PHOTO OF BASQUE
HANDBALL COURT/OUTER WALL AND KIOSK
The First Spanish Basques in Jordan Valley were Jose Navarro and Antonio Azcuenaga
who came to Jordan Valley in 1889 and Augustin Azcuenaga in 1890. Pedro Arritola, Luis Yturraspe, and Cipriano Anacabe came
a little later and soon there was a thriving Basque colony. Some of them became successful sheepmen, and others were skilled
stonemasons, miners, hotelkeepers and merchants.
KIOSK INFORMATION Basque immigrants began building the ball
court or Pelota Frontone in the spring of 1915. It is built of native stone, hand hewn by Basque masons who learned their
trade in Spain. Here, for years, they played Pelota (ball), a game similar to American handball. The Frontone, a large,
tall, and unique building stands in the center of Jordan Valley. It was restored in 1997 with a Basque Fall Festival. The
Frontoia was used for the first time since 1935 with Pelota, Pala, Weightlifting, Basque Dancers and Basque Music. ______________________________________________________________
History/Lore JAI-ALAI: WHERE IT CAME FROM Jai-Alai at the Dania fronton is the 20th century offspring of handball--a game the
ancient Greeks had a word for and that pharaohs may have viewed on the banks of the Nile 4,000 years ago. What
is now the super-speeded up and sophisticated Basque sport of jai-alai developed from a simple game which was played long
before an anonymous Mesopotamian built the first wheel. Handball was old when ancient Greeks called it "pilos"
and played it as a form of exercise outdoors on rough ground. The Romans played "pilatta", while French and English
monarchs tried their royal hands at the game in the 14th and 15th centuries. However, it was the Basques,
those mysterious people with the tongue-twisting language,who polished one-wall handball into what is now the fastest ball
game in the world.
Jai-Alai
at the Dania fronton today is actually "pelota vasca" - Basque ball. In the Basque provinces of Spain and France
that straddle the rugged Pyrenees mountains, "pelota" was played on stone courtyards and against church walls in
the 15th century. Today the game is still played the same way in many small towns. In the Basque language,
jai-alai means "merry festival". It was at religious and holiday festivals that the game became popular. The game
is still a tradition at celebrations in the Basque provinces of France and Spain. Basques first played
pelota with bare hands, then with leather gloves, wooden paddles and primitive rackets. The cesta, the woven basket that is
the throwing and catching tool,came into use in the mid-1800's. Legend has it that a young French
Basque who couldn't afford an expensive leather glove tried hurling the ball with a curved basket which he obtained from
his mother's kitchen. The new basket or "cesta" was to change the concept of the game. More practical designs
for the cesta have evolved and today each one is tailored to the individual player. Jai-Alai also changed
with the discovery of rubber and its use in ball-making. That development transformed "pelota" into the spectacular
sport of speed, skill and courage that thrill Dania fans today.
By the latter part of the 19th century, jai-alai was being played wherever Basques
lived - Mexico, Cuba, the Philippines and South America. Early in the 20th century, at the 1904 St. Louis World's Fair,
the sport was seen for the first time in the United States. Before World War II, jai-alai was played in Havana and such
exotic places as Shanghai and Tientsin, China. Nowadays, it is a popular contemporary sport not only in Spain and France but
also Italy, Mexico, Indonesia, the Philippines and Macao. It was played in the 1992 Barcelona Olympic Games. In the United
States, it is played in Florida, Connecticut and Rhode Island. America's first permanent
jai-alai fronton was built in 1924 on what is now the parking lot of Hialeah race track. Dania Jai-Alai was the second fronton
to be built and opened its doors for the first time in 1953. There are now seven frontons in the United States, five of which
are in Florida.
While
early jai-alai exhibitions in this country featured "partido" games, where matches were played up to 20 or 30 points
and had only two teams, today's game is called "quiniela" jai-alai. The "spectacular
seven" scoring system was introduced in the 1970's to speed up the game and add excitement for bettors. Most games
last from 8 to 14 minutes. According to pedometer studies, each player runs about one mile per game. Jai-Alai's
enduring popularity in Florida and its growing attraction for fans elsewhere may be attributed to the fact that the sport
is both thrilling to watch and simple to understand. Explanation of the Game | Strategy | The Equipment | The Court | The Rules | The Basques | Celebrity Fans | Terminology | The Shots | The Signals | Questions and Answers Home _____________________________________________________________________

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| Photo by Don Paulson Click on photo for link to webphotos |
PHOTO OF LESLIE GULCH HISTORY:
Native Americans fished, hunted, and camped along the Owyhee River in Leslie Gulch 5,000 years before Europeans came
to the area. in 1882, a cattle rancher, Hiram E. Leslie, when working in what was then known as Dugout Gulch, was struck by
lightning; thus, the area was renamed Leslie Gulch. The original Leslie Gulch canyon road long served as a wagon and mail
route between Rockville and Watson. Today, the town of Watson lies at the bottom of the Owyhee Reservoir.
