Welcome to Owyhee County Idaho
 
 
Owyhee County is in the southwest corner of the state of Idaho.
It borders Oregon on the west,
Nevada on the South,
and the Snake River on the East/North.
Owyhee County - 5 million Acres
(Some of which may not yet have been flown over by eagles)
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Managing Horses at the Joyce Ranch circa. 1907
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Historic RanchesYou will ride through these ranches. Cattle were first brought to the area in the 1860s and thousands of them wintered in this mild climate.
- Joyce Ranch
- Located on Sinker Creek. Established in 1865 by Matthew Joyce, still working cattle ranch today. Paul Nettleton operates the upper portion of the Sinker Creek Drainage. If you come in from the west, you will see the sign right before you pass over Sinker Creek.
- Colette
- Located on Castle Creek, has original Stone House, still a working cattle ranch. An out vet check on Day 1 of the Owyhee Canyonlands ride is held on the ranch.
- Montini
- Located near the confluence with the Snake River with Sinker Creek. The stone barn and bunkhouse are still standing, Oregon Trail immigrant stopover. Two out vet checks will be located there on the Arabian Nights Ride.
- Gilmore
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Located up-stream from the Joyce Ranch. It is mostly gone back to nature. An Out Vet Check is held there on day 4 of the Owyhee Canyonlands Ride.
*Interesting Note on name of Sinker Creek: In 1847 prospectors were said to have found gold nuggets so large they used them as fishing sinkers!
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One of the many Petroglyphs near the Snake River
(Owyhee Canyonlands Trail)
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Early PeopleNative peoples are estimated to have been in this area for 14,000 to 15,000 years. You will see examples of their culture preserved in Petroglyphys which you will ride by near the Snake River. Shoshone and Bannock tribes are native to this area and are thought to have acquired horses around the 1700s.
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Newspaper Image of Joe Monaghan
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Unusual Owyhee Women
1.) Jane Mason (Owyhee’s Calamity Jane)- was a cattle and horse rustler around 1899.
2.) Joe Monaghan- lived as a man for 30 years without detection. Worked as a gold miner, cowboy and served on juries at a time when no woman was allowed to! The undertaker discovered her true sex after she had die in 1904!!
3.) Kittie Wilkins: The Horse Queen of Idaho Raised horses from 1885 to 1911. At one time she had 4000 head (see, you don’t have so many after all!!) She exported teams by train to the East Coast and sold many to the US Army.
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Mining in the Owyhee District
(Owyhee Canyonlands Trail)
* These are really ranchers up at the Gilmore Ranch
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Mining in the area - Gold was discovered on Jordan Creek in 1863. The resulting gold rush was responsible for many boomtowns and mines and a population much greater than the county has today. Silver City is known as The Queen of Ghost Towns and has many buildings still standing.
The County Seat was first located at Silver City but was later moved to a more central location at Murphy.
Many people feel that there is still a lot of gold out there just waiting to be found!
Oreana Valley -The introduction of irrigation to the Upper and Lower Snake River Valleys have made thousands of acres of former desert land into productive farmland. Alfalfa, sugar beets and potatoes are grown here. Five cuttings of alfalfa hay are harvested each season.
One interesting note is that the Main Street of Oreana runs true North and South. Surveyors depend on this Initial Point to establish land boundaries everywhere in Idaho.
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Brown's Creek Drainage
(Owyhee Highcountry Trail)
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Geology of the Snake River Basin
The Snake River plain is one of the most widely known and extensive volcanic regions on Earth. The first eruptions began 15 million years ago in near the southwest corner of Idaho. Since that time, volcanic eruptions seem to have migrated eastward at 1 to 2 inches per year, with the most recent volcanic activity having taken place in eastern Idaho and Yellowstone. Basalt lava flows (dark, more fluid flows from the earth’s mantle) have covered much of the original craters and volcanoes, but time has exposed views into the volcanic past in unusual places. Much of the red rock you will see in the canyons is rhyolite, a more viscous lava flow originating as the continental crust is heated from below. Rhyolite extrusions sometimes erupted violently, resulting in flows of hot ash, which welded over time to form tuff, which you will see as light colored stone, similar in appearance to sandstone.
10 million years ago, a series of large lakes began forming, periodically blanketing southwest Idaho. This series of lakes is referred to as Lake Idaho. Marine fossils are abundant in this region from Lake Idaho’s waxing and waning shorelines. The lake was permanently drained 1 million years ago when a then-small tributary of the Salmon River eroded head ward, eventually reaching the lake and causing its waters to drain northward, forming the Snake. (This tributary, eroded by the massive flood of water from Lake Idaho, became the Hells Canyon of the Snake River. The rhyolite canyons you will see (Castle Creek, Sinker Creek, Pickett Creek) were also formed as Lake Idaho drained. Windblown lakebed sediment formed many of the bluffs and 'badlands’ formations that you will see.
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Wagon on Oregon Trail Near Given's Hot Springs
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Given's Hot Springs
In 1879 Oregon Trail pioneers Milford and Mattie Givens discovered and fell in love with the hot springs area that today bears their name. The uncertain promise of the trail ahead proved poor competition for the Idaho site, with its abundance of fish and land animals for sustenance, and naturally hot water to simplify and enhance life. Oregon dreams were exchanged for Idaho reality as the Givens put down roots in this beautiful Owyhee County setting.
With the help of Milford and Mattie's four sons - Berry, Granville, Guy and Jess - a bath-house was built in the early 1900's. That structure included private rooms with soaking tubs.
In 1903 a hotel was built to accommodate the ever-increasing number of guests. An oasis in the desert, the hotel boasted a restaurant, ice cream parlor, and picnic grounds shaded with poplar and fruit trees. Later refinements included a barbershop and post office.
More and a Map!
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'Murphy Melons’ - 15 thousand years ago Lake Bonneville (Eastern Idaho, Utah) broke through its natural dam, unleashing a monumental torrent, which filled the Snake River canyon. Melon boulders of basalt were ripped from the walls of the Snake River canyon, rounded by bumping against one another and deposited in gigantic 'gravel’ bars. Some of these can be seen along Hwy 78 outside of Murphy. Petroglyphs were carved on some of the larger rounded basalt boulders along the Snake River thousands of years ago.
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Redtail Hawk on Browns Creek Loop
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World Birds of Prey Center
The Velma Morrison Interpretive Center at the World Center offers a
unique opportunity to learn about birds of prey. The Interpretive
Center has multi-media exhibits and interactive displays. Visitors can
see live bird presentations and learn how The Peregrine Fund breeds
endangered birds in captivity in preparation for reintroducing them
into the wild.
World Birds of Prey Center
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