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At Pichavaram.
Pichavaram is located near Chidambaram in Cuddalore District, Tamil Nadu, in South India. The nearest railway station is Chidambaram from where it is accessible by road.
Pichavaram is home to the second largest Mangrove forest in the world, and it is one of the unique eco-tourism spots in South India. The backwaters, interconnected by the Vellar and Coleroon river systems, offer abundant scope for water sports such as rowing, kayaking and canoeing. The Pichavaram forest not only offers waterscape and backwater cruises, but also another very rare sight - the mangrove forest trees are permanently rooted in a few feet of water.
The Pichavaram mangroves are considered among the healthiest mangrove occurrence in the world. Pichavaram consists of a number of islands interspersing a vast expanse of water covered with green trees. The area is about 2,800 acres (11 km2) and is separated from the sea by a sand bar which is a patch of extraordinary loveliness.
The Pichavaram mangrove biotope, consisting of rare species like Avicennia and Rhizophara; presents a special attraction, with its peculiar topography and environmental condition. It supports the existence of many rare varieties of economically important shell and finfishes.
Source : Wikipedia
Founded in 1906 by the Jogye order, Dongguk University is one of the few Buddhist affiliated universities in the world. Located on the foothills of Mount Namsan in central Seoul, Dongguk University is a large co-educational university. From the campus you can take a walk directly onto the hiking trails which traverse Namsan (mountain), or explore the grittier, but nonetheless charming Chungmuro neighbourhood and its alleyways.
Accessible from:
Dongguk University Station, Line 3, Exit 6.
1. Front gunner seat, accessible by lowering ladder
2. Pilot position, accessible from the communication room
3. Communication room and droid repair station
4. Main hallway, connects main ramp, living quarters, communication room, both airlocks* and the backside of the ship
5. Living quarters - has 3 beds, table and some basic furniture to accomodate basic minifgure needs
6. Cargo elevator. Can be used to access the lower cargo hold**
7. Right airlock
8. Left airlock and doorway to common room
9. Access to upper level, main gunner seat and Phantom docking bay
10. Armory and gunsmith
11. Dejarik and dining table
12. Kitchen area
13. Bathroom
14. Engine room, houses 2 hyperdive units and signal jammer
15. Main gunner position***
16. Access hatch for the docking bay
17. Phantom Docking bay
*Airlocks cannot be opened due to the structure of the build, they are keeping all the side connections together and play major role to make GHOST swooshable.
** Lower cargo hold access is limited, therfore it's hard to use it for "playing" porpuses. It's possible to put some cargo and boxes while still building this MOC. Cargo will be seen through the large 8x8 grill pieces.
*** Main gun on the top of the ship is fixed and can be reattached at 90 degree increments. I tried to make it freely rotateble but at this scale I didn't want to sacrifce looks for this small function.
Accessible PowerScape 3D play system with shade structures, adaptive whirl and swings, musical instruments, motion activities and much more.
Mount Esja is Reykjavík’s most iconic mountain, rising sharply across the bay and offering one of the most accessible and popular hiking routes in Iceland. Though not a single peak, Esja is a volcanic mountain range formed millions of years ago by basaltic lava flows and shaped by glacial erosion. It stands as a natural backdrop to the capital, visible from much of the city.
One of the most frequented routes leads to Steinn, a large rock outcrop and popular turnaround point for hikers. Reaching Steinn involves a moderately challenging trail that rewards climbers with sweeping views over Reykjavík, Kollafjörður Bay, and the vast Icelandic landscape beyond. Whether hiked in the glow of summer light or the silence before sunrise, the path to Steinn is a favorite among locals and visitors alike—a place where urban life fades into the wilderness.
A photo (again from last year) taken on the Monsal trail looking down towards Water cum Jolly Dale.
Before the re-opening of the tunnels on the trail this view would not have been accessible.
Accessible PowerScape 3D play system with shade structures, adaptive whirl and swings, musical instruments, motion activities and much more.
Photographed during the perfect blue hour moment when twilight deepens but artificial lights shine brightest, this image captures one of Pier 70's most architecturally significant buildings—a beautifully restored power house or pump station that once provided essential utilities to the sprawling shipyard complex. The white painted facade glows against the saturated blue sky, while a massive piece of preserved industrial machinery sits prominently on display, bridging past and present.
The building's classical architectural treatment is immediately striking. This wasn't just another utilitarian industrial structure—the ornate cornice work with its egg-and-dart molding, the series of elegant arched openings along the upper level, and the careful proportioning all suggest this was a building of some importance within the shipyard hierarchy. Power houses and pump stations, though purely functional in purpose, often received architectural embellishment that reflected their critical role in keeping the entire operation running.
Those arched openings, painted dark green or black with multi-paned windows, create a rhythmic pattern across the white facade. Some are illuminated from within, revealing colored light—blues, oranges, and warm whites—that hint at contemporary uses within these historic shells. The variety of interior lighting creates a painterly quality, each window offering a glimpse into different spaces and activities happening simultaneously within the adaptive reuse project.
The piece of industrial equipment displayed in the courtyard is a showstopper. This appears to be a massive flywheel or pump component, painted dark green or black, mounted on a concrete plinth for preservation and interpretation. These machinery artifacts scattered throughout Pier 70 serve as sculptural reminders of the site's industrial heritage, transforming functional equipment into public art that educates visitors about the shipyard's technological history. The scale of this machinery—requiring substantial concrete foundations just to display it—speaks to the magnitude of industrial operations that once took place here.
Modern interventions blend thoughtfully with historic fabric. Metal stairs with contemporary safety railings provide accessible circulation to what appears to be a raised entrance or terrace level. The combination of historic architecture and modern code-compliant access solutions is handled with respect for both preservation principles and contemporary functionality. Black metal railings and stairs provide visual contrast against the white building without competing for attention.
The adjacent structures visible in the frame show the variety of architectural approaches across the Pier 70 site. To the left, colorful elements—red tile roofing and green structural elements—suggest Mediterranean or Spanish Colonial influences, while the white building to the right maintains the industrial aesthetic with its regular window grid and clean lines. This architectural diversity reflects the complex's long development history, with buildings added and modified over decades to meet changing operational needs.
The courtyard or service area in the foreground, with its asphalt paving and yellow-painted curbs, maintains its utilitarian character while obviously being well-maintained for contemporary use. Parking space markings, modern lighting fixtures mounted at pedestrian scale, and clear circulation paths show how the site has been updated for safety and accessibility while preserving its industrial bones. A bicycle visible on the right suggests current occupants use active transportation—very San Francisco.
Blue hour timing transforms what could be a straightforward documentation shot into something atmospheric and evocative. The deep blue sky provides that perfect backdrop that makes white buildings luminous, while the artificial lighting reveals texture, depth, and human activity. This brief window of time—perhaps fifteen minutes when the light balance is just right—requires planning and patience but yields results impossible to achieve in full daylight or complete darkness.
The ornamental details deserve closer attention. That elaborate cornice running the full length of the building required skilled craftsmen to create and considerable expense to restore. The decorative brackets, the modillion blocks, the multiple layers of molding—these elements speak to an era when even industrial buildings received architectural refinement. Preserving these details required careful work by restoration specialists who understand historic materials and techniques.
Looking at the building's massing, you can see how it's designed to house tall equipment. The high ceilings necessary for large pumps or generators created opportunities for those impressive arched window openings that now flood interior spaces with natural light—a happy accident of industrial necessity becoming residential or commercial asset in the building's second life.
The surrounding site context—visible portions of other buildings, the layout of the courtyard, the mix of historic and contemporary elements—shows how Pier 70 functions as a unified historic district rather than isolated buildings. The relationships between structures, the shared architectural vocabulary, and the preserved industrial artifacts create a sense of place that's unique to this location and impossible to replicate elsewhere.
So this week i am no longer self employed as have taken a job with Attain Travel . My first job was yesterday to Blackpool and as i have experience and am trained in using accessible coaches and clamping wheelchairs i was given this job. Seen at Sandbach services YP09NRF a Scania K320 / Irizar I4 C49FL. This was also my first drive of a I4. Photo taken 05/10/17
Grand Cenote. Tulum, Mexico. Oct/2016
A cenote is a natural pit, or sinkhole, resulting from the collapse of limestone bedrock that exposes groundwater underneath. Especially associated with the Yucatán Peninsula of Mexico, cenotes were sometimes used by the ancient Maya for sacrificial offerings.
The term derives from a word used by the low-land Yucatec Maya — ts'onot — to refer to any location with accessible groundwater.[1][2] Cenotes are common geological forms in low latitude regions, particularly on islands, coastlines, and platforms with young post-Paleozoic limestones that have little soil development.
Cenotes are surface connections to subterranean water bodies.[3] While the best-known cenotes are large open water pools measuring tens of meters in diameter, such as those at Chichén Itzá in Mexico, the greatest number of cenotes are smaller sheltered sites and do not necessarily have any surface exposed water. The term cenote has also been used to describe similar karst features in other countries such as Cuba and Australia, in addition to the more generic term of sinkholes.
Cenote water is often very clear, as the water comes from rain water filtering slowly through the ground, and therefore contains very little suspended particulate matter. The groundwater flow rate within a cenote may be very slow. In many cases, cenotes are areas where sections of cave roof have collapsed revealing an underlying cave system, and the water flow rates may be much faster: up to 10 kilometers (6 mi) per day. Cenotes around the world attract cave divers who have documented extensive flooded cave systems through them, some of which have been explored for lengths of 100 km (62 mi) or more.
Source: Wikipedia
Um cenote é uma cavidade natural (algar) ou dolina resultado do impacto de um grande meteoro há 65.5 milhões de anos, evento que extinguiu os dinossauros da terra, fenômeno que deu origem às águas subterrâneas. Especialmente associado com a Península de Iucatã do México, os cenotes eram usados em alguns rituais de sacrifício da civilização Maia. O termo deriva de uma palavra utilizada pelos maias iucatecas das terras baixas, "Ts'onot" refere-se a qualquer local com águas subterrâneas acessíveis. Cenotes são formações geológicas comuns em regiões de baixas latitudes, particularmente em ilhas, regiões costeiras e plataformas com recentes formações calcárias pós-paleozóicas que têm pouco desenvolvimento do solo.
Cenotes são conexões entre a superfície e áreas alagadas subterrâneas.Enquanto os cenotes mais conhecidos são grandes piscinas medindo cerca de 10 metros de diâmetro, como as existentes em Chichén Itzá, o maior número de cenotes são pequenos locais abrigados e não necessariamente tem qualquer água de superfície exposta. O termo cenote também é empregado para descrever formações parecidas conhecidas como carste presentes em outros países como Cuba ou Austrália.
As águas dos cenotes geralmente são límpidas, porque esta provem de filtragem de água de chuva lentamente através do solo e, portanto, contém poucas partículas suspensas. A taxa de fluxo das água subterrânea dentro de um cenote podem ser muito lentas. Em diversos casos, cenotes são áreas onde se(c)ções do teto das cavernas cederam, revelando um sistema de cavernas subjacente e as taxas de fluxo podem ser muito mais rápidas, cerca de 10 km (6,21 mi) por dia. Cenotes ao redor do mundo atraem exploradores de cavernas, que documentaram extensos sistemas de cavernas inundadas através deles, alguns dos quais com cerca de 100 km (62,1 mi) de extensão ou mais.
Fonte: Wikipedia
Lindisfarne Castle is a 16th-century castle located on Holy Island, near Berwick-upon-Tweed, Northumberland, England, much altered by Sir Edwin Lutyens in 1901. The island is accessible from the mainland at low tide by means of a causeway.
The castle is located in what was once the very volatile border area between England and Scotland; the area was also frequently attacked by Vikings.
Taking advantage of the island's strategic location, in 1549, a small fort was built on a high rock known as Beblowe, the highest point of the island, to the north of the monastic buildings, and overlooking the harbour. Military engineer Sir Richard Lee saw only a decayed platform and turf rampart when he inspected the area in 1565. Elizabeth I then had work carried out on the fort, strengthening it and providing gun platforms for the new developments in artillery technology. These works in 1570 and 1571 cost £1191. During the construction work, the priory buildings were used as a source of building stone.
When James I came to power in England, he combined the Scottish and English thrones, and the need for the castle declined. At this time the castle was still garrisoned from Berwick and protected the small Lindisfarne Harbour.
In the eighteenth century, the castle was occupied briefly by Jacobite rebels, but was quickly recaptured by soldiers from Berwick who imprisoned the rebels; they dug their way out and hid for nine days close to nearby Bamburgh Castle before making good their escape.
In later years the castle was used as a coastguard look-out and became something of a tourist attraction. Charles Rennie Mackintosh made a sketch of the old fort in 1901.
In 1901, it became the property of Edward Hudson, a publishing magnate and the owner of Country Life magazine. He had it refurbished in the Arts and Crafts style by Sir Edwin Lutyens. It is said that Hudson and the architect came across the building while touring Northumberland and climbed over the wall to explore inside.
The walled garden, which had originally been the garrison's vegetable plot, was designed by Lutyens' long-time friend and collaborator, Gertrude Jekyll between 1906 and 1912. It is some distance away from the castle itself. Between 2002 and 2006 it was restored to Jekyll's original planting plan which is now held in the Reef Collection at the University of California, Berkeley. The castle, garden and nearby lime kilns have been in the care of the National Trust since 1944 and are open to visitors.
