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Titicaca is a large, deep lake in the Andes on the border of Bolivia and Peru, often called the "highest navigable lake" in the world. By volume of water and by surface area, it is the largest lake in South America.
Puno is a city in southeastern Peru, located on the shore of Lake Titicaca. It is the capital city of the Puno Region and the Puno Province with a population of approximately 140,839.
Peru is a country in western South America. It is bordered in the north by Ecuador and Colombia, in the east by Brazil, in the southeast by Bolivia, in the south by Chile, and in the west by the Pacific Ocean.
Peru is a magical destination, abundant with ancient ruins dating back to the Incas.
Peru is the third largest country in South America, after Brazil and Argentina.
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One of the most iconic supercars of all time - a Mercedes-Benz 300SL 'Gullwing' Coupe - awaits its next driver during the Brooklands Motoring Festival press launch at Brooklands racing circuit, near Weybridge, Surrey, England. Taken on April 4, 2008.
Grantham, St Wulfram's, Gravity Fields Festival. Following a fire in 1222,it was rebuilt with the spire (the 3rd highest on a parish church in England) and west windows completed in 1300. It was enlarged in 1350, 1480 and 1496. It was restored by Sir George Gilbert Scott (completed 1875) who is responsible for the the woodwork, including the roof and angels. The church is grade 1 listed.
Grantham, Lincolnshire, UK - St Wulframs Church, Castlegate and Swinegate.
September 2018
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
Highest Explore Position #488 ~ On January 5th 2008.
Squirrel - Lincoln Inn Fields Park - Holborn, London, England - Thursday December Thirteenth 2007.
18.6.16... Biggest F and I made it to the top of Ben Nevis; UK's highest mountain!! Oh my word it was hard going (hence the pink face!!) but the view from the top was stunning. F and six of his p6 classmates did the climb for Macmillan cancer.
Highest position in Explore: 304 on Wednesday, July 9, 2008
The annual population explosion of billions of shad flies. Good thing their life cycle is short, and you don't even bother washing your car.
Shiva (/ˈʃivə/; Sanskrit: Śiva, meaning "The Auspicious One"), also known as Mahadeva ("Great God"), is a popular Hindu deity. Shiva is regarded as one of the primary forms of God. He is the Supreme God within Shaivism, one of the three most influential denominations in contemporary Hinduism.[2][3] He is one of the five primary forms of God in the Smarta tradition,[2] and "the Destroyer" or "the Transformer"[4] among the Trimurti, the Hindu Trinity of the primary aspects of the divine.
At the highest level, Shiva is regarded limitless, transcendent, unchanging and formless.[5][6][7][8][9] Shiva also has many benevolent and fearsome forms.[10] In benevolent aspects, he is depicted as an omniscient Yogi who lives an ascetic life on Mount Kailash,[4] as well as a householder with wife Parvati and his two children, Ganesha and Kartikeya and in fierce aspects, he is often depicted slaying demons. Shiva is also regarded as the patron god of yoga and arts.[11][12][13]
The main iconographical attributes of Shiva are the third eye on his forehead, the snake Vasuki around his neck, the crescent moon adorning, the holy river Ganga flowing from his matted hair, the trishula as his weapon and the damaru as his instrument. Shiva is usually worshiped in the aniconic form of Lingam
The Sanskrit word Shiva (Devanagari: शिव, śiva) comes from Shri Rudram Chamakam of Taittiriya Samhita (TS 4.5, 4.7) of Krishna Yajurveda. The root word is[17] means auspicious. In simple English transliteration it is written either as Shiva or Siva. The adjective śiva, is used as an attributive epithet not particularly of Rudra, but of several other Vedic deities.[18]
The other popular names associated with Shiva are Mahadev, Mahesh, Maheshwar, Shankar, Shambhu, Rudra, Har, Trilochan, Devendra (meaning Chief of the gods) and Trilokinath (meaning Lord of the three realms).[19][20][21]
The Sanskrit word śaiva means "relating to the god Shiva", and this term is the Sanskrit name both for one of the principal sects of Hinduism and for a member of that sect.[22] It is used as an adjective to characterize certain beliefs and practices, such as Shaivism.[23]
The Tamil word Sivan, Tamil: சிவன் ("Fair Skinned") could have been derived from the word sivappu. The word 'sivappu' means "red" in Tamil language but while addressing a person's skin texture in Tamil the word 'Sivappu' is used for being Fair Skinned.[24][25]
Adi Sankara, in his interpretation of the name Shiva, the 27th and 600th name of Vishnu sahasranama, the thousand names of Vishnu interprets Shiva to have multiple meanings: "The Pure One", or "the One who is not affected by three Gunas of Prakrti (Sattva, Rajas, and Tamas)" or "the One who purifies everyone by the very utterance of His name."[26] Swami Chinmayananda, in his translation of Vishnu sahasranama, further elaborates on that verse: Shiva means "the One who is eternally pure" or "the One who can never have any contamination of the imperfection of Rajas and Tamas".[27]
Shiva's role as the primary deity of Shaivism is reflected in his epithets Mahādeva ("Great god"; mahā "Great" and deva "god"),[28][29] Maheśvara ("Great Lord"; mahā "great" and īśvara "lord"),[30][31] and Parameśvara ("Supreme Lord").[32]
There are at least eight different versions of the Shiva Sahasranama, devotional hymns (stotras) listing many names of Shiva.[33] The version appearing in Book 13 (Anuśāsanaparvan) of the Mahabharata is considered the kernel of this tradition.[34] Shiva also has Dasha-Sahasranamas (10,000 names) that are found in the Mahanyasa. The Shri Rudram Chamakam, also known as the Śatarudriya, is a devotional hymn to Shiva hailing him by many names.[35][36]The worship of Shiva is a pan-Hindu tradition, practiced widely across all of India, Nepal and Sri Lanka.[37][38]The figure of Shiva as we know him today was built up over time, with the ideas of many regional sects being amalgamated into a single figure.[38] How the persona of Shiva converged as a composite deity is not well documented.[39] According to Vijay Nath:
Visnu and Siva [...] began to absorb countless local cults and deities within their folds. The latter were either taken to represent the multiple facets of the same god or else were supposed to denote different forms and appellations by which the god came to be known and worshipped. [...] Siva became identified with countless local cults by the sheer suffixing of Isa or Isvara to the name of the local deity, e.g., Bhutesvara, Hatakesvara, Chandesvara."[40]
Axel Michaels the Indologist suggests that Shaivism, like Vaishnavism, implies a unity which cannot be clearly found either in religious practice or in philosophical and esoteric doctrine. Furthermore, practice and doctrine must be kept separate.[41]
An example of assimilation took place in Maharashtra, where a regional deity named Khandoba is a patron deity of farming and herding castes.[42] The foremost center of worship of Khandoba in Maharashtra is in Jejuri.[43] Khandoba has been assimilated as a form of Shiva himself,[44] in which case he is worshipped in the form of a lingam.[42][45] Khandoba's varied associations also include an identification with Surya[42] and Karttikeya.[46]Many Indus valley seals show animals but one seal that has attracted attention shows a figure, either horned or wearing a horned headdress and possibly ithyphallic[47][48][49] figure seated in a posture reminiscent of the Lotus position and surrounded by animals was named by early excavators of Mohenjo-daro Pashupati (lord of cattle), an epithet of the later Hindu gods Shiva and Rudra.[47][50][51][52] Sir John Marshall and others have claimed that this figure is a prototype of Shiva and have described the figure as having three faces seated in a "yoga posture" with the knees out and feet joined.
While some academics like Gavin Flood[53][54] and John Keay have expressed doubts. John Keay writes that "He may indeed be an early manifestation of Lord Shiva as Pashu- pati", but a couple of his specialties of this figure does not match with Rudra.[55] Writing in 1997 Doris Srinivasan rejected Marshall's package of proto-Siva features, including that of three heads. She interprets what John Marshall interpreted as facial as not human but more bovine, possibly a divine buffalo-man.[56] According to Iravatham Mahadevan symbols 47 and 48 of his Indus script glossary The Indus Script: Texts, Concordance and Tables (1977), representing seated human-like figures, could describe Hindu deity Murugan, popularly known as Shiva and Parvati's son.[57]
Writing in 2002, Gregory L. Possehl concluded that while it would be appropriate to recognize the figure as a deity, its association with the water buffalo, and its posture as one of ritual discipline.[58]Shiva's rise to a major position in the pantheon was facilitated by his identification with a host of Vedic deities, including Purusha, Rudra, Agni, Indra, Prajāpati, Vāyu, and others.[59]Shiva as we know him today shares many features with the Vedic god Rudra,[60] and both Shiva and Rudra are viewed as the same personality in Hindu scriptures. The two names are used synonymously. Rudra, the god of the roaring storm, is usually portrayed in accordance with the element he represents as a fierce, destructive deity.
Hindu text Rig Veda, which is dated to between 1700 and 1100 BC based on linguistic and philological evidence.[61] A god named Rudra is mentioned in the Rig Veda. The name Rudra is still used as a name for Shiva. In RV 2.33, he is described as the "Father of the Rudras", a group of storm gods.[62] Furthermore, the Rudram, one of the most sacred hymns of Hinduism found both in the Rig and the Yajur Vedas and addressed to Rudra, invokes him as Shiva in several instances, but the term Shiva is used as an epithet for the gods Indra, Mitra and Agni many times. Since Shiva means pure, the epithet is possibly used to describe a quality of these gods rather than to identify any of them with the God Shiva.
The identification of Shiva with the older god Rudhra is not universally accepted, as Axel Michaels explains:
Rudra is called "The Archer" (Sanskrit: Śarva),[63] and the arrow is an essential attribute of Rudra.[64] This name appears in the Shiva Sahasranama, and R. K. Sharma notes that it is used as a name of Shiva often in later languages.[65]
The word is derived from the Sanskrit root śarv-, which means "to injure" or "to kill",[66] and Sharma uses that general sense in his interpretive translation of the name Śarva as "One who can kill the forces of darkness".[65] The names Dhanvin ("Bowman")[67] and Bāṇahasta ("Archer", literally "Armed with arrows in his hands")[67][68] also refer to archery.
