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Como,Vincenzo Castella's exhibition. 180x300cm LightJet prints: scans by CastorScan
N3 LightJet prints 180x300 cm on Kodak Endura Paper
Scans by CastorScan
Stampe digitali LightJet 180x300 cm su carta Kodak Endura.
Scansioni da negativi colore Kodak Portra 160NC 12x20 pollici (30x51 cm) realizzate da CastorScan su scanner a tamburo.
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CastorScan's philosophy is completely oriented to provide the highest scan and postproduction
quality on the globe.
We work with artists, photographers, agencies, laboratories etc. who demand a state-of-the-art quality at reasonable prices.
Our workflow is fully manual and extremely meticulous in any stage.
We developed exclusive workflows and profilation systems to obtain unparallel results from our scanners not achievable through semi-automatic and usual workflows.
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CastorScan uses the best scanners in circulation, Dainippon Screen SG-8060P Mark II, the best and most advanced scanner ever made, Kodak-Creo IQSmart 3, a high-end flatbed scanner, and Imacon 848.
The image quality offered by our Dainippon Screen 8060 scanner is much higher than that achievable with the best flatbed scanners or filmscanners dedicated and superior to that of scanners so-called "virtual drum" (Imacon – Hasselblad,) and, of course, vastly superior to that amateur or prosumer obtained with scanners such as Epson V750 etc .
Dainippon Screen SG-8060P Mark II exceeds in quality any other scanner, including Aztek Premier and ICG 380 (in the results, not just in the technical specifications).
8060's main features: 12000 dpi, Hi-Q Xenon lamp, 25 apertures, 2 micron
Aztek Premier's main features: 8000 dpi, halogen lamp, 18 apertures, 3 micron
ICG 380's main features: 12000 dpi, halogen lamp, 9 apertures, 4 micron
Some of the features that make the quality of our drum scanners better than any other existing scan system include:
The scans performed on a drum scanner are famous for their detail, depth and realism.
Scans are much cleaner and show fewer imperfections than scans obtained from CCD scanners, and thus save many hours of cleaning and spotting in postproduction.
Image acquisition by the drum scanner is optically similar to using a microscopic lens that scans the image point by point with extreme precision and without deformation or distortion of any kind, while other scanners use enlarger lenses (such as the Rodenstock-Linos Magnagon 75mm f8 used in the Hasselblad-Imacon scanners) and have transmission systems with rubber bands: this involves mild but effective micro-strain and micro-geometric image distortions and quality is not uniform between the center and edges.
Drum scanners are exempt from problems of flatness of the originals, since the same are mounted on a perfectly balanced transparent acrylic drum; on the contrary, the dedicated film scanners that scan slides or negatives in their plastic frames are subject to quite significant inaccuracies, as well as the Imacon-Hasselblad scanners, which have their own rubber and plastic holders: they do not guarantee the perfect flatness of the original and therefore a uniform definition between center and edge, especially with medium and large size originals, which instead are guaranteed by drum scanners.
Again, drum scanners allow scanning at high resolution over the entire surface of the cylinder, while for example the Hasselblad Imacon scans are limited to 3200 dpi in 120 format and 2000 dpi in 4x5" format (the resolution of nearly every CCD scanner in the market drops as the size of the original scanned is increased).
Drum scanners allow complete scanning of the whole negative, including the black-orange mask, perforations etc, while using many other scanners a certain percentage of the image is lost because it is covered by frames or holders.
Drum scanners use photomultiplier tubes to record the light signal, which are much more sensitive than CCDs and can record many more nuances and variations in contrast with a lower digital noise.
If you look at a monitor at 100% the detail in shadows and darker areas of a scan made with a CCD scanner, you will notice that the details are not recorded in a clear and clean way, and the colors are more opaque and less differentiated. Additionally the overall tones are much less rich and differentiated.
We would like to say a few words about an unscrupulous and deceitful use of technical specifications reported by many manufacturers of consumer and prosumer scanners; very often we read of scanners that promise cheap or relatively cheap “drum scanner” resolutions, 16 bits of color depth, extremely high DMAX: we would like to say that these “nominal” resolutions do not correspond to an actual optical resolution, so that even in low-resolution scanning you can see an enormous gap between drum scanners and these scanners in terms of detail, as well as in terms of DMAX, color range, realism, “quality” of grain. So very often when using these consumer-prosumer scanners at high resolutions, it is normal to get a disproportionate increase of file size in MB but not an increase of detail and quality.
To give a concrete example: a drum scan of a 24x36mm color negative film at 3500 dpi is much more defined than a scan made with mostly CCD scanner at 8000 dpi and a drum scan at 2500 dpi is dramatically clearer than a scan at 2500 dpi provided by a CCD scanner. So be aware and careful with incorrect advertisement.
Scans can be performed either dry or liquid-mounted. The wet mounting further improves cleanliness (helps to hide dirt, scratches and blemishes) and plasticity of the image without compromising the original, and in addition by mounting with liquid the film grain is greatly reduced and it looks much softer and more pleasant than the usual "harsh" grain resulting from dry scans.
We use Kami SMF 2001 liquid to mount the transparencies and Kami RC 2001 for cleaning the same. Kami SMF 2001 evaporates without leaving traces, unlike the traditional oil scans, ensuring maximum protection for your film. Out of ignorance some people prefer to avoid liquid scanning because they fear that their films will be dirty or damaged: this argument may be plausible only in reference to scans made using mineral oils, which have nothing to do with the specific professional products we use.
We strongly reiterate that your original is in no way compromised by our scanning liquid and will return as you have shipped it, if not cleaner.
With respect to scanning from slides:
Our scanners are carefully calibrated with the finest IT8 calibration targets in circulation and with special customized targets in order to ensure that each scan faithfully reproduces the original color richness even in the most subtle nuances, opening and maintaining detail in shadows and highlights. These color profiles allow our scanners to realize their full potential, so we guarantee our customers that even from a chromatic point of view our scans are noticeably better than similar scans made by mostly other scan services in the market.
In addition, we remind you that our 8060 drum scanner is able to read the deepest shadows of slides without digital noise and with much more detail than CCD scanners; also, the color range and color realism are far better.
With respect to scanning from color and bw negatives: we want to emphasize the superiority of our drum scans not only in scanning slides, but also in color and bw negative scanning (because of the orange mask and of very low contrast is extremely difficult for any ccd scanner to read the very slight tonal and contrast nuances in the color negative, while a perfectly profiled 8060 drum scanner – also through the analog gain/white calibration - can give back much more realistic images and true colors, sharper and more three-dimensional).
In spite of what many claim, a meticulous color profiling is essential not only for scanning slides, but also, and even more, for color negatives. Without it the scan of a color negative will produce chromatic errors rather significant, thus affecting the tonal balance and then the naturalness-pleasantness of the images.
More unique than rare, we do not use standardized profiles provided by the software to invert each specific negative film, because they do not take into account parameters and variables such as the type of development, the level of exposure, the type of light etc.,; at the same time we also avoid systems of "artificial intelligence" or other functions provided by semi-automatic scanning softwares, but instead we carry out the inversion in a full manual workflow for each individual picture.
In addition, scanning with Imacon-Hasselblad scanners we do not use their proprietary software - Flexcolor – to make color management and color inversion because we strongly believe that our alternative workflow provides much better results, and we are able to prove it with absolute clarity.
At each stage of the process we take care of meticulously adjusting the scanning parameters to the characteristics of the originals, to extrapolate the whole range of information possible from any image without "burning" or reductions in the tonal range, and strictly according to our customer's need and taste.
By default, we do not apply unsharp mask (USM) in our scans, except on request.
To scan reflective originals we follow the same guidelines and guarantee the same quality standard.
We guarantee the utmost thoroughness and expertise in the work of scanning and handling of the originals and we provide scans up to 12,000 dpi of resolution, at 16-bit, in RGB, GRAYSCALE, LAB or CMYK color mode; unless otherwise indicated, files are saved with Adobe RGB 1998 or ProPhoto RGB color profile.
I love this, it's like being punched in the face by a painting. Pity about the knob addition to everything at Dean Lane of late.
I picked up a Mamiya 645E last week. This was a great find - body, 45mm f/2.8, 80mm f/2.8, and 105-210mm f/4.5. Everything's in great shape and all the lenses even came with B+W UV filters so that was a nice little bonus. I'm almost done shooting my first "test" roll with it to make sure everything is in fact working correctly, and to get a feel for the lenses and operations.
This was shot on a Polaroid Spectra using expired film.
In addition to the RailAir coach in the background, here adjacent to Reading Station is an (at the time) very shiny new Streetdeck. The Streetdeck/Gemini 3 body style is one I never liked to begin with, but somehow this livery makes them look even more ghastly. Mind you, with some of the brand new stuff the manufacturers are coming up with these days, it's like they saw this and were challenged to make something even uglier.
That aside, something this bus got right and I'm disappointed hasn't become more common is the provision of a huge destination display up front, allowing for via points and other information to scroll through while the main destination remains constantly at the bottom, akin to the classic London Transport blinds. I guess most operators aren't prepared to pay for having two destination blinds on the front instead of just one.
18.2.17
Ebenezer Lutheran Church was organized in 1892. The Swedes who settled in the area completed the sanctuary at 1650 W. Foster Ave. in 1908 (with additions in 1929), and the congregation quickly grew to more than 2,000 members. The sanctuary has beautiful Swedish stenciling along the ceiling, stained glass windows that are the largest of their kind and an intricate altarpiece. A 1987 remodeling carefully preserved the historic elements of the sanctuary. The stairs to the balcony on each side are of different styles; lore has it that the architect, also a prominent local homebuilder, constructed them to show prospective clients two options for staircases.
Photograph at Chicago Architecture Center Open House Chicago 2019.
Comfort Market
2800 Rio Linda Blvd
Sacramento, California
I believe the Comfort Market was originally built as an addition in front of a bungalow facing the boulevard, and the 2-story part of that house was added for more residential space in the back when the market expanded into the footprint of the original bungalow. Just a guess.
Snowdonia, or Eryri is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (Yr Wyddfa), which is 1,085 metres (3,560 ft) tall. These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south.
The national park has an area of 823 square miles (2,130 km2) (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough. This is much larger than the area traditionally considered Snowdonia, and in addition to the five ranges above includes the Rhinogydd, Cadair Idris, and Aran ranges and the Dyfi Hills. It also includes most of the coast between Porthmadog and Aberdyfi. The park was the first of the three national parks of Wales to be designated, in October 1951, and the third in the UK after the Peak District and Lake District, which were established in April and May 1951 respectively. The park received 3.89 million visitors in 2015.
The name Snowdon means 'snow hill' and is derived from the Old English elements snāw and dūn, the latter meaning 'hill'. Snowdonia is simply taken from the name of the mountain.
The origins of Eryri are less clear. Two popular interpretations are that the name is related to eryr, 'eagle', and that it means 'highlands' and is related to the Latin oriri ('to rise'). Although eryri is not any direct form of the word eryr in the meaning 'eagle', it is a plural form of eryr in the meaning 'upland'.
Before the boundaries of the national park were designated, "Snowdonia" was generally used to refer to a smaller upland area of northern Gwynedd centred on the Snowdon massif. The national park covers an area more than twice that size, extending south into the Meirionnydd area.
This difference is apparent in books published before 1951. In George Borrow's 1907 Wild Wales he states that "Snowdon or Eryri is no single hill, but a mountainous region, the loftiest part of which is called Y Wyddfa", making a distinction between the summit of the mountain and the surrounding massif. The Mountains of Snowdonia by H. Carr & G. Lister (1925) defines "Eryri" as "composed of the two cantrefs of Arfon and Arllechwedd, and the two commotes of Nant Conwy and Eifionydd", which corresponds to Caernarfonshire with the exception of southwest Llŷn and the Creuddyn Peninsula. In Snowdonia: The National Park of North Wales (1949), F. J. North states that "When the Committee delineated provisional boundaries, they included areas some distance beyond Snowdonia proper".
Snowdonia National Park, also known as Eryri National Park in English and Parc Cenedlaethol Eryri in Welsh, was established in October 1951. It was the third national park in the United Kingdom, following the Peak District and Lake District in April and May of the same year. It covers 827 square miles (2,140 km2) in the counties of Gwynedd and Conwy, and has 37 miles (60 km) of coastline.
The park is governed by the Snowdonia National Park Authority, which has 18 members: 9 appointed by Gwynedd, 3 by Conwy, and 6 by the Welsh Government to represent the national interest. The authority's main offices are at Penrhyndeudraeth.
The park authority used Snowdonia and Snowdon when referring to the national park and mountain in English until February 2023, when it resolved to primarily use the Welsh names, Eryri and Yr Wyddfa. There will be a transitional period of approximately two years in which the authority will continue to use the English names in parentheses — for example "Yr Wyddfa (Snowdon)" — where the context requires.
