Lake Cascade - Winter Magic

Artwork: #83 of 1206 by Photography Moments - Sandi

Tags: nature photographs, landscape photographs, winter photographs, water photographs, red photographs, nature canvas prints, landscape canvas prints, winter canvas prints, water canvas prints, red canvas prints

Featured:

Stop time with art

02/12/2013

Artists News

02/11/2013

All Natural Beauty...

02/10/2013

Title:

Lake Cascade - Winter Magic

Artist:

Photography Moments - Sandi

Medium:

Photograph - Print - Painting - Photography

Description:

Information found on en.wikipedia.org - Cascade Idaho, Lake Cascade, Payette River, Boise National Forest and Winter

Cascade is a rural city in and the county seat of Valley County, Idaho, United States,[4] in the west central part of the state. The population was 939 at the 2010 census, down from 997 in 2000.[5]

Cascade is located on the southeast shore of Lake Cascade, formerly known as "Cascade Reservoir." With the introduction of the Tamarack Resort in 2004, the name was officially changed to sidestep the negative marketing connotations of "reservoir." It was formed by the completion of Cascade Dam, on the north side of the city. Construction by the Bureau of Reclamation began in 1942, was halted during World War II, and completed in 1948.

Cascade was the home of a sizable Boise Cascade sawmill, which closed in May 2001.[6]

The recreational city of McCall is 29 miles (46 km) north, and the village of Donnelly is a little over midway, via Highway 55. The shuttered Tamarack Resort (2004�09) is across the reservoir to the northwest.

Lake Cascade (or originally �Cascade Reservoir�) is located on the North Fork of the Payette River in Valley County, Idaho, USA, in the Boise National Forest. It has a surface area of 47 square miles (122 km2), and is the fourth largest lake or reservoir in the state. The closest cities are Cascade, Donnelly, and McCall.

Following a delay due to World War II, the earthen dam was built by the Bureau of Reclamation, and completed in 1948.[2]

The Payette River is an 82.7-mile-long (133.1 km)[1] river in southwestern Idaho and is a major tributary of the Snake River.

Its headwaters originate in the Sawtooth and Salmon River Mountains at elevations over 10,000 feet (3,000 m). Drainage in the watershed flows primarily from east to west, with the cumulative stream length to the head of the North Fork Payette River being 180 miles (290 km),[1] while to the head of the South Fork the cumulative length is nearly 163 miles (262 km).[1] The combined Payette River flows into an agricultural valley and empties into the Snake River near the city of Payette at an elevation of 2,125 feet (648 m). The Payette River's drainage basin comprises about 3,240 square miles (8,400 km2).[2] It is a physiographic section of the Columbia Plateau province, which in turn is part of the larger Intermontane Plateaus physiographic division. The South Fork of the Payette has its headwaters in the Sawtooth Wilderness, which is part of the Sawtooth National Recreation Area.

The principal tributaries of the Payette River are the North and South forks. The North Fork drains about 950 square miles (2,500 km2), beginning north of McCall and flowing into Payette Lake. The North Fork exits at the southwest end of Payette Lake at 4,990 feet (1,520 m) and flows south in the "Long Valley" of Valley County toward Cascade. It then flows into the Cascade Reservoir, then continues south, accompanied by Highway 55.

The South Fork Payette River drains about 1,200 square miles (3,100 km2), originating on the west side of the Sawtooth Wilderness beneath the 10,211-foot (3,112 m) Mount Payette. It flows past Grandjean and down to Lowman, along Highway 21. The shorter Middle Fork Payette River parallels the lower North Fork 10 miles (16 km) to the east, flowing south and joining the South Fork just southwest of Crouch. Further east, the Deadwood River parallels the Middle Fork and empties into the South Fork just west of Lowman. The main stem of the Payette River is shown on USGS topographic maps as beginning at the confluence of the South and Middle forks.[1]

The North Fork joins the Payette at the village of Banks, at an elevation of 2,790 feet (850 m). The main stem flows south from Banks for 15 miles (24 km) to Horseshoe Bend, then west into Black Canyon Reservoir. Below the reservoir's dam, the river flows past Emmett and Payette, then empties into the Snake River at the Oregon border. The Payette River has an average annual discharge into the Snake River of 2,192,000-acre-foot (2,704 km2) of water.

The Boise National Forest is a US national forest located north and east of the city of Boise, Idaho. It is about 2,654,000 acres (10,740 km2) in size, ranging in elevation from 2,600 to 9,800 feet (800 to 3000 m). The mountainous landscape developed through uplifting, faulting, and stream cutting. Most of the land lies within the Idaho Batholith, a large and highly erodible geologic formation. The major rivers that run through it include the Boise, the Payette and the South and Middle forks of the Salmon River. Portions of the Frank Church-River of No Return Wilderness, the Sawtooth Wilderness, and Sawtooth National Recreation Area are within the forest, although none of these areas are managed by Boise National Forest.

Conifer forest covers most of the Boise National Forest. Tree species include ponderosa pine, Douglas-fir, Engelmann Spruce, lodgepole pine, grand fir, subalpine fir, western larch, and whitebark pine. Shrubs and grasses grow in the non-forested areas. Wildflowers splash color in both forests and shrub-land.

The Forest contains large expanses of summer range for big game species like mule deer and elk. Trout are native to most streams and lakes. Oceangoing salmon and steelhead inhabit tributaries of the Salmon River.

In descending order of land area the forest is located in parts of Valley, Boise, Elmore, Gem, Ada, and Washington counties. Forest headquarters are located in Boise, Idaho. There are local ranger district offices in Cascade, Emmett, Idaho City, Lowman, and Mountain Home.[3]

Winter (/ˈwɪntər/ WIN-tər) is the coldest season of the year in temperate climates, between autumn and spring. At the winter solstice, the days are shortest and the nights are longest, with days lengthening as the season progresses after the solstice.

The tilt of the Earth's axis relative to its orbital plane plays a big role in the weather. The Earth is tilted at an angle of 23.44� to the plane of its orbit, and this causes different latitudes on the Earth to directly face the Sun as the Earth moves through its orbit. It is this variation that primarily brings about the seasons. When it is winter in the Northern Hemisphere, the Southern Hemisphere faces the Sun more directly and thus experiences warmer temperatures than the Northern Hemisphere. Conversely, winter in the Southern Hemisphere occurs when the Northern hemisphere is tilted more toward the Sun. From the perspective of an observer on the Earth, the winter Sun has a lower maximum altitude in the sky than the summer Sun.

During winter in either hemisphere, the lower altitude of the Sun in winter causes the sunlight to hit that hemisphere at an oblique angle. In regions experiencing winter, the same amount of solar radiation is spread out over a larger area. This effect is compounded by the larger distance that the light must travel through the atmosphere, allowing the atmosphere to dissipate more heat. Compared with these effects, the changes in the distance of the earth from the sun are negligible.

Lake Cascade, Winter Magic - Snow Covered Winter Landscapes, Scenic Idaho Landscape Painting Photography

Posted:

Statistics:

Viewed 207 Times  -  Last Visitor from Montezuma, GA on 05/18/2013 at 3:16 PM

Colors:

Image Link:

Sales Sheet:

PDF Sales Sheet