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Devil’s Cornfield
Mesquite Sand Dunes
Death Valley National Park
California
February 2024
Nestled between Stovepipe Wells and Beatty Junction along Highway 190, you'll discover the enigmatic Devil's Cornfield, just a stone's throw east of the Mesquite sand dunes. Here, the landscape is adorned with the distinctive presence of arrowweed (Pluchea sericea), an evergreen plant that weaves tales of its ancient use. Echoing its common name, this remarkable plant once served as the sturdy backbone for crafting arrows by Native Americans, adding a touch of history to the allure of this unique terrain.
For my video; youtu.be/8nzA3b2Zqzg?si=ULf8dc3b-v_M-cr1,
Apslawn, Tasmania, Australia.
Devil’s Corner is home to some of the region’s best wine and food experiences, 360-degree views, and all four seasons in one day.
Alaska Botanical Garden
Anchorage, Alaska
Minolta X-700, MC Rokkor 28mm f/2.8
Ektachrome Copied Into Digital Camera
They call this pool the Devil's Bath, located in Wai-O-Tapu in New Zealand. The color is the result of water mixing with sulphur and ferrous salts. The color changes quite a bit depending on the reflected light and cloud color. I really liked how it photographed with these menacing clouds.
Suria agreed to be photographed in this devil costume one more time just for Red Golden. Not quite as foul looking this time. (See the earlier photo below). She must be mellowing.
Devils Postpile is an unusual landmark located near Mammoth Mountain in eastern California. The hexagonal columns are a result of volcanic activity
This is the 'Mountain Devil' protea. aka: 'Lambertia formosa'
Lambertia formosa, commonly known as 'Mountain Devil', is a shrub of the family Proteaceae, endemic to New South Wales, Australia. It was first described in 1798 by English botanist James Edward Smith.
This one was located along a forest trail in the Ku-ring-gai Wildflower Garden, along Mona Vale Road, at St Ives Chase, in northern Sydney.
For information about 'Lambertia formosa' see the Australian Native Plants Society:
My Canon EOS 5D Mk IV, with the Canon f 2.8. L 100mm macro lens
One of the earliest descriptions of Devils Kitchen, which involved a collapse event there, was retold by long-term resident Albert E. Thompson (1968), "My parents were living in Sedona in the early 1880s and heard the crash when the spot caved in. Mother said the dust from the cave-in filled the air all day and the sun looked like it was shining through heavy smoke. Her brother, Jim James, was the first one to see the new hole in the ground".
In late 1989, a second historic collapse event occurred at Devils Kitchen, enlarging the opening by as much as 1/3rd. The 1989 event was largely limited to the north wall, where a gigantic block, detached along three bounding walls from its caprock, rotated outward into the opening without dropping to a lower elevation. Edges of the newly broken rocks are highly angular and the surface soil has not yet begun to slough off.
Collapse of the southernmost wall of the sinkhole pre-dated historic collapse events and probably represents an early, formative event in the history of Devils Kitchen. In contrast to the fresh, angular appearance of historically broken blocks, blocks of the south wall display rounded edges and the surfaces carry a patina of manganese oxide that suggests open exposure over several hundred years.
The Devils Kitchen sinkhole is the most active of the seven sinkholes in Sedona. It has an opening 150 feet by 90 feet, with the floor situated 35 to 70 feet below the rim. Lindberg estimates that caverns in the Redwall Limestone, could have volumes on the order of 1.3 million cubic feet (a cave roughly 100 feet high and 130 feet in diameter).
Seaford & District Dennis Trident SFZ 404 at Devils Dyke operating on service 77 having just completed its first trip. This bus was new to Brighton & Hove as T819 RFG. Back during it's B&H days this bus operated a lot on the 77 so it was great to be able to have it on this route.
The doors are about to open on the next round of TMD and you do NOT want to miss out on these! Cult isn't just for the ladies!! We have something for EVERYONE! This brand new ring set will ONLY be available at TMD and is NOT available in our mainstore. Don't miss out!
Devil with HUD
- 100% Original Mesh
- Rigged for Jake, Legacy Male, Gianni
- Color Hud
- Baked Textures
TO TMD ---> SLURL: maps.secondlife.com/secondlife/TMD/125/150/22
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"A brave man is a man who dares to look the Devil in the face and tell him he is a Devil."
~ James A. Garfield
"Devil's Cave" near the city of Maastricht. Shot by phone
A quick stop yesterday to check out the Devil's Slide. No line for this ride.
Home » Rock Talk Library » Geologic Wonders - The Devil's Slide
Geologic Wonders - The Devil's Slide
The Devil‘s Slide is one of the more unusual natural form-ations along the wall of Weber Canyon, in Utah. There, two limestone layers, tilted to near vertical, rise 40 feet above the canyon wall with 25 feet separating them. Looking like a large playground slide fit only for the Devil, this site is a tilted remnant of sediments deposited in a sea that occupied Utah‘s distant geologic past. About 170 to 180 million years ago, a shallow sea originating from the north spread south and east over areas of what are now Montana, Wyoming, and Utah. This sea extend as far east as the present-day Colorado River and south into northern Arizona. Over millions of years, massive amounts of sediment accumulated and eventually formed layers of limestone and sandstone. In northern Utah, these rocks are know as the Twin Creeks Formation and are approximately 2700 feet thick. About 75 million years ago, folding and faulting during a mountain-building episode tilted the Twin Creek rock layers to a near-vertical position. Subsequent erosion of softer material has exposed the near vertical limestone layers and created Devil‘s Slide.
Information for this article came from:www.geology.utah.gov
© Lindbloom Photography
Looking out over Devil's Garden in Arches National Park near Moab, Utah. This is a view to the north looking over the fins of Devil's Garden.
Things are a little easier with my daughter at the moment and thank you for all your kind wishes. I hope to start catching up with you all very soon.
Yesterday I had the chance to go out to the Devil's Dyke near Brighton. The 300 ft deep V shaped valley in the South Downs was caused by melting snow waters forming rivers after the last ice age and it makes for an impressive sight and invigorating walking. If you look very carefully, you may see some of the dog walkers at the bottom of the valley.
The piece of concrete to the right is the remains of some long forgotten building, parts of which can be found scattered down the slopes and in the valley itself.
With the mythical "Devil's Wall" (Teufelsmauer) standing proud in the landscape beyond, HSB 99 7243-1 drifts down the grade near Quarmbeck working service train 8962 09.59 Gernrode to Quedlinburg on 3rd March 2026. This former standard gauge alignment of today's metre gauge Selketalbahn has a higher permitted running speed of 50 km/h.
en.wikipedia.org/wiki/Teufelsmauer
© Gordon Edgar - All rights reserved. Please do not use my images without my explicit permission
Carnock Burn, Finnich Glen.
Getting here meant walking up the river which was very cold. Luckily feet warmed up after a couple of minutes.
Bighorn Canyon Reservoir and the Devils Canyon Anticline from the Devil's Canyon Overlook in Bighorn Canyon National Recreation Area jiust across the Wyoming border in Montana.
Sunrise at the Devils Jaw, Senja, Arctic Norway. Didnt quite get the light we hoped for that morning but I did like the reflections in this little pool.
Thanks for all your comments and favs....much appreciated.
Regards
RS