Unlike national parks in other countries, national parks in the UK are made up of both public and private lands under a central planning authority. The makeup of land ownership in the national park is as follows:
More than 26,000 people live within the park, of whom 58.6% could speak Welsh in 2011. While most of the land is either open or mountainous land, there is a significant amount of agricultural activity within the park.
The national park does not include the town of Blaenau Ffestiniog, which forms a unique non-designated enclave within the park boundaries. The town was deliberately excluded from the park when it was established because of its slate quarrying industry. The boundaries of the Peak District National Park exclude the town of Buxton and its adjacent limestone quarries for a similar reason.
The geology of Snowdonia is key to the area's character. Glaciation during a succession of ice ages, has carved from a heavily faulted and folded succession of sedimentary and igneous rocks, a distinctive rocky landscape. The last ice age ended only just over 11,500 years ago, leaving a legacy of features attractive to visitors but which have also played a part in the development of geological science and continue to provide a focus for educational visits. Visiting Cwm Idwal in 1841 Charles Darwin realised that the landscape was the product of glaciation. The bedrock dates largely from the Cambrian and Ordovician periods with intrusions of Ordovician and Silurian age associated with the Caledonian Orogeny. There are smaller areas of Silurian age sedimentary rocks in the south and northeast and of Cenozoic era strata on the Cardigan Bay coast though the latter are concealed by more recent deposits. Low grade metamorphism of Cambrian and Ordovician mudstones has resulted in the slates, the extraction of which once formed the mainstay of the area's economy.
The principal ranges of the traditional Snowdonia are the Snowdon massif itself, the Glyderau, the Carneddau, the Moelwynion and the Moel Hebog range. All of Wales' 3000ft mountains are to be found within the first three of these massifs and are most popular with visitors. To their south within the wider national park are the Rhinogydd and the Cadair Idris and Aran Fawddwy ranges. Besides these well-defined areas are a host of mountains which are less readily grouped though various guidebook writers have assigned them into groups such as the 'Arenigs', the 'Tarrens' and the 'Dyfi hills'.
Snowdon's summit at 1085 metres (3560 feet) is the highest in Wales and the highest in Britain south of the Scottish Highlands. At 905 metres (2970 feet) Aran Fawddwy is the highest in Wales outside of northern Snowdonia; Cadair Idris, at 893 metres (2930 feet), is next in line.
Rivers draining the area empty directly into Cardigan Bay are typically short and steep. From north to south they include the Glaslyn and Dwyryd which share a common estuary, the Mawddach and its tributaries the Wnion and the Eden, the smaller Dysynni and on the park's southern margin the Dyfi. A series of rivers drain to the north coast. Largest of these is the Conwy on the park's eastern margin which along with the Ogwen drains into Conwy Bay. Further west the Seiont and Gwyrfai empty into the western end of the Menai Strait. A part of the east of the national park is within the upper Dee (Dyfrydwy) catchment and includes Bala Lake, the largest natural waterbody in Wales. A fuller list of the rivers and tributaries within the area is found at List of rivers of Wales.
There are few natural waterbodies of any size in Wales; Snowdonia is home to most. Besides Bala Lake, a few lakes occupy glacial troughs including Llyn Padarn and Llyn Peris at Llanberis and Tal-y-llyn Lake south of Cadair Idris. Llyn Dinas, Llyn Gwynant, and Llyn Cwellyn to the south and west of Snowdon feature in this category as do Llyn Cowlyd and Llyn Ogwen on the margins of the Carneddau. There are numerous small lakes occupying glacial cirques owing to the former intensity of glacial action in Snowdonia. Known generically as tarns, examples include Llyn Llydaw, Glaslyn and Llyn Du'r Arddu on Snowdon, Llyn Idwal within the Glyderau and Llyn Cau on Cadair Idris.
There are two large wholly man-made bodies of water in the area, Llyn Celyn and Llyn Trawsfynydd whilst numerous of the natural lakes have had their levels artificially raised to different degrees. Marchlyn Mawr reservoir and Ffestiniog Power Station's Llyn Stwlan are two cases where natural tarns have been dammed as part of pumped storage hydro-electric schemes. A fuller list of the lakes within the area is found at List of lakes of Wales. In 2023, the park standardised its Welsh language lake names, to be also used in English.
The national park meets the Irish Sea coast within Cardigan Bay between the Dovey estuary in the south and the Dwyryd estuary. The larger part of that frontage is characterised by dune systems, the largest of which are Morfa Dyffryn and Morfa Harlech. These two locations have two of the largest sand/shingle spits in Wales. The major indentations of the Dovey, the Mawddach and Dwyryd estuaries, have large expanses of intertidal sands and coastal marsh which are especially important for wildlife: see #Natural history. The northern tip of the national park extends to the north coast of Wales at Penmaen-bach Point, west of Conwy, where precipitous cliffs have led to the road and railway negotiating the spot in tunnels.
There are only three towns within the park boundary, though there are several more immediately beyond it. Dolgellau is the most populous followed by Bala on the eastern boundary and then Harlech overlooking Tremadog Bay. More populous than these is the town of Blaenau Ffestiniog, which is within an exclave, that is to say it is surrounded by the national park but excluded from it, whilst the towns of Tywyn and Barmouth on the Cardigan Bay coast are within coastal exclaves. Llanrwst in the east, Machynlleth in the south and Porthmadog and Penrhyndeudraeth in the west are immediately beyond the boundary but still identified with the park; indeed the last of these hosts the headquarters of the Snowdonia National Park Authority. Similarly the local economies of the towns of Conwy, Bethesda, and Llanberis in the north are inseparably linked to the national park as they provide multiple visitor services. The lower terminus of the Snowdon Mountain Railway is at Llanberis. Though adjacent to it, Llanfairfechan and Penmaenmawr are less obviously linked to the park.
There are numerous smaller settlements within the national park: prominent amongst these are the eastern 'gateway' village of Betws-y-Coed, Aberdyfi on the Dovey (Dyfi) estuary and the small village of Beddgelert each of which attract large numbers of visitors. Other sizeable villages are Llanuwchllyn at the southwest end of Bala Lake (Llyn Tegid), Dyffryn Ardudwy, Corris, Trawsfynydd, Llanbedr, Trefriw and Dolwyddelan.
Six primary routes serve Snowdonia, the busiest of which is the A55, a dual carriageway which runs along the north coast and provides strategic road access to the northern part of the national park. The most important north–south route within the park is the A470 running from the A55 south past Betws-y-Coed to Blaenau Ffestiniog to Dolgellau. It exits the park a few miles to the southeast near Mallwyd. From Dolgellau, the A494 runs to Bala whilst the A487 connects with Machynlleth. The A487 loops around the northwest of the park from Bangor via Caernarfon to Porthmadog before turning in land to meet the A470 east of Maentwrog. The A5 was built as a mail coach road by Thomas Telford between London and Holyhead; it enters the park near Pentrefoelas and leaves it near Bethesda. Other A class roads provide more local links; the A493 down the Dovey valley from Machynlleth and up the coast to Tywyn then back up the Mawddach valley to Dolgellau, the A496 from Dolgellau down the north side of the Mawddach to Barmouth then north up the coast via Harlech to Maentwrog. The A4212 connecting Bala with Trawsfynydd is relatively modern having been laid out in the 1960s in connection with the construction of Llyn Celyn. Three further roads thread their often twisting and narrow way through the northern mountains; A4085 links Penrhyndeudraeth with Caernarfon, the A4086 links Capel Curig with Caernarfon via Llanberis and the A498 links Tremadog with the A4086 at Pen-y-Gwryd. Other roads of note include that from Llanuwchllyn up Cwm Cynllwyd to Dinas Mawddwy via the 545 metre (1788') high pass of Bwlch y Groes, the second highest tarmacked public road in Wales and the minor road running northwest and west from Llanuwchllyn towards Bronaber via the 531 metre (1742') high pass of Bwlch Pen-feidiog.
The double track North Wales Coast Line passes along the northern boundary of the park between Conwy and Bangor briefly entering it at Penmaen-bach Point where it is in tunnel. Stations serve the communities of Conwy, Penmaenmawr, Llanfairfechan and Bangor. The single-track Conwy Valley Line runs south from Llandudno Junction, entering the park north of Betws-y-coed which is served by a station then west up the Lledr valley by way of further stations at Pont-y-pant, Dolwyddelan and Roman Bridge. After passing through a tunnel the passenger line now terminates at Blaenau Ffestiniog railway station. Prior to 1961 the route continued as the Bala and Ffestiniog Railway via Trawsfynydd to Bala joining another former route along the Dee valley which ran southwest via Dolgellau to join the still extant coastal Cambrian Line south of Barmouth. The Pwllheli branch of the Cambrian Line splits from the Aberystwyth branch at Dovey Junction and continues via stations at Aberdovey, Tywyn, Tonfanau, Llwyngwril, Fairbourne and Morfa Mawddach to Barmouth where it crosses the Mawddach estuary by the Grade II* listed wooden Barmouth Bridge, a structure which also provides for walkers and cyclists. Further stations serve Llanaber, Tal-y-bont, Dyffryn Ardudwy, Llanbedr, Pensarn and Llandanwg before reaching Harlech. Tygwyn, Talsarnau and Llandecwyn stations are the last before the line exits the park as it crosses the Dwyryd estuary via Pont Briwet and turns westwards bound for Pwllheli via Penrhyndeudraeth, Porthmadog and Criccieth.
Many sections of dismantled railway are now used by walking and cycling routes and are described elsewhere. The Bala Lake Railway is a heritage railway which has been established along a section of the former mainline route between Bala and Llanuwchllyn. Other heritage railways occupy sections of former mineral lines, often narrow gauge and are described in a separate section.
The national park is served by a growing bus network, branded Sherpa'r Wyddfa (formerly Snowdon Sherpa). Together with the TrawsCymru network of buses this provides a car-free option to tourists and locals wishing to travel across the National Park.
The network was relaunched in July 2022 with a new brand, Sherpa'r Wyddfa, to reflect the National Park's new push for the promotion of Welsh place names. As such the publicity and websites for the newly branded service only use these Welsh names, even for English language users.
Snowdonia is one of the wettest parts of the United Kingdom; Crib Goch in Snowdonia is the wettest spot in the United Kingdom, with an average rainfall of 4,473 millimetres (176.1 in) a year over the 30-year period prior to the mid-2000s. (There is a rainfall gauge at 713 metres, 2340' on the slopes below Crib Goch.)
The earliest evidence for human occupation of the area dates from around 4000–3000 BCE with extensive traces of prehistoric field systems evident in the landscape. Within these are traces of irregular enclosures and hut circles. There are burial chambers of Neolithic and Bronze Age such as Bryn Cader Faner and Iron Age hillforts such as Bryn y Castell near Ffestiniog.
The region was finally conquered by the Romans by AD 77–78. Remains of Roman marching camps and practice camps are evident. There was a Roman fort and amphitheatre at Tomen y Mur. Roads are known to have connected with Segontium (Caernarfon) and Deva Victrix (Chester) and include the northern reaches of Sarn Helen.
There are numerous memorial stones of Early Christian affinity dating from the post-Roman period. The post-Roman hillfort of Dinas Emrys also dates to this time. Churches were introduced to the region in the 5th and 6th centuries. Llywelyn the Great and Llywelyn ap Gruffudd had various stone castles constructed to protect their borders and trade routes. Edward I built several castles around the margins including those at Harlech and Conwy for military and administrative reasons. Most are now protected within a World Heritage Site. Some of Snowdonia's many stone walls date back to this period too. In the Middle Ages, the title Prince of Wales and Lord of Snowdonia (Tywysog Cymru ac Arglwydd Eryri) was used by Llywelyn ap Gruffudd; his grandfather Llywelyn Fawr used the title Prince of north Wales and Lord of Snowdonia.
The 18th century saw the start of industrial exploitation of the area's resources, assisted by the appearance in the late part of the century of turnpike trusts making it more accessible. The engineer Thomas Telford left a legacy of road and railway construction in and around Snowdonia. A new harbour at Porthmadog linked to slate quarries at Ffestiniog via a narrow gauge railway. At its peak in the 19th century the slate industry employed around 12,000 men. A further 1000 were employed in stone quarrying at Graiglwyd and Penmaenmawr. Mining for copper, iron and gold was undertaken during the 18th and 19th centuries, leaving a legacy of mine and mill ruins today. Ruins of the gold industry are found at Cefn Coch on the Dolmelynllyn estate.
The Snowdonia Society is a registered charity formed in 1967; it is a voluntary group of people with an interest in the area and its protection.
Amory Lovins led the successful 1970s opposition to stop Rio Tinto digging up the area for a massive mine.
The park's entire coastline is a Special Area of Conservation, which runs from the Llŷn Peninsula down the mid-Wales coast, the latter containing valuable sand dune systems.
The park's natural forests are of the mixed deciduous type, the commonest tree being the Welsh oak. Birch, ash, mountain-ash and hazel are also common. The park also contains some large (planted) coniferous forested areas such as Gwydir Forest near Betws-y-Coed, although some areas, once harvested, are now increasingly being allowed to regrow naturally.
