Uploaded February 2022 | Updated September 2026, 2 hours ago
Off and on rain finally turned more off than on so we cust our Many Pools Trail hike short. While it lasted it was very pretty.
Many Pools Trail is a 2.3 mile heavily trafficked out and back trail located near Springdale, Utah that features beautiful wild flowers and is rated as moderate. The trail is primarily used for hiking, walking, and nature trips and is accessible year-round.
Less than half a mile east of the small tunnel in the upper East Canyon is a pair of drainages north of Route 9 with many unofficial nicknames. "The Root Canals" (and "The Twins") refers to the drainages' resemblance to a molar's roots on the topo map. East Root Canal is also more popularly known by locals as "Many Pools" because of its many interesting pothole formations. This open wash makes for a lovely leisurely hike in some beautiful sandstone scenery and is most interesting during spring runoff or after recent rainstorms.
Drive along the Zion-Mt. Carmel Highway, heading east from the small tunnel and look for the second drainage on the north side of the highway. Large white monoliths are visible landmarks from the road as well as the hiking route that passes between a small dome-like mountain and a larger mountain to the right. There is a pull-out .8 miles from the end of the small tunnel where you park, before continuing on foot 150 yards east, following the beaten path down into the bowl on the north side of SR-9. Stay in the drainage, going away from the 1930's built culvert. The terrain changes from soft sand to smooth washed stone and walls open up as northern travel leads to potholes, and big slabs of flat stone make a nice walking path. A big rock, that appears to be laying on its side, forms a short slot canyon on the right. Two large Ponderosa Pines and two large Juniper trees offer a momentary reprieve from the sun on a hot summer day while a huge boulder provides a charming backdrop for a dwarf waterfall about a half-mile into this scenic stroll. Soon the "trail" gets steeper as water-gnawed receptacles become more common. To the east is a black-capped hoodoo and impressive views are revealed in all directions. Some distant slickrock is carved with crossbedding similar to that on Checkerboard Mesa and there are many water filled basins.
nmosg.com
Off and on rain finally turned more off than on so we cust our Many Pools Trail hike short. While it lasted it was very pretty.
Many Pools Trail is a 2.3 mile heavily trafficked out and back trail located near Springdale, Utah that features beautiful wild flowers and is rated as moderate. The trail is primarily used for hiking, walking, and nature trips and is accessible year-round.
Less than half a mile east of the small tunnel in the upper East Canyon is a pair of drainages north of Route 9 with many unofficial nicknames. "The Root Canals" (and "The Twins") refers to the drainages' resemblance to a molar's roots on the topo map. East Root Canal is also more popularly known by locals as "Many Pools" because of its many interesting pothole formations. This open wash makes for a lovely leisurely hike in some beautiful sandstone scenery and is most interesting during spring runoff or after recent rainstorms.
Drive along the Zion-Mt. Carmel Highway, heading east from the small tunnel and look for the second drainage on the north side of the highway. Large white monoliths are visible landmarks from the road as well as the hiking route that passes between a small dome-like mountain and a larger mountain to the right. There is a pull-out .8 miles from the end of the small tunnel where you park, before continuing on foot 150 yards east, following the beaten path down into the bowl on the north side of SR-9. Stay in the drainage, going away from the 1930's built culvert. The terrain changes from soft sand to smooth washed stone and walls open up as northern travel leads to potholes, and big slabs of flat stone make a nice walking path. A big rock, that appears to be laying on its side, forms a short slot canyon on the right. Two large Ponderosa Pines and two large Juniper trees offer a momentary reprieve from the sun on a hot summer day while a huge boulder provides a charming backdrop for a dwarf waterfall about a half-mile into this scenic stroll. Soon the "trail" gets steeper as water-gnawed receptacles become more common. To the east is a black-capped hoodoo and impressive views are revealed in all directions. Some distant slickrock is carved with crossbedding similar to that on Checkerboard Mesa and there are many water filled basins.
nmosg.com





![Pecos River Flume - Carlsbad, NM
The Pecos River Flume is an aqueduct carrying irrigation water over the Pecos River. Construction took place from 1889 to 1890 and was part of the Pecos River Reclamation Project. It was originally constructed of wood and spanned 145 feet. It carried water at a depth of 8 feet. In 1902, a flood destroyed the flume and it was subsequently rebuilt using concrete. In 1902, it was identified as the largest concrete aqueduct in the world.
