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Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
Looking south from near the summit plateau of Maol Chean-dearg, with An Ruadh-Stac on the right and Meall nan Ceapairean on the left and Glen Carron in the background between them.
The boulder field in the foreground and the reddish outcrops beyond it are formed from Torridonian sandstone; An Ruadh-Stac and the south spur of Maol Chean-dearg (white triangle on left) are composed of Cambrian quartzite, on which very little can grow.
Stitched from two shots; I posted a different processing of the right hand half back in 2016.
This is Mount Olympus as seen from the East. It was a very foggy day down below. At this height, however, you can just see over the Oquirrh Mountains to the Stansbury Mountains beyond. The high point in the distance beyond the fog is Deseret Peak.
The Cooney and South Cooney Hills rise above the Wheatland Flats southwest of Wheatland in Platte County, Wyoming. The Wheatland Flats are composed of Pleistocene–Quaternary gravel stream terraces resting on an irregular surface of fine-grained Tertiary sediments.
The hills themselves are built of Archean metamorphic rocks. These include supracrustal greenstones and amphibolites—metamorphosed basaltic lavas—layered with chlorite and hornblende schists, micaceous quartzite, and thin beds of calc-silicate and iron formation. Later granitic intrusions, also Archean in age, were metamorphosed to gneiss. Sheared zones in the complex contain quartz-chlorite veins along with graphite, magnetite, epidote, and minor accessory minerals.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
The D&I crosses over the magnificent Sioux Falls on a girder bridge built by the Great Northern in 1919. The rock foundations you see here are made of Sioux quartzite, a type of rock native to the three corners of South Dakota, Minnesota, and Iowa. Significant quartzite mining took place around the falls in the 19th Century. The D&I continues to be a major shipper of quartzite from the LG Everist quarries in Dell Rapids.
This is Britain's most northerly mountain over 2500 feet - Beinn Spionnaidh. In fact it maybe the most northerly mountain full stop. This is the view from neighbouring Cranstackie, which as you can see has a fair coating of loose quartzite boulders. Bienn Spionnaidh is worse in that almost the entire east slope almost down to the shores of Loch Eriboll (the sea loch on the right of this picture) right up to the summit is covered in quartzite. These boulders are rough, they rock and move about, they are like soap when wet and like sandpaper when dry. In other words, Beiinn Spionniadh looks quite gently and rolling, but its actually hard work. However, as they say, nothing worthwhile is easy! When combined with Cranstackie on a day like this was, it's a grand day out with amazing views over Loch Eriboll, the A'Mhoine penisula, to Ben Hope and Ben Loyal towasrds the east; to the north west is the Kyle of Durness, Faraid Head and north west to Cape Wrath; to the south is Foinaven, and to the west are the epic beaches of Sandwood Bay and Oldshoremore. In short it's brilliant and I would be back up there tomorrow if I could.
Zoom in and be there!
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en.wikipedia.org/wiki/Foothills_Erratics_Train
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Nikon Nikkor 18-200mm 1:3.5-5.6 G ED-IF AF-S VR DX
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Transported by wind more than 183 million years ago, tiny grains of quartzite sand covered much of what we now call Utah. These sand dunes, up to 2,500 feet thick, eventually were cemented into stone. Burnt orange to creamy white in color, Navajo sandstone, the predominant rock in the park, is what remains of the ancient desert sand sea. Over time, water has cut and shaped the sandstone to form canyons. Approximately 1.4 million years ago, and as recently as 27,000 years ago, nearby cinder cones erupted, causing lava to flow down these canyons, filling them with basalt. This redirected ancient waterways, eventually carving new canyons.
The quartzite sandstone pillars of Zhangiajie National Park in blue morning light, UNESCO World Heritage,Tianzhan, Wulingyuan Hunnan Province, China. There was thick air pollution throughout eastern China during my trip there, which obscured many of the landscape features and sucked the colour from distant landscapes, but, as in this case, also added atmosphere to an early morning image. This scenery provided inspiration for the movie Avatar.
10/12/2107 www.allenfotowild.com
The breakwater near the ferry terminal on White Head Island in New Brunswick, Canada.
White Head Island is only accessible via a (free) ferry on Grand Manan Island.
It is such rocks, dating back to the Middle Neoproterozoic period and comprised of fine-grained white quartzite interstratified with dark grey to black carbonaceous shale, which are the origins of its namesake.
The colors of Killarney Provincial Park Ontario. Great fall colors against the white quartzite mountains.