Agni[edit]
Rudra and Agni have a close relationship.[69][70] The identification between Agni and Rudra in the Vedic literature was an important factor in the process of Rudra's gradual development into the later character as Rudra-Shiva.[71] The identification of Agni with Rudra is explicitly noted in the Nirukta, an important early text on etymology, which says, "Agni is also called Rudra."[72] The interconnections between the two deities are complex, and according to Stella Kramrisch:
The fire myth of Rudra-Śiva plays on the whole gamut of fire, valuing all its potentialities and phases, from conflagration to illumination.[73]
In the Śatarudrīya, some epithets of Rudra, such as Sasipañjara ("Of golden red hue as of flame") and Tivaṣīmati ("Flaming bright"), suggest a fusing of the two deities.[74] Agni is said to be a bull,[75] and Lord Shiva possesses a bull as his vehicle, Nandi. The horns of Agni, who is sometimes characterized as a bull, are mentioned.[76][77] In medieval sculpture, both Agni and the form of Shiva known as Bhairava have flaming hair as a special feature.[78]
Indra[edit]
According to Wendy Doniger, the Puranic Shiva is a continuation of the Vedic Indra.[79] Doniger gives several reasons for her hypothesis. Both are associated with mountains, rivers, male fertility, fierceness, fearlessness, warfare, transgression of established mores, the Aum sound, the Supreme Self. In the Rig Veda the term śiva is used to refer to Indra. (2.20.3,[80] 6.45.17,[81][82] and 8.93.3.[83]) Indra, like Shiva, is likened to a bull.[84][85] In the Rig Veda, Rudra is the father of the Maruts, but he is never associated with their warlike exploits as is Indra.[86]
The Vedic beliefs and practices of the pre-classical era were closely related to the hypothesised Proto-Indo-European religion,[87][88] and the Indo-Iranian religion.[89] According to Anthony, the Old Indic religion probably emerged among Indo-European immigrants in the contact zone between the Zeravshan River (present-day Uzbekistan) and (present-day) Iran.[90] It was "a syncretic mixture of old Central Asian and new Indo-European elements",[90] which borrowed "distinctive religious beliefs and practices"[89] from the Bactria–Margiana Culture.[89] At least 383 non-Indo-European words were borrowed from this culture, including the god Indra and the ritual drink Soma.[91] According to Anthony,
Many of the qualities of Indo-Iranian god of might/victory, Verethraghna, were transferred to the adopted god Indra, who became the central deity of the developing Old Indic culture. Indra was the subject of 250 hymns, a quarter of the Rig Veda. He was associated more than any other deity with Soma, a stimulant drug (perhaps derived from Ephedra) probably borrowed from the BMAC religion. His rise to prominence was a peculiar trait of the Old Indic speakers.[92]
Later Vedic literature[edit]
Rudra's transformation from an ambiguously characterized deity to a supreme being began in the Shvetashvatara Upanishad (400-200 BC), which founded the tradition of Rudra-Shiva worship. Here they are identified as the creators of the cosmos and liberators of souls from the birth-rebirth cycle. The period of 200 BC to 100 AD also marks the beginning of the Shaiva tradition focused on the worship of Shiva, with references to Shaiva ascetics in Patanjali's Mahabhasya and in the Mahabharata.[54][93]
Early historical paintings at the Bhimbetka rock shelters, depict Shiva dancing, Shiva's trident, and his mount Nandi but no other Vedic gods.[94][95]
Puranic literature[edit]
The Shiva Puranas, particularly the Shiva Purana and the Linga Purana, discuss the various forms of Shiva and the cosmology associated with him.[96]
Tantric literature[edit]
The Tantras, composed between the 8th and 11th centuries, regard themselves as Sruti. Among these the Shaiva Agamas, are said to have been revealed by Shiva himself and are foundational texts for Shaiva Siddhanta.[97]Shaivism[edit]
Main articles: Shaivism and History of Shaivism
Shaivism (Sanskrit: शैव पंथ, śaiva paṁtha) (Kannada: ಶೈವ ಪಂಥ) (Tamil: சைவ சமயம்) is the oldest of the four major sects of Hinduism, the others being Vaishnavism, Shaktism and Smartism. Followers of Shaivism, called "Shaivas", and also "Saivas" or "Saivites", revere Shiva as the Supreme Being. Shaivas believe that Shiva is All and in all, the creator, preserver, destroyer, revealer and concealer of all that is. The tantric Shaiva tradition consists of the Kapalikas, Kashmir Shaivism and Shaiva Siddhanta. The Shiva MahaPurana is one of the purāṇas, a genre of Hindu religious texts, dedicated to Shiva. Shaivism is widespread throughout India, Nepal, and Sri Lanka, mostly. Areas notable for the practice of Shaivism include parts of Southeast Asia, especially Malaysia, Singapore, and Indonesia.
Panchayatana puja[edit]
Main article: Panchayatana puja
Panchayatana puja is the system of worship ('puja') in the Smarta sampradaya of Hinduism. It is said to have been introduced by Adi Shankara, the 8th century AD Hindu philosopher. It consists of the worship of five deities: Shiva, Vishnu, Devi, Surya and Ganesha. Depending on the tradition followed by Smarta households, one of these deities is kept in the center and the other four surround it. Worship is offered to all the deities. The five are represented by small murtis, or by five kinds of stones, or by five marks drawn on the floor.[98]
Trimurti[edit]
Main article: Trimurti
The Trimurti is a concept in Hinduism in which the cosmic functions of creation, maintenance, and destruction are personified by the forms of Brahmā the creator, Vishnu the maintainer or preserver and Śhiva the destroyer or transformer.[99][100] These three deities have been called "the Hindu triad"[101] or the "Great Trinity",[102] often addressed as "Brahma-Vishnu-Maheshwara."
Shiva's form: Shiva has a trident in the right lower arm, and a crescent moon on his head. He is said to be fair like camphor or like an ice clad mountain. He wears five serpents and a garland of skulls as ornaments. Shiva is usually depicted facing the south. His trident, like almost all other forms in Hinduism, can be understood as the symbolism of the unity of three worlds that a human faces - his inside world, his immediate world, and the broader overall world. At the base of the trident, all three forks unite. It is often not shown but Shiva has 6 heads, of which only five (Isana, Tatpurusha, Vamana, Aghora, Sadyojata) are visible while the 6th (Adhomukh) can only be seen by the enlightened.
Third eye: (Trilochana) Shiva is often depicted with a third eye, with which he burned Desire (Kāma) to ashes,[103] called "Tryambakam" (Sanskrit: त्र्यम्बकम् ), which occurs in many scriptural sources.[104] In classical Sanskrit, the word ambaka denotes "an eye", and in the Mahabharata, Shiva is depicted as three-eyed, so this name is sometimes translated as "having three eyes".[105] However, in Vedic Sanskrit, the word ambā or ambikā means "mother", and this early meaning of the word is the basis for the translation "three mothers".[106][107] These three mother-goddesses who are collectively called the Ambikās.[108] Other related translations have been based on the idea that the name actually refers to the oblations given to Rudra, which according to some traditions were shared with the goddess Ambikā.[109] It has been mentioned that when Shiva loses his temper, his third eye opens which can reduce most things to ashes.
Crescent moon: (The epithets "Chandrasekhara/Chandramouli")- Shiva bears on his head the crescent moon.[110] The epithet Candraśekhara (Sanskrit: चन्द्रशेखर "Having the moon as his crest" - candra = "moon"; śekhara = "crest, crown")[111][112][113] refers to this feature. The placement of the moon on his head as a standard iconographic feature dates to the period when Rudra rose to prominence and became the major deity Rudra-Shiva.[114] The origin of this linkage may be due to the identification of the moon with Soma, and there is a hymn in the Rig Veda where Soma and Rudra are jointly implored, and in later literature, Soma and Rudra came to be identified with one another, as were Soma and the moon.[115] The crescent moon is shown on the side of the Lord's head as an ornament. The waxing and waning phenomenon of the moon symbolizes the time cycle through which creation evolves from the beginning to the end.
Ashes: (The epithet "Bhasmaanga Raaga") - Shiva smears his body with ashes (bhasma). The ashes are said to represent the end of all material existence.[116] Some forms of Shiva, such as Bhairava, are associated with a very old Indian tradition of cremation-ground asceticism that was practiced by some groups who were outside the fold of brahmanic orthodoxy.[117] These practices associated with cremation grounds are also mentioned in the Pali canon of Theravada Buddhism.[118] One epithet for Shiva is "inhabitant of the cremation ground" (Sanskrit: śmaśānavāsin, also spelled Shmashanavasin), referring to this connection.[119]
Matted hair: (The epithet "Jataajoota Dhari/Kapardina") - Shiva's distinctive hair style is noted in the epithets Jaṭin, "the one with matted hair",[120] and Kapardin, "endowed with matted hair"[121] or "wearing his hair wound in a braid in a shell-like (kaparda) fashion".[122] A kaparda is a cowrie shell, or a braid of hair in the form of a shell, or, more generally, hair that is shaggy or curly.[123] His hair is said to be like molten gold in color or being yellowish-white.
Blue throat: The epithet Nīlakaṇtha (Sanskrit नीलकण्ठ; nīla = "blue", kaṇtha = "throat").[124][125] Since Shiva drank the Halahala poison churned up from the Samudra Manthan to eliminate its destructive capacity. Shocked by his act, Goddess Parvati strangled his neck and hence managed to stop it in his neck itself and prevent it from spreading all over the universe, supposed to be in Shiva's stomach. However the poison was so potent that it changed the color of his neck to blue.[126][127] (See Maha Shivaratri.)Sacred Ganges: (The epithet "Gangadhara") Bearer of Ganga. Ganges river flows from the matted hair of Shiva.[128][129] The Gaṅgā (Ganges), one of the major rivers of the country, is said to have made her abode in Shiva's hair.[130] The flow of the Ganges also represents the nectar of immortality.
Tiger skin: (The epithet "Krittivasana").He is often shown seated upon a tiger skin,[116] an honour reserved for the most accomplished of Hindu ascetics, the Brahmarishis.[131]
Serpents: (The epithet "Nagendra Haara" or 'Vasoki"). Shiva is often shown garlanded with a snake.[132]
Deer: His holding deer on one hand indicates that He has removed the Chanchalata of the mind (i.e., attained maturity and firmness in thought process). A deer jumps from one place to another swiftly, similar to the mind moving from one thought to another.
Trident: (Trishula): Shiva's particular weapon is the trident.[116] His Trisul that is held in His right hand represents the three Gunas— Sattva, Rajas and Tamas. That is the emblem of sovereignty. He rules the world through these three Gunas. The Damaru in His left hand represents the Sabda Brahman. It represents OM from which all languages are formed. It is He who formed the Sanskrit language out of the Damaru sound.
Drum: A small drum shaped like an hourglass is known as a damaru (ḍamaru).[133][134] This is one of the attributes of Shiva in his famous dancing representation[135] known as Nataraja. A specific hand gesture (mudra) called ḍamaru-hasta (Sanskrit for "ḍamaru-hand") is used to hold the drum.[136] This drum is particularly used as an emblem by members of the Kāpālika sect.[137]
Axe: (Parashu):The parashu is the weapon of Lord Shiva who gave it to Parashurama, sixth Avatar of Vishnu, whose name means "Rama with the axe" and also taught him its mastery.