SOME
HELPFUL HINTS: It is a minimum of 25 miles of dirt roads from Slocum Creek Campground to a Highway (U.S. 95). The
closest available services are located in Jordan Valley, OR (43 miles, and Homedale, ID (40 miles).
DRIVE SLOWLY
AND ENJOY! Rapidly changing weather can affect road and driving conditions, and flash flooding and winter conditions
can prevent access. There may be variable and changing road surface conditions - high clearance vehicles are recommended.
Larger recreation vehicles are not recommended.
A WEALTH OF SPECIAL VALUES!! Unique Geology - The most
striking features fo Leslie Gulch are the diverse and often stark, towering and colorful geologic formations. The Leslie Gulch
Tuff (consolidated volcanic ash), which makes up the bulk of these formations, is a rhyolite ash that erupted from the Mahogany
Mountain caldera in a series of violent explosions about 15.5 million years ago.
Wildlife - In 1965, seventeen
California bighorn sheep were reintroduced into Leslie Gulch. The herd has expanded to over 200 animals. Mule deer and Rocky
Mountain elk are also found in the area. Bird watchers can spot Chukar, numerous song birds, raptors, California quail, northern
flickers, and white-throated swifts. Coyotes, bobcats, bats and many reptiles, including rattlesnakes, also live in leslie
Gulch
Rare Plants - The talus slopes and unique soils of the Leslie Gulch ash-flow tuff support a number of
globally rare plant species. Two annual species are found only in Leslie Gulch drainage (Packard's blazing star and Etter's
groundsel). Grimy ivesia, sterile milvetch, and Owyhee clover are rare perennials found at a few isolated sites in the canyon.
A stand of Ponderosa pine still survives in a Leslie Gulch tributary.
FOR ADDITIONAL INFORMATION AND MAPS CONTACT: Bureau of Land Management 100 Oregon Street Vale OR 97918 541-473-3144 http://www.or.blm.gov/Vale/ CALL THEM FOR ROAD CONDITIONS ____________________________________________________________
Big Horn Sheep at Leslie Gulch _____________________________
NOW AND THEN BUILDING Located in Downtown
Jordan Valley Designed in a showcasing format. Displayed are historical artifacts regional fine art
and buckaroo gear. _________________________________

NATIONAL HISTORIC SITE - JEAN BAPTISTE
CHARBONNEAU, SACAGAWEA'S SON, BURIAL SITE
PART OF OREGON'S HISTORY: Jean Baptiste Charbonneau was
born in 1805 at Fort Mandan in North Dakota. His parents were Toussaint Charbonneau, a French-Canadian interpreter, and Sacagawea,
a Lemhi Shoshone. His birth was attended by Meriwether Lewis while the Corps of Discovery, the group led by Captains Lewis
& Clark, were attempting to find an all-water route across the North American Continent. Mere weeks after his birth,
the boy nicknamed "Pomp" began traveling with his mother as the expedition journeyed from North Dakota to the Pacific
Ocean. Throughout their travels, the young mother and her son symbolized to the Native Americans they encountered that the
group was on a peaceful mission, and literally kept the Corp of Discovery out of harms way. During the expedition, Jean
Baptiste became much adored by Captain Clark, who wanted to "raise him as his own." This was accepted by Sacagawea
and Toussaint, who later put "Pomp" in Clark's care after Sacagawea's death in 1812. He was officially adopted
by Clark about August of 1813. In St. Louis, Missouri, William Clark educated Jean Baptiste. Because of Jean Baptist's
formal education and frontier accomplishments, Prince Paul Wilhelm of Wurttemberg took him back to Europe as his companion.