Northern Snowdonia is the only place in Britain where the Snowdon lily (Gagea serotina), an arctic–alpine plant, is found and the only place in the world where the Snowdonia hawkweed Hieracium snowdoniense grows.
One of the major problems facing the park in recent years has been the growth of Rhododendron ponticum. This fast-growing invasive species has a tendency to take over and stifle native species. It can form massive towering growths and has a companion fungus that grows on its roots producing toxins that are poisonous to any local flora and fauna for a seven-year period after the Rhododendron infestations have been eradicated. As a result, there are a number of desolate landscapes.
Mammals in the park include otters, polecats, feral goats, and pine martens. Birds include raven, red-billed chough, peregrine, osprey, merlin and the red kite. The rainbow-coloured Snowdon beetle (Chrysolina cerealis) is only found in northern Snowdonia.
Snowdonia has a particularly high number of protected sites in respect of its diverse ecology; nearly 20% of its total area is protected by UK and European law. Half of that area was set aside by the government under the European Habitats Directive as a Special Area of Conservation. There are a large number of Sites of special scientific interest (or 'SSSIs'), designated both for fauna and flora but also in some cases for geology. Nineteen of these sites are managed as national nature reserves by Natural Resources Wales. The park also contains twelve Special Areas of Conservation (or 'SACs'), three Special Protection Areas (or 'SPAs') and three Ramsar sites. Some are wholly within the park boundaries, others straddle it to various degrees.
There are numerous SSSIs within the park, the most extensive of which are Snowdonia, Migneint-Arenig-Dduallt, Morfa Harlech, Rhinog, Berwyn, Cadair Idris, Llyn Tegid, Aber Mawddach / Mawddach Estuary, Dyfi, Morfa Dyffryn, Moel Hebog, Coedydd Dyffryn Ffestiniog and Coedydd Nanmor.
The following NNRs are either wholly or partly within the park: Allt y Benglog, Y Berwyn (in multiple parts), Cader Idris, Ceunant Llennyrch, Coed Camlyn, Coed Cymerau, Coed Dolgarrog, Coed Ganllwyd, Coed Gorswen, Coed Tremadog, Coedydd Aber, Coedydd Maentwrog (in 2 parts), Coed y Rhygen, Cwm Glas Crafnant, Cwm Idwal, Hafod Garregog, Morfa Harlech, Rhinog and Snowdon.
The twelve SACs are as follows: Snowdonia SAC which covers much of the Carneddau, Glyderau, and the Snowdon massif, Afon Gwyrfai a Llyn Cwellyn, Corsydd Eifionydd / Eifionydd Fens (north of Garndolbenmaen), the Coedydd Derw a Safleoedd Ystlumod Meirion / Meirionydd Oakwoods and Bat Sites - a series of sites between Tremadog, Trawsfynydd, and Ffestiniog and Beddgelert and extending up the Gwynant. It also includes many of the oakwoods of the Mawddach and its tributaries. Afon Eden – Cors Goch Trawsfynydd, Rhinog, Cadair Idris (in 2 parts), Migneint-Arenig-Dduallt, River Dee and Afon Dyfrdwy a Llyn Tegid (Wales), Mwyngloddiau Fforest Gwydir / Gwydyr Forest Mines (north of Betws-y-Coed) and a part of the Berwyn a Mynyddoedd De Clwyd / Berwyn and South Clwyd Mountains SAC. The Pen Llyn a'r Sarnau / Lleyn Peninsula and the Sarnau SAC covers the entire Cardigan Bay coastline of the park and the sea area and extends above the high water mark at Morfa Harlech, Mochras and around the Dovey and Mawddach estuaries.
The three SPAs are Dovey Estuary / Aber Dyfi (of which a part is within the park), Berwyn (of which a part is within the park) and Migneint-Arenig-Dduallt.
The three designated Ramsar sites are the Dyfi Biosphere (Cors Fochno and Dyfi), Cwm Idwal and Llyn Tegid (Bala Lake).
The area's economy was traditionally centred upon farming and from the early 19th century increasingly on mining and quarrying. Tourism has become an increasingly significant part of Snowdonia's economy during the 20th and 21st centuries.
The extensive farming of sheep remains central to Snowdonia's farming economy.
Significant sections of the park were afforested during the 20th century for timber production. Major conifer plantations include Dyfi Forest, Coed y Brenin Forest between Dolgellau and Trawsfynydd, Penllyn Forest south of Bala, Beddgelert Forest and Gwydyr (or Gwydir) Forest near Betws-y-Coed which is managed as a forest park by Natural Resources Wales.
The region was once the most important producer of slate in the world. Some production continues but at a much reduced level from its peak. The park boundaries are drawn such that much of the landscape affected by slate quarrying and mining lies immediately outside of the designated area.
Construction of a nuclear power station beside Llyn Trawsfynydd began in 1959 with the first power produced in 1965. The site was operational until 1991 though it continues as an employer during its decommissioning phase. Pumped storage hydroelectric schemes are in operation at Llanberis and Ffestiniog.
Research indicates that there were 3.67 million visitors to Snowdonia National Park in 2013, with approximately 9.74 million tourist days spent in the park during that year. Total tourist expenditure was £433.6 million in 2013.
Many of the hikers in the area concentrate on Snowdon itself. It is regarded as a fine mountain, but at times gets very crowded; in addition the Snowdon Mountain Railway runs to the summit.
The other high mountains with their boulder-strewn summits as well as Tryfan, one of the few mountains in the UK south of Scotland whose ascent needs hands as well as feet are also very popular. However, there are also some spectacular walks in Snowdonia on the lower mountains, and they tend to be relatively unfrequented. Among hikers' favourites are Y Garn (east of Llanberis) along the ridge to Elidir Fawr; Mynydd Tal-y-Mignedd (west of Snowdon) along the Nantlle Ridge to Mynydd Drws-y-Coed; Moelwyn Mawr (west of Blaenau Ffestiniog); and Pen Llithrig y Wrach north of Capel Curig. Further south are Y Llethr in the Rhinogydd, and Cadair Idris near Dolgellau.
The park has 1,479 miles (2,380 km) of public footpaths, 164 miles (264 km) of public bridleways, and 46 miles (74 km) of other public rights of way. A large part of the park is also covered by right to roam laws.
The Wales Coast Path runs within the park between Machynlleth and Penrhyndeudraeth, save for short sections of coast in the vicinity of Tywyn and Barmouth which are excluded from the park. It touches the park boundary again at Penmaen-bach Point on the north coast. An inland alternative exists between Llanfairfechan and Conwy, wholly within the park. The North Wales Path, which predates the WCP, enters the park north of Bethesda and follows a route broadly parallel to the north coast visiting Aber Falls and the Sychnant Pass before exiting the park on the descent from Conwy Mountain. The Cambrian Way is a long-distance trail between Cardiff and Conwy that stays almost entirely within the national park from Mallwyd northwards. It was officially recognised in 2019, and is now depicted on Ordnance Survey maps.
The use of the English names for the area has been divisive, with an increase in protests against their use since 2020; these led to the national park authority deciding to use Welsh names as far as legally possible in November 2022. An early example of pressure to deprecate Snowdon and Snowdonia was a 2003 campaign by Cymuned, inspired by campaigns to refer to Ayers Rock as Uluru and Mount Everest as Qomolangma.
In 2020 an e-petition calling for the removal of the English names was put forward to the Senedd, but rejected as responsibility lies with the national park authority. In 2021 an e-petition on the same topic attracted more than 5,300 signatures and was presented to the national park authority.
On 28 April 2021 Gwynedd councillor John Pughe Roberts put forward a motion to use the Welsh names exclusively, calling this a "question of respect for the Welsh language". The motion was not considered and delayed, as the national park authority already appointed a "Welsh Place Names Task and Finish Group" to investigate the issue. The park authority however cannot compel other bodies and/or individuals to stop using the English names, with the proposals facing some criticism.
In May 2021, following the dismissal of the motion, YouGov conducted a poll on Snowdon's name. 60% of Welsh adults supported the English name Snowdon, compared to 30% wanting the Welsh name Yr Wyddfa. Separating by language, 59% of Welsh speakers preferred the Welsh name, but 37% of these still wanted Snowdon to be used as well. 69% of non-Welsh speakers firmly supported Snowdon as the Mountain's name. The proposals to rename Snowdon are usually accompanied with proposals to rename Snowdonia.
On 16 November 2022, Members of the Snowdonia National Park Authority committee voted to use the Welsh names Yr Wyddfa and Eryri to refer to the mountain and the national park, rather than the English names, in materials produced by the authority. The national park authority described the decision as "decisive action" and the authority's head of culture heritage stated that Welsh place names were part of the area's "special qualities" and that other public bodies, English-language press and filming companies have used the Welsh-language names. Before the decision the park had already prioritised the Welsh names by using them first and giving the English names in parentheses. The name "Snowdonia" cannot be abandoned entirely, as it is set in law and so must be used in statutory documents. The authority announced a review of the authority's branding in 2023 to adapt to the new approach to Welsh place names.
Gwynedd is a county in the north-west of Wales. It borders Anglesey across the Menai Strait to the north, Conwy, Denbighshire, and Powys to the east, Ceredigion over the Dyfi estuary to the south, and the Irish Sea to the west. The city of Bangor is the largest settlement, and the administrative centre is Caernarfon. The preserved county of Gwynedd, which is used for ceremonial purposes, includes the Isle of Anglesey.
Gwynedd is the second largest county in Wales but sparsely populated, with an area of 979 square miles (2,540 km2) and a population of 117,400. After Bangor (18,322), the largest settlements are Caernarfon (9,852), Bethesda (4,735), and Pwllheli (4,076). The county has the highest percentage of Welsh speakers in Wales, at 64.4%, and is considered a heartland of the language.
The geography of Gwynedd is mountainous, with a long coastline to the west. Much of the county is covered by Snowdonia National Park (Eryri), which contains Wales's highest mountain, Snowdon (Yr Wyddfa; 3,560 feet, 1,090 m). To the west, the Llŷn Peninsula is flatter and renowned for its scenic coastline, part of which is protected by the Llŷn AONB. Gwynedd also contains several of Wales's largest lakes and reservoirs, including the largest, Bala Lake (Llyn Tegid).
The area which is now the county has played a prominent part in the history of Wales. It formed part of the core of the Kingdom of Gwynedd and the native Principality of Wales, which under the House of Aberffraw remained independent from the Kingdom of England until Edward I's conquest between 1277 and 1283. Edward built the castles at Caernarfon and Harlech, which form part of the Castles and Town Walls of King Edward in Gwynedd World Heritage Site. During the Industrial Revolution the slate industry rapidly developed; in the late nineteenth century the neighbouring Penrhyn and Dinorwic quarries were the largest in the world, and the Slate Landscape of Northwest Wales is now a World Heritage Site. Gwynedd covers the majority of the historic counties of Caernarfonshire and Merionethshire.
In the past, historians such as J. E. Lloyd assumed that the Celtic source of the word Gwynedd meant 'collection of tribes' – the same root as the Irish fine, meaning 'tribe'. Further, a connection is recognised between the name and the Irish Féni, an early ethnonym for the Irish themselves, related to fían, 'company of hunting and fighting men, company of warriors under a leader'. Perhaps *u̯en-, u̯enə ('strive, hope, wish') is the Indo-European stem. The Irish settled in NW Wales, and in Dyfed, at the end of the Roman era. Venedotia was the Latin form, and in Penmachno there is a memorial stone from c. AD 500 which reads: Cantiori Hic Iacit Venedotis ('Here lies Cantiorix, citizen of Gwynedd'). The name was retained by the Brythons when the kingdom of Gwynedd was formed in the 5th century, and it remained until the invasion of Edward I. This historical name was revived when the new county was formed in 1974.
Gwynedd was an independent kingdom from the end of the Roman period until the 13th century, when it was conquered by England. The modern Gwynedd was one of eight Welsh counties created on 1 April 1974 under the Local Government Act 1972. It covered the entirety of the historic counties of Anglesey and Caernarfonshire, and all of Merionethshire apart from Edeirnion Rural District (which went to Clwyd); and also a few parishes of Denbighshire: Llanrwst, Llansanffraid Glan Conwy, Eglwysbach, Llanddoged, Llanrwst and Tir Ifan.
The county was divided into five districts: Aberconwy, Arfon, Dwyfor, Meirionnydd and Anglesey.
The Local Government (Wales) Act 1994 abolished the 1974 county (and the five districts) on 1 April 1996, and its area was divided: the Isle of Anglesey became an independent unitary authority, and Aberconwy (which included the former Denbighshire parishes) passed to the new Conwy County Borough. The remainder of the county was constituted as a principal area, with the name Caernarfonshire and Merionethshire, as it covers most of the areas of those two historic counties. As one of its first actions, the Council renamed itself Gwynedd on 2 April 1996. The present Gwynedd local government area is governed by Gwynedd Council. As a unitary authority, the modern entity no longer has any districts, but Arfon, Dwyfor and Meirionnydd remain as area committees.