Nandī: (The epithet "Nandi Vaahana").Nandī, also known as Nandin, is the name of the bull that serves as Shiva's mount (Sanskrit: vāhana).[138][139] Shiva's association with cattle is reflected in his name Paśupati, or Pashupati (Sanskrit: पशुपति), translated by Sharma as "lord of cattle"[140] and by Kramrisch as "lord of animals", who notes that it is particularly used as an epithet of Rudra.[141] Rishabha or the bull represents Dharma Devata. Lord Siva rides on the bull. Bull is his vehicle. This denotes that Lord Siva is the protector of Dharma, is an embodiment of Dharma or righteousness.
Gaṇa: The Gaṇas (Devanagari: गण) are attendants of Shiva and live in Kailash. They are often referred to as the bhutaganas, or ghostly hosts, on account of their nature. Generally benign, except when their lord is transgressed against, they are often invoked to intercede with the lord on behalf of the devotee. Ganesha was chosen as their leader by Shiva, hence Ganesha's title gaṇa-īśa or gaṇa-pati, "lord of the gaṇas".[142]
5 heads: Shiva is known as panchavactra means 5 heads which indicates 5 elements.
Arms: Shiva has 4 arms which resembles 4 vedas
Mount Kailāsa: Mount Kailash in the Himalayas is his traditional abode.[116] In Hindu mythology, Mount Kailāsa is conceived as resembling a Linga, representing the center of the universe.[143]
Varanasi: Varanasi (Benares) is considered to be the city specially loved by Shiva, and is one of the holiest places of pilgrimage in India. It is referred to, in religious contexts, as Kashi.[144]
LINGAM
Apart from anthropomorphic images of Shiva, the worship of Shiva in the form of a lingam, or linga, is also important.[145][146][147] These are depicted in various forms. One common form is the shape of a vertical rounded column. Shiva means auspiciousness, and linga means a sign or a symbol. Hence, the Shivalinga is regarded as a "symbol of the great God of the universe who is all-auspiciousness".[148] Shiva also means "one in whom the whole creation sleeps after dissolution".[148] Linga also means the same thing—a place where created objects get dissolved during the disintegration of the created universe. Since, according to Hinduism, it is the same god that creates, sustains and withdraws the universe, the Shivalinga represents symbolically God Himself.[148] Some scholars, such as Monier Monier-Williams and Wendy Doniger, also view linga as a phallic symbol,[149][150] although this interpretation is disputed by others, including Christopher Isherwood,[151] Vivekananda,[152] Swami Sivananda,[153] and S.N. Balagangadhara.[154]
JYOTHIRLINGAM
The worship of the Shiva-Linga originated from the famous hymn in the Atharva-Veda Samhitâ sung in praise of the Yupa-Stambha, the sacrificial post. In that hymn, a description is found of the beginningless and endless Stambha or Skambha, and it is shown that the said Skambha is put in place of the eternal Brahman. Just as the Yajna (sacrificial) fire, its smoke, ashes, and flames, the Soma plant, and the ox that used to carry on its back the wood for the Vedic sacrifice gave place to the conceptions of the brightness of Shiva's body, his tawny matted hair, his blue throat, and the riding on the bull of the Shiva, the Yupa-Skambha gave place in time to the Shiva-Linga.[155][156] In the text Linga Purana, the same hymn is expanded in the shape of stories, meant to establish the glory of the great Stambha and the superiority of Shiva as Mahadeva.[156]
The sacred of all Shiva linga is worshipped as Jyotir linga. Jyoti means Radiance, apart from relating Shiva linga as a phallus symbol, there are also arguments that Shiva linga means 'mark' or a 'sign'. Jyotirlinga means "The Radiant sign of The Almighty". The Jyotirlingas are mentioned in Shiva Purana.[157]Shiva forms a Tantric couple with Shakti [Tamil : சக்தி ], the embodiment of energy, dynamism, and the motivating force behind all action and existence in the material universe. Shiva is her transcendent masculine aspect, providing the divine ground of all being. Shakti manifests in several female deities. Sati and Parvati are the main consorts of Shiva. She is also referred to as Uma, Durga (Parvata), Kali[158] and Chandika.[159] Kali is the manifestation of Shakti in her dreadful aspect. The name Kali comes from kāla, which means black, time, death, lord of death, Shiva. Since Shiva is called Kāla, the eternal time, Kālī, his consort, also means "Time" or "Death" (as in "time has come"). Various Shakta Hindu cosmologies, as well as Shākta Tantric beliefs, worship her as the ultimate reality or Brahman. She is also revered as Bhavatārini (literally "redeemer of the universe"). Kālī is represented as the consort of Lord Shiva, on whose body she is often seen standing or dancing. Shiva is the masculine force, the power of peace, while Shakti translates to power, and is considered as the feminine force. In the Vaishnava tradition, these realities are portrayed as Vishnu and Laxmi, or Radha and Krishna. These are differences in formulation rather than a fundamental difference in the principles. Both Shiva and Shakti have various forms. Shiva has forms like Yogi Raj (the common image of Himself meditating in the Himalayas), Rudra (a wrathful form) and Natarajar (Shiva's dance are the Lasya - the gentle form of dance, associated with the creation of the world, and the Tandava - the violent and dangerous dance, associated with the destruction of weary worldviews – weary perspectives and lifestyles).
The five mantras[edit]
Five is a sacred number for Shiva.[160] One of his most important mantras has five syllables (namaḥ śivāya).[161]
Shiva's body is said to consist of five mantras, called the pañcabrahmans.[162] As forms of God, each of these have their own names and distinct iconography:[163]
Sadyojāta
Vāmadeva
Aghora
Tatpuruṣha
Īsāna
These are represented as the five faces of Shiva and are associated in various texts with the five elements, the five senses, the five organs of perception, and the five organs of action.[164][165] Doctrinal differences and, possibly, errors in transmission, have resulted in some differences between texts in details of how these five forms are linked with various attributes.[166] The overall meaning of these associations is summarized by Stella Kramrisch:
Through these transcendent categories, Śiva, the ultimate reality, becomes the efficient and material cause of all that exists.[167]
According to the Pañcabrahma Upanishad:
One should know all things of the phenomenal world as of a fivefold character, for the reason that the eternal verity of Śiva is of the character of the fivefold Brahman. (Pañcabrahma Upanishad 31)[168]
Forms and roles[edit]
According to Gavin Flood, "Shiva is a god of ambiguity and paradox," whose attributes include opposing themes.[169] The ambivalent nature of this deity is apparent in some of his names and the stories told about him.
NATARAJA
The depiction of Shiva as Nataraja (Sanskrit: naṭarāja, "Lord of Dance") is popular.[199][200] The names Nartaka ("dancer") and Nityanarta ("eternal dancer") appear in the Shiva Sahasranama.[201] His association with dance and also with music is prominent in the Puranic period.[202] In addition to the specific iconographic form known as Nataraja, various other types of dancing forms (Sanskrit: nṛtyamūrti) are found in all parts of India, with many well-defined varieties in Tamil Nadu in particular.[203] The two most common forms of the dance are the Tandava, which later came to denote the powerful and masculine dance as Kala-Mahakala associated with the destruction of the world. When it requires the world or universe to be destroyed, Lord Śiva does it by the tāṇḍavanṛtya.[204][205] and Lasya, which is graceful and delicate and expresses emotions on a gentle level and is considered the feminine dance attributed to the goddess Parvati.[206][207] Lasya is regarded as the female counterpart of Tandava.[207] The Tandava-Lasya dances are associated with the destruction-creation of the world.[208][209][210]
Dakshinamurthy[edit]
Main article: Dakshinamurthy
Dakshinamurthy, or Dakṣiṇāmūrti (Tamil:தட்சிணாமூர்த்தி, Telugu: దక్షిణామూర్తి, Sanskrit: दक्षिणामूर्ति),[211] literally describes a form (mūrti) of Shiva facing south (dakṣiṇa). This form represents Shiva in his aspect as a teacher of yoga, music, and wisdom and giving exposition on the shastras.[212] This iconographic form for depicting Shiva in Indian art is mostly from Tamil Nadu.[213] Elements of this motif can include Shiva seated upon a deer-throne and surrounded by sages who are receiving his instruction.[214]
ARDHANARISWARA:
An iconographic representation of Shiva called (Ardhanārīśvara) shows him with one half of the body as male and the other half as female. According to Ellen Goldberg, the traditional Sanskrit name for this form (Ardhanārīśvara) is best translated as "the lord who is half woman", not as "half-man, half-woman".[215] According to legend, Lord Shiva is pleased by the difficult austerites performed by the goddess Parvati, grants her the left half of his body. This form of Shiva is quite similar to the Yin-Yang philosophy of Eastern Asia, though Ardhanārīśvara appears to be more ancient.Shiva is often depicted as an archer in the act of destroying the triple fortresses, Tripura, of the Asuras.[216] Shiva's name Tripurantaka (Sanskrit: त्रिपुरान्तक, Tripurāntaka), "ender of Tripura", refers to this important story.[217] In this aspect, Shiva is depicted with four arms wielding a bow and arrow, but different from the Pinakapani murti. He holds an axe and a deer on the upper pair of his arms. In the lower pair of the arms, he holds a bow and an arrow respectively. After destroying Tripura, Tripurantaka Shiva smeared his forehead with three strokes of Ashes. This has become a prominent symbol of Shiva and is practiced even today by Shaivites.Shiva, like some other Hindu deities, is said to have several incarnations, known as Avatars. Although Puranic scriptures contain occasional references to "ansh" avatars of Shiva, the idea is not universally accepted in Saivism.[218] The Linga Purana speaks of twenty-eight forms of Shiva which are sometimes seen as avatars.[219] According to the Svetasvatara Upanishad, he has four avatars.[220]
In the Hanuman Chalisa, Hanuman is identified as the eleventh avatar of Shiva and this belief is universal. Hanuman is popularly known as “Rudraavtaar” “Rudra” being a name of “Shiva”.[221] Rama– the Vishnu avatar is considered by some to be the eleventh avatar of Rudra (Shiva).[222][223]
Other traditions regard the sage Durvasa,[224][225][226][227] the sage Agastya, the philosopher Adi Shankara and Ashwatthama as avatars of Shiva. Other forms of Shiva include Virabhadra and Sharabha.Maha Shivratri is a festival celebrated every year on the 13th night or the 14th day of the new moon in the Shukla Paksha of the month of Maagha or Phalguna in the Hindu calendar. This festival is of utmost importance to the devotees of Lord Shiva. Mahashivaratri marks the night when Lord Shiva performed the 'Tandava' and it is the day that Lord Shiva was married to Parvati.[228] The holiday is often celebrated with special prayers and rituals offered up to Shiva, notably the Abhishek. This ritual, practiced throughout the night, is often performed every three hours with water, milk, yogurt, and honey. Bel (aegle marmelos) leaves are often offered up to the Hindu god, as it is considered necessary for a successful life. The offering of the leaves are considered so important that it is believed that someone who offers them without any intentions will be rewarded greatly.[229]
Buddhism[edit]
Shiva is mentioned in Buddhist Tantra. Shiva as Upaya and Shakti as Prajna.[230] In cosmologies of buddhist tantra, Shiva is depicted as active, skillful, and more passive.[231]
Sikhism[edit]
The Japuji Sahib of the Guru Granth Sahib says, "The Guru is Shiva, the Guru is Vishnu and Brahma; the Guru is Paarvati and Lakhshmi."[232] In the same chapter, it also says, "Shiva speaks, the Siddhas speak."