While living abroad for six years, Jean Baptiste traveled extensively, even Africa. He returned to the United States in 1829,
and could not resist the frontier. He again returned to the West, working as a guide, trapper, gold miner, magistrate, and
mountain man. At the age of 61, he set out from California to Montana- the scene of the latest gold strike. While crossing
the icy waters of the Owyhee River, he contracted pneumonia and died at the Inskip State Station on May 16, 1866, near today's
Danner, Oregon. This was not the end of this great American mountain man. His grave was rediscovered in the 1960's,
dedicated August 6, 1971, and recognized as a Registered National Historic Place on March 14, 1973. A rededication ceremony
of Jean Baptiste Charbonneau's grave site occurred on June 24, 2000. On May 16, 2005, the date of "Pomp's"
death, a Wreath-laying Ceremony was planned by the Idaho Chapter, Lewis and Clark Trail Heritage Foundation, Idaho State Historical
Society, and the residents of Jordan Valley were to meet at his grave site in Danner, Oregon, to honor the 200th birthday
of the youngest member of the Lewis and Clark Expeditions. It was held instead at the Jordan Valley School Old gym because
of inclement weather. The Ceremony started at 1:30 p.m. with guest speakers and area school students in attendance.
SEE PHOTO BELOW ________________________________________________________
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PHOTO OF INSIDE OF BALL COURT/PLAYING SURFACE
HISTORY OF THE SPANISH
BASQUES: The Spanish Basques or Euskaldunak as they call themselves in their own language, Euskara, claim to be the oldest
unmixed race in Europe. Euskara is totally unintelligible to the Spanish and is related in no way to any other language. Their
original home was the Pyrennees Mountains. Their history is an account of repeated and determined efforts to defend the rights
and privileges (fueros) that they, as a distinct people, have enjoyed down through the centuries. In 1201, they stubbornly
rejected a union with other provinces in Spain until they were guaranteed certain rights.
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1798
| HISTORY
OF JAI-ALAI
The first indoor fronton was built in Marquena, Spain.
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| 1898 | Cesta punta was introduced in Cuba. |
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| 1904 | The
first Jai-alai fronton in America was built in St. Louis, MO during the 1904 World's Fair. It opened on May 15. However,
after only two months, the Jai-alai operations ended and the fronton later became the Winter Garden skating rink. |
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| 1924 | The first fronton in Miami
was built as part of the Hialeah complex. |
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| 1925 | The New Orleans fronton was built. |
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| 1926 | On September 18, the original Miami fronton was destroyed by a hurricane. Jai-alai was first played professionally at the Miami fronton.
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| 1927 | Jai-alai began in Chicago at the Rainbo Fronton ( Rainbo Gardens). |
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| 1934 | Wagering on Jai-alai was
legalized. |
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| 1938
| Jai-alai was introduced at the Hippodrome in New York, NY, but play only took one short
season. |
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| 1947 | Fronton Palacio in Tijuana, Mexico opened. |
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| 1953 | Dania Jai-alai and Tampa
Jai-alai opened. |
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| 1955 | West Palm Beach Jai-alai opened. |
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| 1959 | Daytona Jai-alai opened.
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| 1962 | Orlando Jai-alai opened. |
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| 1968 | The use of helmets was mandated. A players strike led to the blacklisting of many players. |
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| 1971 | Melbourne Jai-alai in Florida opened.
