Pam examining thick moss growth on the sedimentary rock of Treman gorge. These layers of shale, sandstone, siltstone formed at the bottom of a broad, shallow sea over 380 million years ago.
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Pam examines the moss
Towards the bottom of the 223 Cliff Stair steps moss takes over the Devonian shale of the cliff wall surface. Here, the cliff shelters the wall from sunlight 365 days a year.
Cliff Stair Wall, autumn Moss
Robert H. Treman New York State Park.
Click for a slideshow of this sequence Lucifer Falls and Cliff Stair Views
Brink of Lucifer FallsLucifer Falls Overlook from the Gorge TrailLucifer Falls from Rim Trail OverlookPam on the Cliff StaircaseUnidentified TreeThis geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease and, in the Scottish Highlands, “red-shanks” for the deep red color of the stalks, seen in this photograph. Robert H. Treman New York State Park. Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.Autumn foot BridgeWoman on Footbridge, ContemplationOver the bridge
Copyright 2023 All Rights Reserved Michael Stephen Wills
This geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease.
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Cliff Stair Wall, autumn Geranium and mosses
Scottish Highlands residents call these wild geraniums “red-shanks” for the deep red color of the stalks, seen in both photographs.
This geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease and, in the Scottish Highlands, “red-shanks” for the deep red color of the stalks, seen in this photograph. Robert H. Treman New York State Park. Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.
Robert H. Treman New York State Park.
Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.
Click for a slideshow of this sequence Cliff Stair Views
Lucifer Falls from Rim Trail OverlookLucifer Falls from Rim Trail OverlookUnidentified TreePam on the Cliff StaircaseCliff Stair Wall, autumn with fern generationsCliff Stair Wall, autumn Geranium and mossesThis geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease and, in the Scottish Highlands, “red-shanks” for the deep red color of the stalks, seen in this photograph. Robert H. Treman New York State Park. Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.Wild geranium leaves tinged with autumn color above a gathering of spent oak and elm leaves. Robert H. Treman New York State Park of the Finger Lakes Region.
Copyright 2023 All Rights Reserved Michael Stephen Wills
Each autumn, species of fern turns yellow towards a winter death. Here we see growing from Devonian shale, both the yellowed and desiccated fern fronds. Robert H. Treman New York State Park.
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Cliff Stair Wall, autumn with fern generations
Click for a slideshow of this sequence Cliff Stair views
Lucifer Falls from Rim Trail OverlookPam on the Cliff StaircaseCliff Stair Wall, autumn with hemlock
Copyright 2023 All Rights Reserved Michael Stephen Wills
On a day in late October 2017 Pam and Mike did a photography walk. Here is Pam pausing to pose during a descent into the gorge on the cliff staircase after visiting the overlook high above Lucifer Falls, Robert H. Treman New York State Park in the Finger Lakes Region.
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Pam on the Cliff Staircase
Grasses, hemlock saplings, goldenrod, spent leaves and ferns on the wall of the 223 Cliff Stair steps.
Cliff Stair Wall, autumn with hemlock
Click for a slideshow of this sequence of Lucifer Falls view from the overlook.
Pam on the Cliff StaircaseCliff Stair Wall, autumn with hemlock
Copyright 2023 All Rights Reserved Michael Stephen Wills
The canyon below 110 foot Reavis Falls is a wild place of transcendent beauty.
With the afternoon in front of me, the trip back to camp was a slow pleasure. On the way in, I noted several stopping points to capture photographs. Here a natural rock sluice offers a foot tall waterfall, mirroring Reavis Falls, bracketed by white igneous stone.
This same stone offers a screen, the bright spring sun throwing the sparse leaves into sharp relief.
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