In Dasam Granth, Guru Gobind Singh have mentioned two avtars of Rudra: Dattatreya Avtar and Parasnath Avtar.[233]
Others[edit]
The worship of Lord Shiva became popular in Central Asia through the Hephthalite (White Hun) Dynasty,[234] and Kushan Empire. Shaivism was also popular in Sogdiana and Eastern Turkestan as found from the wall painting from Penjikent on the river Zervashan.[235] In this depiction, Shiva is portrayed with a sacred halo and a sacred thread ("Yajnopavita").[235] He is clad in tiger skin while his attendants are wearing Sodgian dress.[235] In Eastern Turkestan in the Taklamakan Desert.[235] There is a depiction of his four-legged seated cross-legged n a cushioned seat supported by two bulls.[235] Another panel form Dandan-Uilip shows Shiva in His Trimurti form with His Shakti kneeling on her right thigh.[235][236] It is also noted that Zoroastrian wind god Vayu-Vata took on the iconographic appearance of Shiva.[236]
Kirant people, a Mongol tribe from Nepal, worship a form of Shiva as one of their major deity, identifying him as the lord of animals. It is also said that the physical form of Shiva as a yogi is derived from Kirants as it is mentioned in Mundhum that Shiva took human form as a child of Kirant. He is also said to give Kirants visions in form of a male deer.
In Indonesia, Shiva is also worshiped as Batara Guru. In the ancient times, all kingdoms were located on top of mountains. When he was young, before receiving his authority of power, his name was Sang Hyang Manikmaya. He is first of the children who hatched from the eggs laid by Manuk Patiaraja, wife of god Mulajadi na Bolon. This avatar is also worshiped in Malaysia. Shiva's other form in Indonesian Hinduism is "Maharaja Dewa" (Mahadeva).[237]
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Highest position: 29 on Sunday, September 7, 2008
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Sir Thomas Elder had his main house Birksgate at Urrbrae. From his summer house at Mount Lofty Summit he could overlook Piccadilly Valley and use his telescope to look at his ships at Port Adelaide. He was the main owner and director of the Adelaide Steamship Company in addition to his finance, banking and pastoral interests.
Mount Lofty Summit.
Captain Collet Barker came exploring here and along the Sturt River in 1831. A few weeks later he was killed near Lake Alexandrina. Earlier the summit had been sighted and named by Captain Matthew Flinders when he sailed up the Gulf in 1802. A cairn of stones was erected on the summit in 1865 with a table and chairs for picnickers and a wooden flagstaff. In 1885 the wooden flagstaff was replaced with a stone tower and trig station. 1901 for the centenary of the summit’s naming by Capt. Matthew Flinders the current obelisk was built to honour Flinders. It was unveiled by the Governor Lord Tennyson in March 1902. At 727 metres high the summit is the highest point near Adelaide but there are quite a many peaks higher than this in SA. The summit was purchased by the government in 1945 and added to Cleland Conservation Park. The old 1958 built tearooms at the summit were replaced with the new summit restaurant in 1997.
Mount Lofty House. Arthur Hardy an early pastoralist and vigneron reached SA in 1836. He was a successful colonist and built his first home called Birksgate at Glen Osmond in 1851. This was later sold and was named Claremont. During the 1850s he amassed 1,000 acres near Mt Lofty summit. In 1856 he built a grand summer house near the Summit which he named Mount Lofty House. By 1859 he had planted acres of vines and walnut trees near Mt Lofty House. In 1863 Arthur Hardy moved into Mt Lofty House as his permanent residence. As his fortunes changed he sold Mt Lofty House. It had various owners - Alfred Watts, Frank Stokes, Arthur Waterhouse and J.W Richardson before being almost totally destroyed by the Ash Wednesday Bushfires on 16 February 1983. The ruins were purchased and restored and re-opened in 1986. More accommodation was added in a sympathetic style and it became the Mercure Grand Hotel and restaurant.
Arthur’s seat later the Stawell School. George Tinline, a wealthy pastoralist, investor and manager of the Bank of South Australia from 1839 and brother-in-law of Alexander Borthwick Murray built a cottage on this plot in 1858 before he returned to England in 1863. The unfinished Tinline Court House was sold in 1871 and bought by Gavin Young who employed architects to complete the house in 1875. He named it Arthur’s Seat as the land was originally owned by Arthur Hardy. Later owners included Henry Teesdale Smith before it was purchased in 1926 by Patience Hawker and Mabel Hardy as premises for Stawell School. The school accepted both day and boarding students and the girls were taught to “develop their individuality” through art, literature and music. Traditional subjects of French, Latin, science, history and geography completed the curriculum. The list of girls included some from most of the great pastoral families of SA- Gebhardt, Hawker, Cudmore, Dutton, Bowman, Davenport, Kidman, Melrose, Murray, Robertson etc. In 1927 the school started with 23 pupils but this increased to 40 in the next year. For many the school was both a finishing school and traditional school but with petrol rationing numbers dwindled in 1939 and the school moved from Arthurs Seat to a property in Mills Terrace North Adelaide. The school company ceased operations in 1940. Patience Howard (née Hawker) went on to be the first woman to stand for parliament in SA in 1948 as a Labor Party candidate for the Upper House but she was not successful. When the Stawell School closed in 1940 the property was used as a convalescent home for the Australian Women’s Army Service before it was sold in 1943. It was destroyed in the 1983 Ash Wednesday bushfires but has public access as it is now owned by the SA government.
Eurilla House. Another of the grand Summit houses was built in 1875 for Sir William Milne a local MP and owner of wineries and distilleries. His businesses began at Nairne around 1840 and in 1846 he took over Patrick Auld’s winery at Burnside, now Auldana. In politics he held several ministries including Commissioner of Crown Lands. He helped establish the Torrens land titles system for us. He was also a Director of the Moonta Mining Company. His main home was Sunnyside at Glen Osmond off Portrush Road. In 1917 after his death Eurilla was purchased by Sir Lavington Bonython in 1939. It was destroyed in the 1983 bushfires and has now been rebuilt on a smaller scale.
Korralla House later St Michael’s Monastery. This house became St. Michael’s Monastery in 1946. It was a refuge for the spiritually ill and troubled. Korralla House was bequeathed to the Anglican Church by Audine O’Leary, nee Bakewell upon her death in 1945. Her ancestor John Warren Bakewell bought a cottage when the Hills railway was constructed. He then employed architects Grainger and Naish in 1885 to design an 8 roomed house plus gate house and stables and coach house. In 1901 a ballroom as added. The Bakewell mansion had the finest views of all houses along Summit Road. Korralla means “seen from afar”. John Bakewell, 1845-1922, was a lawyer, businessman, research chemist and author. He had a chemical laboratory built into Korralla House which was used by Sir William Bragg who got a Nobel Prize for physics (work on X-rays) in 1915. In 1946 the Anglican Church offered it to the English Brothers Society of the Sacred Mission which had been founded in England 1894. During World War 2 Korralla House housed American officers on recreation leave with all comforts laid on including visits by professional women! St. Michael’s Monastery, along with its priceless library of 40,000 theology books was destroyed in 1983 on Ash Wednesday.
Carminow House and tower. This mansion was built in 1885 for Sir Thomas Elder. It was built with gas lighting, showers and bathrooms and inside flushing toilets. Later it was owned from 1902 by Sir Langdon Bonython, a proprietor of the Advertiser newspaper. Sir Thomas Elder had his main house called Birksgate at Urrbrae but from his summer house Carminow he could overlook Piccadilly Valley and use his telescope to look at his ships at Port Adelaide. He was the main owner and director of the Adelaide Steamship Company in addition to his finance, banking and pastoral interests. The house was eventually inherited by Kim Bonython. But during World War Two it was used to house up to 120 troops at a time and neighbouring Eurilla housed 80 troops.
The Leadhills & Wanlockhead Railway is Britain's highest adhesion railway, reaching 1498 feet above sea level at Hillend summit, it was originally built in 1900 for the Caledonian Railway Company.
Clyde, Leadhills and Wanlockhead Locomotive No 6 was built by Hunslet Locomotives , Leeds in 1975, as locomotive number HE6347. This Locomotive has a six cylinder water cooled Perkins diesel engine producing sixty horse power to its four wheels via a torque converter and chain drive.
Highest position: #127 on Friday, July 6, 2007
HDR of Trinity Road from Weymouth Town Bridge, about 2pm, Tuesday 2nd January 2007
"Glory to God in the highest; and on earth Peace to men of good will." ~ Luke 2:14
MEDITATION
"...Jesus Christ came to bring us the kingdom of God. He is the true King who offers Peace, Joy, and Everlasting Life for those who accept His kingship. Does the King of glory find a welcome entry in your heart and home? Do your walls echo with the praise of His glory?"
PRAYER
"Lord Jesus Christ, may You always be the King of my heart and the Ruler of my home. Let Your Peace reign in my life that I may find Joy in Your presence now and forever."
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I am Honored to have this Image in use at:
~ jesuslovesmeintlministries.com
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Filename - Glory to God - DSC_0799 Ocean Sunset NR ClEC Orton efct - paint Radiance efct Tint blu Bob Vingette efct 2013
Following the Son...
Blessings,
Sharon 🌻
God's Beauty In Nature is calling us into a deeper relationship with Him...
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Art4TheGlryOfGod Photography by Sharon
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Faith, Hope & Love in daily Art meditations...
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The Alps are the highest and most extensive mountain range system that lies entirely in Europe, separating Southern from Central and Western Europe and stretching approximately 1,200 kilometres across eight Alpine countries: France, Switzerland, Monaco, Italy, Liechtenstein, Austria, Germany, and Slovenia
Titicaca is a large, deep lake in the Andes on the border of Bolivia and Peru, often called the "highest navigable lake" in the world. By volume of water and by surface area, it is the largest lake in South America.