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| 1973 | Ocala Jai-alai in Florida opened. |
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| 1974 | Fort Pierce Jai-alai opened. |
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| 1976 | Hartford Jai-alai and Bridgeport Jai-alai, both in Connecticut, opened. Newport Jai-alai in Rhode Island opens. |
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| 1977 | Milford Jai-alai opened. |
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| 1978 | Big Bend Jai-alai in Florida
opened. |
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| 1992 to 2003 | Many of the major Jai-alai
frontons in Connecticut, Rhode Island and Florida closed down. |
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| 2004 | In April 4, the ground-breaking ceremony for Hamilton Jai-alai was held. It is the first new fronton
in 22 years. |
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JORDAN CRATERS NOTICE PERSON (circled)
The Owyhee uplands are part of the Basin and Range physiographic province. The Basin and Range is an area of fault-block
topography, mountain ranges running north to south separated by broad basins. "The
Owyhee uplands lie in the northwest corner of the Great Basin. This region differs from the rest of the province in that it
is a flat deeply dissected plateau with little interior drainage where fault-block topography is less pronounced. The drainage
basin of the Owyhee River encompasses the uplands. Originating in Nevada, the Owyhee River flows northerly through Idaho and
Oregon to join the Snake River near Adrian, Oregon. In spite of low rainfall in the area, steep gradients give the the [sic]
river and its tributaries well-defined drainage patterns and deep canyons. Cutting through the uplands over 6,000 feet above
sea level, the river drops to approximately 2,000 feet where it joins the Snake. Small streams flowing in from the hills are
largely intermittent." (Orr E. L. and W. N. Orr. 1999, Geology of Oregon. Kendall/Hunt Publishing Co., p 79)
The geological background of this province is based in volcanic activity which started in the Miocene. There are deep
volcanic deposits of basalts, tuffs and tuffaceous sediments. While basalt is prevalent, other features include rhyolite,
diatomaceous deposits, new sedimentary deposits and new surface lava. The episodes of deposition affecting the Owyhee uplands
include the Owyhee Basalts that erupted onto the plateau 13-12 million years ago and the ash-flow tufts from the Steens mountains
around the same time. In a few areas there has been relatively recent volcanism, of special note is Jordan Craters. The Jordan Craters lava flow is located in the Owyhee uplands on the plateau. It is a 75 square
kilometer olivine basalt flow that is extremely recent by geological time. Potassium argon (K-Ar) dating shows that it is
no older than 30,000 years. However, "studies based on growth rates of lichen and weathering rates of exposed and unexposed
basalt suggest that the flow may be between 4,000 and 9,000 years old". "Additionally the southeasterly flowing
lava altered ancestral drainage patterns, giving rise to a natural dam and the formation of two small lakes (Upper and Lower
Cow Lakes)" (Wood and Kienle 1990. Volcanoes of North America: United States and Canada. Cambridge University Press,
p 211)
INFORMATION WEBSITES ABOUT THE JORDAN CRATERS:
http://vulcan.wr.usgs.gov/Volcanoes/Oregon/JordanCraters/description_jordan_craters.html
http://www.volcano.si.edu/world/volcano.cfm?vnum=1202-9-
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COW LAKES 14 MILES WEST OF JORDAN VALLEY _______________________________

PHOTO OF THREE FINGERS ROCK (can be seen near
the Oregon-Idaho border on Hwy. 95)
WHERE TO GO --- WHAT TO SEE
Jordan Valley is located on U.S.
Hwy. 95, between Idaho and Nevada in Southeastern Oregon. Come and visit with us! Jordan Valley is the center for many fascinating side trips, from a few miles to
25 or 35 miles distance. Scenery of the area has been compared to places as magnificent as the Grand Canyon.
• Succor
Creek Canyon is a scenic canyon, with many interesting rock formations. A rock hound's paradise. • Silver City, Idaho—An
abandoned mining town to explore, with Old Hotel and homes. • Antelope Reservoir-- Trout fishing and boating. • Leslie Gulch--
Rock formations of rugged beauty, ending at Owyhee Reservoir where there is good fishing for bass and crappie. • Owyhee Breaks--
From Mahogany Mountain – a view comparable to Grand Canyon's beauty. • Jordan Crater-- Active less than
2500 years ago, explore in and around, with dead lava flows. • Rattlesnake Caves-- A large cave abounding with
rattlesnakes. •
Rome Cliffs-- Fascinating rock formations resembling castles, at Rome, Oregon • Owyhee River-- Excellent white
water rafting and kayaking, fishing. • DeLamar Silver Mine—Located in the Owyhee Mountains, at one time a large
producer of silver and gold, and no longer in operation. • Big Loop Rodeo-- 20' Loop horse roping and
events. Every 3rd weekend in May – nationally acclaimed with many vendors. • Cow Lakes—Two lakes about
14 miles west of Jordan Valley, with boat ramps and restrooms. • Jordan Valley Pelota Frontoia-- Basque
Handball Court built in 1915, restored in 1997. • Jean Baptiste Charbonneau's Historic Gravesite-- Son of
Sacagawea & Toussaint Charbonneau (Lewis & Clark Expedition), buried in Danner, some 15 miles from Jordan Valley. • Everywhere—Petrified wood,
Indian relics, agates, crystals, etc can be found in the vicinity of Jordan Valley.
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| CLICK ON LINK BELOW OR ON PHOTO FOR MORE INFO: |
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PILLARS OF ROME WEST OF JORDAN
VALLEY
ENTRANCE TO JORDAN VALLEY CITY PARK Dedication plaque, Bell, and Peacepole
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