The pre-1996 boundaries were retained as a preserved county for a few purposes such as the Lieutenancy. In 2003, the boundary with Clwyd was adjusted to match the modern local government boundary, so that the preserved county now covers the two local government areas of Gwynedd and Anglesey. Conwy county borough is now entirely within Clwyd.
A Gwynedd Constabulary was formed in 1950 by the merger of the Anglesey, Caernarfonshire and Merionethshire forces. A further amalgamation took place in the 1960s when Gwynedd Constabulary was merged with the Flintshire and Denbighshire county forces, retaining the name Gwynedd. In one proposal for local government reform in Wales, Gwynedd had been proposed as a name for a local authority covering all of north Wales, but the scheme as enacted divided this area between Gwynedd and Clwyd. To prevent confusion, the Gwynedd Constabulary was therefore renamed the North Wales Police.
The Snowdonia National Park was formed in 1951. After the 1974 local authority reorganisation, the park fell entirely within the boundaries of Gwynedd, and was run as a department of Gwynedd County Council. After the 1996 local government reorganisation, part of the park fell under Conwy County Borough, and the park's administration separated from the Gwynedd council. Gwynedd Council still appoints nine of the eighteen members of the Snowdonia National Park Authority; Conwy County Borough Council appoints three; and the Welsh Government appoints the remaining six.
There has been considerable inwards migration to Gwynedd, particularly from England. According to the 2021 census, 66.6% of residents had been born in Wales whilst 27.1% were born in England.
The county has a mixed economy. An important part of the economy is based on tourism: many visitors are attracted by the many beaches and the mountains. A significant part of the county lies within the Snowdonia National Park, which extends from the north coast down to the district of Meirionnydd in the south. But tourism provides seasonal employment and thus there is a shortage of jobs in the winter.
Agriculture is less important than in the past, especially in terms of the number of people who earn their living on the land, but it remains an important element of the economy.
The most important of the traditional industries is the slate industry, but these days only a small percentage of workers earn their living in the slate quarries.
Industries which have developed more recently include TV and sound studios: the record company Sain has its HQ in the county.
The education sector is also very important for the local economy, including Bangor University and Further Education colleges, Coleg Meirion-Dwyfor and Coleg Menai, both now part of Grŵp Llandrillo Menai.
The proportion of respondents in the 2011 census who said they could speak Welsh.
Gwynedd has the highest proportion of people in Wales who can speak Welsh. According to the 2021 census, 64.4% of the population aged three and over stated that they could speak Welsh,[7] while 64.4% noted that they could speak Welsh in the 2011 census.
It is estimated that 83% of the county's Welsh-speakers are fluent, the highest percentage of all counties in Wales.[9] The age group with the highest proportion of Welsh speakers in Gwynedd were those between ages 5–15, of whom 92.3% stated that they could speak Welsh in 2011.
The proportion of Welsh speakers in Gwynedd declined between 1991 and 2001,[10] from 72.1% to 68.7%, even though the proportion of Welsh speakers in Wales as a whole increased during that decade to 20.5%.
The Annual Population Survey estimated that as of March 2023, 77.0% of those in Gwynedd aged three years and above could speak Welsh.
Notable people
Leslie Bonnet (1902–1985), RAF officer, writer; originated the Welsh Harlequin duck in Criccieth
Sir Dave Brailsford (born 1964), cycling coach; grew up in Deiniolen, near Caernarfon
Duffy (born 1984), singer, songwriter and actress; born in Bangor, Gwynedd
Edward II of England (1284–1327), born in Caernarfon Castle
Elin Fflur (born 1984), singer-songwriter, TV and radio presenter; went to Bangor University
Bryn Fôn (born 1954), actor and singer-songwriter; born in Llanllyfni, Caernarfonshire.
Wayne Hennessey (born 1987), football goalkeeper with 108 caps for Wales; born in Bangor, Gwynedd
John Jones (c. 1530 – 1598), a Franciscan friar, Roman Catholic priest and martyr; born at Clynnog
Sir Love Jones-Parry, 1st Baronet (1832–1891), landowner and politician, co-founder of the Y Wladfa settlement in Patagonia
T. E. Lawrence (1888–1935), archaeologist, army officer and inspiration for Lawrence of Arabia, born in Tremadog
David Lloyd George (1863–1945), statesman and Prime Minister; lived in Llanystumdwy from infancy
Sasha (born 1969), disc jockey, born in Bangor, Gwynedd
Sir Bryn Terfel (born 1965), bass-baritone opera and concert singer from Pant Glas
Sir Clough Williams-Ellis (1883–1978), architect of Portmeirion
Owain Fôn Williams, (born 1987), footballer with 443 club caps; born and raised in Penygroes, Gwynedd.
Hedd Wyn (1887–1917), poet from the village of Trawsfynydd; killed in WWI
pictionid66555378 - cataloghoover00262 - title--hoover collection image--photo by f. cannon 8-4-96 - filenamehoover00262.tif---The images in this collection belong to the
Bob Hoover Legacy Foundation. In addition to digitizing these images, the San Diego Air and Space Museum cares for and manages them. Note: This material may be protected by Copyright Law (Title 17 U.S.C.)-
In addition to my Amsterdam project I also wanted to build a windmill. It is loosely based on the windmills at Kinderdijk in the Netherlands and the windmill at Rövershagen in Northern Germany.
The mill has an octagonal shaped base and a roof (also called cap) that rotates. It is built in a modular way. The first two levels are fully furnished. On the ground floor there is a pottery workshop with a kiln, a pottery wheel, shelves for clay, different types of glaze and finished items. On the second floor there is the apartement of the potter.
The shape of the mill was quite challenging and I wanted to quit the build more than once. But I like how it turned out.
~ Wat Buddhist Temple ~
Yesterday we went to the Annual Thai Buddhist Annual Spring Festival. The temple is modest but very nicely done and offers some interesting photo opportunities. The festival includes Thai food for sale to eat on site as well as to take home. In addition they had a band and played Thai music and everyone danced and had a good time. I was amazed at the number of people that attended and how much fun they all have together. Always a first to be had and this was a good one for me.
1309 25th Street
Sacramento, California
This commercial addition in front of a Dutch colonial house appears to be office space nowadays. If it's not currently occupied, it surely looks turnkey ready.
An unusual addition to the Portway in Bristol. Somebody in January 2014 has erected letters on one side of the Avon Gorge to spell Bristoland. This is clearly a nod towards the famous Hollywood sign on Mount Lee in Los Angeles. That sign, created in 1923, originally spelled "Hollywoodland" but the "land" part was removed in 1949. This sign seems to have already lost its "O" but that is doubtless unintentional!
Schweiz / Nidwalden - Vierwaldstättersee
seen from Stanserhorn
gesehen vom Stanserhorn
Lake Lucerne (German: Vierwaldstättersee, literally "Lake of the four forested settlements" (in English usually translated as forest cantons), French: lac des Quatre-Cantons, Italian: lago dei Quattro Cantoni) is a lake in central Switzerland and the fourth largest in the country.
Geography
The lake has a complicated shape, with several sharp bends and four arms. It starts in the south–north bound Reuss Valley between steep cliffs above the Urnersee from Flüelen towards Brunnen to the north before it makes a sharp bend to the west where it continues into the Gersauer Becken. Here is also the deepest point of the lake with 214 m (702 ft). Even further west of it is the Buochser Bucht, but the lake sharply turns north again through the narrow opening between the Unter Nas (lower nose) of the Bürgenstock to the west and the Ober Nas (upper nose) of the Rigi to the east to reach the Vitznauer Bucht. In front of Vitznau below the Rigi the lake turns sharply west again to reach the center of a four-arm cross, called the Chrütztrichter (Cross Funnel). Here converge the Vitznauer Bucht with the Küssnachtersee from the north, the Luzernersee from the west, and the Horwer Bucht and the Stanser Trichter to the south, which is to be found right below the northeast side of the Pilatus and the west side of the Bürgenstock. At the very narrow pass between the east dropper of the Pilatus (called Lopper) and Stansstad the lake reaches its southwestern arm at Alpnachstad on the steep southern foothills of the Pilatus, the Alpnachersee. The lake drains its water into the Reuss in Lucerne from its arm called Luzernersee (which literally translates as Lake of Lucerne).
The entire lake has a total area of 114 km² (44 sq mi) at an elevation of 434 m (1,424 ft) a.s.l., and a maximum depth of 214 m (702 ft). Its volume is 11.8 km³. Much of the shoreline rises steeply into mountains up to 1,500 m above the lake, resulting in many picturesque views including those of the mountains Rigi and Pilatus.
The Reuss enters the lake at Flüelen, in the part called Urnersee (Lake of Uri, in the canton of Uri) and exits at Lucerne. The lake also receives the Muota at Brunnen, the Engelberger Aa at Buochs, and the Sarner Aa at Alpnachstad.
It is possible to circumnavigate the lake by train and road, though the railway route circumvents the lake even on the north side of the Rigi via Arth-Goldau. Since 1980, the A2 motorway leads through the Seelisberg Tunnel in order to reach the route to the Gotthard Pass in just half an hour in Altdorf, Uri right south of the beginning of the lake in Flüelen.
Steamers and other passenger boats ply between the different villages and towns on the lake. It is a popular tourist destination, both for native Swiss and foreigners, and there are many hotels and resorts along the shores. In addition, the meadow of the Rütli, traditional site of the founding of the Swiss Confederation, is on the Urnersee shore. A 35 km commemorative walkway, the Swiss Path, was built around the Lake of Uri to celebrate the country's 700th anniversary in 1991.
Archaeologists surveying the lake-bed (during the construction of a pipeline) from 2019 to 2021 found the remains of a Bronze Age village with artifacts dating to around 1000 BC. Later, the new findings indicated that the area was settled 2,000 years earlier than historians previously thought.
Lake Lucerne borders on the three original Swiss cantons of Uri, Schwyz, and Unterwalden (which today is divided into the cantons of Obwalden and Nidwalden), as well as the canton of Lucerne, thus the name Vierwaldstättersee (lit.: Lake of the Four Forested Settlements). Many of the oldest communities of Switzerland are along the shore, including Küssnacht, Weggis, Vitznau, Gersau, Brunnen, Altdorf, Buochs, and Treib.
Lake Lucerne is singularly irregular and appears to lie in four different valleys, all related to the conformation of the adjoining mountains. The central portion of the lake lies in two parallel valleys whose direction is from west to east, the one lying north, the other south of the ridge of the Bürgenstock. These are connected through a narrow strait, scarcely one kilometre wide, between the two rocky promontories called respectively Unter Nas and Ober Nas (Lower and Upper Nose). It is not unlikely that the southern of these two divisions of the lake—called Buochser Bucht—formerly extended to the west over the isthmus whereon stands the town of Stans, thus forming an island of the Bürgenstock. The west end of the main branch of the lake, whence a comparatively shallow bay extends to the town of Lucerne, is intersected obliquely by a deep trench whose south-west end is occupied by the branch called Alpnachersee, while the north-east branch forms the long arm of Küssnacht, Küssnachtersee. These both lie in the direct line of a valley that stretches with scarcely a break in between the Uri Alps and the Emmental Alps. At the eastern end of the Gersauer Becken, where the containing walls of the lake-valley are directed from east to west, it is joined at an acute angle by the arm of Uri, or the Urnersee, lying in the northern prolongation of the deep cleft that gives a passage to the Reuss, between the Uri Alps and the Glarus Alps.
The Urnersee occupies the northernmost and deep portion of the great cleft of the Reuss Valley, which has cut through the Alpine ranges from the St Gotthard Pass to the neighbourhood of Schwyz. From its eastern shore the mountains rise in almost bare walls of rock to a height of from 3,000 to 4,000 ft (910 to 1,220 m) above the water. The two highest summits are the Fronalpstock and the Rophaien (2078 m). Between them the steep glen or ravine of the Riemenstaldener Tal descends to Sisikon, the only village with Flüelen right on the shore on that side of the Urnersee. On the opposite or western shore, the mountains attain still greater dimensions. The Niederbauen Chulm is succeeded by the Oberbauenstock, and farther south, above the ridge of the Scharti, appear the snowy peaks of the Gitschen and the Uri Rotstock (2,928 m). In the centre opens the Reuss Valley, backed by the rugged summits of the Urner and Glarner Alps.
The breadth of these various sections of the lake is very variable, but is usually between one and two miles (3 km). The lake's surface, whose mean height above the sea is 434 metres, is the lowest point of the cantons of Uri, Obwalden and Nidwalden. Originally the lake was susceptible to variations in level and flooding along its shoreline. Between 1859 and 1860, the introduction of a needle dam in the Reuss in the city of Lucerne, just upstream from the Spreuerbrücke, allowed the lake level to be stabilised.
The culminating point of the lake's drainage basin, as well as Central Switzerland, is the Dammastock at 3,630 metres above sea level.