Puno is a city in southeastern Peru, located on the shore of Lake Titicaca. It is the capital city of the Puno Region and the Puno Province with a population of approximately 140,839.
Peru is a country in western South America. It is bordered in the north by Ecuador and Colombia, in the east by Brazil, in the southeast by Bolivia, in the south by Chile, and in the west by the Pacific Ocean.
Peru is a magical destination, abundant with ancient ruins dating back to the Incas.
Peru is the third largest country in South America, after Brazil and Argentina.
We hiked up and then camped on top of Cerro Blano, the most elevated sand dune in the world at 2,078 meters (over 6,800 feet) above sea level. As the sun lowered, I made my way to the very top and used the peak as a leading line to the horizon, which started to light up in a purple glow. Cerro Blanco is also flanked by hundreds of small badland mountains seen thousands of feet below.
-Cerro Blanco in the Sechura Desert, Nazca, Peru
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Wast Water or Wastwater is a lake located in Wasdale, a valley in the western part of the Lake District National Park, England. The lake is almost 3 miles (4.8 km) long and more than one-third mile (500 m) wide. It is a glacial lake, formed in a glacially 'over-deepened' valley. It is the deepest lake in England at 258 feet (79 m). The surface of the lake is about 200 feet (60 m) above sea level, while its bottom is over 50 feet (15 m) below sea level. It is owned by the National Trust.
The head of the Wasdale Valley is surrounded by some of the highest mountains in England, including Scafell Pike, Great Gable and Lingmell. The steep slopes on the southeastern side of the lake, leading up to the summits of Whin Rigg and Illgill Head, are known as the "Wastwater Screes" or on some maps as "The Screes". These screes formed as a result of ice and weathering erosion on the rocks of the Borrowdale Volcanic Group, that form the fells to the east of the lake, towards Eskdale. They are approximately 2,000 feet (600 m), from top to base, the base being about 200 feet (60 m) below the surface of the lake.
A path runs the length of the lake, through the boulders and scree fall at the base of the craggy fell-side. On the northwestern side are the cliffs of Buckbarrow (a part of Seatallan) and the upturned-boat shape of Yewbarrow. Wast Water is the source of the River Irt which flows into the Irish Sea near Ravenglass.
Both the lake and Wasdale Screes are protected as Sites of Special Scientific Interest and under European Union law as Special Areas of Conservation.
"Wastwater" comes from "Wasdale" plus English "water". " 'Wasdale lake' or 'the lake of Vatnsá, lake river'. The present name rather curiously contains the reflexes of both Old Norse 'vatn' 'water', 'lake', and Old English 'wæter' 'water', with the meaning 'lake' probably influenced by the Old Norse 'vatn'.
The valley is pronounced as in was, not with a hard a: the name of the lake similarly but with a soft "s" as in "thou wast". The lake is named "Wast Water" on Ordnance Survey maps but "Wastwater" is used with roughly equal frequency, including by its owner, the National Trust, along with the Cumbria Tourist Board, and the Lake District National Park Authority.
In 1976, The Wasdale Lady in the Lake, Margaret Hogg, was murdered by her husband and her body was disposed of in the lake. She was found after eight years, with her body preserved like wax due to the lack of oxygen in the water.
In February 2005 it was reported that a "gnome garden" complete with picket fence had been placed in the lake as a point of interest for divers to explore. It was removed from the bottom of Wastwater after three divers died in the late 1990s. It is thought the divers spent too much time too deep searching for the ornaments. Police divers report a rumour that the garden had been replaced at a depth beyond the lowest the police were allowed to dive.
PC Kenny McMahon, a member of the North West Police Underwater Search Unit, said
Wastwater is quite clear at the bottom, but there's nothing to see. At a depth of about 48 m [157 ft], divers had taken gnomes down and put a picket fence around them. But several years ago there were a number of fatalities and the Lake District National Park Authority asked us to get rid of them. We went down there, put them in bags and removed the lot. But now there's a rumour about a new garden beyond the 50 m [160 ft] depth limit. As police divers we can't legally dive any deeper so, if it exists, the new garden could have been purposefully put out of our reach.
Water was first pumped from the lake during World War II to supply the Royal Ordnance Factory at Drigg. It is pumped to the nearby Sellafield nuclear facility as an industrial water supply. The Nuclear Decommissioning Authority is allowed to extract from the lake a maximum of 4,000,000 imperial gallons (18,000 m3) a day to use on that site.
On 9 September 2007, Wast Water was announced as the winner of a vote to determine "Britain's Favourite View" by viewers of ITV.
The Lake District, also known as the Lakes or Lakeland, is a mountainous region and national park in Cumbria, North West England. It is primarily famous for the Cumbrian Mountains, its lake and coastal scenery, and for its literary associations with William Wordsworth and other Lake Poets, Beatrix Potter, and John Ruskin.
The Cumbrian mountains, or fells, include England's tallest mountains: Scafell Pike (978 m (3,209 ft)), Helvellyn (950 m (3,120 ft)), Skiddaw (931 m (3,054 ft)), and Cross Fell (893 m (2,930 ft)), which all have a topographical prominence of more than 600m. The region contains sixteen major lakes. They include Windermere, which with a length of 18 km (11 miles) and an area of 14.73 km2 (5.69 square miles) is both the longest and largest lake in England, and Wast Water, which at 79 metres (259 ft) is the deepest lake in England.
The Lake District National Park was established in 1951, and covers an area of 2,362 km2 (912 square miles), the bulk of the region. It was designated a UNESCO World Heritage Site in 2017.
National Park
The Lake District National Park includes all of the central Lake District, though the town of Kendal, some coastal areas, and the Lakeland Peninsulas are outside the park boundary. The area was designated a national park on 9 May 1951, a month after the Peak District, the first UK national park. It retained its original boundaries until 2016 when it was extended by 3% in the direction of the Yorkshire Dales National Park to incorporate areas land of high landscape value around the Lune Valley.
The national park received 18.14 million tourist visitors in 2022. This equates to 29.15 million tourist days, counting visits of greater than three hours. It is the largest of the thirteen national parks in England and Wales and the second largest in the UK after the Cairngorms National Park. Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. The area of the national park, with the exception of the 2016 extension, was designated a World Heritage Site in 2017 as a cultural landscape. This was the fourth attempt to list the park, after two attempts in the 1980s and one in 2012 failed.
The park is governed by the National Park Authority, which is based at offices in Kendal. It runs a visitor centre on Windermere at a former country house called Brockhole, Coniston Boating Centre, and Information Centres. The Park Authority has 20 members: six appointed by Westmorland and Furness Council, four by Cumberland Council, and ten by the Secretary of State for Environment, Food, and Rural Affairs.
Human geography
The precise extent of the Lake District was not defined traditionally, but is slightly larger than that of the National Park[citation needed], the total area of which is about 2,362 square kilometres (912 sq mi). The park extends just over 51 kilometres (32 mi) from east to west and nearly 64 kilometres (40 mi) from north to south, with areas such as the Lake District Peninsulas to the south lying outside the National Park.
Settlement
There are only a few major settlements within this mountainous area: the towns of Keswick, Windermere, Ambleside, and Bowness-on-Windermere are the four largest. Significant settlements close to the boundary of the national park include Carlisle, Barrow-in-Furness, Kendal, Ulverston, Dalton-in-Furness, Whitehaven, Workington, Cockermouth, Penrith, Millom and Grange-over-Sands; each of these has important economic links with the area. Other villages are Coniston, Threlkeld, Glenridding, Pooley Bridge, Broughton-in-Furness, Grasmere, Newby Bridge, Staveley, Lindale, Gosforth and Hawkshead. The economies of almost all are intimately linked with tourism. Beyond these are a scattering of hamlets and many isolated farmsteads, some of which are still tied to agriculture;[citation needed] others now function as part of the tourist economy.
Communications
Roads
The Lake District is very nearly contained within a box of trunk routes and major A roads. It is flanked to the east by the A6 road, which runs from Kendal to Penrith (though the National Park extension approved in 2015 is east of the A6); across its southern fringes by the A590, which connects the M6 to Barrow-in-Furness, and the A5092, and across its northern edge by the A66 trunk road between Penrith and Workington. The A595 (linking the A66 with the A5092) forms the park boundary from Calder Bridge to Holmrook, then crosses the coastal plain of the park until turning inland at the Whicham Valley, forming much of the park boundary again until joining the A5092 at Grizebeck.
Besides these, a few A roads penetrate the area itself, notably the A591 which runs north-westwards from Kendal to Windermere and then on to Keswick. It continues up the east side of Bassenthwaite Lake. "The A591, Grasmere, Lake District" was short-listed in the 2011 Google Street View awards in the Most Romantic Street category. The A593 and A5084 link the Ambleside and Coniston areas with the A590 to the south whilst the A592 and A5074 similarly link Windermere with the A590. The A592 also continues northwards from Windermere to Ullswater and Penrith by way of the Kirkstone Pass.
Some valleys which are not penetrated by A roads are served by B roads. The B5289 serves Lorton Vale and Buttermere and links via the Honister Pass with Borrowdale. The B5292 ascends the Whinlatter Pass from Lorton Vale before dropping down to Braithwaite near Keswick. The B5322 serves the valley of St John's in the Vale whilst Great Langdale is served by the B5343. Other valleys such as Little Langdale, Eskdale and Dunnerdale are served by minor roads. The last of these is connected with the first two by the Wrynose and Hardknott passes respectively; both of these passes are known for their steep gradients and are together one of the most popular climbs in the United Kingdom for cycling enthusiasts. A minor road through the Newlands Valley connects via Newlands Hause with the B5289 at Buttermere. Wasdale is served by a cul-de-sac minor road,[a] as is Longsleddale and the valleys at Haweswater and Kentmere. There are networks of minor roads in the lower-lying southern part of the area, connecting numerous communities between Kendal, Windermere, and Coniston.
Railways and ferries
The West Coast Main Line skirts the eastern edge of the Lake District and the Cumbrian Coast Line passes through the southern and western fringes of the area. A single railway line, the Windermere Branch Line, penetrates from Kendal to Windermere via Staveley. Railways once served Broughton-in-Furness and Coniston (closed to passengers in 1958) and another ran from Penrith to Cockermouth via Keswick (closed west of Keswick in 1966 and completely in 1972). Part of the track of the latter is used by the improved A66 trunk road.
The Cumbrian Coast line has three stations within the boundaries of the national park (and additionally Drigg, about a third of a mile from the park boundary). The line gives railway enthusiasts and others a flavour of a pre-Beeching railway line, with features like manually operated level crossing gates, as well as giving a good connection to the steam railway into Eskdale and providing access for cyclists and serious walkers to the Western Fells.