Lutyens used upturned disused boats (herring busses) as sheds. In 2005, two of the boats were destroyed by arson. They were replaced in 2006 and the third boat has now been renovated by the National Trust. The replacement of the two burned boats by two new boat sheds features on a DVD Diary of an Island. This shows a fishing boat from Leith being cut in half in a boatyard in Eyemouth and the two "sheds" being transported to the island and lifted into place by crane.
The Spanish architect Enric Miralles used Lutyens' upturned herring busses as an inspiration for his design of the Scottish Parliament Building in Edinburgh.
The castle was closed for major renovation and restoration works from November 2016 to April 2018.
The entrance to the castle is quite dramatic and involves a steep climb around the rocky base. Lutyens's original slope was unprotected by either rails or fences in an attempt to emphasise the exposed nature of the site. When the future George V and Queen Mary visited in 1908, it is said they were alarmed by the slope and the cobbled surface.
Once inside the castle, the entrance hall is sectioned off by large stone pillars, somewhat reminiscent of a church nave with the dark reddish-brown of the stone contrasting with the whitewashed plasterwork. The space is completed by a bare stone floor.
The kitchen is almost as bare, and is dominated by a large stone fireplace. Here, as at Castle Drogo, Lutyens uses the space in interesting ways. Throughout the castle, he has used stone, brick, slate and wood to create simple forms, and uses textures to demonstrate a rustic, spartan life-style. Despite being a castle it remains a homely space where the human scale is room size, but with incongruous architectural elements. In the scullery there is a tiny window over a stone sink surrounded by the mechanism used to operate the portcullis.
After descending to the dining room one is inside the remnants of the Tudor fort. The vaults here and in the adjacent ship room are entirely functional as they support the gun battery above. The wide chimney-piece contains an old bread-oven; here Lutyens has emphasised the age of the room with Neo-Gothic traceried windows framed by curtains which swing out to lie flat along the wall. One of the end walls is painted a rich Prussian blue, which contrasts with the herring-bone patterned red-brick floor.
Next door is the ship room where a green wall fulfils a similar role. The furniture is in keeping, with much dark wood in the tables and cabinets. The few upholstered chairs and sofas have now faded to gentle tones. The largest bedroom, the east, is bright and airy and again has curtains on pull-out poles. The long gallery was a new space created by Lutyens, intended to echo the grand galleries of Elizabethan and Jacobean houses. The scale is much smaller, but again the use of exposed stone arches and oak beams provides a grand yet rustic feel. Further on, an upper gallery has a raised platform at one end. From here an oak door leads onto the upper battery with its views along the coastline. The music room at the castle was used by Guilhermina Suggia, and a cello is left in the room today to mark her frequent visits.
Lindisfarne Castle has been used as a filming location including; Cul-de-sac (1966); The Tragedy of Macbeth (1971); Cold Feet (1998–2003); The Scarlet Pimpernel (1982); Wolfblood and Reign.
Nowadays the only Routemasters still operated by Transport for London drive two 'heritage routes' linking famous landmarks.
Some of the reasons for replacing them were that they are not wheelchair accessible and that they require two people to operate them, a driver and a conductor, who you can see here on the aft balcony.
A sand spit reaches out from Chesterman Beach to Frank Island and is accessible only at low tide. Vancouver Island, BC
Everyone has a right to access our public lands, but few of Glacier's trails were created with accessibility in mind.
A first step to addressing limits to accessibility is to identify them.
Glacier and the National Park Service are using tools—like the orange, one-wheeled device a ranger is pictured here using—to evaluate trails in the park using the High Efficiency Trail Assessment Process (HETAP).
HETAP identifies trail variables: grade, cross-slope, trail width, surface material, and more.
This data allows park managers to prioritize future trail improvements, and allow visitors in the future to make more informed decisions.
The North of England Lead Mining Museum, better known as Killhope, is an industrial museum near the village of Cowshill, County Durham, England. The museum stands on the site of the former Park Level Mine, which is being restored to show the workings of a 19th-century lead mine.
The museum is located alongside the Killhope Burn, about 4 km upstream from Cowshill, and is accessible via the A689 road between Stanhope, County Durham and Alston, Cumbria.
It is situated in the heart of the North Pennines, Area of Outstanding Natural Beauty, an area that, in 2003, was designated the first Geopark in Great Britain.
The museum is open every day between 1 April and 31 October, but is closed (except to pre-booked groups) during the winter months, when weather conditions in the area can be severe. A bus service operates through Weardale; services usually terminate at Cowshill, but some summer services will continue to Killhope on request.
Lead ore in the North Pennines occurs in mineralised veins within the Carboniferous rocks of the area. Until the mid-19th century, exploitation of these ore bodies was mostly confined to surface excavations and vertical shafts. From 1818, mining in the area was controlled by W B Lead Co, a mining company established by the Blacketts, a prominent Newcastle family which had leased mining rights in Weardale from the Bishop of Durham.
In 1853, W B Lead began driving the Park Level Mine, which eventually intersected 11 mineral veins. As the mine developed, so did the surface workings. In 1858, a "mineshop" was built to accommodate the miners; the population density in such a remote area was very low and, until then, miners had been faced with a long daily walk to and from the mine. In 1862, storage bays ("bouse teams") were constructed, to store the raw lead ore (the "bouse"), and washing rakes were installed, in which water was used to separate the lead ore in the bouse from the waste material. In 1878, soon after the mine struck the richest of the veins, the Park Level Mill was brought into operation, to speed up the process of washing the ore. The main feature of the mill was a large waterwheel, the "Killhope Wheel".
Not long after the Park Level Mill came into use, the price of lead plummeted, rendering lead-mining in Weardale uneconomic and, in 1883, W B Lead closed all of its operations in the district. The Park Level Mine was taken over by another company, Weardale Lead, which continued to operate it until 1910, when production ceased. The mine was re-opened briefly in 1916, during the First World War, after which it lay derelict for over 60 years, during which time the buildings crumbled and any equipment that could be removed was salvaged for scrap.
Between 1818 and 1883, records show that W B Lead extracted over 31,200 tonnes of lead concentrates from the Killhope operations; between 1884 and 1916, Weardale Lead extracted a further 9,000 tonnes. Taking in the period before 1818, for which there are no records, it is thought that total output from Killhope may have exceeded 60,000 tonnes. In addition, 180 tonnes of zinc concentrates were recovered in the 1950s by treatment of some of the waste material.
By 1980, the Killhope Wheel was facing demolition, the washing floor had become a marshy field, and the rest of the site was decaying. In that year, the Durham County Council took over the site and began a programme of restoration. First to be restored was the "mineshop", which was opened to the public in May 1984. The Killhope Wheel was restored to working order in 1991 and the mine itself was opened in 1996.
It had been hoped that the existing mine could be restored to allow access by the public, but though the Park Level was found to be generally in sound condition, and the first 100 metres has been used as an access route, the area in the vicinity of the first vein workings was badly collapsed and unsafe. Reconstruction therefore consisted of constructing a new 'artificial' mine within a chamber that was excavated from the surface. Within this artificial mine, the rock surfaces are actually fibreglass casts, taken not just from Killhope but also from mines in the Nenthead district in nearby Cumbria. Despite their artificial nature, the casts faithfully represent the appearance and texture of the real rock.
One of the main features of the reconstructed mine is the Killhope Wheel, a 10-metre-diameter metal waterwheel. This was constructed by the Tyneside firm of William Armstrong. Although other waterwheels were used in and around the mine, this was the largest, and the only one to survive the decades of neglect. It has now been restored to full working order.
The museum has won several awards: it was the North East's Small Visitor Attraction of the Year in 2008, and was the inaugural winner of the Guardian's Family-Friendly Museum award in 2004.
Other lead mining remains in the area
Other interpretive sites in the area are the Heritage Centre at Allenheads, in Northumberland, and the Nenthead Mines Heritage Centre, a short distance away in Cumbria.
Numerous traces of Weardale's lead mining industry can still be seen and the Durham Dales Centre in Stanhope produces guides to a Lead Mining Trail that covers many of the more accessible sites.
Other disused lead mines in County Durham are:
Low Slitt Mine, Westgate
Middlehope Shield, Westgate
Brandon Walls Mine, Rookhope
Rookhope Old Smelt Mill
Feldon Smelt Mill
Coldberry Mine, Middleton-in-Teesdale
Middle Greenlaws, Daddry Shield
Derwent Lead Mines
Lady Rake Mine, Harwood
Greenhurth Mine, Harwood
Pike Law Mines, Newbiggin, Teesdale
County Durham, officially simply Durham is a ceremonial county in North East England. The county borders Northumberland and Tyne and Wear to the north, the North Sea to the east, North Yorkshire to the south, and Cumbria to the west. The largest settlement is Darlington, and the county town is the city of Durham.
The county has an area of 2,721 km2 (1,051 sq mi) and a population of 866,846. The latter is concentrated in the east; the south-east is part of the Teesside built-up area, which extends into North Yorkshire. After Darlington (92,363), the largest settlements are Hartlepool (88,855), Stockton-on-Tees (82,729), and Durham (48,069). For local government purposes the county comprises three unitary authority areas—County Durham, Darlington, and Hartlepool—and part of a fourth, Stockton-on-Tees. The county historically included the part of Tyne and Wear south of the River Tyne, and excluded the part of County Durham south of the River Tees.
The west of the county contains part of the North Pennines uplands, a national landscape. The hills are the source of the rivers Tees and Wear, which flow east and form the valleys of Teesdale and Weardale respectively. The east of the county is flatter, and contains by rolling hills through which the two rivers meander; the Tees forms the boundary with North Yorkshire in its lower reaches, and the Wear exits the county near Chester-le-Street in the north-east. The county's coast is a site of special scientific interest characterised by tall limestone and dolomite cliffs.
What is now County Durham was on the border of Roman Britain, and contains survivals of this era at sites such as Binchester Roman Fort. In the Anglo-Saxon period the region was part of the Kingdom of Northumbria. In 995 the city of Durham was founded by monks seeking a place safe from Viking raids to house the relics of St Cuthbert. Durham Cathedral was rebuilt after the Norman Conquest, and together with Durham Castle is now a World Heritage Site. By the late Middle Ages the county was governed semi-independently by the bishops of Durham and was also a buffer zone between England and Scotland. County Durham became heavily industrialised in the nineteenth century, when many collieries opened on the Durham coalfield. The Stockton and Darlington Railway, the world's first public railway to use steam locomotives, opened in 1825. Most collieries closed during the last quarter of the twentieth century, but the county's coal mining heritage is remembered in the annual Durham Miners' Gala.
Remains of Prehistoric Durham include a number of Neolithic earthworks.
The Crawley Edge Cairns and Heathery Burn Cave are Bronze Age sites. Maiden Castle, Durham is an Iron Age site.
Brigantia, the land of the Brigantes, is said to have included what is now County Durham.
There are archaeological remains of Roman Durham. Dere Street and Cade's Road run through what is now County Durham. There were Roman forts at Concangis (Chester-le-Street), Lavatrae (Bowes), Longovicium (Lanchester), Piercebridge (Morbium), Vindomora (Ebchester) and Vinovium (Binchester). (The Roman fort at Arbeia (South Shields) is within the former boundaries of County Durham.) A Romanised farmstead has been excavated at Old Durham.
Remains of the Anglo-Saxon period include a number of sculpted stones and sundials, the Legs Cross, the Rey Cross and St Cuthbert's coffin.
Around AD 547, an Angle named Ida founded the kingdom of Bernicia after spotting the defensive potential of a large rock at Bamburgh, upon which many a fortification was thenceforth built. Ida was able to forge, hold and consolidate the kingdom; although the native British tried to take back their land, the Angles triumphed and the kingdom endured.
In AD 604, Ida's grandson Æthelfrith forcibly merged Bernicia (ruled from Bamburgh) and Deira (ruled from York, which was known as Eforwic at the time) to create the Kingdom of Northumbria. In time, the realm was expanded, primarily through warfare and conquest; at its height, the kingdom stretched from the River Humber (from which the kingdom drew its name) to the Forth. Eventually, factional fighting and the rejuvenated strength of neighbouring kingdoms, most notably Mercia, led to Northumbria's decline. The arrival of the Vikings hastened this decline, and the Scandinavian raiders eventually claimed the Deiran part of the kingdom in AD 867 (which became Jórvík). The land that would become County Durham now sat on the border with the Great Heathen Army, a border which today still (albeit with some adjustments over the years) forms the boundaries between Yorkshire and County Durham.
Despite their success south of the river Tees, the Vikings never fully conquered the Bernician part of Northumbria, despite the many raids they had carried out on the kingdom. However, Viking control over the Danelaw, the central belt of Anglo-Saxon territory, resulted in Northumbria becoming isolated from the rest of Anglo-Saxon Britain. Scots invasions in the north pushed the kingdom's northern boundary back to the River Tweed, and the kingdom found itself reduced to a dependent earldom, its boundaries very close to those of modern-day Northumberland and County Durham. The kingdom was annexed into England in AD 954.
In AD 995, St Cuthbert's community, who had been transporting Cuthbert's remains around, partly in an attempt to avoid them falling into the hands of Viking raiders, settled at Dunholm (Durham) on a site that was defensively favourable due to the horseshoe-like path of the River Wear. St Cuthbert's remains were placed in a shrine in the White Church, which was originally a wooden structure but was eventually fortified into a stone building.
