|
Granite Wash Pass
Granite Wash Pass is a gap between the Granite Wash Mountains and the Little Harquahala Mountains, in La Paz County, Arizona. Granite Wash Pass is located at the southwest end of the Granite Wash Mountains and the northwest end of the Little Harquahala Mountains. The apex of the pass is at an elevation of . History The Granite Wash Pass has been a route between the Colorado River and the interior of Arizona from November 1863 when teamsters Gird and Sage discovered a route what became the La Paz–Wikenburg Road through Granite Wash Pass. In the early years a waterhole, Granite Water existed within the pass. The maps of the route in later years, Granite Water is no longer mentioned. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gap (landform)
A gap is a geological formation that is a low point or opening between hills or mountains or in a ridge or mountain range. It may be called a col, notch, mountain pass, pass, saddle (landform), saddle, water gap, or wind gap, and geomorphology, geomorphologically is most often carved by water erosion from a freshet, stream or a river. Gaps created by freshets are often, if not normally, devoid of water through much of the year, their streams being dependent upon the meltwaters of a snow pack. Gaps sourced by small spring (hydrology), springs will generally have a small stream excepting perhaps during the most arid parts of the year. Water gaps of necessity often cut entirely through a mountain chain, barrier barrier ridge, range and riverine gaps may create canyons such as the riverine gaps of the Danube River, Lehigh River Gorge, the Colorado River's Grand Canyon and the Genesee River. Such cuttings may expose millennia of strata in the local rock column writing the geologic reco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite Wash Mountains
The Granite Wash Mountains are a short, arid, low elevation mountain range of western-central Arizona, in the southeast of La Paz County. The range borders a slightly larger range southeast, the Little Harquahala Mountains; both ranges form a section on the same water divide between two desert washes. The washes flow in opposite directions, one northwest to the Colorado River, the other southeast to the Gila River. Description The range is northwest-by-southeast trending and is in a region of about thirty landforms, plains, valleys, and mountain ranges, called the Maria fold and thrust belt. The region is in the Basin and Range and three mountain ranges are in a parallel, northwest-by-southeast trending thrust belt, with two intervening valleys. The Granite Wash Mountains are attached to the southwest end of the Harcuvar Mountains, the center range of the 3 basin and range-thrusted mountains. The Granite Wash range is on the same water divide as the Little Harquahala's and at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Harquahala Mountains
The Little Harquahala Mountains are a small, arid, low-elevation mountain range of western-central Arizona, in the southeast of La Paz County. The range is northwest-by-southeast-trending and is in a region of about thirty landforms, plains, valleys, and mountain ranges called the Maria fold and thrust belt. The region is in the Basin and Range and three mountain ranges are in a parallel, northwest-by-southeast-trending thrust belt, with two intervening valleys. The Little Harquahala Range borders the second valley and third mountain range, the McMullen Valley and Harquahala Mountains, on their southwest borders. The range is a section of a water divide for tributaries to two river watersheds on the Gila and Colorado Rivers. An even smaller range is connected north on the water divide, the 8-mile (13 km) long Granite Wash Mountains. Maria fold and thrust belt The three mountain ranges and two valleys bordered to the northeast: * Buckskin Mountains ** Butler Valley (Arizo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Paz County, Arizona
La Paz County is the 15th county in the U.S. state of Arizona, located in the western part of the state. As of the 2020 census, its population was 16,557, making it the second-least populous county in Arizona. The county seat is Parker. The name of the county is the Spanish word for "the peace", and is taken from the early settlement (now ghost town) of La Paz along the Colorado River. History La Paz County was established in 1983 after voters approved separating the northern portion of Yuma County, making it the only county to be established after Arizona became a state in 1912, and currently the second youngest county in the United States (behind the consolidated city-county of Broomfield, Colorado, which was established in 2001). The county did not have a large enough tax base to begin supporting a separate county government immediately and had to rely on state money at first. As a result, Arizona laws were changed to make splitting other existing counties much more d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colorado River
The Colorado River ( es, Río Colorado) is one of the principal rivers (along with the Rio Grande) in the Southwestern United States and northern Mexico. The river drains an expansive, arid drainage basin, watershed that encompasses parts of seven U.S. states and two Mexican states. The name Colorado derives from the Spanish language for "colored reddish" due to its heavy silt load. Starting in the central Rocky Mountains of Colorado, it flows generally southwest across the Colorado Plateau and through the Grand Canyon before reaching Lake Mead on the Arizona–Nevada border, where it turns south toward the Mexico–United States border, international border. After entering Mexico, the Colorado approaches the mostly dry Colorado River Delta at the tip of the Gulf of California between Baja California and Sonora. Known for its dramatic canyons, whitewater rapids, and eleven National parks of the United States, U.S. National Parks, the Colorado River and its tributaries are a v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arizona