The narrow gauge Ravenglass and Eskdale Railway runs from Ravenglass on the west coast up Eskdale as far as Dalegarth Station near the hamlet of Boot, catering for tourists. Another heritage railway, the Lakeside and Haverthwaite Railway, runs between Lake Windermere and Haverthwaite, and tourists can connect at Lakeside with the boats up the lake to Bowness.
A vehicle-carrying cable ferry, the Windermere Ferry, runs frequent services across Windermere. There are also seasonal passenger boats on Coniston Water, Derwent Water, and Ullswater.
Footpaths and bridleways
There are many paths over which the public has a right of way, all of which are signposted at their origin on public roads and at some other points. Within the area of the National Park in 2012 there were 2,159 km (1,342 mi) of public footpaths, 875 km (544 mi) of public bridleways, 15 km (9 mi) of restricted byways and 30 km (19 mi) of byways open to all traffic. There is also a general "right to roam" in open country, which includes approximately 50% of the national park.
Many of these tracks arose centuries ago and were used either as ridge highways (such as along High Street) or as passes for travelling across the ridges between settlements in the valleys. Historically these paths were not planned for reaching summits, but more recently they are used by fell walkers for that purpose. The Coast to Coast Walk, which crosses the north of England from the Irish Sea to the North Sea, traverses the national park from west to east.
Bridleways are intended for horse riding and walkers, with cyclists also permitted to use them. Cyclists must give way to all other bridleway users. Motor vehicles are only allowed on "byways open to all traffic" (green lanes) but in practice Traffic Regulation Orders have been brought in on several prohibiting motor traffic, although a system of permits operates on Gatesgarth Pass.
Land ownership
Most of the land within the national park is in private ownership, with about 55% registered as agricultural land. Landowners include:
Individual farmers and other private landowners, with more than half of the agricultural land farmed by the owners.
The National Trust owns around 25% of the total area (including some lakes and land of significant landscape value).
The Forestry Commission and other investors in forests and woodland.
United Utilities (owns 8%)
Lake District National Park Authority (owns 3.9%)
Physical geography
The Lake District is a roughly circular upland massif, deeply dissected by a broadly radial pattern of major valleys which are largely the result of repeated glaciations over the last 2 million years. The apparent radial pattern is not from a central dome, but from an axial watershed extending from St Bees Head in the west to Shap in the east. Most of these valleys display the U-shaped cross-section characteristic of glacial origin and often contain long narrow lakes in bedrock hollows, with tracts of relatively flat ground at their infilled heads, or where they are divided by lateral tributaries (Buttermere-Crummock Water; Derwent Water-Bassenthwaite Lake).[b] Smaller lakes known as tarns occupy glacial cirques at higher elevations. It is the abundance of both which has led to the area becoming known as the Lake District.
Many of the higher fells are rocky, while moorland predominates lower down. Vegetation cover in better-drained areas includes bracken and heather, although much of the land is boggy, due to the high rainfall. Deciduous native woodland occurs on many of the steeper slopes below the tree line, but with native oak supplemented by extensive conifer plantations in many areas, particularly Grizedale Forest in the generally lower southern part of the area. The Lake District extends to the sea to the west and south.
The highest mountain in England, Scafell Pike (978m/3210'), has a far-reaching view on a clear day, ranging from the Galloway Hills of Scotland, the Mourne Mountains in Northern Ireland, the Isle of Man, and Snowdonia in Wales.
Cumbrian Mountains
Lake District is located in the Lake DistrictScafell PikeScafell PikeScafellScafellScafellScafellHelvellynHelvellynSkiddawSkiddawHigh StreetHigh StreetGrasmoorGrasmoorConiston Old ManConiston Old ManGreat GableGreat GableKendalKendalPenrithPenrithKeswickKeswickAmblesideAmblesideCockermouthCockermouthWindermereWindermereGrasmereGrasmere
Major fells and towns shown within the National Park
Lake District
The mountains (or 'fells') of the Lake District are known as the "Cumbrian Mountains", "Cumbrian Fells" or "Lakeland Fells". The four highest fells exceed 3,000 feet (914 m). These are:
Scafell Pike, 978 m (3,209 ft)
Scafell, 965 m (3,166 ft)
Helvellyn, 951 m (3,120 ft)
Skiddaw, 931 m (3,054 ft)
Northern Fells
The Northern Fells are a clearly defined range of hills contained within a 13 km (8 mi) diameter circle between Keswick in the southwest and Caldbeck in the northeast. They culminate in the 931 m (3,054 ft) peak of Skiddaw. Other notable peaks are Blencathra (also known as Saddleback) (868 m (2,848 ft)) and Carrock Fell. Bassenthwaite Lake occupies the valley between this massif and the North Western Fells.
North Western Fells
The North Western Fells lie between Borrowdale and Bassenthwaite Lake to the east and Buttermere and Lorton Vale to the west. Their southernmost point is at Honister Pass. This area includes the Derwent Fells above the Newlands Valley and hills to the north amongst which are Dale Head, Robinson. To the north stand Grasmoor, highest in the range at 852 m (2,795 ft), Grisedale Pike and the hills around the valley of Coledale, and in the far northwest is Thornthwaite Forest and Lord's Seat. The fells in this area are rounded Skiddaw slate, with few tarns and relatively few rock faces.
Western Fells
The Western Fells lie between Buttermere and Wasdale, with Sty Head forming the apex of a large triangle. Ennerdale bisects the area, which consists of the High Stile ridge north of Ennerdale, the Loweswater Fells in the far northwest, the Pillar group in the southwest, and Great Gable (899 m (2,949 ft)) near Sty Head. Other tops include Seatallan, Haystacks and Kirk Fell. This area is craggy and steep, with the impressive pinnacle of Pillar Rock its showpiece. Wastwater, located in this part, is England's deepest lake.
Central Fells
The Central Fells are lower in elevation than surrounding areas of fell, peaking at 762 m (2,500 ft) at High Raise. They take the form of a ridge running between Derwent Water in the west and Thirlmere in the east, from Keswick in the north to Langdale Pikes in the south. A spur extends southeast to Loughrigg Fell above Ambleside. The central ridge running north over High Seat is exceptionally boggy.
Eastern Fells
The Eastern Fells consist of a long north-to-south ridge, the Helvellyn range, running from Clough Head to Seat Sandal with the 950 m (3,118 ft) Helvellyn at its highest point. The western slopes of these summits tend to be grassy, with rocky corries and crags on the eastern side. The Fairfield group lies to the south of the range and forms a similar pattern with towering rock faces and hidden valleys spilling into the Patterdale valley. It culminates in the height of Red Screes overlooking the Kirkstone Pass.
Far Eastern Fells
The Far Eastern Fells refers to all of the Lakeland fells to the east of Ullswater and the A592 road running south to Windermere. At 828 m (2,717 ft), the peak known as High Street is the highest point on a complex ridge that runs broadly north-south and overlooks the hidden valley of Haweswater to its east. In the north of this region are the lower fells of Martindale Common and Bampton Common whilst in the south are the fells overlooking the Kentmere valley. Further to the east, beyond Mardale and Longsleddale is Shap Fell, an extensive area consisting of high moorland, more rolling and Pennine in nature than the mountains to the west.
Southern Fells
The Southern Fells occupy the southwestern quarter of the Lake District. They can be regarded as comprising a northern grouping between Wasdale, Eskdale, and the two Langdale valleys, a southeastern group east of Dunnerdale and south of Little Langdale, and a southwestern group bounded by Eskdale to the north and Dunnerdale to the east.
The first group includes England's highest mountains: Scafell Pike in the centre, at 978 m (3,209 ft) and Scafell one mile (1.6 km) to the southwest. Though it is slightly lower, Scafell has a 700 ft (210 m) rockface, Scafell Crag, on its northern side. This group also includes the Wastwater Screes overlooking Wasdale, the Glaramara ridge overlooking Borrowdale, the three tops of Crinkle Crags, Bowfell and Esk Pike. The core of the area is drained by the infant River Esk. Collectively these are some of the Lake District's most rugged hillsides.
The second group, otherwise known as the Furness Fells or Coniston Fells, have as their northern boundary the steep and narrow Hardknott and Wrynose passes. The highest are Old Man of Coniston and Swirl How which slightly exceed 800 m (2,600 ft).
The third group to the west of the Duddon includes Harter Fell and the long ridge leading over Whitfell to Black Combe and the sea. The south of this region consists of lower forests and knolls, with Kirkby Moor on the southern boundary. The southwestern Lake District ends near the Furness peninsula and Barrow-in-Furness, a town which many Lake District residents rely on for basic amenities.
Southeastern area
The southeastern area is the territory between Coniston Water and Windermere and east of Windermere towards Kendal and south to Lindale. There are no high summits in this area which are mainly low hills, knolls and limestone cuestas such as Gummer's How and Whitbarrow. Indeed, it rises only as high as 333 m (1,093 ft) at Top o' Selside east of Coniston Water; the wide expanse of Grizedale Forest stands between the two lakes. Kendal and Morecambe Bay stand at the eastern and southern edges of the area.
Valleys
The main radial valleys are (clockwise from the south) Dunnerdale, Eskdale, Wasdale, Ennerdale, the Vale of Lorton, and Buttermere valley, the Derwent Valley and Borrowdale, the Ullswater valley, Haweswater valley, Longsleddale, the Kentmere valley, those converging on the head of Windermere - Grasmere, Great Langdale and Little Langdale, and the Coniston Water valley. The valleys break the mountains up into blocks, which have been described by various authors in different ways. The most frequently encountered approach is that made popular by Alfred Wainwright who published seven separate area guides to the Lakeland Fells.
Only one of the lakes in the Lake District is called by that name, Bassenthwaite Lake. All the others such as Windermere, Coniston Water, Ullswater and Buttermere are meres, tarns and waters, with mere being the least common and water being the most common. The major lakes and reservoirs in the National Park are given below.
Bassenthwaite Lake
Brotherswater
Buttermere
Coniston Water
Crummock Water
Derwent Water
Devoke Water
Elter Water
Ennerdale Water
Esthwaite Water
Grasmere
Haweswater Reservoir
Hayeswater
Loweswater
Rydal Water
Thirlmere
Ullswater
Wast Water
Windermere
Woodlands
Below the tree line are wooded areas, including British and European native oak woodlands and introduced softwood plantations. The woodlands provide habitats for native English wildlife. The native red squirrel is found in the Lake District and a few other parts of England. In parts of the Lake District, the rainfall is higher than in any other part of England. This gives Atlantic mosses, ferns, lichen, and liverworts the chance to grow. There is some ancient woodland in the National Park. Management of the woodlands varies: some are coppiced, some pollarded, some left to grow naturally, and some provide grazing and shelter.