Once the City of Durham had been founded, the Bishops of Durham gradually acquired the lands that would become County Durham. Bishop Aldhun began this process by procuring land in the Tees and Wear valleys, including Norton, Stockton, Escomb and Aucklandshire in 1018. In 1031, King Canute gave Staindrop to the Bishops. This territory continued to expand, and was eventually given the status of a liberty. Under the control of the Bishops of Durham, the land had various names: the "Liberty of Durham", "Liberty of St Cuthbert's Land" "the lands of St Cuthbert between Tyne and Tees" or "the Liberty of Haliwerfolc" (holy Wear folk).
The bishops' special jurisdiction rested on claims that King Ecgfrith of Northumbria had granted a substantial territory to St Cuthbert on his election to the see of Lindisfarne in 684. In about 883 a cathedral housing the saint's remains was established at Chester-le-Street and Guthfrith, King of York granted the community of St Cuthbert the area between the Tyne and the Wear, before the community reached its final destination in 995, in Durham.
Following the Norman invasion, the administrative machinery of government extended only slowly into northern England. Northumberland's first recorded Sheriff was Gilebert from 1076 until 1080 and a 12th-century record records Durham regarded as within the shire. However the bishops disputed the authority of the sheriff of Northumberland and his officials, despite the second sheriff for example being the reputed slayer of Malcolm Canmore, King of Scots. The crown regarded Durham as falling within Northumberland until the late thirteenth century.
Following the Battle of Hastings, William the Conqueror appointed Copsig as Earl of Northumbria, thereby bringing what would become County Durham under Copsig's control. Copsig was, just a few weeks later, killed in Newburn. Having already being previously offended by the appointment of a non-Northumbrian as Bishop of Durham in 1042, the people of the region became increasingly rebellious. In response, in January 1069, William despatched a large Norman army, under the command of Robert de Comines, to Durham City. The army, believed to consist of 700 cavalry (about one-third of the number of Norman knights who had participated in the Battle of Hastings), entered the city, whereupon they were attacked, and defeated, by a Northumbrian assault force. The Northumbrians wiped out the entire Norman army, including Comines, all except for one survivor, who was allowed to take the news of this defeat back.
Following the Norman slaughter at the hands of the Northumbrians, resistance to Norman rule spread throughout Northern England, including a similar uprising in York. William The Conqueror subsequently (and successfully) attempted to halt the northern rebellions by unleashing the notorious Harrying of the North (1069–1070). Because William's main focus during the harrying was on Yorkshire, County Durham was largely spared the Harrying.
Anglo-Norman Durham refers to the Anglo-Norman period, during which Durham Cathedral was built.
Matters regarding the bishopric of Durham came to a head in 1293 when the bishop and his steward failed to attend proceedings of quo warranto held by the justices of Northumberland. The bishop's case went before parliament, where he stated that Durham lay outside the bounds of any English shire and that "from time immemorial it had been widely known that the sheriff of Northumberland was not sheriff of Durham nor entered within that liberty as sheriff. . . nor made there proclamations or attachments". The arguments appear to have prevailed, as by the fourteenth century Durham was accepted as a liberty which received royal mandates direct. In effect it was a private shire, with the bishop appointing his own sheriff. The area eventually became known as the "County Palatine of Durham".
Sadberge was a liberty, sometimes referred to as a county, within Northumberland. In 1189 it was purchased for the see but continued with a separate sheriff, coroner and court of pleas. In the 14th century Sadberge was included in Stockton ward and was itself divided into two wards. The division into the four wards of Chester-le-Street, Darlington, Easington and Stockton existed in the 13th century, each ward having its own coroner and a three-weekly court corresponding to the hundred court. The diocese was divided into the archdeaconries of Durham and Northumberland. The former is mentioned in 1072, and in 1291 included the deaneries of Chester-le-Street, Auckland, Lanchester and Darlington.
The term palatinus is applied to the bishop in 1293, and from the 13th century onwards the bishops frequently claimed the same rights in their lands as the king enjoyed in his kingdom.
The historic boundaries of County Durham included a main body covering the catchment of the Pennines in the west, the River Tees in the south, the North Sea in the east and the Rivers Tyne and Derwent in the north. The county palatinate also had a number of liberties: the Bedlingtonshire, Islandshire and Norhamshire exclaves within Northumberland, and the Craikshire exclave within the North Riding of Yorkshire. In 1831 the county covered an area of 679,530 acres (2,750.0 km2) and had a population of 253,910. These exclaves were included as part of the county for parliamentary electoral purposes until 1832, and for judicial and local-government purposes until the coming into force of the Counties (Detached Parts) Act 1844, which merged most remaining exclaves with their surrounding county. The boundaries of the county proper remained in use for administrative and ceremonial purposes until the Local Government Act 1972.
Boldon Book (1183 or 1184) is a polyptichum for the Bishopric of Durham.
Until the 15th century, the most important administrative officer in the Palatinate was the steward. Other officers included the sheriff, the coroners, the Chamberlain and the chancellor. The palatine exchequer originated in the 12th century. The palatine assembly represented the whole county, and dealt chiefly with fiscal questions. The bishop's council, consisting of the clergy, the sheriff and the barons, regulated judicial affairs, and later produced the Chancery and the courts of Admiralty and Marshalsea.
The prior of Durham ranked first among the bishop's barons. He had his own court, and almost exclusive jurisdiction over his men. A UNESCO site describes the role of the Prince-Bishops in Durham, the "buffer state between England and Scotland":
From 1075, the Bishop of Durham became a Prince-Bishop, with the right to raise an army, mint his own coins, and levy taxes. As long as he remained loyal to the king of England, he could govern as a virtually autonomous ruler, reaping the revenue from his territory, but also remaining mindful of his role of protecting England’s northern frontier.
A report states that the Bishops also had the authority to appoint judges and barons and to offer pardons.
There were ten palatinate barons in the 12th century, most importantly the Hyltons of Hylton Castle, the Bulmers of Brancepeth, the Conyers of Sockburne, the Hansards of Evenwood, and the Lumleys of Lumley Castle. The Nevilles owned large estates in the county. John Neville, 3rd Baron Neville de Raby rebuilt Raby Castle, their principal seat, in 1377.
Edward I's quo warranto proceedings of 1293 showed twelve lords enjoying more or less extensive franchises under the bishop. The repeated efforts of the Crown to check the powers of the palatinate bishops culminated in 1536 in the Act of Resumption, which deprived the bishop of the power to pardon offences against the law or to appoint judicial officers. Moreover, indictments and legal processes were in future to run in the name of the king, and offences to be described as against the peace of the king, rather than that of the bishop. In 1596 restrictions were imposed on the powers of the chancery, and in 1646 the palatinate was formally abolished. It was revived, however, after the Restoration, and continued with much the same power until 5 July 1836, when the Durham (County Palatine) Act 1836 provided that the palatine jurisdiction should in future be vested in the Crown.
During the 15th-century Wars of the Roses, Henry VI passed through Durham. On the outbreak of the Great Rebellion in 1642 Durham inclined to support the cause of Parliament, and in 1640 the high sheriff of the palatinate guaranteed to supply the Scottish army with provisions during their stay in the county. In 1642 the Earl of Newcastle formed the western counties into an association for the King's service, but in 1644 the palatinate was again overrun by a Scottish army, and after the Battle of Marston Moor (2 July 1644) fell entirely into the hands of Parliament.
In 1614, a Bill was introduced in Parliament for securing representation to the county and city of Durham and the borough of Barnard Castle. The bishop strongly opposed the proposal as an infringement of his palatinate rights, and the county was first summoned to return members to Parliament in 1654. After the Restoration of 1660 the county and city returned two members each. In the wake of the Reform Act of 1832 the county returned two members for two divisions, and the boroughs of Gateshead, South Shields and Sunderland acquired representation. The bishops lost their secular powers in 1836. The boroughs of Darlington, Stockton and Hartlepool returned one member each from 1868 until the Redistribution of Seats Act 1885.
The Municipal Corporations Act 1835 reformed the municipal boroughs of Durham, Stockton on Tees and Sunderland. In 1875, Jarrow was incorporated as a municipal borough, as was West Hartlepool in 1887. At a county level, the Local Government Act 1888 reorganised local government throughout England and Wales. Most of the county came under control of the newly formed Durham County Council in an area known as an administrative county. Not included were the county boroughs of Gateshead, South Shields and Sunderland. However, for purposes other than local government, the administrative county of Durham and the county boroughs continued to form a single county to which the Crown appointed a Lord Lieutenant of Durham.
Over its existence, the administrative county lost territory, both to the existing county boroughs, and because two municipal boroughs became county boroughs: West Hartlepool in 1902 and Darlington in 1915. The county boundary with the North Riding of Yorkshire was adjusted in 1967: that part of the town of Barnard Castle historically in Yorkshire was added to County Durham, while the administrative county ceded the portion of the Borough of Stockton-on-Tees in Durham to the North Riding. In 1968, following the recommendation of the Local Government Commission, Billingham was transferred to the County Borough of Teesside, in the North Riding. In 1971, the population of the county—including all associated county boroughs (an area of 2,570 km2 (990 sq mi))—was 1,409,633, with a population outside the county boroughs of 814,396.
In 1974, the Local Government Act 1972 abolished the administrative county and the county boroughs, reconstituting County Durham as a non-metropolitan county. The reconstituted County Durham lost territory to the north-east (around Gateshead, South Shields and Sunderland) to Tyne and Wear and to the south-east (around Hartlepool) to Cleveland. At the same time it gained the former area of Startforth Rural District from the North Riding of Yorkshire. The area of the Lord Lieutenancy of Durham was also adjusted by the Act to coincide with the non-metropolitan county (which occupied 3,019 km2 (1,166 sq mi) in 1981).
In 1996, as part of 1990s UK local government reform by Lieutenancies Act 1997, Cleveland was abolished. Its districts were reconstituted as unitary authorities. Hartlepool and Stockton-on-Tees (north Tees) were returned to the county for the purposes of Lord Lieutenancy. Darlington also became a third unitary authority of the county. The Royal Mail abandoned the use of postal counties altogether, permitted but not mandatory being at a writer wishes.
As part of the 2009 structural changes to local government in England initiated by the Department for Communities and Local Government, the seven district councils within the County Council area were abolished. The County Council assumed their functions and became the fourth unitary authority. Changes came into effect on 1 April 2009.
On 15 April 2014, North East Combined Authority was established under the Local Democracy, Economic Development and Construction Act 2009 with powers over economic development and regeneration. In November 2018, Newcastle City Council, North Tyneside Borough Council, and Northumberland County Council left the authority. These later formed the North of Tyne Combined Authority.
In May 2021, four parish councils of the villages of Elwick, Hart, Dalton Piercy and Greatham all issued individual votes of no confidence in Hartlepool Borough Council, and expressed their desire to join the County Durham district.
In October 2021, County Durham was shortlisted for the UK City of Culture 2025. In May 2022, it lost to Bradford.
Eighteenth century Durham saw the appearance of dissent in the county and the Durham Ox. The county did not assist the Jacobite Rebellion of 1715. The Statue of Neptune in the City of Durham was erected in 1729.
A number of disasters happened in Nineteenth century Durham. The Felling mine disasters happened in 1812, 1813, 1821 and 1847. The Philadelphia train accident happened in 1815. In 1854, there was a great fire in Gateshead. One of the West Stanley Pit disasters happened in 1882. The Victoria Hall disaster happened in 1883.
One of the West Stanley Pit disasters happened in 1909. The Darlington rail crash happened in 1928. The Battle of Stockton happened in 1933. The Browney rail crash happened in 1946.
The First Treaty of Durham was made at Durham in 1136. The Second Treaty of Durham was made at Durham in 1139.
The county regiment was the Durham Light Infantry, which replaced, in particular, the 68th (Durham) Regiment of Foot (Light Infantry) and the Militia and Volunteers of County Durham.
RAF Greatham, RAF Middleton St George and RAF Usworth were located in County Durham.
David I, the King of Scotland, invaded the county in 1136, and ravaged much of the county 1138. In 17 October 1346, the Battle of Neville's Cross was fought at Neville's Cross, near the city of Durham. On 16 December 1914, during the First World War, there was a raid on Hartlepool by the Imperial German Navy.
Chroniclers connected with Durham include the Bede, Symeon of Durham, Geoffrey of Coldingham and Robert de Graystanes.
County Durham has long been associated with coal mining, from medieval times up to the late 20th century. The Durham Coalfield covered a large area of the county, from Bishop Auckland, to Consett, to the River Tyne and below the North Sea, thereby providing a significant expanse of territory from which this rich mineral resource could be extracted.
King Stephen possessed a mine in Durham, which he granted to Bishop Pudsey, and in the same century colliers are mentioned at Coundon, Bishopwearmouth and Sedgefield. Cockfield Fell was one of the earliest Landsale collieries in Durham. Edward III issued an order allowing coal dug at Newcastle to be taken across the Tyne, and Richard II granted to the inhabitants of Durham licence to export the produce of the mines, without paying dues to the corporation of Newcastle. The majority was transported from the Port of Sunderland complex, which was constructed in the 1850s.