The Stiperstones is a distinctive hill in the county of Shropshire, and is a quartzite ridge formed some 480 million years ago. During the last Ice Age the summit stood out above the glaciers and was subject to constant freezing and thawing which shattered the quartzite into a mass of jumbled scree surrounding several residual rocky tors. One of them is pictured here. At 1,759 ft above sea level it is the second-highest hill in the county, surpassed only by Brown Clee Hill (1,772 ft). Stiperstones' five-mile summit ridge is crowned by several rugged, jagged outcrops of rock silhouetted against the sky. The area around the Stiperstones was associated with lead-mining for hundreds of years with its heyday being in the 19th century. But all the mines closed long ago.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
Yosemite Nationalpark, so ziemlich genau vor 26 Jahren.
Nach dem Ranger-Talk sind wird noch eine Weile geblieben, hier oben an diesem spektakulären Aussichtspunkt. Während unterhalb die Wasser des Navada-Fall ohne Unterlass in die Tiefe donnern, geht im Hintergrund der Vollmond über der Sierra Nevada auf.
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Yosemite National Park, almost exactly 26 years ago.
After the ranger talk, we stayed a while up here at this spectacular viewpoint. While the waters of Nevada Falls thundered into the depths below without ceasing, the full moon rose over the Sierra Nevada in the background.
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Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
Bow Fiddle Rock is a natural sea arch near Portknockie on the north-eastern coast of Scotland. It is so called because it resembles the tip of a fiddle bow. It is composed of Quartzite, a metamorphic rock which was originally quartz sandstone.
This rock is part of the Cullen Quartzite formation which is seen along the coast between Buckie and Cullen. The formation is some 2,400m thick and dates from the Neoproterozoic Era, 1,000 to 541 million years ago.
An auto repair shop makes homage to the history of camels in the Quartzite, AZ area. In the 1850's the US Army experimented with the use of camels for transportation of good in the desert. While the camels performed well, the mule drivers were unhappy with the encroachment of these animals on their domain. When the Civil War broke out, the camel experiment was discontinued but their legend lives on.
Happy Waterfall Wednesday!
Zhangjiajie National Forest Park has been noted for its otherworldly appearance since ancient times, and the landscape has served as the backdrop for works of art across the centuries. Within the scenic area can be found more than 3,000 quartzite sandstone columns, carved by water and wind erosion across millions of years.
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An absolutely beautiful October day for a visit to Wisconsin's most popular State Park. Over 3 million people visit the park every year, and it is extremely busy and popular in October when the fall colors appear. There are no gas-powered boats allowed on the lake, creating a very peaceful and quiet scene. The 500ft quartzite bluffs were created during the last Ice Age, 15,000 years ago, and are very popular with hikers and climbers. The trails on this east bluff are the most difficult in the park, and take about an hour to reach the top, where you will find Balanced Rock, and Devil's Doorway.
Devil's Lake State Park
Baraboo, Wisconsin, USA
Approaching the summit after ascending via the excellent stalkers' path in Coire Lair. This was the last photo I took that day as it shortly started raining, the clouds came down and we trudged over the three summits with no views.
This mountain is in the Moine Thrust Zone, where layers of Precambrian Torridonian sandstone (foreground and right) and Cambrian quartzite (the summit and the col further along) have got folded over each other rather like a rucked-up carpet.
Tintic quartzite, rising up from the lake, makes a perfect viewing ground to survey avian activity on nearby Egg Island. It's also a beautiful place to catch a sunset.
Errigal, situated in Gweedore, Is part of the “Seven Sisters” chain of mountains and is the highest in Donegal. Errigal is known for its pinkish glow during sunsets due to its quartzite.
The sunlit Creag Dubh (900m) (upper right), is the easternmost summit on the Great Ridge of Beinn Dubh, which stretches off to the left (west) above. There are five other summits along the ridge before the final descent in the far distance. The entire ridge is estimated to take 10 hours to walk.
Beinn Eighe is a complex mountain massif in the Torridon area of the Highlands of Scotland. Two of its summits (not including Creag Dubh) are classified as Munros. The name Beinn Eighe comes from the Scottish Gaelic meaning File Mountain. It has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour.
The massif partially seen on the far left of the image is the beginning of the Liathach ridge, which features another two Munros. The descent from the far end of that ridge is directly into Torridon.
Loch Clair is to the south of the A896, which passes along Glen Torridon below Beinn Eighe on its way from Kinlochewe in the east to Torridon in the west.
This was taken in late afternoon as the clouds moved in from the west. Even though it was October, the midges were in abundance here, so despite nets, we didn't stay long.
The Oquirrh Mountains above Tooele are pictured in the background. There are several parts of Stansbury Island that would be very challenging to reach. This appeared to be among the worst. If this rock formation is named I've been unable so far to discover what that name is.
Sandstone, quartzite, sky, in Coire Mhic Fhearchair, Beinn Eighe, Torridon, Highlands.
From a transparency original taken with a Nikon FM2n camera & scanned with a Nikon LS2000 SCSI film scanner. Tonal refinement & dust spotting in a legacy version of Photoshop.
