Reaching Reavis Falls, once you find the canyon mouth, is three-fourths of a mile of boulder hopping and bushwacking over and around landslides, deep pools and fallen trees. Odds are you will be the only person in the canyon for weeks, if not months. Expect to be surprised. In this chapter you will (finally) visit the falls themselves.
A Camp in the Canyon
Click me for the chapter about the environment around the mouth of Reavis Canyon below the falls.
The Last Mile
Here is an overview of the last third mile of Reavis Canyon. You can see the wall of the falls nestled in the folds of ridges towards the top, just off center.
On the lower right is a large landslide and, below there, it is complete chaos.
The vegetation grows shoulder to shoulder with interleaved branches. You will not get through there. The solution is to find a way around, usually over and around house-sized boulders.
The image was captured from Google Earth
After almost two hours of picking my way, there was a flicker of light. The fall waters were sparkling in the sunlight high above the cottonwood trees, in full Mach bloom, and the still leafless Arizona Sycamores.
This was my view of Reavis Falls from the canyon on a March day before the Arizona Sycamores have leaved. The falls are the tiny patch of white to the left of midline where the earth meets the sky. Jumbles of infallen boulders and thick growth of sycamores, oaks and fully leaved cottonwoods cloak the falls.
Another 30 minutes of canyoneering brought me to the foot of the falls.
At the Foot of Reavis Falls
Looking up at Reavis Falls from a 20 foot tall mound of talus.
These are boulders washed down at flood time.
The rock wall is thick with microorganisms, fungi and mosses.
After clambering around the talus pile I found this angle….
An Arizona Sycamore, before the spring leafing, at the Foot of Reavis Falls
Talus at the Foot of Reavis Falls
The Reavis Falls talus is large boulders carried down Reavis Creek and washed over the falls at flood time as well as blocks fractured from the cliff face. You can see the base of the Sycamore from the previous photograph.
The falls are formed where Reavis Creek flows over a solid mass of rock. The talus is composed mostly of this red rock. From the edge of this cliff to the base, where the falls hit the canyon floor, is all of 140 feet. This is a far as you can proceed into the canyon without some serious climbing skills.
It is possible to climb around the canyon by climbing up the ridge from which I captured the Cedar Basin Hoodoos. See my posts below for this location (you need to work it our for yourself).
This is NOT the last post of the series. From here I will focus on the beauty of Reavis Falls and the canyon that holds them.
It was a four-day expedition so there are a few chapters covering the approach to the Falls:
The Superstition Wilderness was born from volcanic eruption and in some places (Peters Mesa) the earth still rumbles.
Here in Reavis Canyon it is the huge spring runoff that builds the environment, grinding and scouring the canyon. In my chapter The Mouth of Reavis Canyon is the story of this aspect of the canyon.
The history of this spot is written on these volcanic and igneous rocks and boulders, the uprooted tree roots and fresh water.
The tire must have washed down from Reavis Ranch.
A Canyon of Wonder and Beauty
In this chapter I present, in the header, the lovely dawn sky of that day, and a tiny corner of a rock jumble in Reavis Creek. There is a large format version of the sky in my previous post, “The Mouth of Reavis Canyon.”
Rivulets and Rocks
Copyright 2023 Michael Stephen Wills All Rights Reserved
Here is the same view, in daylight. As I hiked toward the canyon mouth below Reavis Falls, looking up I saw this prominant cliff against the sky.
Here is the path I took toward the falls. The campsite is to the lower right, the falls are toward the center and left. My approach to the camp is on the right, moving toward the top. For another view of this location see Reavis Canyon Camp.
The mouth of Reavis Canyon below the falls is choked with vegetation and infallen rocks and boulders. The far slopes are thick with the poles of young saguaros. There are hoodoos, as well. In the photograph, below, one hoodoo is catching morning light. See the chapters Hoodoos on the Descent to Reavis Falls and Cedar Basin Hoodoos for more views of the hoodoos around Reavis Falls.
Hoodoos visible from the mouth of Reavis Canyon below the falls. Look toward the far slope.
Flood damage in Reavis Canyon below the falls. Note the scouring at the base of these trees and the broken limbs. This is NOT a place to be in spring thaw.
Massive spring flooding scours the canyon floor.
Flood damage in Reavis Canyon below the falls.
There is beauty to be found, as well. Freshly fallen rough rocks contrast with water smoothed boulders and the water surface.
Copyright 2023 Michael Stephen Wills All Rights Reserved
After spreading 15,000 square feet of crabcrass/fertilizer and before attending a frigid first baseball game of a grandson, I capture eight photographs of five different flowers from our home.
More about the Magnolia, from Wikipedia: The name Magnolia first appeared in 1703 in the Genera of Charles Plumier (1646–1704), for a flowering tree from the island of Martinique (talauma). It was named after the French botanist Pierre Magnol.
More about the Hydrangea, from Wikipedia: Hydrangea is derived from Greek and means ‘water vessel’ (from ὕδωρ húdōr “water” + ἄγγος ángos or αγγεῖον angeîon “vessel”), in reference to the shape of its seed capsules.