Among other early industries, lead-mining was carried on in the western part of the county, and mustard was extensively cultivated. Gateshead had a considerable tanning trade and shipbuilding was undertaken at Jarrow, and at Sunderland, which became the largest shipbuilding town in the world – constructing a third of Britain's tonnage.[citation needed]
The county's modern-era economic history was facilitated significantly by the growth of the mining industry during the nineteenth century. At the industry's height, in the early 20th century, over 170,000 coal miners were employed, and they mined 58,700,000 tons of coal in 1913 alone. As a result, a large number of colliery villages were built throughout the county as the industrial revolution gathered pace.
The railway industry was also a major employer during the industrial revolution, with railways being built throughout the county, such as The Tanfield Railway, The Clarence Railway and The Stockton and Darlington Railway. The growth of this industry occurred alongside the coal industry, as the railways provided a fast, efficient means to move coal from the mines to the ports and provided the fuel for the locomotives. The great railway pioneers Timothy Hackworth, Edward Pease, George Stephenson and Robert Stephenson were all actively involved with developing the railways in tandem with County Durham's coal mining industry. Shildon and Darlington became thriving 'railway towns' and experienced significant growths in population and prosperity; before the railways, just over 100 people lived in Shildon but, by the 1890s, the town was home to around 8,000 people, with Shildon Shops employing almost 3000 people at its height.
However, by the 1930s, the coal mining industry began to diminish and, by the mid-twentieth century, the pits were closing at an increasing rate. In 1951, the Durham County Development Plan highlighted a number of colliery villages, such as Blackhouse, as 'Category D' settlements, in which future development would be prohibited, property would be acquired and demolished, and the population moved to new housing, such as that being built in Newton Aycliffe. Likewise, the railway industry also began to decline, and was significantly brought to a fraction of its former self by the Beeching cuts in the 1960s. Darlington Works closed in 1966 and Shildon Shops followed suit in 1984. The county's last deep mines, at Easington, Vane Tempest, Wearmouth and Westoe, closed in 1993.
Postal Rates from 1801 were charged depending on the distance from London. Durham was allocated the code 263 the approximate mileage from London. From about 1811, a datestamp appeared on letters showing the date the letter was posted. In 1844 a new system was introduced and Durham was allocated the code 267. This system was replaced in 1840 when the first postage stamps were introduced.
According to the Encyclopædia Britannica Eleventh Edition (1911): "To the Anglo-Saxon period are to be referred portions of the churches of Monk Wearmouth (Sunderland), Jarrow, Escomb near Bishop Auckland, and numerous sculptured crosses, two of which are in situ at Aycliffe. . . . The Decorated and Perpendicular periods are very scantily represented, on account, as is supposed, of the incessant wars between England and Scotland in the 14th and 15th centuries. The principal monastic remains, besides those surrounding Durham cathedral, are those of its subordinate house or "cell," Finchale Priory, beautifully situated by the Wear. The most interesting castles are those of Durham, Raby, Brancepeth and Barnard. There are ruins of castelets or peel-towers at Dalden, Ludworth and Langley Dale. The hospitals of Sherburn, Greatham and Kepyer, founded by early bishops of Durham, retain but few ancient features."
The best remains of the Norman period include Durham Cathedral and Durham Castle, and several parish churches, such as St Laurence Church in Pittington. The Early English period has left the eastern portion of the cathedral, the churches of Darlington, Hartlepool, and St Andrew, Auckland, Sedgefield, and portions of a few other churches.
'Durham Castle and Cathedral' is a designated UNESCO World Heritage Site. Elsewhere in the County there is Auckland Castle.
Labrador Nature Reserve (Chinese: 拉柏多自然保护区), also locally known as Labrador Park (拉柏多公园), is located in the southern part of the main island of Singapore. It is an oasis of tranqulity and natural wonder. It contains the only rocky sea-cliff on the mainland that is accessible to the public. - Wiki
A female soldier of the Bundeswehr wearing winter camouflage participates in military exercises during a visit by German Defense Minister Ursula von der Leyen at the Bundeswehr combat training center on January 28, 2014 in Letzlingen, Germany. According to a recently-published report, a majority of Bundeswehr members see the integration of women into the armed forces as problematic. The Bundeswehr became accessible to women ten years ago.
Accessible PowerScape 3D play system with shade structures, adaptive whirl and swings, musical instruments, motion activities and much more.
A shocking gap since the last post - apologies.
The Rive Dove is the focus for a new photographic art exhibition at Bakewell Visitor Centre this Spring. ‘Liquid Light’ by Michéla Griffith, whose photographs of water and light are often mistaken for paintings, is on display in the Peak District Photography Gallery until Tuesday May 3. Entry to the exhibition is free of charge, it is fully accessible and is open every day from 9.30am to 5.00pm.
April Coughlin from the Elevator Action Group with Rise and Resist - Activists from the Elevator Action Group with Rise and Resist took a subway ride with NYCT President Andy Byford on April 13, 2018. The trip illuminated some of the problems with signage, separate fare payment systems, boarding areas, and many other accessibility issues. Byford plans to incorporate accessibility priorities in a comprehensive corporate plan expected to be released in May. (Photo by Erik McGregor)
Everyone has a right to access our public lands, but few of Glacier's trails were created with accessibility in mind.
A first step to addressing limits to accessibility is to identify them.
Glacier and the National Park Service are using tools—like the orange, one-wheeled device pictured here alongside two rangers and a measuring tape—to evaluate trails in the park using the High Efficiency Trail Assessment Process (HETAP).
HETAP identifies trail variables: grade, cross-slope, trail width, surface material, and more.
This data allows park managers to prioritize future trail improvements, and allow visitors in the future to make more informed decisions.
Hardknott Pass is a hill pass between Eskdale and the Duddon Valley in the Lake District National Park, Cumbria, England. The tarmac-surfaced road, which is the most direct route from the central Lake District to West Cumbria, shares the title of steepest road in England with Rosedale Chimney Bank in North Yorkshire. It has a maximum gradient of 1 in 3 (about 33%).
The pass takes its name from Hard Knott which is derived from the Old Norse harthr (hard) and knutr (craggy hill).
A single track road runs between Eskdale in the west to the edge of the neighbouring Wrynose Pass in the east. On the western side is Harter Fell and the remains of Hardknott Roman Fort (200 metres (660 ft) above sea level).
The Hardknott Pass stands at a maximum elevation of 393 m (1,289 ft). The road descends steeply at a gradient of 30% (1 in 3) into the Duddon Valley. At the eastern end of the pass is Cockley Beck farm, built in the 1860s and owned by the National Trust. The route from Hardknott leads eastward towards the Wrynose Pass and Ambleside.
The pass is described as one of the most challenging roads in Britain. A series of hairpin bends make visibility difficult in various places, and the road surface is in poor condition and slippery when wet. The pass is often closed in winter due to ice that makes the route impassable for vehicles. Traffic ascending the pass has priority as advised by the Highway Code.
The challenging 1 in 3 gradients, steeper than the mountain stages of European bicycle races including the Tour de France and the Giro d'Italia, draw endurance cyclists. It is part of the annual Fred Whitton Challenge, a 112-mile ride around the Lake District. An "average" cyclist who was trained over six weeks for a 2019 Eurosport documentary called England's Toughest Climb failed to complete the route.
A road over the pass was built by the Romans around AD 110 to link the coastal fort and baths at Ravenglass with their garrisons at Ambleside and Kendal. The Romans called this road the Tenth Highway. The road fell into disrepair after the Romans left Britain in the early 5th century, becoming an unpaved packhorse route used to transport lead and agricultural goods. By the early Middle Ages, it was known as the Waingate ("cart road") or Wainscarth ("cart pass"): there is an 1138 record of a party of monks traversing it in an oxcart. Hardknott pass and its surrounding area fell within the domain of the Lords of Millom, being situated between the headwaters of the Esk and Duddon. Grazing and hunting rights were given to the monks of Furness Abbey by the Lords of Millom in the 13th century, which they held until the Dissolution of the Monasteries (1536–41).
In the 1880s an association of hoteliers, the English Lake District Association, financed improvements to the road in the hope of encouraging tourist excursions by carriage; by 1891 the scheme was judged to be "not the success that was anticipated". Nevertheless, the route had some popularity with cyclists and early motorists, with the Cyclists' Touring Club 1911 Guide to North-West England describing the old coach road as "difficult going West, cruel coming East". The first motor vehicles were taken over the Hardknott and Wrynose passes, from the Eskdale side, in 1913.
In 1936, the Cumberland Highways Committee considered, and rejected, a proposal to make the pass more accessible to motorised vehicles by laying down a new road surface and making other improvements. However, during the Second World War the War Office used the area for tank training, completely destroying the existing road surface. After the war the damage was repaired and the road tarmaced. A decade after the local government had rejected opening the highway to vehicles, the war's legacy had inadvertently created a direct motor route between Ambleside and Eskdale for the first time.
The courses of the Roman and modern roads are not identical. The Roman highway is to the north of the modern road on the western side of the pass and to the south on the eastern side.
The Lake District, also known as the Lakes or Lakeland, is a mountainous region and national park in Cumbria, North West England. It is primarily famous for the Cumbrian Mountains, its lake and coastal scenery, and for its literary associations with William Wordsworth and other Lake Poets, Beatrix Potter, and John Ruskin.
The Cumbrian mountains, or fells, include England's tallest mountains: Scafell Pike (978 m (3,209 ft)), Helvellyn (950 m (3,120 ft)), Skiddaw (931 m (3,054 ft)), and Cross Fell (893 m (2,930 ft)), which all have a topographical prominence of more than 600m. The region contains sixteen major lakes. They include Windermere, which with a length of 18 km (11 miles) and an area of 14.73 km2 (5.69 square miles) is both the longest and largest lake in England, and Wast Water, which at 79 metres (259 ft) is the deepest lake in England.
The Lake District National Park was established in 1951, and covers an area of 2,362 km2 (912 square miles), the bulk of the region. It was designated a UNESCO World Heritage Site in 2017.
National Park
The Lake District National Park includes all of the central Lake District, though the town of Kendal, some coastal areas, and the Lakeland Peninsulas are outside the park boundary. The area was designated a national park on 9 May 1951, a month after the Peak District, the first UK national park. It retained its original boundaries until 2016 when it was extended by 3% in the direction of the Yorkshire Dales National Park to incorporate areas land of high landscape value around the Lune Valley.
The national park received 18.14 million tourist visitors in 2022. This equates to 29.15 million tourist days, counting visits of greater than three hours. It is the largest of the thirteen national parks in England and Wales and the second largest in the UK after the Cairngorms National Park. Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. The area of the national park, with the exception of the 2016 extension, was designated a World Heritage Site in 2017 as a cultural landscape. This was the fourth attempt to list the park, after two attempts in the 1980s and one in 2012 failed.
The park is governed by the National Park Authority, which is based at offices in Kendal. It runs a visitor centre on Windermere at a former country house called Brockhole, Coniston Boating Centre, and Information Centres. The Park Authority has 20 members: six appointed by Westmorland and Furness Council, four by Cumberland Council, and ten by the Secretary of State for Environment, Food, and Rural Affairs.
Human geography
The precise extent of the Lake District was not defined traditionally, but is slightly larger than that of the National Park[citation needed], the total area of which is about 2,362 square kilometres (912 sq mi). The park extends just over 51 kilometres (32 mi) from east to west and nearly 64 kilometres (40 mi) from north to south, with areas such as the Lake District Peninsulas to the south lying outside the National Park.
Settlement
There are only a few major settlements within this mountainous area: the towns of Keswick, Windermere, Ambleside, and Bowness-on-Windermere are the four largest. Significant settlements close to the boundary of the national park include Carlisle, Barrow-in-Furness, Kendal, Ulverston, Dalton-in-Furness, Whitehaven, Workington, Cockermouth, Penrith, Millom and Grange-over-Sands; each of these has important economic links with the area. Other villages are Coniston, Threlkeld, Glenridding, Pooley Bridge, Broughton-in-Furness, Grasmere, Newby Bridge, Staveley, Lindale, Gosforth and Hawkshead. The economies of almost all are intimately linked with tourism. Beyond these are a scattering of hamlets and many isolated farmsteads, some of which are still tied to agriculture;[citation needed] others now function as part of the tourist economy.
Communications
Roads
The Lake District is very nearly contained within a box of trunk routes and major A roads. It is flanked to the east by the A6 road, which runs from Kendal to Penrith (though the National Park extension approved in 2015 is east of the A6); across its southern fringes by the A590, which connects the M6 to Barrow-in-Furness, and the A5092, and across its northern edge by the A66 trunk road between Penrith and Workington. The A595 (linking the A66 with the A5092) forms the park boundary from Calder Bridge to Holmrook, then crosses the coastal plain of the park until turning inland at the Whicham Valley, forming much of the park boundary again until joining the A5092 at Grizebeck.
Besides these, a few A roads penetrate the area itself, notably the A591 which runs north-westwards from Kendal to Windermere and then on to Keswick. It continues up the east side of Bassenthwaite Lake. "The A591, Grasmere, Lake District" was short-listed in the 2011 Google Street View awards in the Most Romantic Street category. The A593 and A5084 link the Ambleside and Coniston areas with the A590 to the south whilst the A592 and A5074 similarly link Windermere with the A590. The A592 also continues northwards from Windermere to Ullswater and Penrith by way of the Kirkstone Pass.