The flume and its surrounding area have been reclaimed by the city of Carlsbad and transformed into a tourist attraction, with park improvements along the river and spotlights to give a spectacular nightly view.
The Pecos River, in New Mexico and Texas, is yet another river at risk of drying up soon. It runs for around 926 miles and runs from the Sangre de Cristo Mountains near Santa Fe, New Mexico into the eastern part of the state of Texas before emptying into the Rio Grande just below the Hwy 90 bridge west of Del Rio.
The Pecos River (Spanish: Río Pecos) originates in north-central New Mexico near Santa Fe and flows into Texas, emptying into the Rio Grande. Its headwaters are on the eastern slope of the Sangre de Cristo mountain range in Mora County north of Pecos, NM, at an elevation of over 12,000 feet. The river flows for 926 miles before reaching the Rio Grande near Del Rio.
The name Pecos derives from the Keresan (Native American language) term for the Pecos Pueblo, [pæyokona]. The river was also historically referred to as the Río Natagés for the Mescalero people.
The river played a large role in the exploration of Texas by the Spanish.
On June 6, 1990, 20.5 miles of the Pecos River from its headwaters to the townsite of Tererro received National Wild and Scenic River designation.
nmosg.com Pecos River Flume - Carlsbad, NM](https://i.ytimg.com/vi/YiKJ38bcSCY/mqdefault.jpg)



![San Jose, New Mexico on the Pecos River June 2022
San Jose was founded in 1803 when allotments of land were made to 45 men and two women by the Spanish government of New Mexico. The purpose of the settlement, and others in the Pecos River valley, was to defend the eastern flanks of the New Mexican settlements from Indian attacks, especially by the Apaches. Many of the early settlers were landless genizaros. Many of the comancheros and ciboleros who traded with the Comanche and hunted bison on the Great Plains came from San Jose and other Pecos Valley settlements.
The original adobe homes were built closely together around a square, which could be closed for defense in times of Indian raids. In March 1803, nine years after the founding of San Jose, Pedro Rautista Pino, acting on orders of the governor, partitioned the land to the 47 heads of households of San Jose.
After the establishment of the Santa Fe Trail in 1821, San Jose became one of the many stops along the trail in the Pecos River Valley.
In May 1826, permission was granted, by the Bishop of Durango, to erect a church at San Jose. San Jose was under the jurisdiction of Nuestra Senora de Los Angeles church at the Pecos Pueblo until nearby San Miguel Del Vado was made a parish and provided with a priest.
In 1846, a passenger stagecoach service was established between Independence, Missouri and Santa Fe. The stagecoach route, which crossed the Pecos River ford at San Jose, had regular mail service by 1849 and daily passenger service by 1862. The stagecoach station was probably located in the southeast corner of the plaza.
As a result of the trade caravans and stagecoaches traveling along the trail, San Jose prospered and grew in population. This traffic became more important after the settlement of Las Vegas, as caravans began to bypass San Miguel and traveling a shorter route directly to San Jose.
In 1879, the construction of the Atchison, Topeka, and Santa Fe Railroad began in New Mexico. Once completed, the railroad bypassed San Jose, and traffic along the Santa Fe Trail all but ended. A steady decline in San Jose’s population followed.
Route 66 made its way through the village in 1926, probably stimulating the economy. However, it was short-lived and rerouted in 1937. Later, when the highway was replaced by U.S. 85 and I-25, the highways bypassed the town. An old Route 66 era steel truss bridge sits abandoned at the end of County Road B41D. Near the old bridge was the original Santa Fe Trail crossing of the Pecos River.
The Pecos River (Spanish: Río Pecos) originates in north-central New Mexico near Santa Fe and flows into Texas, emptying into the Rio Grande. Its headwaters are on the eastern slope of the Sangre de Cristo mountain range in Mora County north of Pecos, NM, at an elevation of over 12,000 feet. The river flows for 926 miles before reaching the Rio Grande near Del Rio.
The name “Pecos” derives from the Keresan (Native American language) term for the Pecos Pueblo, [p’æyok’ona]. The river was also historically referred to as the Río Natagés for the Mescalero people.
The river played a large role in the exploration of Texas by the Spanish.
On June 6, 1990, 20.5 miles of the Pecos River from its headwaters to the townsite of Tererro received National Wild and Scenic River designation.
nmosg.com San Jose, New Mexico on the Pecos River June 2022](https://i.ytimg.com/vi/ZRotaT4ardY/mqdefault.jpg)