Name
The name of Vierwaldstättersee is first used in the 16th century. Before the 16th century, the entire lake was known as Luzerner See "Lake Lucerne", as remains the English (and partly Italian, as Lago di Lucerna) usage. The (three) "Waldstätte(n)" (lit.: "forested sites/settlements", in English usually translated as forest cantons[6]) since the 14th century were the confederate allies of Uri, Schwyz and Unterwalden. The notion of "Four Waldstätten" (Vier Waldstätten), with the addition of the canton of Lucerne, is first recorded in the 1450s, in an addition to the "Silver Book" of Egloff Etterlin of Lucerne.
The nine different parts of the lake have individual designations:
Urnersee ("Lake of Uri"): The first part of the lake, at the mouth of the Reuss between Flüelen and Brunnen.
Gersauer Becken ("Basin of Gersau") next to Gersau below the Rigi massif is the deepest part of the lake.
Buochser Bucht ("Bay of Buochs"): The bay of Bouchs, where the Engelberger Aa enters the lake.
Vitznauer Bucht ("Bay of Vitznau"): The part between the Bürgenstock and Rigi.
Alpnachersee ("Lake of Alpnach"): the almost separate, southern arm below the southern mountainside of Pilatus near Alpnach.
Stanser Trichter ("Funnel of Stans"): The part north of the Pilatus, west of Bürgenstock, and in front of Hergiswil and Stansstad.
Küssnachtersee ("Lake of Küssnacht"): The most northern arm, west of the Rigi with Küssnacht SZ at its northern end.
Chrütztrichter ("Cross Funnel"): The meeting point of Stanser Trichter, Luzernersee, Küssnachtersee, and Vitznauer Bucht.
Luzernersee ("Lake of Lucerne"): in German usage now limited to the bay at Lucerne as far as Meggenhorn, with its effluence of the Reuss.
Navigation
The lake is navigable, and has formed an important part of Switzerland's transport system for many centuries, and at least since the opening of the first track across the Gotthard Pass in 1230. This trade grew with the opening of a new mail coach road across the pass in 1830. This road had its northern terminus at Flüelen at the extreme eastern end of the lake, and the lake provided the only practical onward link to Lucerne, and hence the cities of northern Switzerland and beyond.
Whilst the development of Switzerland's road and rail networks has relieved the lake of much of its through traffic, it continues to be used by a considerable number of vessels, both private and public. Much of this usage is tourist or leisure oriented, but the lake continues to provide practical public and cargo transport links between the smaller lakeside communities.
Passenger boats of the Schifffahrtsgesellschaft des Vierwaldstättersees (SGV) provide services on the lake, including many run by historic paddle steamers. The SGV serves 32 places along the shore of the lake, with interchange to both main line and mountain railways at various points. Under separate management, the Autofähre Beckenried-Gersau provides a car ferry service between Beckenried, on the south bank of the lake, and Gersau on the north.
Cargo barges, to a local design known as Nauen, are still used on the lake. Some have been converted for use as party boats. Other barges are used by the gravel dredging industry that operates on the lake, using large dredgers to obtain sand and gravel for use in the construction industry.
Cultural references
Beethoven's Moonlight Sonata derives its name from an 1832 description of the first movement by poet and music critic Ludwig Rellstab, who compared it to moonlight shining upon Lake Lucerne.
Gioacchino Rossini uses this in his William Tell Overture Section A: Sunrise over the Alps.
Rowing
Lake Lucerne has twice been used as a venue for the European Rowing Championships: in 1908 and then in 1926. The nearby Rotsee has since 1933 been used for rowing regattas instead.
Tourism
On the way south, the English discovered the mountains of central Switzerland. Several spa and bathing resorts such as Weggis or Gersau were created. In 1871, the very first rack railway in Europe, the Vitznau-Rigi Railway, was opened. In 1889 the steepest cog railway in the world was built from Alpnachstad to Mount Pilatus. Mark Twain described an ascent to the Rigi, which led to the blossoming of Swiss tourism in the United States in the 19th century. One of the largest steamship fleets in Europe operates with five steamships on Lake Lucerne.
In the area surrounding the lake and on terraces at medium height (for example Morschach and Seelisberg) there are numerous places for tourists. The Rigi, Pilatus, the Bürgenstock, the Stanserhorn, the Buochserhorn, and the two legends, the Urirotstock and the Fronalpstock are attractive panoramic mountains near Lake Lucerne. Most of them can be reached by mountain railways, some of which have their valley station near boat stations on the lake.
There are numerous locations on the lake that are important in Swiss cultural and tourism history: Rütli, Tellsplatte, Tell Chapel, Carving Tower of Stansstad, Neu-Habsburg, Schillerstein, Treib, Astrid Chapel (Küssnacht) and Meggenhorn Castle.
Watersports
Different sports are possible in some separate areas due to the water and wind conditions. The lake is accessible from boat and yacht harbors, to lake resorts and pools (e.g. the Lido pool in Lucerne, built in 1929 by Arnold Berger). Therefore, the lake can be easily accessible from both shores. The See-Club Luzern was founded in 1881, which is now Switzerland's largest rowing club, as well as the Reuss Luzern rowing club (Ruderclub Reuss Luzern) in 1904. The Lucerne Yacht Club (Yachtclub Luzern) has existed since 1941 and has been running since 1966 a boathouse and buoy field on Churchill-Quai in Lucerne.
The Brunnen water sports club (Wassersportclub Brunnen), founded in 1958, held on Lake Lucerne in the first years of its existence international motorboat races and water ski championships. In 1965 the association chose a new name for the club: Lake Lucerne Water Sports Club (Wassersport-Club Vierwaldstättersee). The Central Switzerland Motorboat Club (Motorbootclub Zentralschweiz) was established in 1980 and the Hergiswil Water Sports Club (Wassersportclub Hergiswil) in 1986. SchweizMobil has created a canoe tour across Lake Lucerne between Brunnen and Gersau. Due to the wind in the Reuss Valley, the southern part of Lake Uri between the campground at Gruonbachstrand in Flüelen and Isleten is a center of windsurfing.
Diving
There are about ten places where you can dive without a boat in Lake Lucerne. The water is rather chilly all year round and therefore mostly very clear. In Lake Uri, at Sisikon, one can dive to a fragmented steep vertical wall, at the northern portal of the Schieferneggtunnel. The Lediwrack Bruno lies in front of Brunnen at a depth of 15 meters. Other well-known diving spots are in front of Vitznau, Weggis, Gersau and Hergiswil.
(Wikipedia)
The Stanserhorn is a mountain in Switzerland, located in the canton of Nidwalden near to the border with Obwalden, with the peak at 1,898 metres (6,227 ft) above sea level.
It is a popular tourist destination, which can be reached from the adjacent town of Stans by a funicular railway and cable car, or via walking routes from Stans or Dallenwil.
History
The first public transport route to the peak was started in 1891 and completed in 1893, a three section funicular railway. The builders were the business partners Franz Josef Bucher-Durrer and Josef Durrer-Gasser.
The first section started from Stans town, through the low pastures above the town and over three level crossings, to an intermediate station at Kälti (also sometimes spelt Chälti). The second section continued through forest to another intermediate station at Bluematt (also sometimes spelt Blumatt), then the third section crossed the high pastures and the exposed slope leading up to the summit station and hotel. This third section included a 160 metres (520 ft) long tunnel and a number of avalanche protection walls; the final section of it was carried on a stone embankment. Each section was electrically powered (making it one of the world's first electrically powered mountain railways), with the complete trip to the summit taking 45 minutes.
The railway ran a tourist service until 1970, when on the night of the 2/3 October the funicular cable was struck by lightning. This started a fire which destroyed the summit hotel and the driving engine for the third section in its basement. As a result of this, and also the imminent expiry of the concession, the second funicular section stopped operating in 1974. Part of the driving engine of this section can be seen today outside the summit buildings, while parts of two cars can still be seen at the former Bluematt station.
A new cable car was built to replace the two upper funicular sections, which started operation in May 1975. The first funicular section continued in operation, as it does to this day.
In 2001 a revolving restaurant was built at the summit station, and in 2003 an outside observation deck was added.
In 2010 construction work started on a new cable car to replace the 1975 installation. This was to be a new design, the world's first "CabriO" double deck open top cable car, built by Garaventa. Carrying 60 passengers per cabin with room for 30 on the open deck, passengers are able to observe the mountain scenery as well as the cable and engineering installations during the six-minute journey. While this new cable car was being built, the first funicular section and its original wooden cars were renovated. The final run of the former cable car was on 23 October 2011;[8] the renovated funicular and new "CabriO" were opened on 29 June 2012.
Visiting
he funicular railway and cable car normally run daily from mid-April to mid-November.
The journey to the top starts in Stans town at the original 1893 bottom station (450 metres (1,480 ft) elevation), close to Stans railway station on the Luzern-Engelberg line. The journey, on the original wooden funicular wagons, takes 9 minutes to the Kälti intermediate station (714 metres (2,343 ft) altitude). From here the "CabriO" cable car takes 61⁄4 minutes to the summit station (1,850 metres (6,070 ft) altitude). The cable car closely follows the route of the original second and third stage funiculars, and the remains of the track and the Bluematt station can still be seen.
The summit buildings include a self-service restaurant, three meeting/dining rooms, a souvenir shop, and a sun terrace and observation deck.
From the summit buildings, a round trip walk is available around the summit (30 minutes), or to the peak at 1,898 metres (6,227 ft) altitude. From the peak, on a clear day, as well as the mountains around there are views as far as Alsace and the Black Forest in Germany. Ten lakes in total are visible: the Zugersee, Wichelsee, Vierwaldstättersee, Sempachersee, Sarnersee, Hallwilersee, Gerzensee, Bannalpsee, Baldeggersee and Alpnachersee.
A variety of hiking trail routes are available down to Bluematt-Kälti-Stans, Ahornhütte-Büren, Wiesenberg-Dallenwil, or Wirzweli-Wolfenschiessen. The routes to/from the summit are closed in winter or in bad weather.
(Wikipedia)
Der Vierwaldstättersee (französisch Lac des Quatre-Cantons; italienisch Lago dei Quattro Cantoni, Lago di Lucerna; rätoromanisch Lai dals Quatter Chantuns) ist ein von Bergen der Voralpen umgebener Alpenrandsee in der Zentralschweiz. Er liegt auf dem Gebiet der Kantone Uri, Schwyz, Unterwalden (d. h. Nid- und Obwalden) und Luzern. Die grössten Orte am Ufer sind Luzern, Küssnacht, Horw und Brunnen. Der See ist 114 km² gross, liegt auf einer Höhe von 433 m ü. M. und ist 214 m tief. Da es sich um einen charakteristischen Zungenbeckensee mit mehreren Zweigbecken handelt, ist die Uferlänge im Bezug zur Seefläche mit etwa 150 km relativ gross.
Name
Seinen Namen hat der Vierwaldstättersee von den vier an ihn angrenzenden Waldstätten (heutige Kantone). Bis ins 16. Jahrhundert wurde die Bezeichnung Luzerner See verwendet.
Entstehung
Der Vierwaldstättersee entstand in den Eiszeiten, u. a. der letzten Eiszeit, durch Erosion des Reussgletschers. Der See bildete sich als Gletscherrandsee am Ende der Eiszeit vor rund 12'000 Jahren. Im Gletschergarten Luzern zeigt eine Dokumentation die Geschichte der Alpen, der Eiszeiten und der Gletscher in den Zentralalpen.
Geographie
Zufluss
Die Hauptzuflüsse des Vierwaldstättersees sind die Reuss mit der Einmündung bei Flüelen und Seedorf, die Engelberger Aa bei Buochs, die Sarner Aa bei Alpnachstad und die Muota bei Brunnen. Die Reuss fliesst mit einem starken Gefälle aus dem Gotthardmassiv und führt grosse Mengen Geschiebe mit sich, so dass sich das Reussdelta im Laufe der Zeit um 10 km nach Norden in den Urnersee hinein erweitert hat.
Im Urnersee im Bereich des Reussdeltas zwischen Flüelen und Seedorf wurde von 2001 bis 2005 mit dem Ausbruchmaterial des Umfahrungstunnels Flüelen und des Gotthard-Basistunnels der Seegrund teilweise wieder aufgeschüttet. Es entstanden Flachwasserzonen, die durch den Kiesabbau verschwunden waren, und einige neue Inseln: die Neptuninseln und die Inselgruppe Lorelei. Einige der Inseln sind Vogelschutzgebiet. Im Naturschutzgebiet erlaubt der Reussdeltaturm die Beobachtung der Fauna.
Kleinere in den Vierwaldstättersee einmündende Gewässer sind der Gruonbach, der Isitaler Bach, der Riemenstaldnerbach, der Cholbach von Emmetten, der Lielibach bei Beckenried, der Teuffibach, der Melbach, die Kleine Schliere bei Alpnachstad, zehn Bäche am Ostabhang des Pilatus (darunter Mülibach, Steinibach bei Horw, Widenbach, Fridbach, Feldbach und Steinibach bei Hergiswil) und der Würzenbach in Luzern.