Some valleys which are not penetrated by A roads are served by B roads. The B5289 serves Lorton Vale and Buttermere and links via the Honister Pass with Borrowdale. The B5292 ascends the Whinlatter Pass from Lorton Vale before dropping down to Braithwaite near Keswick. The B5322 serves the valley of St John's in the Vale whilst Great Langdale is served by the B5343. Other valleys such as Little Langdale, Eskdale and Dunnerdale are served by minor roads. The last of these is connected with the first two by the Wrynose and Hardknott passes respectively; both of these passes are known for their steep gradients and are together one of the most popular climbs in the United Kingdom for cycling enthusiasts. A minor road through the Newlands Valley connects via Newlands Hause with the B5289 at Buttermere. Wasdale is served by a cul-de-sac minor road,[a] as is Longsleddale and the valleys at Haweswater and Kentmere. There are networks of minor roads in the lower-lying southern part of the area, connecting numerous communities between Kendal, Windermere, and Coniston.
Railways and ferries
The West Coast Main Line skirts the eastern edge of the Lake District and the Cumbrian Coast Line passes through the southern and western fringes of the area. A single railway line, the Windermere Branch Line, penetrates from Kendal to Windermere via Staveley. Railways once served Broughton-in-Furness and Coniston (closed to passengers in 1958) and another ran from Penrith to Cockermouth via Keswick (closed west of Keswick in 1966 and completely in 1972). Part of the track of the latter is used by the improved A66 trunk road.
The Cumbrian Coast line has three stations within the boundaries of the national park (and additionally Drigg, about a third of a mile from the park boundary). The line gives railway enthusiasts and others a flavour of a pre-Beeching railway line, with features like manually operated level crossing gates, as well as giving a good connection to the steam railway into Eskdale and providing access for cyclists and serious walkers to the Western Fells.
The narrow gauge Ravenglass and Eskdale Railway runs from Ravenglass on the west coast up Eskdale as far as Dalegarth Station near the hamlet of Boot, catering for tourists. Another heritage railway, the Lakeside and Haverthwaite Railway, runs between Lake Windermere and Haverthwaite, and tourists can connect at Lakeside with the boats up the lake to Bowness.
A vehicle-carrying cable ferry, the Windermere Ferry, runs frequent services across Windermere. There are also seasonal passenger boats on Coniston Water, Derwent Water, and Ullswater.
Footpaths and bridleways
There are many paths over which the public has a right of way, all of which are signposted at their origin on public roads and at some other points. Within the area of the National Park in 2012 there were 2,159 km (1,342 mi) of public footpaths, 875 km (544 mi) of public bridleways, 15 km (9 mi) of restricted byways and 30 km (19 mi) of byways open to all traffic. There is also a general "right to roam" in open country, which includes approximately 50% of the national park.
Many of these tracks arose centuries ago and were used either as ridge highways (such as along High Street) or as passes for travelling across the ridges between settlements in the valleys. Historically these paths were not planned for reaching summits, but more recently they are used by fell walkers for that purpose. The Coast to Coast Walk, which crosses the north of England from the Irish Sea to the North Sea, traverses the national park from west to east.
Bridleways are intended for horse riding and walkers, with cyclists also permitted to use them. Cyclists must give way to all other bridleway users. Motor vehicles are only allowed on "byways open to all traffic" (green lanes) but in practice Traffic Regulation Orders have been brought in on several prohibiting motor traffic, although a system of permits operates on Gatesgarth Pass.
Land ownership
Most of the land within the national park is in private ownership, with about 55% registered as agricultural land. Landowners include:
Individual farmers and other private landowners, with more than half of the agricultural land farmed by the owners.
The National Trust owns around 25% of the total area (including some lakes and land of significant landscape value).
The Forestry Commission and other investors in forests and woodland.
United Utilities (owns 8%)
Lake District National Park Authority (owns 3.9%)
Physical geography
The Lake District is a roughly circular upland massif, deeply dissected by a broadly radial pattern of major valleys which are largely the result of repeated glaciations over the last 2 million years. The apparent radial pattern is not from a central dome, but from an axial watershed extending from St Bees Head in the west to Shap in the east. Most of these valleys display the U-shaped cross-section characteristic of glacial origin and often contain long narrow lakes in bedrock hollows, with tracts of relatively flat ground at their infilled heads, or where they are divided by lateral tributaries (Buttermere-Crummock Water; Derwent Water-Bassenthwaite Lake).[b] Smaller lakes known as tarns occupy glacial cirques at higher elevations. It is the abundance of both which has led to the area becoming known as the Lake District.
Many of the higher fells are rocky, while moorland predominates lower down. Vegetation cover in better-drained areas includes bracken and heather, although much of the land is boggy, due to the high rainfall. Deciduous native woodland occurs on many of the steeper slopes below the tree line, but with native oak supplemented by extensive conifer plantations in many areas, particularly Grizedale Forest in the generally lower southern part of the area. The Lake District extends to the sea to the west and south.
The highest mountain in England, Scafell Pike (978m/3210'), has a far-reaching view on a clear day, ranging from the Galloway Hills of Scotland, the Mourne Mountains in Northern Ireland, the Isle of Man, and Snowdonia in Wales.
Cumbrian Mountains
Lake District is located in the Lake DistrictScafell PikeScafell PikeScafellScafellScafellScafellHelvellynHelvellynSkiddawSkiddawHigh StreetHigh StreetGrasmoorGrasmoorConiston Old ManConiston Old ManGreat GableGreat GableKendalKendalPenrithPenrithKeswickKeswickAmblesideAmblesideCockermouthCockermouthWindermereWindermereGrasmereGrasmere
Major fells and towns shown within the National Park
Lake District
The mountains (or 'fells') of the Lake District are known as the "Cumbrian Mountains", "Cumbrian Fells" or "Lakeland Fells". The four highest fells exceed 3,000 feet (914 m). These are:
Scafell Pike, 978 m (3,209 ft)
Scafell, 965 m (3,166 ft)
Helvellyn, 951 m (3,120 ft)
Skiddaw, 931 m (3,054 ft)
Northern Fells
The Northern Fells are a clearly defined range of hills contained within a 13 km (8 mi) diameter circle between Keswick in the southwest and Caldbeck in the northeast. They culminate in the 931 m (3,054 ft) peak of Skiddaw. Other notable peaks are Blencathra (also known as Saddleback) (868 m (2,848 ft)) and Carrock Fell. Bassenthwaite Lake occupies the valley between this massif and the North Western Fells.
North Western Fells
The North Western Fells lie between Borrowdale and Bassenthwaite Lake to the east and Buttermere and Lorton Vale to the west. Their southernmost point is at Honister Pass. This area includes the Derwent Fells above the Newlands Valley and hills to the north amongst which are Dale Head, Robinson. To the north stand Grasmoor, highest in the range at 852 m (2,795 ft), Grisedale Pike and the hills around the valley of Coledale, and in the far northwest is Thornthwaite Forest and Lord's Seat. The fells in this area are rounded Skiddaw slate, with few tarns and relatively few rock faces.
Western Fells
The Western Fells lie between Buttermere and Wasdale, with Sty Head forming the apex of a large triangle. Ennerdale bisects the area, which consists of the High Stile ridge north of Ennerdale, the Loweswater Fells in the far northwest, the Pillar group in the southwest, and Great Gable (899 m (2,949 ft)) near Sty Head. Other tops include Seatallan, Haystacks and Kirk Fell. This area is craggy and steep, with the impressive pinnacle of Pillar Rock its showpiece. Wastwater, located in this part, is England's deepest lake.
Central Fells
The Central Fells are lower in elevation than surrounding areas of fell, peaking at 762 m (2,500 ft) at High Raise. They take the form of a ridge running between Derwent Water in the west and Thirlmere in the east, from Keswick in the north to Langdale Pikes in the south. A spur extends southeast to Loughrigg Fell above Ambleside. The central ridge running north over High Seat is exceptionally boggy.
Eastern Fells
The Eastern Fells consist of a long north-to-south ridge, the Helvellyn range, running from Clough Head to Seat Sandal with the 950 m (3,118 ft) Helvellyn at its highest point. The western slopes of these summits tend to be grassy, with rocky corries and crags on the eastern side. The Fairfield group lies to the south of the range and forms a similar pattern with towering rock faces and hidden valleys spilling into the Patterdale valley. It culminates in the height of Red Screes overlooking the Kirkstone Pass.
Far Eastern Fells
The Far Eastern Fells refers to all of the Lakeland fells to the east of Ullswater and the A592 road running south to Windermere. At 828 m (2,717 ft), the peak known as High Street is the highest point on a complex ridge that runs broadly north-south and overlooks the hidden valley of Haweswater to its east. In the north of this region are the lower fells of Martindale Common and Bampton Common whilst in the south are the fells overlooking the Kentmere valley. Further to the east, beyond Mardale and Longsleddale is Shap Fell, an extensive area consisting of high moorland, more rolling and Pennine in nature than the mountains to the west.
Southern Fells
The Southern Fells occupy the southwestern quarter of the Lake District. They can be regarded as comprising a northern grouping between Wasdale, Eskdale, and the two Langdale valleys, a southeastern group east of Dunnerdale and south of Little Langdale, and a southwestern group bounded by Eskdale to the north and Dunnerdale to the east.
The first group includes England's highest mountains: Scafell Pike in the centre, at 978 m (3,209 ft) and Scafell one mile (1.6 km) to the southwest. Though it is slightly lower, Scafell has a 700 ft (210 m) rockface, Scafell Crag, on its northern side. This group also includes the Wastwater Screes overlooking Wasdale, the Glaramara ridge overlooking Borrowdale, the three tops of Crinkle Crags, Bowfell and Esk Pike. The core of the area is drained by the infant River Esk. Collectively these are some of the Lake District's most rugged hillsides.
The second group, otherwise known as the Furness Fells or Coniston Fells, have as their northern boundary the steep and narrow Hardknott and Wrynose passes. The highest are Old Man of Coniston and Swirl How which slightly exceed 800 m (2,600 ft).
The third group to the west of the Duddon includes Harter Fell and the long ridge leading over Whitfell to Black Combe and the sea. The south of this region consists of lower forests and knolls, with Kirkby Moor on the southern boundary. The southwestern Lake District ends near the Furness peninsula and Barrow-in-Furness, a town which many Lake District residents rely on for basic amenities.
Southeastern area
The southeastern area is the territory between Coniston Water and Windermere and east of Windermere towards Kendal and south to Lindale. There are no high summits in this area which are mainly low hills, knolls and limestone cuestas such as Gummer's How and Whitbarrow. Indeed, it rises only as high as 333 m (1,093 ft) at Top o' Selside east of Coniston Water; the wide expanse of Grizedale Forest stands between the two lakes. Kendal and Morecambe Bay stand at the eastern and southern edges of the area.
Valleys
The main radial valleys are (clockwise from the south) Dunnerdale, Eskdale, Wasdale, Ennerdale, the Vale of Lorton, and Buttermere valley, the Derwent Valley and Borrowdale, the Ullswater valley, Haweswater valley, Longsleddale, the Kentmere valley, those converging on the head of Windermere - Grasmere, Great Langdale and Little Langdale, and the Coniston Water valley. The valleys break the mountains up into blocks, which have been described by various authors in different ways. The most frequently encountered approach is that made popular by Alfred Wainwright who published seven separate area guides to the Lakeland Fells.
Only one of the lakes in the Lake District is called by that name, Bassenthwaite Lake. All the others such as Windermere, Coniston Water, Ullswater and Buttermere are meres, tarns and waters, with mere being the least common and water being the most common. The major lakes and reservoirs in the National Park are given below.
Bassenthwaite Lake
Brotherswater
Buttermere
Coniston Water
Crummock Water
Derwent Water
Devoke Water
Elter Water
Ennerdale Water
Esthwaite Water
Grasmere
Haweswater Reservoir
Hayeswater
Loweswater
Rydal Water
Thirlmere
Ullswater
Wast Water
Windermere
Woodlands
Below the tree line are wooded areas, including British and European native oak woodlands and introduced softwood plantations. The woodlands provide habitats for native English wildlife. The native red squirrel is found in the Lake District and a few other parts of England. In parts of the Lake District, the rainfall is higher than in any other part of England. This gives Atlantic mosses, ferns, lichen, and liverworts the chance to grow. There is some ancient woodland in the National Park. Management of the woodlands varies: some are coppiced, some pollarded, some left to grow naturally, and some provide grazing and shelter.
Coast
The Lake District extends to the coast of the Irish Sea from Drigg in the north to Silecroft in the south, encompassing the estuaries of the Esk and its tributaries, the Irt and the Mite. The intertidal zone of the combined estuaries includes sand, shingle and mudflats, and saltmarsh. The dune systems on either side of the estuary are protected as nature reserves; Drigg Dunes and Gullery to the north and Eskmeals Dunes[31] to the south. South of the estuary, the coast is formed in low cliffs of glacial till, sands, and gravels.
The district also extends to the tidal waters of Morecambe Bay and several of its estuaries alongside the Furness and Cartmel Peninsulas, designated on M6 motorway signposts as the "Lake District Peninsulas", and the southern portions of which lie outside the park. These are the Duddon Estuary, the Leven Estuary, and the western banks and tidal flats of the Kent Estuary. These areas are each characterised by sand and mudflats of scenic and wildlife interest. The coast is backed by extensive flats of raised marine deposits left when the relative sea level was higher.
