Dane County, Wisconsin
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This is the same scene as my previous one, just a few weeks before. Danes Dyke is a popular Nature Reserve just outside Flamborough village, E. Yorkshire, UK.
f/11, 51 mm, 1 sec at ISO 200. Manual exposure & 2 sec timer.
Tiller Myle's Jacket for TMD
FashionNatic Mateo Jeans
REBELLION Connor Boots
Exile Julian Hair
[Rezz Room] Great Dane Animesh
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The Dane Valley and the Danebower Chimney. The chimney was built for ventilation of the nearby colliery and is a scheduled monument.
Woke up this morning and thought its cold, so i found some nice reminders of the warm summer to come.
This was taken en route to Three Shires Head
Military Street in Dane was one of many location on the former C&NW line from Madison to Reedsburg that still featured wig-wag signals until just recently. While these signals were removed a few months after this image was made in late 2011, the last ones on the line in Baraboo survived until spring 2016 before being retired.
WSOR L467 is westbound on the Reedsburg Sub near Dane, Wisconsin behind a pair of consecutively-numbered ex-NS GP59s which were acquired by Watco early last year and painted in WSOR colors.
WSOR L467 crawls west through Dane, Wisconsin on former C&NW rails with a pair of ex-NS GP59s still in fresh WSOR livery and a train of mostly covered hoppers for the elevator at Rock Springs.
Walking with friends and their Dane XI, the colours match so well :)
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The start or is it the end of Danes Dyke at Bempton Cliffs. The mist beginning to fall again.
Danes Dyke is a 2-mile (3.2 km) long ditch that runs north to south isolating the seaward 5 square miles (13 km2) of the headland. The dyke and the steep cliffs make the enclosed territory and its two boat launching beaches, North and South Landings, easily defended. Despite its name, the dyke is prehistoric in origin, and Bronze Age arrowheads were found when it was excavated by Pitt-Rivers in 1879. It is a Local Nature Reserve.
Taken at one of the dog parks in Ottawa. These Danes have such long legs. It's a wonder that they have so much control when they are running about. The shot is blurry, but I found it interesting...
The Dane John Mound, also known as the Dane John Gardens, is a former Roman cemetery dating from the 1st Century AD. It was converted into a motte-and-bailey castle by William the Conquerer in 1066 and abandoned in 1123 when a second castle was built. Between 1790 and 1803 it was turned into the current civic gardens.
Photography © Jeremy Sage
One of my first of many attempts at selective color, masking, and blending filters. This half-Great Dane dog was a willing subject to my post processing experiments.
Built in 2005 in the modern style, the Dane County Courthouse is a ten story triangular building, In the background can been seen the Wisconsin State Capitol, which also houses the Wisconsin Supreme Court.
It was gorgeous.
Staffordshire Mooorlands near the River Dane about a mile (maybe more) from Lud's Church.
19th October 2024
Porlock Bay is on the Bristol Channel, between Hurlstone Point and Porlock Weir in Somerset. The coastline includes shingle ridges, salt marshes and a submerged forest. Much of the coastline is under the care of the National Trust, and the coastline forms part of the South West Coast Path.
Porlock Weir lies about 1.5 miles west of Porlock, and is a small settlement which has grown up around the harbour. It is a popular visitor attraction.
Like most ports in West Somerset, the harbour is tidal but has a small home-based flotilla of yachts and is visited by many more in spring and summer. The port has existed for over 1,000 years. The Anglo-Saxon chronicle reports that in 1052 Harold Godwinson came from Ireland with nine ships and plundered the area and even before that in 86 AD it was visited by Danes. In the 18th and 19th centuries coal from south Wales was the main cargo, and in World War II pit props cut from local forests were exported the other way.
The shingle ridge that protects Porlock from the sea developed about 8000 years ago after the last ice age, as sea levels rose and cliffs to the west eroded. Since then, there has been a continual process of change, with deep core samples taken from the Marsh showing that the ridge has moved inland at different periods, with sporadic breaching and ‘healing' events as part of the natural cycle of evolution of the barrier.
The construction of groynes along Porlock Beach, in the early 19th century, was designed to interrupt and reduce the thinning and instability of the ridge to protect the main road.
Print and Digital uncensored magazine featuring the best of my work with Dane: www.magcloud.com/browse/issue/2400171