Gliederung
Der Vierwaldstättersee besteht aus mehreren Seebecken und Buchten:
Der Urnersee erstreckt sich von der Einmündung der Reuss bei Seedorf 11 km in nördlicher Richtung bis nach Brunnen
Der Gersauer See (auch Gersauer Becken oder Gersauerbecken) führt 14 km von Ost nach West von Brunnen nach Ennetbürgen, wo die Engelberger Aa in den See mündet. In der Mitte zwischen Beckenried und Gersau erreicht der See mit 214 m Tiefe seine tiefste Stelle.
Der Chrüztrichter (Kreuztrichter) bildet im Westen des Weggiser Beckens das eigentliche Zentrum des nördlichen Seeteils. Von ihm zweigen vier Hauptarme (Trichter) ab:
Das Weggiserbecken (östlicher Arm des Kreuztrichters) liegt südlich von Weggis und verläuft von Ost nach West. Es führt zwischen Hertenstein im Norden und dem Bürgenstock im Süden hin zur Seemitte. Es wird auch Vitznauerbecken genannt.
Der Stanser Trichter (südwestlicher Arm des Kreuztrichters). Im Südwesten davon liegen
die Horwerbucht und
der Alpnachersee, der zwischen Acheregg und Stansstad durch eine nur 100 Meter breite Engstelle, über die eine Brücke führt, vom restlichen See abgetrennt wird und am Südfuss des Pilatus liegt.
der Küssnachtersee (nordöstlicher Arm aus dem Kreuztrichter) zweigt zwischen Hertenstein und Meggenhorn in nordöstlicher Richtung nach Küssnacht, am Nordrand des Rigimassivs gelegen, ab.
der relativ kurze Luzernersee (auch Luzerner Bucht) ist zugleich nordwestlicher Arm des Kreuztrichters und Schlussteil des Sees. Er verläuft nach Nordwesten nach Luzern.
Abfluss
In Luzern verlässt die Reuss den See, kontrolliert mit einem Regulierwehr, und fliesst durch das Mittelland zur Aare.
Strömungen
Durch das verhältnismässig warme Wasser der Reuss und den Föhn, der das Wasser ständig umschichtet, ist der Urnersee am Grund wärmer und leichter als das Wasser im Gersauer Becken. Durch diesen Temperaturunterschied strömen jeden Frühling gewaltige Wassermassen vom Gersauer Becken in die Tiefen des Urnersees. Ähnliche Tiefenwasserströmungen bestehen auch vom Alpnachersee in das Gersauer Becken.
Wasserqualität und Temperaturen
Das Wasser bleibt durchschnittlich dreieinhalb Jahre im Seebecken und hat Trinkwasserqualität. Die Eidgenössische Forschungsanstalt für Limnologie der Eawag überwacht die Wasserqualität. Im Sommer erreicht der See eine Temperatur von 22 °C. 1929 und 1963 froren der Alpnachersee und die Luzerner Bucht zu. Aus dem 17. und 19. Jahrhundert sind Vereisungen des ganzen Vierwaldstättersees dokumentiert. 1684 und 1685 konnte das Gersauer Becken auf dem Eis überquert werden.
Klima und Vegetation
Das Klima rund um den föhnbegünstigten und von Bergen geschützten Vierwaldstättersee ist im Vergleich zu anderen Regionen der deutschsprachigen Schweiz relativ mild; die Vegetation gleicht zum Teil derjenigen des Kantons Tessin. Die mittlere Tageshöchst-/-tiefsttemperatur beträgt in Luzern 2,6 °C (Januar) und 23,5 °C (Juli). In Altdorf südlich des Sees liegen die Werte bei 3,9 °C (Januar) und 23,0 °C im Juli (Klimamittel der Jahre 1961–1990). An den Seeufern wachsen Hanfpalmen, Feigen, Yuccas, Zypressen, Opuntien, Edelkastanien und andere südländische Pflanzenarten.
Die Edelkastanien wurden bis ins 19. Jahrhundert wirtschaftlich als Nahrungsmittel genutzt. Mit der Verbreitung der Kartoffel nahm die Bedeutung der Kastanie jedoch ab. Noch heute findet in Greppen regelmässig ein Kastanienmarkt, die sogenannte Chestene-Chilbi statt. An den Marktständen werden Kastanienprodukte und regionale Spezialitäten angeboten.
Naturgefahren
Hochwasser in Luzern August 2005
Nach dem Erdbeben vom 18. September 1601 entstanden Tsunamis im Vierwaldstättersee mit vermutlich bis zu 4 Meter hohen Flutwellen. Ein weiteres solches Ereignis soll im Jahr 1687 stattgefunden haben. Auch vom Genfersee ist ein Binnentsunami-Ereignis aus dem Jahr 563 bekannt, und vom Lauerzersee aus dem Jahr 1806.
Die Folgen der allgemeinen Erderwärmung in den Alpen werden auch für den Vierwaldstättersee und seine Umgebung diskutiert. Das Hochwasser 2005 mit diversen Muren und Erdrutschen könnte als Warnsymptom verstanden werden.
Seit 1861 wird der Wasserspiegel des Vierwaldstättersees durch die Reusswehranlage in Luzern etwa zwei bis drei Meter über dem natürlichen mittleren Wasserstand gehalten.
Verkehr
Schifffahrt
Auf dem See verkehren die Schiffe der Schifffahrtsgesellschaft des Vierwaldstättersees (SGV) zu den zahlreichen Schiffstationen. Bis zum Bau der Axenstrasse in den Jahren 1863 bis 1865 war der Wasserweg die einzige aus dem Norden mögliche Verbindung zum Kanton Uri, zum Gotthardpass und damit auch der einzige Weg von den Städten im Nordwesten Europas nach Mailand und zu den italienischen Häfen am Mittelmeer. Das gilt auch für die Pilgerwege des Mittelalters nach Rom. Noch heute verkehren auf dieser Strecke die grossen Raddampfer der SGV Stadt Luzern (das Flaggschiff der SGV) Uri, Unterwalden, Gallia und Schiller.
Autofähre Beckenried–Gersau
Zwischen Beckenried und Gersau verkehrt die Autofähre Beckenried–Gersau. Auf dem See fahren ausserdem Lastschiffe privater Transportunternehmen.
Beim Zusammenstoss des Nauens Schwalmis mit dem Motorschiff Schwalbe vor Horw starben am 12. Oktober 1944 zwanzig Gäste einer 33-köpfigen Hochzeitsgesellschaft aus der Region Entlebuch. Die Unfallursache konnte nicht restlos geklärt werden. Es war das bislang grösste Unglück der Schweiz mit einem motorisierten Schiff.
Strasse und Schiene
Seit dem Bau der Gotthardstrasse, der Gotthardbahn (Eröffnung 1882), der Gotthardautobahn (1982) und der Eisenbahnschnellfahrstrecken von AlpTransit (NEAT) zum Gotthard-Basistunnel (2016) tangieren grosse internationale Verkehrswege die Gegend um den Vierwaldstättersee. In Flüelen wechselten vor dem Bau der Eisenbahn die Reisenden von den Bergpässen vom Maultier oder der Postkutsche auf das Schiff. Am östlichen Ufer führt die Axenstrasse mit vielen Tunnels und Galerien von Flüelen über Sisikon nach Brunnen. Sie ist Bestandteil der A4. Die Bahnlinie führt mehrheitlich unterirdisch von Flüelen nach Brunnen. Auf dem Weg nach Küssnacht erinnern alte, restaurierte Hotelbauten an die Zeit des frühen Tourismus im 19. Jahrhundert.
Zwischen Hergiswil und Stansstad führen Strassenbrücken (Kantonsstrasse und Autobahn A2) und eine Eisenbahnbrücke der Luzern-Stans-Engelberg-Bahn bei der Lopper-Halbinsel über eine Landenge im See.
Der 1991 auf alten Verkehrswegen angelegte Wanderweg mit der Bezeichnung Weg der Schweiz führt rund um den südlichsten Teil des Sees, den Urnersee.
Luftverkehr
Zwischen Buochs und Ennetbürgen bei Stans liegt der Flugplatz Buochs, der früher fast nur von der Schweizer Armee und den Pilatus-Flugzeugwerken benutzt wurde. Heute steht der Flugplatz dem zivilen Flugverkehr offen. Der Militärflugplatz Alpnach wird von der Schweizer Armee als Helikopterbasis genutzt.
Hängegleiter und Gleitschirme nutzen bei geeignetem Wetter die Thermik der Felswände über den steilen Ufern des Sees. Die beliebtesten Fluggebiete für Gleitschirme um den Vierwaldstättersee sind der Pilatus, die Rigi, das Gebiet von Emmetten, das Stanserhorn und das ganze Engelbergertal. Beim Fliegen sind die Kontrollzonen der Flugplätze Alpnach, Buochs und Emmen zu beachten.
Geschichte
Zu den frühesten menschlichen Spuren am See gehörten die neolithischen Seeufersiedlungen aus dem 5. bis 4. Jahrtausend v. Chr. bei Stansstad-Kehrsiten. Zahlreiche Ortsnamen weisen auf eine keltische, später gallorömische Besiedlung hin. In Alpnach fand sich eine römische Villa. Spätestens im 7. Jahrhundert liessen sich Alemannen nieder.
Am Ausfluss der Reuss entstand im 12. und 13. Jahrhundert die Stadt Luzern, rund um den See die Länderorte Uri, Schwyz und Unterwalden. Diese erlangten die Hoheit über das sie verbindende Gewässer bis hin zur Seemitte, sieht man von der Fläche in der Verlängerung des Bürgenbergs bis vor Hertenstein ab. Diese gelangte 1378 zusammen mit dessen Nordflanke an Luzern. Dennoch kam es bis 1967 – zwischen Nidwalden und Luzern – zu Auseinandersetzungen um Fischereirechte und Grenzstreitigkeiten. Da es extrem schwierig war, Strassen um den See zu bauen, war das Gewässer zugleich eine Hauptverkehrsader.
Kirchlich bildete der Raum vom Hochmittelalter bis 1821 das Dekanat Luzern bzw. das Vierwaldstätterkapitel im Bistum Konstanz. Danach wurde der Raum auf die Bistümer Chur und Basel aufgeteilt. Über den See oder an ihm entlang führten früher Pilgerwege nach Rom. Auch der westwärts nach Santiago de Compostela führende Jakobsweg führt von Einsiedeln nach Brunnen. Von hier führt er weiter westlich mit dem Schiff nach Luzern oder über den Alpnachersee nach Süden zum Brünigpass.
Im Gegensatz zum offenen See, auf dem frei gefischt werden durfte, gehörten die Uferstreifen zur Gemeinmarch der Siedlungsgenossen. Nur ihre Fischer durften dort ausfahren. Daneben bestanden herrschaftliche Rechte wie die Fischämter von St. Leodegar in Luzern. Aus derlei Organisationsformen gingen etwa 1465 die Luzerner Rohrgesellen oder 1607 die St.-Niklausen-Bruderschaft von Stansstad hervor. Auch hier konnten Fischereirechte zu heftigen Auseinandersetzungen führen, wie 1655 zwischen Luzern und Nidwalden. Statuten für den Fischmarkt finden sich in Luzern schon im ältesten Ratsbüchlein (um 1318).
Nach der Helvetik wurde die Fischerei in allen Orten zu einem Hoheitsrecht der Kantone. 1890 schlossen sich die Kantone zum Fischereikonkordat Vierwaldstättersee zusammen. Noch Ende des 20. Jahrhunderts beschäftigten 27 Betriebe rund 40 Vollzeitarbeitskräfte.
Der regionale Markt mit Luzern als Mittelpunkt und der Verkehr über den Gotthard führten zum Aufbau eines Transportwesens. In Flüelen wurde 1313 ein Reichszoll erwähnt, Anfang des 14. Jahrhunderts sind in Luzern Lagerhäuser bezeugt, ähnlich wie in anderen Orten.
Im 17. Jahrhundert bestanden in Alpnach fünf Fahrrechte, in Brunnen arbeiteten 60 Schiffsleute. 1687 kam es zum Abschluss eines Schifffahrtsvertrags, der bis ins 19. Jahrhundert Bestand hatte. 1837 begann die Dampfschifffahrt, 1870 entstand die Schifffahrtsgesellschaft des Vierwaldstättersees. Sie verdrängte die lokalen Schifffahrtsgenossenschaften. Ab 1859 entstand im Einzugsgebiet des Sees ein Eisenbahn-, Bergbahn- und Strassennetz, was den Tourismus stark anwachsen liess und eine entsprechende Infrastruktur hervorbrachte. Ab Ende des 19. Jahrhunderts wurde die Sand- und Kiesgewinnung zu einem expandierenden Industriezweig.
