Oregon Department of Forestry. Retrieved February 29, 2008.
  4. ^ a b Byrne, John V. "An Erosional Classification for the Northern Oregon Coast", Annals of the Association of American Geographers, Vol. 54, No. 3. (Sep. 1964), pp. 329–335.
  5. ^ Geology of the Luckiamute River Watershed, Upper Willamette Basin, Polk and Benton Counties, Oregon. (PDF) Western Oregon University. Retrieved February 29, 2008.
  6. ^ Geologic Map of the Tillamook Highlands, Northwest Oregon Coast Range. U.S. Geological Survey. Retrieved February 29, 2008.
  7. ^ a b c From the Forest to the Sea: A Story of Fallen Trees. Tree Dictionary. Retrieved February 29, 2008.
  8. ^ a b c d Macnab, James A. Biotic Aspection in the Coast Range Mountains of Northwestern Oregon. Ecological Monographs, Vol. 28, No. 1. (Jan. 1958), pp. 21–54.
  9. ^ Private Forests. Oregon Department of Forestry. Retrieved February 29, 2008.
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