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Fifes Peaks
Fifes Peaks is a compact group of summits and spires from an eroded volcanic cone located in Yakima County in Washington state. Fifes Peaks is situated in the Cascade Range on the east side of the crest, within the Norse Peak Wilderness. The Fifes Peaks are remnants of a now extinct caldera which exploded 25 million years ago with volcanic activity extending from 20 to 30 million years ago. Principal summits * Fifes Peaks West Peak - 6,880+ ft * Fifes Peaks Central Peak- 6,793 ft * Fifes Peaks East Peak - 6,375 ft * Mainmast - 6,400+ ft * Cannonhole Pinnacle - 6,600+ ft * Teddy Bear Pinnacle - 6260 ftBeckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. History Fifes Peaks were named for Thomas X. Fife (1853-1922), a placer miner. Thomas, his brothers, and their father John, mined in the area near Chinook Pass. Tom homesteaded at Goose Prairie, near Bumping Lake. Camp Fife, the Boy Scout Camp at Goose Prair ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yakima County, Washington
Yakima County is a county in the U.S. state of Washington. As of the 2020 census, its population was 256,728. The county seat and largest city is Yakima. The county was formed out of Ferguson County in January 1865 and is named for the Yakama tribe of Native Americans. Yakima County comprises the Yakima, WA Metropolitan Statistical Area and is Washington state's largest majority-Hispanic county as of 2020. History The area that now comprises Yakima County was part of the Oregon Country at the start of the nineteenth century, inhabited both by fur prospectors from Canada, and Americans seeking land for agricultural and mineral-extraction opportunities. Unable to resolve which country should control this vast area, the Treaty of 1818 provided for joint control. By 1843, the Provisional Government of Oregon had been established, although at first there were questions as to its authority and extent. During its existence, that provisional government formed the area north of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weather Front
A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For instance, cold fronts can bring bands of thunderstorms and cumulonimbus precipitation or be preceded by squall lines, while warm fronts are usually preceded by stratiform precipitation and fog. In summer, subtler humidity gradients are known as dry lines can trigger severe weather. Some fronts produce no precipitation and little cloudiness, although there is invariably always a wind shift. Cold fronts generally move from west to east, whereas warm fronts move poleward, although any direction is possible. Occluded fronts are a hybrid merge of the two, and stationary fronts are stalled in their motion. Cold fronts and cold occlusions move faster than warm fronts and warm occlusions because the dense air behind them can lift as well as pus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