Coast
The Lake District extends to the coast of the Irish Sea from Drigg in the north to Silecroft in the south, encompassing the estuaries of the Esk and its tributaries, the Irt and the Mite. The intertidal zone of the combined estuaries includes sand, shingle and mudflats, and saltmarsh. The dune systems on either side of the estuary are protected as nature reserves; Drigg Dunes and Gullery to the north and Eskmeals Dunes[31] to the south. South of the estuary, the coast is formed in low cliffs of glacial till, sands, and gravels.
The district also extends to the tidal waters of Morecambe Bay and several of its estuaries alongside the Furness and Cartmel Peninsulas, designated on M6 motorway signposts as the "Lake District Peninsulas", and the southern portions of which lie outside the park. These are the Duddon Estuary, the Leven Estuary, and the western banks and tidal flats of the Kent Estuary. These areas are each characterised by sand and mudflats of scenic and wildlife interest. The coast is backed by extensive flats of raised marine deposits left when the relative sea level was higher.
Spotted not far from the Olympic Museum in Lausanne, this Portuguese Ducato! This is my highest Portuguese plate, on the road since this month only!
Distance from home: 1920 km.
Highest Explore Position #257 ~ On August Thirteenth 2008.
Chipmunk - Wingham Wildlife Park, Kent, England - Sunday August 10th 2008.
Click here to see the Larger image
Eastern American chipmunks are found in forests, but also in suburban gardens and city parks, as long as there are rocks, stumps, or fallen logs to provide perching sites and cover for burrow entrances. They dig complex burrows with many entrances and chambers as well as short escape tunnels, and each chipmunk defends a small area around its burrow, threatening, chasing, and even fighting with a neighbor who invades the space. The chipmunks spend the winter underground, but venture to the surface occasionally on mild, sunny days. They enter torpor for a few days at a time, and then arouse to feed on stored nuts and seeds. Life expectancy in the wild is slightly more than a year.
You can tell the chipmunk from any other mammal by the two white and three dark racing stripes across the eyes on both sides of this small mammal's face. Look for a small sprightly ground squirrel about the size of an orange, with a small stocky and muscular body, a white underbelly and a furry tail. Chipmunks are fun to watch because they are always busily looking around, searching for food, or carrying food in their large cheek pouches to store somewhere for later. Look for this rodent's tell-tail scurrying - quick as a flash - low to the ground with their tail up and flickering like a flag. Don't confuse the chipmunk with the 13-lined ground squirrel. They are always alert and ready to take action from predators like hawks, owls, weasels, mink, red fox, cats and people.
Sometimes called "chipppie" or "chipping squirrel" because of its calls that are easy to recognize - listen for a low "chuck-chuck-chuck" or a higher pitched "chit-chit-chit-chit" when it is in danger or you are nearby.
In the winter, chipmunks partially hibernate, sometimes sleeping for weeks in November, but they also wake to eat or go leave the burrow and go outside.
Chipmunks often leave behind leftover piles of fruit pulp and pieces of shell from nuts they ate from nearby trees.
This "big chipmunk" has a 5 ½-6 ½ inch body with a tail of 4 1/2 inches. It is larger than the Least chipmunk. The fur is a rusty brown color on the back and sides, with a white underbelly and necklace. The stripes on this chipmunk's sides and back stop at the rump. You'll find this critter living anywhere in Wisconsin with forests, brushy areas, and gardens. It likes rock piles & fences, and building foundations.
The eastern chipmunk lives in open hardwood forests, brushy or rocky areas, and yards. It eats mostly seeds, fruits and nuts of woody plants (acorns from oaks, samaras from maples, and a variety of berries). Sometimes it will eat insects like cicadas and grasshoppers, bird eggs, snails, small snakes, and garden bulbs.
When not scurrying around, it lives in underground burrows that may be short and simple, or very complex with many rooms for storage, sleeping, a dump, a latrine, and many hidden entrances. Some burrows even have a pantry that can store up to one half of a bushel of nuts and other food that can be carried in its cheeks! Have you ever heard the term "chipmunk cheeks?"
The females give birth to their litter of young midsummer, with four or five young. The babies are born hairless, blind and helpless.
Sexual Dimorphism: None
Length: Average: 255 mm ~ Range: 215-285 mm
Weight: Average: 130 g ~ Range: 80-150 g
Spotted at Montreux main station, this Portuguese plate! I usually don't take pictures of Portuguese plates, as there are many of them in Switzerland (there is a strong Portuguese community in Switzerland), but this one is my personnal highest!
Distance from home: 1935 km.
From Wikipedia, the free encyclopedia
Devils Tower
Matȟó Thípila (Lakota)
Devils Tower, 2017
Highest point
Elevation 5,112 ft (1,558 m) NAVD 88[1]
Coordinates 44°35′25″N 104°42′55″WCoordinates: 44°35′25″N 104°42′55″W [2]
Geography
Location Crook County, Wyoming, United States
Parent range Bear Lodge Mountains, part of the Black Hills
Topo map USGS Devils Tower
Geology
Mountain type Laccolith
Climbing
First ascent William Rogers and Willard Ripley, July 4, 1893
Easiest route Durrance Route
Devils Tower National Monument
IUCN category III (natural monument or feature)
Map showing the location of Devils Tower National Monument
Map showing the location of Devils Tower National Monument
Location in the United States
Nearest city Hulett, Wyoming
Coordinates 44°35′26″N 104°43′0″W
Area 1,346 acres (5.45 km2)[3]
Established September 24, 1906[4]
Visitors 496,210 (in 2016)[5]
Governing body National Park Service
Website Devils Tower National Monument
Devils Tower (also Bear Lodge Butte[6]) is a laccolithic butte composed of igneous rock in the Bear Lodge Mountains (part of the Black Hills) near Hulett and Sundance in Crook County, northeastern Wyoming, above the Belle Fourche River. It rises dramatically 1,267 feet (386 m) above the Belle Fourche River, standing 867 feet (265 m) from summit to base. The summit is 5,112 feet (1,559 m) above sea level.
Devils Tower was the first declared United States National Monument, established on September 24, 1906, by President Theodore Roosevelt. The monument's boundary encloses an area of 1,347 acres (545 ha).
In recent years, about 1% of the monument's 400,000 annual visitors climbed Devils Tower, mostly using traditional climbing techniques.[7]
Name
Devils Tower, 1900
The name Devil's Tower originated in 1875 during an expedition led by Colonel Richard Irving Dodge, when his interpreter reportedly misinterpreted a native name to mean "Bad God's Tower".[8] All information signs in that area use the name "Devils Tower", following a geographic naming standard whereby the apostrophe is eliminated.[9]
Native American names for the monolith include: "Bear's House" or "Bear's Lodge" (or "Bear's Tipi", "Home of the Bear", "Bear's Lair"; Cheyenne, Lakota Matȟó Thípila, Crow Daxpitcheeaasáao "Home of Bears"[10]), "Aloft on a Rock" (Kiowa), "Tree Rock", "Great Gray Horn",[8] and "Brown Buffalo Horn" (Lakota Ptehé Ǧí).[citation needed]
In 2005, a proposal to recognize several Native American ties through the additional designation of the monolith as Bear Lodge National Historic Landmark met with opposition from United States Representative Barbara Cubin, arguing that a "name change will harm the tourist trade and bring economic hardship to area communities".[11] In November 2014, one Arvol Looking Horse again proposed renaming the geographical feature "Bear Lodge", and submitted the request to the United States Board on Geographic Names. A second proposal was submitted to request that the U.S. acknowledge the "offensive" mistake in keeping the current name and to rename the monument and sacred site Bear Lodge National Historic Landmark. The formal public comment period ended in fall 2015. Local state senator Ogden Driskill opposed the change.[12][13] The name was not changed.[14][not in citation given]
Geological history
Red sandstone and siltstone cliffs above the Belle Fourche River
Map of Wyoming National Parks and landmarks, showing Devils Tower (upper right) far east of Yellowstone (upper left), north across the state from Cheyenne.
The landscape surrounding Devils Tower is composed mostly of sedimentary rocks. The oldest rocks visible in Devils Tower National Monument were laid down in a shallow sea during the mid- to late-Triassic period, 225 to 195 million years ago. This dark red sandstone and maroon siltstone, interbedded with shale, can be seen along the Belle Fourche River. Oxidation of iron minerals causes the redness of the rocks. This rock layer is known as the Spearfish Formation.
Above the Spearfish Formation is a thin band of white gypsum, called the Gypsum Springs Formation. This layer of gypsum was deposited during the Jurassic period, 195 to 136 million years ago.
Created as sea levels and climates repeatedly changed, gray-green shales (deposited in low-oxygen environments such as marshes) were interbedded with fine-grained sandstones, limestones, and sometimes thin beds of red mudstone. This composition, called the Stockade Beaver member, is part of the Sundance Formation. The Hulett Sandstone member, also part of the Sundance Formation, is composed of yellow fine-grained sandstone. Resistant to weathering, it forms the nearly vertical cliffs that encircle the Tower.
During the Paleocene Epoch, 56 to 66 million years ago, the Rocky Mountains and the Black Hills were uplifted. Magma rose through the crust, intruding into the existing sedimentary rock layers.[15]
Theories of formation
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Phonolite porphyry, the rock type of which Devils Tower is made
Close-up of the columns
Geologists Carpenter and Russell studied Devils Tower in the late 19th century and came to the conclusion that it was formed by an igneous intrusion. Modern geologists agree that it was formed by the intrusion of igneous material, but not on exactly how that process took place. Several believe the molten rock comprising the Tower might not have surfaced; others are convinced the tower is all that remains of what once was a large explosive volcano.
In 1907, scientists Darton and O'Hara decided that Devils Tower must be an eroded remnant of a laccolith. A laccolith is a large mass of igneous rock which is intruded through sedimentary rock beds without reaching the surface, but makes a rounded bulge in the sedimentary layers above. This theory was quite popular in the early 20th century, since numerous studies had earlier been done on laccoliths in the Southwest.
Other theories have suggested that Devils Tower is a volcanic plug or that it is the neck of an extinct volcano. Presumably, if Devils Tower is a volcanic plug, any volcanics created by it — volcanic ash, lava flows, volcanic debris — would have been eroded away long ago. Some pyroclastic material of the same age as Devils Tower has been identified elsewhere in Wyoming.
The igneous material that forms the Tower is a phonolite porphyry intruded about 40.5 million years ago,[16] a light to dark-gray or greenish-gray igneous rock with conspicuous crystals of white feldspar.[17] As the magma cooled, hexagonal (and sometimes 4-, 5-, and 7-sided) columns formed, each about six feet in diameter. As the rock continued to cool, the vertical columns shrank in cross-section (horizontally) and cracks began to occur at 120-degree angles, generally forming compact 6-sided columns. The nearby Missouri Buttes, 3.5 miles (5.6 km) to the northwest of Devils Tower, are also composed of columnar phonolite of the same age. Devils Postpile National Monument in California and Giant's Causeway in Northern Ireland, are also columnar basalt, which are superficially similar, but with columns typically 2 feet (0.61 m) diameter.