Rotterdam - Depot Boijmans Van Beuningen, the world’s first fully accessible art depot, will open its doors in September 2021 at Museumpark in the centre of Rotterdam. With this construction completion, now the museum and the users can start to inhabit the building and fill its spaces with priceless art. Although it will take another year before the real opening, the completion is a special moment . 7,000 lucky persons can make a safe quick visit in 3 days in September 2020.
The assignment for MVRDV Architects was to offer a glimpse behind the scenes of the museum world and make the whole art collection accessible to the public. The reflective round volume responds to its surroundings. The Depot features exhibition halls, a rooftop garden, and a restaurant, in addition to an enormous amount of storage space for art and design.
Depot Boijmans Van Beuningen is the first depot in the world that offers access to a complete collection. The dynamics of the depot are different from those of the museum: no exhibitions are held here, but you can - independently or with a guide - browse through 151,000 art objects. You can also take a look at, for example, conservation and restoration.. Surface 15,000 m²
MVRDV has completed the bowl-like Depot Boijmans Van Beuningen in Rotterdam's Museumpark, which is covered in mirrored glass and topped by a rooftop forest. The art storage facility, which will open to the public in autumn 2021, has been built to house the art collection of the Museum Boijmans Van Beuningen in one place for the first time since 1935. Depot Boijmans Van Beuningen contains a mix of storage spaces alongside areas for art maintenance, both of which will be made accessible to visitors after the artwork has been moved there. This makes the facility the first publicly accessible art depot in the world, according to MVRDV Architects, and will offer a new type of experience for museum-goers in the Netherlands.
The Depot Boijmans Van Beuningen measures 12 metres in height and encompasses 15,000 m2. The budget was € 55,000,000. To help reduce its visual impact, MVRDV clad the depot in 1,664 reflective glass panels so that it blends in with its surroundings in the OMA-designed Museumpark. Its bowl-shape was also developed to minimise its footprint. The rooftop features 75 birch trees. Its reflective facade wears the trappings of whatever surrounds it: people passing by, Museumpark's leafy grounds, the clouds, and Rotterdam's dynamic city skyline. Thanks to this reflection, the building is already fully integrated into its surroundings, despite its not insignificant size.
Inside, the building contains several storage spaces alongside studios for the curators and areas for the maintenance of the art. The storage spaces are divided into five different climate zones so that the artefacts can be stored and exhibited according to their specific temperature and humidity requirements, which can vary depending on the materials used to make them. According to MVRDV, the focal point of the depot is its central atrium, which is filled with overlapping staircases and suspended glass display cases that will eventually be filled with art chosen by the museum's curators. This atrium will connect the storage and exhibition spaces to the curators' studios, and offer visitors rare access and insights into how the museum cares and maintains its collection. Once open to the public, the Museum Boijmans Van Beuningen's artwork will be displayed throughout the entire building, including on its rooftop restaurant and sculpture garden. The rooftop forest is covered with 75 tall birch trees and was incorporated by the studio to make up for the lost green space and provide views across the city.
MVRDV is an architecture studio based in Rotterdam, which was founded by Winy Maas, Jacob van Rijs and Nathalie de Vries in 1991. The studio won a competition to design the Depot Boijmans Van Beuningen in 2014.
It was developed by the studio with BAM Bouw & Techniek and will be made open to the public after its interiors are completed and the artwork has been moved inside.
Couple walking along Accessible Path at Multnomah Falls in the Columbia River Gorge National Scenic Area
The KOM League
Flash Report
for
Friday, November 13, 2020
For those who care, this Flash Report is accessible by going to: www.flickr.com/photos/60428361@N07/50597060261/
In a note shared with a few readers on November 12 the following statement was made. “Can you imagine having a Friday 13th in the year 2020? I’m optimistic and believing it will not be a bad omen—Amen?” That message elicited many responses. However, around 5:00 a. m. a message was received from a faithful reader that stated “Charlie Pride RIP.” That was news to the old batboy and this response was sent in response to that terse e-mail. “He and Mickey Mantle used to run around together in Dallas. Mickey's mother-in-law told him she'd like to meet Charlie. Mrs. Johnson told me that around two in the morning, shortly thereafter, Mickey came into her bedroom and announced that Pride was in the living room and to get out of bed and meet him.”
Since it was now Friday the 13th a decision was made to look further into the Charlie Pride story and as a result this message was sent to the person apprising me of Pride’s passing.
“Charlie's death has been greatly exaggerated. He is not dead nor doth he sleep in Biblical jargon” www.wideopencountry.com/charley-pride-death-hoax/
With that rumor out of the way it might bode well that this Friday the 13th will be a great day.
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A great loss
In the October 18, 2020 edition of this publication the following paragraph concluded that report. “This publication regrettably carries the news of many deaths. Someone who has read this and other KOM league publication since their inception is now facing the end of their days. That person happens to have known me longer than anyone currently living. It has become my task, duty, honor or whatever to write that person’s obituary. It is a difficult assignment to reduce to a few paragraphs the scope of a life that has now reached 85 years and if the Good Lord permits will be 86 within the next five weeks.”
On Halloween the person mentioned in the previous paragraph left this world for a much better place. The obituary along with a picture of the deceased is carried on this link: www.knellmortuary.com/obituaries/Janice-Elaine-Pinter?obI...
If you availed yourself of perusing that link you will know that the deceased was the sister of this here guy writing the story. But, there is more to the story. Very few people had as much confidence in the KOM league publications than the deceased. When it was opined the writing effort should come to an end my sister would always have a reason why that shouldn’t happen. On one occasion her opinion was that her little brother did more good befriending the old ballplayers and helping them than he ever did in the various churches he pastored. After thinking over that observation for a little while the little brother concurred.
It was always “Little Brother’s” idea that something would cause the KOM league reports to come to a merciful end if not by death but due to another happenstance. When my sister departed, although she hadn’t read any of the material for a few years, the first inclination was that now was the time to shut it down.
A coincidence?
On the same day of the death of Janice Pinter a letter was penned by a long time reader. It didn’t reach the “KOM League Office and Dusty Baseball Register Archives” until November 2. The letter, which was sent in place of an e-mail, had some things that are direct quotes. “A strong suggestion—quit attempting to stop writing. It is not possible to stop.”
Since the aforementioned came from a guy calling himself “Ol Clark” it was necessary to keep reading. Bill Clark is the real name and he has been around the sports world and the actual world many times. He is a living storehouse of great stories which he promises he’s going to share with the world in the form of three books. This writer is dubious that three will be sufficient.
Much of Clark’s baseball archives were destroyed in a fire, two years ago, but I’m sure much of that remains in his total recall memory bank. So, I await his upcoming literary works as much as pondering what to do about continuation of these reports. However, a constant reminder will be ever present. Clark concluded his remarks by stating “So—writers write even when no one reads them.” And for clinchers he said “No charge for the sermon.”
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In the spirit of the times
With the spread of the Chinese plague one is always concerned about the elderly and those with immune deficient conditions. As readers are aware most of the former KOM leaguers are either at least 90 or are so close to it they can see it on the horizon.
At the start of 2020, the top five oldest living former KOM leaguers included Nicholas Timothy Kucher. In going through the listing of Nick or Nicholas Kucher’s, who passed away, there wasn’t anything located in an obituary listing. On a whim his name was entered into Ancestry.com and there was a Find-A-Grave citation for the former KOM leaguer. www.findagrave.com/memorial/214613060/nicholas-kucher
At that juncture an even more concentrated effort was made to find an obituary for the former Ponca City Dodger was undertaken. Even the standby source, Jack Morris, couldn’t locate one either. At that point Morris was advised that an attempt would be made to come up with some information on the deceased.
Nicholas Timothy Kucher was born November 1, 1924 in New York City to Alex and Mary Kucher who were Polish immigrants. On his Sporting News card the word “Ukrainian” is typed on the top of that document as shown here. digital.la84.org/digital/collection/p17103coll3/id/112856...
Upon reaching the age of 18 he signed up for the draft and was listed as living at 315 E. 9th St. in New York and was employed by the Baker and Taylor Company at 55 5th Avenue. He filled out his card as being 6’ and weighing 170 with a scar on his left forehead. It would not have been possible for him to call his employer to report being unable to come to work, for any reason, since the family didn’t own a telephone.
Upon reporting to Ponca City in late April of 1947 this profile was shared under the heading “Meet the Dodgers.” Nick Kucher—is an outfielder, 22 years old and played his first competitive baseball with the Seward Park high school in his home town, New York city. A first baseman in prep school, he worked both the initial sack and the outfield with a semi-pro club last season (1946). He served three years in the marines, including duty at Okinawa and Saipan, and was discharged in 1945. He stands an even 6 feet, weight 172 pound and is single. A lefthanded batter and thrower, Kucher trained at Thomasville, N. C. this spring.”
What led to Kucher coming to Ponca City is contained in this late April, 1947 edition of the Ponca City News. “…Business Manager Owen Martinez announced the trade of George Schneider, 18-year-old New York city lad who has been here since last weekend, for Nick Kucher of the class C Three Rivers, Quebec, club. Schneider left Ponca City by plane in an effort to arrive at Three Rivers in time for the Canadian-American league’s opening game today. Kucher is due here this weekend.”
Upon Kucher’s arrival the KOM league season had not commenced but the Ponca City club was playing exhibition contests around the area. The first game he ever saw was from the bench as his new team was playing the Oklahoma A & M Agvets at Stillwater. This was long before that school was known as the Oklahoma State Cowboys. The Ponca City News reported “Nick Kucher, an outfielder who came in last weekend from Thomasville, N. C., on a trade with Three Rivers, Quebec was on the bench at Stillwater with a sprained ankle will probably be out of play a week, his doctor says.”
When the KOM league season began Kucher was in the outfield playing both right and centerfield but not at the same time. In his first nine games he hit nearly .300 but by his 18th contest his average slipped to the .200 level and his baseball days in the KOM league were history. In a long ago conversation with Kucher he blamed the bad ankle for his not being able to perform at the level he wanted.
Not long after leaving Ponca City Kucher returned to New York and married Anne Zatowsky on January 16, 1948. They lived happily ever after until her death in 2017. When this source communicated with the Kucher’s they lived in East Northport, New York at 154 Cedar Road. They later moved to Commack, New York. I believe that Nick even lived in Scottsdale, Arizona for a time in his later years.
It can’t be determined the day and month Kucher passed away but it was in 2020. Thus, he was either 95-96 when St. Peter came calling.
The ninety two year-old penny
Most of what is contained in this article came from scrapbooks kept by a young female fan of the 1946-48-49 and 1950 Ponca City Dodgers. It is my belief she fell in and out of love with someone on each of those teams. Her scrapbooks followed her to California where they were kept for over 60 years before she finally contacted Gale Wade and offered them to him. Wade, who had played at Ponca City in 1947 and 48, didn’t want those items and suggested she get in touch with a fellow who writes about the KOM league.
In those scrapbooks are hundreds of photos of Ponca City and other KOM league players that included future big leaguers Jim Baxes, Chris Kitsos, Gale Wade and former Dodger Boyd Bartley. The scrapbooks featured many social events such as picnics. Most every box score of Ponca City home games is in those scrapbooks along with a comment about the game inserted by the “keeper of the scrapbooks.” In some places a memento of a game or from a social gathering was included.
For over a decade Yours truly has looked at those scrapbooks, from time to time. One item placed under a box score was a penny scotch taped thereto. It dawned on me, in looking at that page, to decipher the number of games in which Nick Kucher played, that the tape was still holding the penny in place. Peeling back the taped it was a bit exciting to anticipate the date on the penny knowing it had to have been minted in 1947 or earlier. What was on the front of the Lincoln head—wheat ear coin was “1928-D.” On top of that it was in good condition. At the time it was placed in the scrapbook it was only 19 years old.
So, I guess I could offer that penny to some reader for their thoughts. Do I have to say “A penny for your thoughts?”
Who remains?
When a former KOM leaguer passes away a quick check is made to see how many of his teammates remain. As of this moment I believe the list includes: William Skeen, Dale Hendricks, George Fisher, Larry Tarbell and Gale Wade. Robert Clark Taylor and Phillip Adams were never located although there is a high level of suspicion where they currently reside.
In reviewing the list of the members of the 1947 Ponca City Dodgers who were once contacted and then nothing being heard from or about them in a long time included John Dominic Ferluga and Donald Andrew Tisnerat.
John Ferluga was a native of Seattle, Washington born 10/28/1926. He graduated from Queen Ann High School in 1946 and was the opening day hurler for the 1947 Ponca City Dodgers. That was the only game in which he played with them. There has never been an obituary located for him but a listing from his high school alumni publication shows he passed away on 2/13/2017 in Renton, WA.
Donald Andrew Tisnerat was born 4/14/1927 in Long Beach, CA . He also pitched for the 1947 Ponca City Club. He had graduated from David Starr Jordan high school in Long Beach and served in the U. S. Navy during WW II. He lived in a number of places and when this source contacted him a couple of decades ago he was living in Las Vegas, NV. That is where he passed away on 6/29/2014. He was buried at the Riverside National Cemetery in Riverside, CA. That is a spectacular and somber place. en.wikipedia.org/wiki/Riverside_National_Cemetery
Bilder vom freien Training! --- de-de.facebook.com/OppenHaalerSeifenkistenrennen/ --- Alle Fotos entstanden an für jeden zugänglichen, öffentlichen Orten. Sofern ich an diesen Orten von einem Fotografierverbot Kenntnis hatte, habe ich dieses Fotografierverbot strikt beachtet! Es ist nicht meine Absicht, die Rechte Dritter zu verletzen.
