Best dating in wicklow mountains to see in denver co

best dating in wicklow mountains to see in denver co

County Wicklow is blessed with some of Ireland’s most beautiful landscapes from coastal beaches and cliffs to hills and mountains. It is no wonder that it is also one of Ireland’s best Walking destinations. Browse walks by time, location, theme, difficulty and length, etc… WICKLOW WALKS LIST (with downloadable maps): Browse by length, location, type, theme, difficulty, etc… There is a walk in Wicklow to suit any level or difficulty. Click here to browse through the various walks in Wicklow. THE WICKLOW WAY: The Wicklow Way is Ireland’s longest linear walk and runs for 130 km through the mounta .

best dating in wicklow mountains to see in denver co

Gorgeous fall foliage and interesting history! What a great tour! I was originally skeptical of taking a large-scale tour, but this was so worth it. Easy pick up from O'Connell street and a comfortable bus. The scenery was incredible ... who knew Ireland had such beautiful fall foliage?! Every stop was gorgeous and our guide, John, was full of knowledge (and a bit of humor). Each stop was perfectly timed and the pub lunch was delicious (get the Guinness stew!).

I highly recommend this tour! Philip, our guide, was fantastic! Knowledgeable and not too pushy. A natural, knew how to deal with an international clientele. His crisp and precise English was a joy to listen to........disappointing only for those who are looking for an Irish accent. The only minus point....and this has nothing to do with Philip.....was the misleading information about the embarking bus stop.....the Printsafe shop on Nassau Street was already closed and the company bus stop sign was too small and old to be recognised.

Luckily we took the trouble to seek the assistance from a tourism office a day before the trip. Late arrivals on the day might have been due to the lack of such a (no longer) clear meeting point. "Opposite Knobs and Knockers" should be a better indication as the shop is still there. Simply amazing, fun and just a great time altogether. Aisling and James were excelent - everything was thoroughly explained and made interesting and fun. I got to hold a lamb, so I'd say it was a perfect experience just from that.

We got a bit of rain, but since I love the rain and the cold, for me it was just the perfect weather. All in all, a perfect day out on the beautiful Irish countryside.


best dating in wicklow mountains to see in denver co

best dating in wicklow mountains to see in denver co - Dublin to Wicklow Mountains


best dating in wicklow mountains to see in denver co

The Wicklow Mountains (: Sléibhte Chill Mhantáin, : ) form the largest continuous upland area in the . They occupy the whole centre of and stretch outside its borders into the counties of , and . Where the extend into County Dublin, they are known locally as the Dublin Mountains ( Sléibhte Bhaile Átha Cliath). The highest peak is at 925 metres (3,035 feet).

Wicklow Mountains Cuala Dublin Mountains Country Province Leinster Counties , , and : Leinster Chain Borders on Geology to , , -, The mountains are primarily composed of surrounded by an envelope of - and much older rocks such as .

They were pushed up during the at the start of the period and form part of the Leinster Chain, the largest continuous area of granite in Ireland and Britain. The mountains owe much of their present topography to the effects of the , which deepened the valleys and created and lakes. Copper and lead have been the main metals mined in the mountains and a brief occurred in the 18th century. Several major have their source in the mountains, such as the , , and rivers. is the tallest in Ireland at 121 metres (397 feet).

A number of these rivers have been harnessed to create reservoirs for for Dublin and its surroundings. The Wicklow Mountains experience a with mild, damp summers and cool, wet winters.

The dominant habitat of the uplands consists of , and upland . The uplands support a number of bird species, including and . The valleys are a mixture of and woodland. The mountains have been inhabited since times and a number of typical monuments, in particular a series of , survive to the present day. The at , founded in the late 6th century by , was an important centre of the . Following the invasion in the 12th century, the Wicklow Mountains became a stronghold and hiding place for Irish opposed to English rule.

The and families carried out a campaign of harassment against the settlers for almost five centuries. Later the mountains harboured rebels during the . Rebel activity died out after the construction of the at the start of the 19th century and the mountains began to attract tourists to the ruins at Glendalough and to admire the mountain scenery. The Wicklow Mountains continue to be a major attraction for tourism and recreation.

The entire upland area is designated as a and as a under law. The was established in 1991 to conserve the local and landscape. The Wicklow Mountains take their name from which in turn takes its name from .

The origin of the name is from the Wykynglo or Wykinlo. The Irish name for Wicklow, Cill Mhantáin, means "Church of Mantan", named after an apostle of . Wicklow was not established as a county until 1606; before that it had been part of . During the medieval period, prior to the establishment of County Wicklow, the English administration in Dublin referred to the region as the Leinster Mountains.

An early name for the whole area of the Wicklow Mountains was , later Cuala. The Irish name for mountain is Ó Cualann ("lump of Cuala"). There are also historic names for various territories in the mountains held by local : the north part of Wicklow and south Dublin was known as Cualann or Fir Chualann ("men of Cuala"), anglicized 'Fercullen', while the takes its name from the territory of .

A sept of the called the Gaval Rannall possessed the area around , known as Gaval-Rannall or Ranelagh. The mountains were also formerly known as Sliabh Ruadh or the Red Mountains. , Wicklow's highest mountain The Wicklow Mountains are the largest area of continuous high ground in Ireland, having an unbroken area of over 500 km 2 (190 sq mi) above 300 metres (980 ft). They occupy the centre of and extend into Counties , and .