1859–1860 wurde mit dem Bau des Luzerner Nadelwehrs die Basis für eine Regulierung des Wasserpegels gelegt. Zugleich belasteten Kiesabbau, das Wachstum der Orte und der unkontrollierte Häuserbau, dazu Gewässerverschmutzung und Wassersport den See. Daher entstand 1916 das Hydrobiologische Laboratorium (1960 in die ETH Zürich integriert), das im Bereich des Gewässerschutzes tätig wurde und bis heute die Kantone berät. 1953 wurde der Gewässerschutz in der Bundesverfassung verankert, aber erst das revidierte Gewässerschutzgesetz von 1971 ermöglichte es schliesslich die Sanierung des Sees bis 1987 voranzutreiben. Bereits ab 1980 versorgten sich Luzern, Bürgenstock sowie Küssnacht, Horw und Weggis mit Trinkwasser aus dem See. 1973 setzten die Uferkantone einen Landschaftsschutzplan in Kraft, dessen Umsetzung der 1984 gegründete Landschaftsschutzverband Vierwaldstättersee vorantreibt.
Kulturelle und historische Eigenheiten des Seegebietes sind der Kommunalismus, die eigenständige Rezeption der italienischen Renaissance und des Barock oder der Einfluss der Gegenreformation, aber auch die Kleinräumigkeit des lokalen Brauchtums und der Mundarten.
Tourismus
Fremdenverkehr
Auf dem Weg in den Süden entdeckten Engländer die Bergwelt der Innerschweiz. Es entstanden mehrere Kur- und Badeorte wie Weggis oder Gersau. 1871 eröffnete man die allererste Zahnradbahn Europas, die Vitznau-Rigi-Bahn. 1889 baute man von Alpnachstad auf den Pilatus die heute immer noch steilste Zahnradbahn der Welt. Einen Aufstieg auf die Rigi beschrieb Mark Twain, was in den USA des 19. Jahrhunderts zum Aufblühen des Schweizer Tourismus führte. Auf dem Vierwaldstättersee verkehrt mit fünf Dampfschiffen eine der grössten Dampfschiffflotten Europas.
In der Umgebung des Sees und auf Terrassen in mittlerer Höhe (wie z. B. Morschach und Seelisberg) liegen zahlreiche Tourismusorte. Attraktive Aussichtsberge nahe am Vierwaldstättersee sind die Rigi, der Pilatus, der Bürgenstock, das Stanserhorn, das Buochserhorn, die beiden Mythen, der Uri Rotstock und der Fronalpstock. Die meisten davon sind mit Bergbahnen erreichbar, die teilweise ihre Talstation in der Nähe von Schiffstationen am See haben.
Am See befinden sich zahlreiche Örtlichkeiten mit Bedeutung in der Schweizer Kultur- und Tourismusgeschichte: Rütli, Tellsplatte, Tellskapelle, Schnitzturm von Stansstad, Neu-Habsburg, Schillerstein, Treib, Astrid-Kapelle (Küssnacht) und Schloss Meggenhorn.
Wassersport
In den einzelnen Seebereichen sind wegen den Wasser- und den Windverhältnissen verschiedene Sportarten möglich.Von Boots- und Yachthäfen, See- und Strandbädern (z. B. das 1929 von Arnold Berger gebaute Strandbad Lido in Luzern) und von andern Uferabschnitten aus ist der See zugänglich. 1881 wurde der See-Club Luzern gegründet, der heute der grösste Ruderclub der Schweiz ist, 1904 der Ruderclub Reuss Luzern. Seit 1941 besteht der Yachtclub Luzern, der am Churchill-Quai in Luzern seit 1966 ein Bootshaus und ein Bojenfeld betreibt. Der im Jahr 1958 gebildete Wassersportclub Brunnen führte in den ersten Jahren seines Bestehens auf dem Vierwaldstättersee internationale Motorbootrennen und Wasserskimeisterschaften durch. 1965 wählte der Verein den neuen Namen Wassersport-Club Vierwaldstättersee. 1980 entstand der Motorbootclub Zentralschweiz, 1986 der Wassersportclub Hergiswil. SchweizMobil hat eine Kanutour über den Vierwaldstättersee zwischen Brunnen und Gersau beschrieben. Der südliche Teil des Urnersees zwischen dem Campingplatz am Gruonbachstrand in Flüelen und Isleten ist wegen des Windes im Reusstal ein Zentrum des Windsurfens.
Tauchsport
Es gibt etwa zehn Plätze, an denen man ohne Boot im Vierwaldstättersee tauchen kann. Das Wasser ist ganzjährig eher kühl und deshalb meist sehr klar. Die zerklüftete Steilwand bei Sisikon, am nördlichen Portal des Schieferneggtunnels, kann man seit einem Erdrutsch und dem Verschütten eines Parkplatzes, der auch als Einstieg genutzt wurde, nicht mehr von Land aus betauchen. Vor Brunnen liegt das Lediwrack Bruno auf 15 Meter Tiefe. Weiter bekannte Tauchplätze liegen vor Vitznau, Weggis, Gersau und Hergiswil.
Wirtschaft
In mehreren Gemeinden am Vierwaldstättersee befinden sich an den leicht zugänglichen Bergflanken im Uferbereich seit Jahrhunderten Steinbrüche, die teilweise noch heute genutzt werden. Das Gestein gelangt auf dem Seeweg kostengünstig zu Verbrauchern oder Bahnhöfen. Die auffälligen Eingriffe in die Naturlandschaft stiessen schon früh auf Kritik seitens der Landschaftschutzorganisationen. 1930 wies ein Bericht auf die Zunahme der Grossanlagen hin: «Zwei Steinbrüche [liegen] im Urner See zwischen Seedorf und Isleten, vier zwischen Beckenried und Treib, einer in der Matt unter dem Bürgenstock, einer zwischen Kehrsiten und Stansstad, fünf im Alpnachersee, einer am Lopperberg zwischen Stansstad und Hergiswil, einer bei Greppen, einer zwischen Vitznau und Gersau, zwei zwischen Gersau und Brunnen». Bei Kehrsiten am Bürgenstock baut die Holcim in einem Schotterwerk harten Kieselkalk ab, der auch in den Brüchen Schwibogen und Rotzloch gewonnen wird, während vier andere Nidwaldner Steinbrüche im Uferbereich aufgelassen sind. Der Landschaftschutzverband Vierwaldstättersee begleitet die Entwicklung einzelner Steinbruchprojekte.
Seit 1891 baut das Unternehmen Arnold & Co. Sand- und Kieswerk AG bei Flüelen mit Schwimmbaggern Kies aus dem Schwemmfächer vor dem Delta der Reuss ab, wofür sie dem Kanton Uri Konzessionsgebühren entrichtet. Heute sind nur noch der vierte und fünfte Schwimmbagger aus den 1950er und 1960er Jahren in umgebautem Zustand im Einsatz. Die Flotte der Arnold + Co. AG umfasst etwa fünfzehn Nauen. Zwischen 2001 und 2005 legte das Unternehmen im Urnersee mit Schutt aus dem NEAT-Stollen Amsteg und der Umfahrung Flüelen sechs Inseln an.
Auch bei Beckenried und anderen Stellen wird vor den Flussmündungen Kies abgebaut.
Mitte April 1957 wurde ein Telefonkabel von Spissenegg nach Stansstad im See verlegt. Die Teilverkabelung des Vierwaldstättersees hatte zwei Gründe: Die damalige Bezirkskabelanlage war durch den Bau des neuen Autobahnabschnittes Horw-Stans erheblich gefährdet. Der Schutz der Kabel hätte aber zu kostspieligen Sicherungsmassnahmen geführt. Da die Seekabellegung in diesem Fall preiswerter und der Bedarf an zusätzlichen Leitungen gross war, bewilligte die Telefondirektion in Bern das Projekt.
100 Jahre zuvor, 1854, wurde exakt auf dieser Strecke das erste, in den Telegrafenwerkstätten in Bern eigens hergestellte Seetelefonkabel verlegt. Es diente zur Verbindung der anschliessenden oberirdischen Telegrafenlinien Luzern-Brünig-Interlaken.
Belastung mit Munition
Zwischen 1918 und 1967 entsorgten Schweizer Munitionsfabriken ihre Produktionsabfälle im Vierwaldstätter-, Brienzer- sowie Thunersee. Die Gesamtmenge, welche in bis zu 200 Metern Tiefe im Vierwaldstättersee versenkt wurde, wird auf 3'300 Tonnen geschätzt, 2'800 Tonnen im Urnersee sowie 500 Tonnen im Gersauer Becken.
Namensverwandtschaften
Der Jacobiweiher im Stadtwald von Frankfurt am Main wird im Volksmund seiner Form wegen Vierwaldstättersee genannt.
Auch ein künstlicher See im Zoo Berlin wird aus dem gleichen Grund Vierwaldstättersee genannt.
(Wikipedia)
Das Stanserhorn ist ein 1897 m ü. M. hoher Berg im Schweizer Kanton Nidwalden, der Hausberg von Stans und liegt in den Urner Alpen an der Grenze zum Kanton Obwalden.
Geographie
Das Stanserhorn liegt zwischen den Ortschaften Stans, Ennetmoos, Kerns, Dallenwil und Oberdorf, südlich des Vierwaldstättersees und somit (gemäss SOIUSA) in den Unterwaldner Voralpen. An der Südostflanke des Stanserhorns liegt auf einer Höhe von 1226 m ü. M. der kleine Ferienort Wirzweli.
Die Rundsicht reicht von den nahen Alpengipfeln bis hin zu den Vogesen im Elsass (Frankreich) und zum Feldberg im Schwarzwald (Deutschland). Dazwischen sind zehn grössere Seen auszumachen: Zugersee, Wichelsee, Vierwaldstättersee, Sempachersee, Sarnersee, Hallwilersee, Gerzensee, Bannalpsee, Baldeggersee und Alpnachersee.
Erschliessung
Die beiden Bergbahnpioniere Franz Josef Bucher-Durrer und Josef Durrer-Gasser begannen im Juni 1891 mit dem Bau der Stanserhorn-Bahn, die wegen der grossen Streckenlänge von knapp 4 km in drei getrennten Standseilbahn-Sektionen von Stans über Kälti und Alp Blumatt auf den Gipfel führte. Die Bahn wurde am 23. August 1893 eröffnet, gleichzeitig mit dem ebenfalls neu errichteten Hotel Stanserhorn Kulm. 1895 wurde auf dem Gipfel ein elektrischer Scheinwerfer mit der «Kraft von 22'000 Normalkerzen» installiert, um damit auf das Stanserhorn als Attraktion aufmerksam zu machen. Durch einen Kurzschluss in der Station Blumatt wurde am 2. Oktober 1970 ein Brand ausgelöst, wodurch der Antrieb der 3. Sektion, das Hotel und das Scheinwerferaggregat zerstört wurden. Anstatt des Hotels wird seitdem ein Restaurant auf dem Gipfel betrieben.
Nachdem 1974 der Betrieb der Standseilbahn eingestellt worden war, wurde 1975 die Luftseilbahn Kälti–Stanserhorn eröffnet, die nun zusammen mit der ursprünglichen 1. Sektion den Berg erschloss. Seit 2012 kann man mit der doppelstöckigen «CabriO-Bahn» auf das Stanserhorn fahren. Das offene Oberdeck der Seilbahnkabine kann während der Fahrt über eine Wendeltreppe erreicht werden, die Kabine fasst 60 Personen, das Oberdeck davon 30.
Als Touristenattraktion wurde 2001 das Drehrestaurant Rondorama eröffnet. Von der sich im Innern des Gebäudes drehenden Plattform hat man eine Rundsicht auf die umliegenden Berge und Seen. Ein Murmeltiergehege und ein ausgeschilderter Gipfelrundgang von rund 30 Minuten ergänzen das Angebot auf dem Stanserhorn, das auch als 5-Sterne-Berg und Faulenzer-Berg vermarktet wird. Auf der Route vom Stanserhorn zur Wirzweli befindet sich der Geo-Weg (Bergwanderung im Schwierigkeitsgrad T2 gemäss SAC-Wanderskala), der gemeinsam durch die Organisationen Nidwaldner Wanderwege, Pro Natura und WWF Unterwalden realisiert wurde.
Das Stanserhorn wird von Drachenfliegern und Gleitschirmpiloten benutzt, es gilt als Hausberg des grössten und ältesten noch aktiven Drachenfliegerclubs der Schweiz, des Deltaclubs Stans. An sonnigen Tagen – vor allem an den Wochenenden – finden von April bis Oktober jeweils um die Mittagszeit viele Starts statt.
(Wikipedia)
The addition the historic Amos Building takes place during heavy lake effec snow in downtown Syracuse. Wooden trusses arrive and await installation. www.dailydieseldose.com for more!
In addition to 44 published novels, Philip K. Dick (1928-1982) wrote approximately 121 short stories, most of which appeared in science fiction magazines during his lifetime. "Solar Lottery" was his first book. Although Dick spent most of his career as a writer in near-poverty, eleven popular films based on his works have been produced, including Blade Runner, Total Recall, A Scanner Darkly, Minority Report, Paycheck, Next, Screamers, The Adjustment Bureau and Impostor. In 2005, Time magazine named Ubik one of the hundred greatest English-language novels published since 1923. In 2007, Dick became the first science fiction writer to be included in The Library of America series.