Sollte dennoch eine Privatperson, Institution oder Firma ihre Rechte durch meine Fotos beeinträchtigt sehen, genügt ein freundlicher Hinweis und ich nehme das beanstandete Foto aus meinem Fotostream.
---
All photos were taken for every accessible, public place. If I had knowledge of a photography ban in these places, I strictly observed this photography ban! It is not my intention to violate the rights of third parties.
Should nevertheless a private person, institution or company see their rights impaired by my photos, a friendly note is sufficient and I take the offending photo from my photo stream.
Accessible Pedestrian Signal: lean entire body weight, I mean, press black button for count of 5, feel a click, feel the button vibrate when walk light comes on and hear the chirps telling you it's OK to go cross the road.
These seem to often be broken - button won't click, sound won't chirp. So if you want to help your fellow citizens get around easily - press one of these buttons to see if it works. If not, call or tweet 311! Easy, quick! :)
Liberty Equality Accessibility
Rassemblement des personnes en situation de handicap pour un véritable changement, vers une république inclusive_Paris_Mai 2025
Gathering of people with disabilities for a truly inclusive republic_Paris_Mai 2025
www.magd.ox.ac.uk/discover-magdalen/
To celebrate its 550th anniversary Magdalen College, Oxford has commissioned the Turner Prize-winning artist Mark Wallinger to create his first-ever dedicated permanent artwork.
Two years in development, the sculpture Y was unveiled on St Mary Magdalen Day 2008. William Waynflete, Bishop of Winchester founded Magdalen College in 1458. It is one of the best-known colleges in the University of Oxford and is known internationally for its high academic standing.
The College has many fine buildings. The Cloisters, Chapel, Founder’s Tower and Hall were built in the Gothic style in the later part of the 15th century. The Great Tower, a pictorial symbol of Oxford, is famous for the May Day event when the College choir sings an ancient hymn at dawn. The Georgian New Buildings, which blend into the College Gardens and grounds, were completed in 1733. The buildings sit amid a hundred acres of lawns, woodlands and riverside walks, which are publicly accessible, and there is a deer herd that has been in existence for over 300 years.
Addison’s Walk, named after the great essayist of the 18th century and father of English journalism, is about a mile in length and goes by the River Cherwell around a great water meadow. Beyond the end of Addison’s Walk is a tranquil field known as Bat Willow Meadow, which is where the new commission is sited. Maps of the grounds of Magdalen College are available from the Porters’ Lodge or they can be downloaded from the Magdalen website.
Over the past twenty years Mark Wallinger has established an international reputation with major solo exhibitions in London, Birmingham, Liverpool, Val-de-Marne, Frankfurt, Aarau, Basel, Milan, New York and Chicago.
His work encompasses a wide range of media, including painting, photography, sculpture, video and installation, and it takes art history, mythology, religion, politics, national identity and popular culture as its subject matter. Wallinger studied at Chelsea School of Art in 2001, and in Goldsmiths' College. He exhibited in Young British Artists II at the Saatchi Collection in 1993 and at the Royal Academy of Art's Sensation exhibition in 1997.
His Time and relative dimensions in space derived from a residency and was shown at Oxford University Museum of Natural History in 2001 and in the same year he represented Britain in the 49th Venice Biennale. The artist is best known for Ecce Homo, a life-size sculpture of Jesus Christ which inaugurated the Fourth Plinth in Trafalgar Square in 1999, and State Britain, his 2007 re-creation at Tate Britain of Brian Haw's protest display outside parliament. He was a Turner Prize nominee in 1995 and won the award in 2007, and he is one of five internationally acclaimed artists who have been commissioned to produce proposals for the Ebbsfleet Landmark Project, which will be one of the biggest artworks in the United Kingdom.
From City of St.Catharines Guide to Accessible information & Communication training. December 5, 2011
Regardless of their disabilities, all Ontarians have the same rights to communicate as individuals without a disability; rights that are protected by the Ontario Human Rights Code.
Organizations must be prepared to provide alternative formats of traditional communication tools. This includes written documents, reports, brochures, and forms and also extends to multi-media tools, such as videos and website.
Must provide accessible formats
Upon Request
In a Timely Manner
At NO extra cost!
The Information and Communications Standard section under the Integrated Accessibility Regulation provides guidance for providing accessible communication.
Not just the law but good customer service, too
StatsCan estimates that by 2026 one of every five people living in Canada will be a senior. As people age, they have greater incidences of hearing loss, low vision, cognitive impairments and lessened mobility and dexterity.
Approximately 836,000 Canadians identified themselves as having a seeing disability in a 2007 StatsCan study, while approximately 10 per cent of Canada’s population suffers from some form of hearing lost.
Add to this the 10 per cent of Canadians who have a learning disability and it is easy to see that in the future increasing numbers of residents and customers will require some kind of alternative format to access information from the City.
By providing accessible communications, we will increase the number of people who can access information, reaching a greater number of our residents.
And that is good customer service.
Use Plain Language
Plain Language is text that the reader can read and understand the first time.
It sounds easy enough, but text is often cluttered with acronyms, jargon and complex sentence structure.
Text that is clear and easy to read benefits customers with learning disabilities and low literacy skills. It improves comprehension for all users and allows for easy adaptation to other formats.
When writing plain language, remember to:
•Keep your intended audience in mind
•Use an active voice
•Shorten sentences
•Use everyday words
•Eliminate jargon
•Use simple sentence structure and grammar
Other notes:
Align Left (justified text causes problems)
Watch Font size (no less than 12 point font)
Use styles / style sheets for formatting
Use Tables for data not formatting
Provide alternative text for charts and pictures
Caption videos
Anthroposophy, a philosophy founded by Rudolf Steiner, postulates the existence of an objective, intellectually comprehensible spiritual world accessible to direct experience through inner development. More specifically, it aims to develop faculties of perceptive imagination, inspiration and intuition through cultivating a form of thinking independent of sensory experience, and to present the results thus derived in a manner subject to rational verification. In its investigations of the spiritual world, anthroposophy aims to attain the precision and clarity attained by the natural sciences in their investigations of the physical world.
Anthroposophical ideas have been applied practically in many areas including Steiner/Waldorf education, special education (most prominently through the Camphill Movement), agriculture, medicine, ethical banking, organizational development, and the arts.
Architecture
The First Goetheanum, designed by Steiner in 1920, Dornach, Switzerland.
Steiner himself designed around thirteen buildings, many of them significant works in a unique, organic—expressionist architectural style. Foremost among these are his designs for the two Goetheanum buildings in Dornach, Switzerland. Thousands of further buildings have been built by later generations of anthroposophic architects.
Architects who have been strongly influenced by the anthroposophic style include Imre Makovecz in Hungary, Hans Scharoun and Joachim Eble in Germany, Erik Asmussen in Sweden, Kenji Imai in Japan, Thomas Rau, Anton Alberts and Max van Huut in Holland, Christopher Day and Camphill Architects in the UK, Thompson and Rose in America, Denis Bowman in Canada, and Walter Burley Griffin and Gregory Burgess in Australia.
One of the most famous contemporary buildings by an anthroposophical architect is ING House, an ING Bank building in Amsterdam, which has received several awards for its ecological design and approach to a self-sustaining ecology as an autonomous building and example of sustainable architecture. Designed by Ton Alberts, as remarked by Akbar ! :-)
www.magd.ox.ac.uk/discover-magdalen/
To celebrate its 550th anniversary Magdalen College, Oxford has commissioned the Turner Prize-winning artist Mark Wallinger to create his first-ever dedicated permanent artwork.
Two years in development, the sculpture Y was unveiled on St Mary Magdalen Day 2008. William Waynflete, Bishop of Winchester founded Magdalen College in 1458. It is one of the best-known colleges in the University of Oxford and is known internationally for its high academic standing.
The College has many fine buildings. The Cloisters, Chapel, Founder’s Tower and Hall were built in the Gothic style in the later part of the 15th century. The Great Tower, a pictorial symbol of Oxford, is famous for the May Day event when the College choir sings an ancient hymn at dawn. The Georgian New Buildings, which blend into the College Gardens and grounds, were completed in 1733. The buildings sit amid a hundred acres of lawns, woodlands and riverside walks, which are publicly accessible, and there is a deer herd that has been in existence for over 300 years.
Addison’s Walk, named after the great essayist of the 18th century and father of English journalism, is about a mile in length and goes by the River Cherwell around a great water meadow. Beyond the end of Addison’s Walk is a tranquil field known as Bat Willow Meadow, which is where the new commission is sited. Maps of the grounds of Magdalen College are available from the Porters’ Lodge or they can be downloaded from the Magdalen website.
Over the past twenty years Mark Wallinger has established an international reputation with major solo exhibitions in London, Birmingham, Liverpool, Val-de-Marne, Frankfurt, Aarau, Basel, Milan, New York and Chicago.
His work encompasses a wide range of media, including painting, photography, sculpture, video and installation, and it takes art history, mythology, religion, politics, national identity and popular culture as its subject matter. Wallinger studied at Chelsea School of Art in 2001, and in Goldsmiths' College. He exhibited in Young British Artists II at the Saatchi Collection in 1993 and at the Royal Academy of Art's Sensation exhibition in 1997.
His Time and relative dimensions in space derived from a residency and was shown at Oxford University Museum of Natural History in 2001 and in the same year he represented Britain in the 49th Venice Biennale. The artist is best known for Ecce Homo, a life-size sculpture of Jesus Christ which inaugurated the Fourth Plinth in Trafalgar Square in 1999, and State Britain, his 2007 re-creation at Tate Britain of Brian Haw's protest display outside parliament. He was a Turner Prize nominee in 1995 and won the award in 2007, and he is one of five internationally acclaimed artists who have been commissioned to produce proposals for the Ebbsfleet Landmark Project, which will be one of the biggest artworks in the United Kingdom.
Diploria strigosa - fossil symmetrical brain coral colony in the reef facies of the Cockburn Town Member, upper Grotto Beach Formation at the Cockburn Town Fossil Reef, western margin of San Salvador Island.
The Cockburn Town Fossil Reef is a well-preserved, well-exposed Pleistocene fossil reef. It consists of non-bedded to poorly-bedded, poorly-sorted, very coarse-grained, aragonitic fossiliferous limestones (grainstones and rubblestones), representing shallow marine deposition in reef and peri-reef facies. Cockburn Town Member reef facies rocks date to the MIS 5e sea level highstand event (early Late Pleistocene). Dated corals in the Cockburn Town Fossil Reef range in age from 114 to 127 ka.
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The surface bedrock geology of San Salvador consists entirely of Pleistocene and Holocene limestones. Thick and relatively unforgiving vegetation covers most of the island’s interior (apart from inland lakes). Because of this, the most easily-accessible rock outcrops are along the island’s shorelines.
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Stratigraphic Succession in the Bahamas:
Rice Bay Formation (Holocene, <10 ka), subdivided into two members (Hanna Bay Member over North Point Member)
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Grotto Beach Formation (lower Upper Pleistocene, 119-131 ka), subdivided into two members (Cockburn Town Member over French Bay Member)
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Owl's Hole Formation (Middle Pleistocene, ~215-220 ka & ~327-333 ka & ~398-410 ka & older)
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San Salvador’s surface bedrock can be divided into two broad lithologic categories:
1) LIMESTONES
2) PALEOSOLS
The limestones were deposited during sea level highstands (actually, only during the highest of the highstands). During such highstands (for example, right now), the San Salvador carbonate platform is partly flooded by ocean water. At such times, the “carbonate factory” is on, and abundant carbonate sediment grains are generated by shallow-water organisms living on the platform. The abundance of carbonate sediment means there will be abundant carbonate sedimentary rock formed after burial and cementation (diagenesis). These sea level highstands correspond with the climatically warm interglacials during the Pleistocene Ice Age.
Based on geochronologic dating on various Bahamas islands, and based on a modern understanding of the history of Pleistocene-Holocene global sea level changes, surficial limestones in the Bahamas are known to have been deposited at the following times (expressed in terms of marine isotope stages, “MIS” - these are the glacial-interglacial climatic cycles determined from δ18O analysis):
1) MIS 1 - the Holocene, <10 k.y. This is the current sea level highstand.
2) MIS 5e - during the Sangamonian Interglacial, in the early Late Pleistocene, from 119 to 131 k.y. (sea level peaked at ~125 k.y.)
3) MIS 7 - ~215 to 220 k.y. - late Middle Pleistocene
4) MIS 9 - ~327-333 k.y. - late Middle Pleistocene
5) MIS 11 - ~398-410 k.y. - late Middle Pleistocene
Bahamian limestones deposited during MIS 1 are called the Rice Bay Formation. Limestones deposited during MIS 5e are called the Grotto Beach Formation. Limestones deposited during MIS 7, 9, 11, and perhaps as old as MIS 13 and 15, are called the Owl’s Hole Formation. These stratigraphic units were first established on San Salvador Island (the type sections are there), but geologic work elsewhere has shown that the same stratigraphic succession also applies to the rest of the Bahamas.