Arizona ( ; nv, Hoozdo Hahoodzo ; ood, Alĭ ṣonak ) is a state in the Southwestern United States. It is the 6th largest and the 14th most populous of the 50 states. Its capital and largest city is Phoenix. Arizona is part of the Four Corners region with Utah to the north, Colorado to the northeast, and New Mexico to the east; its other neighboring states are Nevada to the northwest, California to the west and the Mexican states of Sonora and Baja California to the south and southwest. Arizona is the 48th state and last of the contiguous states to be admitted to the Union, achieving statehood on February 14, 1912. Historically part of the territory of in New Spain, it became part of independent Mexico in 1821. After being defeated in the Mexican–American War, Mexico ceded much of this territory to the United States in 1848. The southernmost portion of the state was acquired in 1853 through the Gadsden Purchase. Southern Arizona is known for its desert cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Paz–Wikenburg Road
La Paz–Wikenburg Road was a wagon road from 1863 and from 1866 a stagecoach route between the Colorado River landings at La Paz, Arizona, La Paz, Olive City, Arizona, Olive City and Mineral City, Arizona, Mineral City to the mining town of Wickenburg, Arizona. From Wickenburg roads led to other new mining camps and districts in the interior of Arizona Territory. From 1862, when the river changed its course, La Paz was isolated on the slough of the old river channel over from the new river channel. In 1866, the road head changed to the new river landing of Ehrenburg, Arizona, Ehrenburg, where the Bradshaw Trail wagon and stagecoach road from San Bernardino, California, crossed the Colorado River at Bradshaw's Ferry. References {{DEFAULTSORT:La Paz-Wikenburg Road La Paz–Wikenburg Road, 1863 establishments in the United States Geography of La Paz County, Arizona Geography of Yavapai County, Arizona Geography of Maricopa County, Arizona Historic trails and roads in Ariz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite Water, Arizona Territory
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alwa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Flood Of 1862
The Great Flood of 1862 was the largest flood in the recorded history of Oregon, Nevada, and California, occurring from December 1861 to January 1862. It was preceded by weeks of continuous rains and snows in the very high elevations that began in Oregon in November 1861 and continued into January 1862. This was followed by a record amount of rain from January 9–12, and contributed to a flood that extended from the Columbia River southward in western Oregon, and through California to San Diego, and extended as far inland as Idaho in the Washington Territory, Nevada and Utah in the Utah Territory, and Arizona in the western New Mexico Territory. The event dumped an equivalent of of water in California, in the form of rain and snow, over a period of 43 days. Immense snowfalls in the mountains of far western North America caused more flooding in Idaho, Arizona, New Mexico, as well as in Baja California and Sonora, Mexico the following spring and summer, as the snow melted. The even ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Wells, La Paz County, Arizona
Desert Wells, originally Desert Station, a stagecoach station on the La Paz–Wickenburg Road in the 1870s, is a populated place in La Paz County, Arizona, United States. It lies at an elevation of and is located 4.7 miles west-southwest of Vicksburg on U.S. Route 60. History Desert Wells was originally known as Desert Station, a stagecoach station on the La Paz–Wickenburg Road, in what was then Yuma County. It lay 26 miles from Tyson's Wells to the west and 20 miles from Flint's on Centennial Wash to the east. In 1875, it was seen by Martha Summerhayes, and later described in her book ''Vanished Arizona'': At night we arrived at Desert Station. There was a good ranch there, kept by Hunt and Dudley, Englishmen, I believe. I did not see them, but I wondered who they were and why they staid in such a place. They were absent at the time; perhaps they had mines or something of the sort to look after. One is always imagining things about people who live in such extraordinary plac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arizona And California Railroad
The Arizona and California Railroad is a class III short line railroad that was a subdivision of the Atchison, Topeka and Santa Fe Railway (ATSF). The ARZC began operations on May 9, 1991, when David Parkinson of the ParkSierra RailGroup purchased the line from the Santa Fe Railway. ParkSierra Railgroup was purchased in January 2002 by shortline railroad holding company RailAmerica. The Genesee & Wyoming shortline railroad holding company purchased RailAmerica in December 2012. ARZC's main commodities are petroleum gas, steel, and lumber; the railroad hauls around 12,000 carloads per year. Route At Cadiz, California, the railroad begins in the interchange with the BNSF Railway and continues southeast across the Mojave Desert to Rice, then east to cross the Colorado River Arizona/California state line at Parker, Arizona. The railroad continues southeast to Hope near Vicksburg then northeast to Matthie (near Wickenburg, Arizona). At Matthie, ARZC has trackage rights over the nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.png "Click for more on -> Arizona")