More about these Quince, from Wikipedia: Although all quince species have flowers, gardeners in the West often refer to these species as “flowering quince”, since Chaenomeles are grown ornamentally for their flowers, not for their fruits.
More about Forsythia, from Wikipedia: The genus is named after William Forsyth (1737–1804), a Scottish botanist who was a royal head gardener and a founding member of the Royal Horticultural Society.
More about Forsythia, from Wikipedia: Narcissus is a genus of predominantly spring flowering perennial plants of the amaryllis family, Amaryllidaceae. Various common names including daffodil, narcissus, and jonquil are used to describe all or some members of the genus. Narcissus has conspicuous flowers with six petal-like tepals surmounted by a cup- or trumpet-shaped corona. The flowers are generally white and yellow (also orange or pink in garden varieties), with either uniform or contrasting colored tepals and corona.
Copyright 2023 Michael Stephen Wills All Rights Reserved
I read the New York Times on our porch on a spring Sunday afternoon, taking a moment to capture these fair weather cumulus clouds. Visible are Ithaca’s East Hill, downtown, and a forsythia bush in flower.
More about the flowers, from Wikipedia: Forsythias are popular early spring flowering shrubs in gardens and parks, especially during Eastertide; Forsythias are nicknamed the “Easter Tree”, the symbol of the coming spring.
More about this view, from Wikipedia: Cumulus clouds can form in lines stretching over 480 kilometers (300 mi) long called cloud streets. These cloud streets cover vast areas and may be broken or continuous. They form when wind shear causes horizontal circulation in the atmosphere, producing the long, tubular cloud streets. They generally form during high-pressure systems, such as after a cold front.
Copyright 2023 Michael Stephen Wills All Rights Reserved
The combination of water vapor in all its forms and the sun dipping below the horizon combined to form these magical images.
Maxfield Parrish refined his art to duplicate these effects in oil.
Parrish’s art is characterized by vibrant colors; the color Parrish blue was named after him. He achieved such luminous color through glazing. This process involves applying layers of translucent paint and oil medium (glazes) over a base rendering. Parrish usually used a blue and white monochromatic underpainting.
His paintings/illustrations were unique in that they depicted a highly idealized fantasy world that was accessible to the public. Although you will rarely see a glimpse of that color in reality, he was and still is linked with a particularly bright shade of blue that coated the skies of his landscapes. And it was not an easy task for him to complete. He invented a time-consuming process that involved a cobalt blue base and white undercoating, which he then coated with a series of thin alternating coatings of oil and varnish. When exposed to ultraviolet light, the resins he employed, known as Damar, fluoresce a shade of yellow-green, giving the painted sky its distinctive turquoise tint.
Reference: “Maxfield Parrish” from Wikipedia
Copyright 2023 Michael Stephen Wills All Rights Reserved
Cumulonimbus (from Latin cumulus ‘heaped’, and nimbus ‘rainstorm’) is a dense, towering vertical cloud, typically forming from water vapor condensing in the lower troposphere that builds upward carried by powerful buoyant air currents.
Above the lower portions of the cumulonimbus the water vapor becomes ice crystals, such as snow and graupel, the interaction of which can lead to hail and to lightning formation, respectively. When occurring as a thunderstorm these clouds may be referred to as thunderheads. Cumulonimbus can form alone, in clusters, or along squall lines.
Graupel also called soft hail, hominy snow, or snow pellets, is precipitation that forms when supercooled water droplets in air are collected and freeze on falling snowflakes, forming 2–5 mm (0.08–0.20 in) balls of crisp, opaque rime.
Graupel is distinct from hail and ice pellets in both formation and appearance. However, both hail and graupel are common in thunderstorms with cumulonimbus clouds, though graupel also falls in winter storms, and at higher elevations as well.
These clouds can produce lightning and other dangerous severe weather, such as tornadoes, hazardous winds, and large hailstones. Cumulonimbus progresses from overdeveloped cumulus congestus clouds and may further develop as part of a supercell. Cumulonimbus is abbreviated Cb.
Reference: “Cumulonumbus Cloud” and “Graupel” from Wikipedia
Copyright 2023 Michael Stephen Wills All Rights Reserved
In more recent centuries Loughcrew became the seat of a branch of the Norman-Irish Plunkett family, whose most famous member became the martyred St Oliver Plunkett. The family church stands in the grounds of Loughcrew Gardens. With its barren isolated location, Sliabh na Caillí became a critical meeting point throughout the Penal Laws for Roman Catholics. Even though the woods are now gone an excellent example of a Mass Rock can still be seen on the top of Sliabh na Caillí today. The Plunketts were involved in running the Irish Confederacy of the 1640s and were dispossessed in the Cromwellian Settlement of 1652. Their estate at Loughcrew was assigned by Sir William Petty to the Napier Family c.1655. The Napiers are descended from Sir Robert Napier who was Chief Baron of the Exchequer of Ireland in 1593.
Michael Stephen Wills Photography 
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