During times of lowstands (= times of climatically cold glacial intervals of the Pleistocene Ice Age), weathering and pedogenesis results in the development of soils. With burial and diagenesis, these soils become paleosols. The most common paleosol type in the Bahamas is calcrete (a.k.a. caliche; a.k.a. terra rosa). Calcrete horizons cap all Pleistocene-aged stratigraphic units in the Bahamas, except where erosion has removed them. Calcretes separate all major stratigraphic units. Sometimes, calcrete-looking horizons are encountered in the field that are not true paleosols.
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Subsurface Stratigraphy of San Salvador Island:
The island’s stratigraphy below the Owl’s Hole Formation was revealed by a core drilled down ~168 meters (~550-feet) below the surface (for details, see Supko, 1977). The well site was at 3 meters above sea level near Graham’s Harbour beach, between Line Hole Settlement and Singer Bar Point (northern margin of San Salvador Island). The first 37 meters were limestones. Below that, dolostones dominate, alternating with some mixed dolostone-limestone intervals. Reddish-brown calcretes separate major units. Supko (1977) infers that the lowest rocks in the core are Upper Miocene to Lower Pliocene, based on known Bahamas Platform subsidence rates.
In light of the successful island-to-island correlations of Middle Pleistocene, Upper Pleistocene, and Holocene units throughout the Bahamas (see the Bahamas geologic literature list below), it seems reasonable to conclude that San Salvador’s subsurface dolostones may correlate well with sub-Pleistocene dolostone units exposed in the far-southeastern portions of the Bahamas Platform.
Recent field work on Mayaguana Island has resulted in the identification of Miocene, Pliocene, and Lower Pleistocene surface outcrops (see: www2.newark.ohio-state.edu/facultystaff/personal/jstjohn/...). On Mayaguana, the worked-out stratigraphy is:
- Rice Bay Formation (Holocene)
- Grotto Beach Formation (Upper Pleistocene)
- Owl’s Hole Formation (Middle Pleistocene)
- Misery Point Formation (Lower Pleistocene)
- Timber Bay Formation (Pliocene)
- Little Bay Formation (Upper Miocene)
- Mayaguana Formation (Lower Miocene)
The Timber Bay Fm. and Little Bay Fm. are completely dolomitized. The Mayaguana Fm. is ~5% dolomitized. The Misery Point Fm. is nondolomitized, but the original aragonite mineralogy is absent.
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The stratigraphic information presented here is synthesized from the Bahamian geologic literature.
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Supko, P.R. 1977. Subsurface dolomites, San Salvador, Bahamas. Journal of Sedimentary Petrology 47: 1063-1077.
Bowman, P.A. & J.W. Teeter. 1982. The distribution of living and fossil Foraminifera and their use in the interpretation of the post-Pleistocene history of Little Lake, San Salvador, Bahamas. San Salvador Field Station Occasional Papers 1982(2). 21 pp.
Sanger, D.B. & J.W. Teeter. 1982. The distribution of living and fossil Ostracoda and their use in the interpretation of the post-Pleistocene history of Little Lake, San Salvador Island, Bahamas. San Salvador Field Station Occasional Papers 1982(1). 26 pp.
Gerace, D.T., R.W. Adams, J.E. Mylroie, R. Titus, E.E. Hinman, H.A. Curran & J.L. Carew. 1983. Field Guide to the Geology of San Salvador (Third Edition). 172 pp.
Curran, H.A. 1984. Ichnology of Pleistocene carbonates on San Salvador, Bahamas. Journal of Paleontology 58: 312-321.
Anderson, C.B. & M.R. Boardman. 1987. Sedimentary gradients in a high-energy carbonate lagoon, Snow Bay, San Salvador, Bahamas. CCFL Bahamian Field Station Occasional Paper 1987(2). (31) pp.
1988. Bahamas Project. pp. 21-48 in First Keck Research Symposium in Geology (Abstracts Volume), Beloit College, Beloit, Wisconsin, 14-17 April 1988.
1989. Proceedings of the Fourth Symposium on the Geology of the Bahamas, June 17-22, 1988. 381 pp.
1989. Pleistocene and Holocene carbonate systems, Bahamas. pp. 18-51 in Second Keck Research Symposium in Geology (Abstracts Volume), Colorado College, Colorado Springs, Colorado, 14-16 April 1989.
Curran, H.A., J.L. Carew, J.E. Mylroie, B. White, R.J. Bain & J.W. Teeter. 1989. Pleistocene and Holocene carbonate environments on San Salvador Island, Bahamas. 28th International Geological Congress Field Trip Guidebook T175. 46 pp.
1990. The 5th Symposium on the Geology of the Bahamas, June 15-19, 1990, Abstracts and Programs. 29 pp.
1991. Proceedings of the Fifth Symposium on the Geology of the Bahamas. 247 pp.
1992. The 6th Symposium on the Geology of the Bahamas, June 11-15, 1992, Abstracts and Program. 26 pp.
1992. Proceedings of the 4th Symposium on the Natural History of the Bahamas, June 7-11, 1991. 123 pp.
Boardman, M.R., C. Carney, B. White, H.A. Curran & D.T. Gerace. 1992. The geology of Columbus' landfall: a field guide to the Holcoene geology of San Salvador, Bahamas, Field trip 3 for the annual meeting of the Geological Society of America, Cincinnati, Ohio, October 26-29, 1992. Ohio Division of Geological Survey Miscellaneous Report 2. 49 pp.
Carew, J.L., J.E. Mylroie, N.E. Sealey, M. Boardman, C. Carney, B. White, H.A. Curran & D.T. Gerace. 1992. The 6th Symposium on the Geology of the Bahamas, June 11-15, 1992, Field Trip Guidebook. 56 pp.
1993. Proceedings of the 6th Symposium on the Geology of the Bahamas, June 11-15, 1992. 222 pp.
Lawson, B.M. 1993. Shelling San Sal, an Illustrated Guide to Common Shells of San Salvador Island, Bahamas. San Salvador, Bahamas. Bahamian Field Station. 63 pp.
1994. The 7th Symposium on the Geology of the Bahamas, June 16-20, 1994, Abstracts and Program. 26 pp.
1994. Proceedings of the 5th Symposium on the Natural History of the Bahamas, June 11-14, 1993. 107 pp.
Carew, J.L. & J.E. Mylroie. 1994. Geology and Karst of San Salvador Island, Bahamas: a Field Trip Guidebook. 32 pp.
Godfrey, P.J., R.L. Davis, R.R. Smtih & J.A. Wells. 1994. Natural History of Northeastern San Salvador Island: a "New World" Where the New World Began, Bahamian Field Station Trail Guide. 28 pp.
Hinman, G. 1994. A Teacher's Guide to the Depositional Environments on San Salvador Island, Bahamas. 64 pp.
Mylroie, J.E. & J.L. Carew. 1994. A Field Trip Guide Book of Lighthouse Cave, San Salvador Island, Bahamas. 10 pp.
1995. Proceedings of the Seventh Symposium on the Geology of the Bahamas, June 16-20, 1994. 134 pp.
1995. Terrestrial and shallow marine geology of the Bahamas and Bermuda. Geological Society of America Special Paper 300.
1996. The 8th Symposium on the Geology of the Bahamas, May 30-June 3, 1996, Abstracts and Program. 21 pp.
1996. Proceedings of the 6th Symposium on the Natural History of the Bahamas, June 9-13, 1995. 165 pp.
1997. Proceedings of the 8th Symposium on the Geology of the Bahamas and Other Carbonate Regions, May 30-June 3, 1996. 213 pp.
Curran, H.A., B. White & M.A. Wilson. 1997. Guide to Bahamian Ichnology: Pleistocene, Holocene, and Modern Environments. San Salvador, Bahamas. Bahamian Field Station. 61 pp.
1998. The 9th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 4-June 8, 1998, Abstracts and Program. 25 pp.
Wilson, M.A., H.A. Curran & B. White. 1998. Paleontological evidence of a brief global sea-level event during the last interglacial. Lethaia 31: 241-250.
1999. Proceedings of the 9th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 4-8, 1998. 142 pp.
2000. The 10th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 8-June 12, 2000, Abstracts and Program. 29+(1) pp.
2001. Proceedings of the 10th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 8-12, 2000. 200 pp.
Bishop, D. & B.J. Greenstein. 2001. The effects of Hurricane Floyd on the fidelity of coral life and death assemblages in San Salvador, Bahamas: does a hurricane leave a signature in the fossil record? Geological Society of America Abstracts with Programs 33(4): 51.
Gamble, V.C., S.J. Carpenter & L.A. Gonzalez. 2001. Using carbon and oxygen isotopic values from acroporid corals to interpret temperature fluctuations around an unconformable surface on San Salvador Island, Bahamas. Geological Society of America Abstracts with Programs 33(4): 52.
Gardiner, L. 2001. Stability of Late Pleistocene reef mollusks from San Salvador Island, Bahamas. Palaios 16: 372-386.
Ogarek, S.A., C.K. Carney & M.R. Boardman. 2001. Paleoenvironmental analysis of the Holocene sediments of Pigeon Creek, San Salvador, Bahamas. Geological Society of America Abstracts with Programs 33(4): 17.
Schmidt, D.A., C.K. Carney & M.R. Boardman. 2001. Pleistocene reef facies diagenesis within two shallowing-upward sequences at Cockburntown, San Salvador, Bahamas. Geological Society of America Abstracts with Programs 33(4): 42.
2002. The 11th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 6th-June 10, 2002, Abstracts and Program. 29 pp.
2004. The 12th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 3-June 7, 2004, Abstracts and Program. 33 pp.
2004. Proceedings of the 11th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 6-10, 2002. 240 pp.
Martin, A.J. 2006. Trace Fossils of San Salvador. 80 pp.
2006. Proceedings of the 12th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 3-7, 2004. 249 pp.
2006. The 13th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 8-June 12, 2006, Abstracts and Program. 27 pp.
Mylroie, J.E. & J.L. Carew. 2008. Field Guide to the Geology and Karst Geomorphology of San Salvador Island. 88 pp.
2008. Proceedings of the 13th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 8-12, 2006. 223 pp.
2008. The 14th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 12-June 16, 2006, Abstracts and Program. 26 pp.
2010. Proceedings of the 14th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 12-16, 2008. 249 pp.
2010. The 15th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 17-June 21, 2010, Abstracts and Program. 36 pp.
2012. Proceedings of the 15th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 17-21, 2010. 183 pp.
2012. The 16th Symposium on the Geology of the Bahamas and Other Carbonate Regions, June 14-June 18, 2012, Abstracts with Program. 45 pp.
Wildhorse Creek Wild and Scenic River as it spills from Wildhorse Lake, July 10, 2018, by Greg Shine, BLM.
Take yourself on a challenging hike down to Wildhorse Lake and Wildhorse Creek Wild and Scenic River, below the Steens Mountain rim. Don't forget that you need to hike back out, though!
The lake is accessible from a trail starting at the Wildhorse Lake Overlook, which is just off the Steens Mountain Loop Road near the summit.
Wildhorse Lake (and nearby Little Wildhorse Lake) provide vernal high elevation pools, talus and cliffs, willows, and adjacent upland vegetation which together provide a diversity of wildlife habitats.
Wildhorse Creek Wild and Scenic River provides habitat for California bighorn sheep and a variety of wildlife from headwaters to canyon mouths. Species such as pika can be found at upper elevations. They also contain interesting and unique assemblages of vegetative communities.
Know Before You Go:
• Limited water sources – carry enough water and food to last your entire trip, and do not drink from untested water sources.
• Ticks, mosquitoes, and rattlesnakes in certain areas during spring and summer.
• Weather conditions – the mountain’s high elevation can cause rapid temperature changes. Blustery, 100-degree days are common and snow can fall year-round. Be prepared for sudden lightning storms, snow, rain, and high winds.
• Long distances between services – including gas stations, phones, and cell phone reception. Let someone at home know where you plan to go and when you plan to return. Phone service should not be relied on for emergency communication. Always start your trip with a full tank of fuel and call ahead for current information about fuel availability in the Steens Mountain area. Fuel may be available in the towns of Fields, Frenchglen, Crane, or the Narrows.
• Rough terrain – deep canyons and rocky slopes are a natural party of the rugged mountain territory. Elevation can change from less than 4,000 feet to over 9,000 feet in just a few miles. We recommend high clearance or 4x4 vehicles for primitive roads, including the steep and rocky portion of the Steens Mountain Loop Road near South Steens Campground. The rest of the Steens Mountain Loop Road can accommodate passenger cars at lower speeds. High quality tires are a must for all vehicles, even when traveling on maintained routes.
• Livestock and wildlife on roadways – much of southeast Oregon is open range. Be alert, drive with caution, and plan to share roadways with cattle, deer, elk, antelope, wild horses, and rabbits!
• Staying Found – the remote nature and vast landscape of the Steens Mountain area may leave even the most experienced traveler directionally confused or just plain lost. Traveling with a current map of the area is essential! Don’t hesitate to talk to locals - area landowners and Federal employees are generally visible in the Steens Mountain area. We welcome your visit and have information to help you.
More Info: www.blm.gov/visit/wildhorse-creek-wild-scenic-river
www.blm.gov/programs/recreation/recreation-activities/ore...
Contact:
Bums District
Bureau of Land Management
28910 Hwy 20 West
Hines, OR 97738
541-573-4400