New addition!! I’ve been having fun with the Canon 20D but when I found a 50D body that was cheap but wouldn’t turn on, figured it was worth a shot.
Hooked up the grip from the 20D that was charged up, still nothing.
Tested another CF card and it came alive!!
Reformatted the one it had, works like new!
Now to eventually find a canon lens 😂
I only have the two lensbaby lenses and the Olympus adapter (only good within so many feet).
Debating on letting the Lensbaby composer go so I can find a prime lens.
#newtome #leapoffaith #itsalive #canon #dslr #canon50d
Grade I listed historic hall constructed in the 1400's with additions in 1590.
"Blencow or Blencowe is a small village near Penrith, Cumbria. It is divided by the River Petteril into Great Blencow to the south and Little Blencow to the north. Great Blencow is in the civil parish of Dacre while Little Blencow is within Greystoke parish.
The village shares its name with the Blencowe family. The "cow" part of the name is compared with the "gow" in Glasgow.
Adam de Blencowe was awarded land by Edward III in 1358 and the original family home was built in Great Blencow. Now little remains. Subsequently, in the 15th or 16th century the family built a new home, the current Blencowe Hall, just to the west of Little Blencow. It consists of two fortified pele towers joined by connecting buildings. It sustained substantial damage during the English Civil War, now evident externally as a deep gash on the front of the western tower. This was imaginatively restored in the late 20th century. The family continued to own the hall until 1802, when it was sold to the Duke of Norfolk. There is an active Blencowe Families Association who celebrate their connections with this village.
Blencow at one time had a very well known grammar school founded by Thomas Burbank in 1577. It was the first free grammar school in the north of England. Among its pupils were Lord Ellenborough, Lord Chief Justice and George Whitehead, a prominent Quaker. The original school was rebuilt in 1795 and continued to provide an education for boys (although no longer free) until 1911, when it closed. For a time it was used as a meeting place for the village, but was converted to a private residence, Burbank House, in 1917." - info from Wikipedia.
Summer 2019 I did a solo cycling tour across Europe through 12 countries over the course of 3 months. I began my adventure in Edinburgh, Scotland and finished in Florence, Italy cycling 8,816 km. During my trip I took 47,000 photos.
Now on Instagram.
Become a patron to my photography on Patreon.
This addition to the Class 35 variations carries the lighter blue with white window frames and small yellow panels that several member of the class actually carried. But there are detail differences, principally the small aluminium arrow symbols under each cab window (rather than the large white version centrally placed on the bodyside). The white window surrounds suited the Class 35 particularly well; and the feature was quickly re-instated after several members had received small yellow warning panels on a plain blue body. When the darker Monestral blue was introduced with full yellow ends, the latter colour replaced the white areas on the cab sides - possibly one of the few applications of the corporate scheme that really suited the lines of the locomotive (29-Mar-10).
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This angle shows some of the changes to the Hope Remains house over the years.The addition on the left contains the decaying kitchen and a modern(?) bathroom.The wrap-around porch obviously came later,with the decision to put a metal roof on it.The original structure(shown better in the other view of the house pic)has a green shingle roof,and seems to be the the most structurally sound(though I didn't go upstairs)part of the house.
A photo c. 1900 photo of the first High School (albeit an expanded and altered building from the original) in Wichita, KS. The original High School building was built by W.H. Sternberg (1832 - 1906) who was the most prolific designer and builder in the Wichita area during one of the greatest economic booms in U.S. history.
This was still the first high school in Wichita as there were no other high school buildings yet, but it was much expanded from the original building. The original building is the portion on the right which has the square limestone-linteled windows on the second floor. Undoubtedly the expansion / alteration project was let out for bid and it's not yet known who built the addition. The entire structure is no longer standing. It was located between Second Street and Third Street on the east side of Emporia.
W.H. Sternberg built more of the civic buildings than any other contractor in the late 1800s... "probably twice as many as have been put by any other contractor in the city", Portrait And Biographical Album of Sedgwick County, Kan., Chapman Brothers 1888, pgs. 190 - 191. In addition to putting up more of the commercial and government buildings than anyone else he also designed and erected most of the large, upscale homes of the day. Sternberg was well known within elite circles as being the best contractor because he not only had the best workers and did the best quality work, but he offered unique, trend-setting designs in residential style. Many (but not most) of Sternberg's surviving works are listed on a State or National Historic Register. Among some of Sternberg's works that are now listed on the National Register of Historic Places are:
1)Sternberg Mansion
2)Friends University Administration Building
3)Sedgwick County Courthouse
4)Eaton Hotel (formerly the Carey Hotel)
5)Occidental Hotel Building
6)Methodist Episcopal Church in Norwich New York (brick)
Sternberg's unique residential designs include ideas suggestive of Stanford White and Issac G. Perry (both prominent architects from New York State). Sternberg built structures architected by both of these prominent architects. In addition to creating stunning homes on the outside, Sternberg was also known for creating comfortable, usable homes on the inside such as using spaces and angles that seemed to enlarge the interior spaces of the home - giving the home a "grand" effect but at the same time following a floor plan that provided the occupant with easy comfort and use. Many of Sternberg's floor plans are similar and many of the exterior features on his homes reappear from one home to another. The height of style was Sternberg's own home at 1065 N. Waco Avenue in Wichita, KS which was built (in part) to showcase all of the trend-setting designs that could reasonably be fabricated. A model home of sorts, this strategy worked well for Sternberg and home buyers flocked to Sternberg to have him design and build their new home. Following is a quote from the Portrait And Biographical Album of Sedgwick County, Kan; Chapman Brothers 1888, pages 190 - 191, "The residence of Mr. Sternberg, a handsome and costly structure, is beautifully located on a rise of ground commanding a fine view of its surroundings. Within and without it bears the evidence of refined tastes and ample means, and is universally admired by all who have occasion to pass it." The Monday, September 6th, 1886 Beacon contained an article about the construction of Sternberg mansion, "Mr. Sternberg is building for his own use a fine residence on the corner of 10th and Waco streets. Judging it by the foundation it will be one of the largest and finest in the city."
Regarding the expanded high school above, it's not yet known if this school was named after someone. It was common during the day to name schools after notable literary or academically influential persons. Following is a brief history of schools in Wichita, KS, taken from "A History of Wichita Schools" written in 1893...
"In 1868, the first cabin was built where the city of Wichita now stands. In 1870, the town was founded. In 1871, the first church and first schoolhouse were built. In 1872, the first railroad was constructed, the first bank opened, and the first newspaper started. The population increased from the occupants of one cabin, in 1868, to 50, as indicated by the census of 1870; 4,911, by the census of 1880; 23,835, by the census of 1890, and 28,000, the estimate in 1892.
Following the first cabins came the first schoolhouse, with William Finn, now a resident of Sedgwick, as schoolmaster. Mr. Finn's school commenced November 1, 1869, and continued three months. His average attendance was 17. His salary was to be $45 per month, and was to be raised by subscription. Mr. Finn sent to Topeka for the books for his school, paying for them out of his own pocket. Not half of the money subscribed was raised, and Mr. Finn, at the end of the term, was $50 in debt, although he had a little money of his own when he started. Through the kindly assistance of Hon. J. R. Mead, who was one of his patrons and friends, Mr. Finn purchased a surveying outfit, and left the profession of teaching.
Mr. Finn was an excellent young man, and his school a success. He has furnished us with a cut of the dugout which was his schoolhouse. It stood at the north of the present site of the city. It was about 13 feet square, had a dormer window, and was covered with a dirt roof."
Dugouts and sod buildings were common ways of building in the early days on the prairie. These weren't as dismal and dirty as might be thought. Many had cloth (sheets or flour sacks sewn together) or paper attached to the ceiling rafters (like ceiling tiles today) - which kept the dirt (and snakes) from falling down and the interior walls were frequently plastered with a mixure of mud and dried prairie grass (finished off pretty smoothly) and sometimes painted with a white wash of burnt gypsum. Most early schools however did have dirt floors, but with a manufactured window or two and a few kerosene lanterns they were reasonably light and fairly warm in the winter and fairly cool in the summer.
Your thoughts, comments, ideas, stories and additional information about this photo or this place are welcome and appreciated.
This photos is courtesy of the Wichita Public Library.
Home addition with patio walkway, columns, and lighting built in the North Potomac area of Rockville, Maryland. Complete with Tesla charging station.
Our second visit to the Sir Seewoosagur Ramgoolam Botanical Garden (commonly known as the Pamplemousses Botanical Garden) in Mauritius. This time we wandered without a guide.
The garden was first constructed by Pierre Poivre (1719 – 1786) in 1770, and it covers an area of around 37 hectares.
In addition to its famous giant waterlilies, the garden also features spices, ebonies, tropical fruit trees, sugar canes, and 85 varieties of palms from Central America, Asia, Africa and the islands around the Indian Ocean. Many trees have been planted by world leaders and royalty, including Princess Margaret, Indira Gandhi, François Mitterrand and Robert Mugabe.
The newest addition to the Devil's Tail Press is a circa 1960 Hohner-IV A5 press made in West Germany by Otto Hohner Maschinenfabrik. This particular model has all the bells and whistles that were provided with this line of machines, the other models I through III had some, but not all of the features of this press. The most unique feature is an ejection feature that knocks the printed item (card stock) into a tray on the side of the press. It will take a bit of refurbishing, but the equipment dealer from whom I purchased it kept the important parts greased and oiled as protection from the salt air of the Pacific Ocean, which was only a few blocks from their shop.
East Elevation: The house was designed around three existing trees.
Project Name: Three Trees
Project Type: Addition and remodel to a house
Location: Eagle Rock, CA
Designer: Jeremy Levine Design
This imposing edifice is the Walloomsac Inn. My husband could barely get the car stopped before I bailed out to shoot this place. Seeing the sign across the front I thought it was reasonably safe to shoot it as it said "Inn." "Inn" sounds friendly. After I had explored all sides and angles I walked up on the porch and read the sign which read and I paraphrase "This is a private residence - don't knock - don't think about knocking - get the hell off my porch."
Not so sure I would want to trust the emergency fire exit.
Located in the Old Bennington Historic District, the Walloomsac Inn is the oldest inn in the State of Vermont. The building was constructed in 1764, with additions and alterations to the roof throughout the late 1700s and 1800s. Five prominent families owned and operated the inn throughout its life; the inn served the stagecoach road until the 1850s. Important figures such as Thomas Jefferson, James Madison, Rutherford B. Hayes and Benjamin Harrison have stayed at the inn. Although its name has been changed a few times, it was most recently known as the Walloomsac Inn. (various sources)
Film: Kodak Ektachrome E100VS
Camera: Minolta 600si, Tamron 20-40mm lens
Image by: Leslie Hunsberger
Bennington, VT Jul 2001
A bank of small lockers was custom color matched to the Viking range and wall mounted for storage of dishes, glasses and serving pieces.
Behind modern additions is the original early 1970s shop front - and that wonderful perspex lettering!
The latest addition to the First Potteries fleet is Volvo B7TL/Alexander ALX 400 W217XBD (32057) which came from Leicester earlier this week to join recent arrivals and sister vehicles 32053-6 at Newcastle-under-Lyme depot. However as the four previous arrivals seem to have pushed four Olympians, including one of the famous 'G' reg Leyland examples out of service it sadly wouldn't be unreasonable to expect that the arrival of this one will displace the last Leyland - it was still parked with the 'in-service' buses today though. 32057 is seen leaving Newcastle-under-Lyme bus station bound for Hanley on a 25, 11/04/2014.
I mentioned the other day that I had a welcomed home an old friend to my camera bag...here it is. "No, not the kitty...the lens that took this shot". LOL! I purchased a Nikon 24-70mm F/2.8 AF-S, a lens which I had previously owned from 2007-2011 before selling it because I wasn't using much. But as soon as I sold it I was missing it, and I had bought a bunch of other glass trying to replace this lens. Well, the other glass is now on eBay to offset the purchase and then some.
Now about this kitty... Joey had been wanting a kitty for some time now, and by happenstance my wife and Joey ran into a lady who used to work at one of the daycare's he attended when he was 3-4. She had a kitten that she thought would be perfect for him. So we went over to her house today and the lady was right, the little 9 week old kitty was PERFECT, and then we saw this little lady. She was a rescue kitty that was found on the side of the road. She was so young when she was found that her eyes weren't even opened yet. The vet thought that she wouldn't make it through the night, but she did! I am not sure how many weeks old she is, but she fits in one of my hands. She adopted me, so both kitties came home with us.
One of the secondhand bought hoppers that Conrad Yelvington got, used to work coal service but got patched and re-stenciled. I'll give this the reporting marks CYXX 83371 as I built straight from it.
This pretty female House Sparrow seemed to be enjoying the latest addition to my garden today. As you will see below it's a small birdbath which I purchased recently and I'm using to soak mealworms in for the birds. I did this last year and it was a big success, especially with the young Blackbirds when they arrived : )