Devils Tower did not visibly protrude out of the landscape until the overlying sedimentary rocks eroded away. As the elements wore down the softer sandstones and shales, the more resistant igneous rock making up the tower survived the erosional forces. As a result, the gray columns of Devils Tower began to appear as an isolated mass above the landscape.
As rain and snow continue to erode the sedimentary rocks surrounding the Tower's base, more of Devils Tower will be exposed. Nonetheless, the exposed portions of the Tower still experience certain amounts of erosion. Cracks along the columns are subject to water and ice erosion. Erosion due to the expansion of ice along cracks and fractures within rock formations is common in colder climates, a prime example being the featured formations at Bryce Canyon National Park. Portions, or even entire columns, of rock at Devils Tower are continually breaking off and falling. Piles of broken columns, boulders, small rocks, and stones, called scree, lie at the base of the tower, indicating that it was once wider than it is today.[15]
Native American culture
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A sign informs visitors of the Native American heritage.
According to the Native American tribes of the Kiowa and Lakota, a group of girls went out to play and were spotted by several giant bears, who began to chase them. In an effort to escape the bears, the girls climbed atop a rock, fell to their knees, and prayed to the Great Spirit to save them. Hearing their prayers, the Great Spirit made the rock rise from the ground towards the heavens so that the bears could not reach the girls. The bears, in an effort to climb the rock, left deep claw marks in the sides, which had become too steep to climb. Those are the marks which appear today on the sides of Devils Tower. When the girls reached the sky, they were turned into the stars of the Pleiades.
Another version tells that two Sioux boys wandered far from their village when Mato the bear, a huge creature that had claws the size of tipi poles, spotted them, and wanted to eat them for breakfast. He was almost upon them when the boys prayed to Wakan Tanka the Creator to help them. They rose up on a huge rock, while Mato tried to get up from every side, leaving huge scratch marks as he did. Finally, he sauntered off, disappointed and discouraged. The bear came to rest east of the Black Hills at what is now Bear Butte. Wanblee, the eagle, helped the boys off the rock and back to their village. A painting depicting this legend by artist Herbert A. Collins hangs over the fireplace in the visitor's center at Devils Tower.
In a Cheyenne version of the story, the giant bear pursues the girls and kills most of them. Two sisters escape back to their home with the bear still tracking them. They tell two boys that the bear can only be killed with an arrow shot through the underside of its foot. The boys have the sisters lead the bear to Devils Tower and trick it into thinking they have climbed the rock. The boys attempt to shoot the bear through the foot while it repeatedly attempts to climb up and slides back down leaving more claw marks each time. The bear was finally scared off when an arrow came very close to its left foot. This last arrow continued to go up and never came down.[18]
Wooden Leg, a Northern Cheyenne, relates another legend told to him by an old man as they were traveling together past the Devils Tower around 1866–1868. An Indian man decided to sleep at the base of Bear Lodge next to a buffalo head. In the morning he found that both he and the buffalo head had been transported to the top of the rock by the Great Medicine with no way down. He spent another day and night on the rock with no food or water. After he had prayed all day and then gone to sleep, he awoke to find that the Great Medicine had brought him back down to the ground, but left the buffalo head at the top near the edge. Wooden Leg maintains that the buffalo head was clearly visible through the old man's spyglass. At the time, the tower had never been climbed and a buffalo head at the top was otherwise inexplicable.[19]
The buffalo head gives this story special significance for the Northern Cheyenne. All the Cheyenne maintained in their camps a sacred teepee to the Great Medicine containing the tribal sacred objects. In the case of the Northern Cheyenne, the sacred object was a buffalo head.[20]
Recent history
Ponderosa pine forest east of Devils Tower
Fur trappers may have visited Devils Tower, but they left no written evidence of having done so. The first documented Caucasian visitors were several members of Captain William F. Raynolds' 1859 expedition to Yellowstone. Sixteen years later, Colonel Richard I. Dodge escorted an Office of Indian Affairs scientific survey party to the massive rock formation and coined the name Devils Tower.[21] Recognizing its unique characteristics, the United States Congress designated the area a U.S. forest reserve in 1892 and in 1906 Devils Tower became the nation's first National Monument.[22]
The 1977 movie Close Encounters of the Third Kind used the formation as a plot element and as the location of its climactic scenes.[23][24] Its release was the cause of a large increase in visitors and climbers to the monument.[25]
Climbing
Main article: Durrance Route
Old climbing ladder on Devil's Tower
In recent years, climbing Devils Tower has increased in popularity. The first known ascent of Devils Tower by any method occurred on July 4, 1893, and is accredited to William Rogers and Willard Ripley, local ranchers in the area. They completed this first ascent after constructing a ladder of wooden pegs driven into cracks in the rock face. A few of these wooden pegs are still intact and are visible on the tower when hiking along the 1.3-mile (2.1 km) Tower Trail at Devils Tower National Monument. Over the following thirty years many climbs were made using this method before the ladder fell into disrepair. The man most famous for climbing the tower is Fritz Wiessner, who summited with William P. House and Lawrence Coveney in 1937. This was the first ascent using modern climbing techniques. Wiessner led the entire climb free, placing only a single piece of fixed gear, a piton, which he later regretted, deeming it unnecessary.
In 1941 George Hopkins parachuted onto Devils Tower, without permission, as a publicity stunt resulting from a bet. He had intended to descend by a 1,000 ft (300 m) rope dropped to him after successfully landing on the butte, but the package containing the rope, a sledge hammer and a car axle to be driven into the rock as an anchor point slid over the edge. As the weather deteriorated, a second attempt was made to drop equipment, but Hopkins deemed it unusable after the rope became snarled and frozen due to the rain and wind. Hopkins was stranded for six days, exposed to cold, rain and 50 mph (80 km/h) winds before a mountain rescue team led by Jack Durrance, who had successfully climbed Devils Tower in 1938, finally reached him and brought him down.[26][27] His entrapment and subsequent rescue was widely covered by the media of the time.[28]
Today, hundreds of climbers scale the sheer rock walls of Devils Tower each summer. The most common route is the Durrance Route, which was the second free route established in 1938. There are many established and documented climbing routes covering every side of the tower, ascending the various vertical cracks and columns of the rock. The difficulty of these routes range from relatively easy to some of the most challenging in the world. All climbers are required to register with a park ranger before and after attempting a climb. No overnight camping at the summit is allowed; climbers return to base on the same day they ascend.[29]
The Tower is sacred to several Plains tribes, including the Lakota, Cheyenne and Kiowa. Because of this, many Indian leaders objected to climbers ascending the monument, considering this to be a desecration. The climbers argued that they had a right to climb the Tower, since it is on federal land. A compromise was eventually reached with a voluntary climbing ban during the month of June when the tribes are conducting ceremonies around the monument. Climbers are asked, but not required, to stay off the Tower in June. According to the PBS documentary In the Light of Reverence, approximately 85% of climbers honor the ban and voluntarily choose not to climb the Tower during the month of June. However, several climbers along with the Mountain States Legal Foundation sued the Park Service, claiming an inappropriate government entanglement with religion.[30]
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EXPLORE : April 15, 2008 # 92
(Highest position)
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And when just the two of us are there...
You won't have to ask if I still care...
Cause as the time turns the page..
My LOVE won't age at all...
You are in my though....
You are in my days.....
And in my HEART always....my Dearest!!
Have a sweet dream tonight...
I will always send you nice sunshine, sweet smile and warm love from Thailand, my Dearest...
Ich liebe dich..I LOVE YOU now and Forever...
J-A-S-M-I-N-E...
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DATA: www.ancientcity.com
The Phanom Rung Sanctuary, Buri Ram
The Phanom Rung Stone Sanctuary is located in Buri Ram Province, on an extinct volcano. Built in accordance with Hinduism beliefs of the Shiva sect, the sanctuary had been constructed and used as a religious center for years. The construction presumably began around the 10th century A.D. and finished within the 13th century A.D. When King Jayavarman VII adopted Mahayana Buddhism, the function of the Hindu sanctuary had been changed to serve as a Mahayana monastery.
The site is approached from the east along the first three-leveled platforms leading to the first passage. Then, there is a causeway lined with blunted stone pillars in parallel rows. The path of stone uprights then leads to the Naga Bridge. Far on the northern side of the cross-shaped passage is a laterite pavilion or Phlabphla called the Elephant Shelter. At the end of the bridge is a terraced staircase with 5 landings leading up to the sanctuary. Beyond the bridge is a vast platform which has a passage that will lead to the Naga Bridge, right in front of the central gate of the gallery. The gate is the first entrance which will direct travellers to the inner courtyard of the prasat, by crossing another Naga Bridge that connects the gate with the main prang.
The most important part, the main prang, is situated right at the center of the inner court yard of the sanctuary. The building has a rectangular shape with re-entrant angles at the corners. The square mondop was built adjacent to the main prang. The architectural designs that were carved on the prang such as the posts at the door frame, pillars on the walls, lintels, porticos and pediments, depict designs of floras, leaves, hermits, gods and god desses and characters from religious myths: Vishnu (Narai) resting on Ananta, the Naga king and Shiva dancing, for example.
The decorations found on the lintels and frontal pediments of the main prang help indicate the age of the main building together with the staircase and the Naga Bridge; they are believed to have been constructed around the 12th century A.D. On the grounds of the inner courtyard, southwest of the main prang is a small prang with no roof. The carvings, pediments and lintels of this prang express that the minor prang was built before the main prang, around the 11th century A.D.
There are remains of the brick base of the prang were also discovered on the northeast of the main prang and dated back to the 10th century A.D. Another structure made of laterite stands on the southeast of the main prang and dated to the 13th century A.D. The laterite structure is con temporary to the building which is known as Rong Chang Phueak (the Elephant Shelter).
For more information, please visit www.ancientcity.com
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The Phanom Rung Sanctuary (Buri Ram Province), the Ancient City (Muang Boran), Samutprakan, Thailand...
The Go Ahead London DEL’s have entered service in a very haphazard fashion. This is Bexleyheath allocated DEL133, which entered service in mid November but is still the only one above DEL119 in traffic.
The Electroliner is seen on the stand at Thamesmead Town Centre while on the 401.
13.1.26.
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2021 Edge morning Light on Highest Observation Deck in the Western Hemisphere so far - Hudson Yards Skyscraper Day Clock cloudless 11/28/2021 view from Hells Kitchen Clinton architecture skylines sunlight NYC skyline New York City art city scape cityscape Fall weather blue sky seen from 34th Street