Robber Den, Ardrishaig. The inclusion of the type of rock over which the water flows is for my benefit - the underlying geology on this hill is deceptively complex, with schist, phyllites, metadolerite and quartzite all making an appearance, it will be interesting to see how it alters the flora later in the year.
The view across Coire Lair to Beinn Liath Mhor from Fuar Tholl in North West Scotland. The juxtaposition of the dark Torridonian sandstone and the pale quartzite scree is characteristic of this part of the Highalnds.
Lichens growing on Baraboo quartzite, Devil's Lake State Park, Wisconsin. Colonies of this type of lichen tend to coalesce into larger colonies when they collide.
The quartzite is a deep red and the lichens are gray-green.
Cambrian quartzite beside the Mountain Trail in Beinn Eighe NNR. The "pipes", a little under 1 cm in diameter, are fossils of worm burrows from about 500 million years ago, here seen in cross section.
The quartzite was originally laid down as sandstone but metamorphosed by heat and pressure deep under the Earth's surface, losing the "grain" of the sandstone but not, in this instance, the fossils. A similar process is responsible for turning limestone into marble and, while chemically different, quartzite and marble can look quite similar, especially when the former doesn't contain fossils.
Very little plant life grows where quartzite is exposed as, being largely pure silicon dioxide, it doesn't break down to useful nutrients when it weathers, resulting in large areas of greyish-white exposed rock and scree, as illustrated on a large scale on Beinn Eighe itself, Foinaven and a number of other mountains in Scotland.
O vale do rio Olo, a montante das Fisgas de Ermelo, no Parque Natural do Alvão, exibe uma paisagem marcada por encostas cobertas de pinheiros e vegetação autóctone em tons outonais. O rio Olo, que se origina nas serranias próximas a Lamas de Olo, percorre 36 km até desaguar no rio Tâmega, atravessando áreas com formações rochosas graníticas e quartzíticas. Esta região é notável pelas suas cascatas, onde o Olo apresenta uma das maiores quedas de água da Europa, com um desnível superior a 250 metros ao longo de 1,5 km. A biodiversidade local e o interesse geológico contribuem para a importância desta área, assim como os vestígios do uso histórico das águas do Olo para moinhos e a pesca de espécies como truta e barbo. As serras do Marão e Alvão formam o pano de fundo, complementando a beleza natural deste ambiente.
The valley of the River Olo, upstream of the Fisgas de Ermelo, in the Alvão Natural Park, displays a landscape marked by pine-covered slopes and autochthonous vegetation in autumn tones. The River Olo, which originates in the mountains near Lamas de Olo, runs for 36 km until it flows into the River Tâmega, crossing areas with granite and quartzite rock formations. This region is notable for its waterfalls, where the Olo has one of the largest waterfalls in Europe, with a drop of more than 250 meters over 1.5 km. The local biodiversity and geological interest contribute to the importance of this area, as do the traces of the historical use of the waters of the Olo for mills and the fishing of species such as trout and barbel. The Marão and Alvão mountains form the backdrop, complementing the natural beauty of this environment.
Minutes before sunrise, first light strikes the stunning escarpment along the eastern face of the Snowy Range and reflects in the beautiful calm waters of Lake Marie, in the Medicine Bow National Forest, Wyoming.
I've been fascinated from afar with the Snowy Range for quite a few years now, but hadn't made it there until we took an extra day and headed that way last month after fighting the crowds in Rocky Mountain National Park for a couple of days.
What we found in this part of the Medicine Bow was even more awesome than I'd hoped. It's one of those places that's actually very accessible, but has the appealing, uncrowded feel and wonder of a far more remote location. A great trail system (that I need to explore much further) weaves among and between the stunning alpine lakes, meadows and rockfalls nestled beneath the soaring cliffs and quartzite mountains.
And speaking of quartzite, I'm not sure I've ever seen so much in one place. The Snowy Range is aptly named, not just because it gets a lot of snow in winter, but also because there is so much quartz in its exposed rocks that it appears almost snow-capped year round in many lighting conditions. Beneath the higher peaks, boulder fields of bright quartz blends scatter here and there among blue waters, firs and autumn-toned undergrowth. A beautiful and fascinating place.
Thanks for viewing!
This is a familiar location for a lot of avid Ontario hikers, but a perspective which is a little less hammered home than others. This is the top of a really well known vantage point, but by largely ignoring the vantage point itself, you can really showcase the rugged landscape that Killarney is known for. Fall is really unlike any other time for this type of hike.
I never get tired of sunrise light on quartzite!
Taken with a Canon 5DIV and a 24-70 f/2.8Lii with a Lee landscape polarizer. Processed in Camera Raw and Photoshop