The general direction of the mountain ranges is from north-east to south-west. They are formed into several distinct groups: that of in the north, on the boundary of Dublin and Wicklow; , , and in the centre; and in the west; and to the south.

To the east, separated from the rest of the range by the Vartry Plateau, is the group comprising the , and . is the highest peak in the Wicklow Mountains at 925 metres (3,035 feet) and the 13th highest in Ireland. It is also the highest peak in and is the only Irish to be found outside of . stands at 757 metres (2,484 feet). There are a total of 39 peaks over 600 metres (2,000 feet) in the Wicklow Mountains.

There are only three passes through the mountains under 600 metres (2,000 feet) with the (498 metres (1,634 feet)) and the (478 metres (1,567 feet)) being the highest road passes in the country. The pointed - summit of (left) contrasts with the rounded summit of (right) The Wicklow Mountains are primarily composed of surrounded by an envelope of - and much older rocks such as . The oldest rocks are the quartzites of the Bray Group that include and the and mountains.

These from deposited in the deep waters of the primeval during the (542-488 million years ago). Layers of sediment continued to form and along the ocean floor mixed with pushed up as Iapetus began to shrink by the process of during the period (488-443 million years ago).

These rocks now underlie the of the Vartry Plateau between the Bray Group and the main range. Iapetus closed up completely at the end of the period (443-415 million years ago) and the Wicklow Mountains were during the main phase of the at the start of the period (415-358 million years ago) when the continents of and . The collision pushed up a large of granite, known as the Leinster Chain: this is the largest continuous area of granite in Ireland and Britain and runs from the coast at in County Dublin to in County Wexford and includes the Wicklow and Mountains.

The heat generated by the collision metamorphosed the slates and shales surrounding the granite into which formed an aureole (shell) around the granite. The process of has removed much of the surrounding schist from the mountain tops, exposing the underlying granite. Some remnants of the schist roof remain on some of the mountain tops, most notably . The round granite topped peaks contrast with the sharper schist peaks: for example, (granite) and (schist).

The twin lakes of Lough Bray The last major geological event to shape the Wicklow Mountains was the during the (2.6 million to 11,700 years ago). The ice and moulded the valleys into the that characterises the Wicklow Glens, such as and Glenmacnass.

As the ice melted, small glaciers were left in where now dam lakes such as at Loughs Bray and Nahanagan. Corries without lakes also occur, such as the North Prison and South Prison of Lugnaquilla. Escaping cut narrow rocky gorges at several locations including the , the Devil's Glen and . , such as and the lakes of Glendalough, also formed.

Mining and quarrying The zone of collision between the continental plates that led to the formation of the Wicklow Mountains also led to and the formation of Ireland's most significant metalliferous belt. The most important mining sites have been at and . Mining has taken place at Avoca since at least the (c. 2,500–600 BCE). Iron ore extraction took place between the 12th and 17th centuries before being replaced by lead mining up to the mid 18th century.

The principal activity from 1720 to the closure of the last mine in 1982 was . has also been extracted at certain times and, in smaller quantities, gold, silver and . Lead mining has been the principal activity in the Glendalough valley and its neighbouring valleys of Glendasan and Glenmalure.

Lead was first discovered in Glendasan in the early 19th century and the lead veins were later followed through mountain to Glendalough. Mining on a smaller scale took place in Glenmalure. Ore from these mines was shipped to for processing. The last mine closed in 1957. Miners' village in In 1795, a local schoolmaster discovered gold in the Aughatinavought River, a tributary of the since renamed Gold Mines River that rises on the slopes of mountain.

During the subsequent , some 80 kilograms (180 pounds) of gold was recovered from the river by local prospectors, including a single nugget weighing 682 grams (24.1 ounces), the largest lump of gold ever discovered in Ireland and Britain. The mine workings were subsequently seized by the British government who extracted a further 300 kilograms (660 pounds) of gold.

Various attempts have been made to locate the on Croghan Kinsella but to no avail. Granite from the Wicklow Mountains has been used as a material for many buildings in Wicklow and Dublin and beyond. The quarries at have provided material for buildings such as the on in Dublin, lighthouse and .

Similarly, quarries at provided stone for such buildings as the on and the Industry and Commerce building on in Dublin. Barnacullia, on the slopes of Mountain, supplied paving stones to . The quarry at supplied granite for Dún Laoghaire Harbour and the . The falls as , the tallest waterfall in Ireland The Wicklow Mountains are the source of several major .

Since the thin cannot hold great quantities of water, many of these rivers exhibit a flashy , filling rapidly after heavy rain.

The rises between the mountains of and Tonduff at Liffey Head Bog. One of the major of the Liffey, the , rises nearby on slopes on . The King's River rises on and joins the Liffey near . The rises on the slopes of Djouce mountain. Nearby, the rises between Tonduff and War Hill, falling as the , Ireland's tallest waterfall at 121 metres (397 feet), over a cliff formed by a glacier at the contact point between the granite and mica-schist of the Wicklow Mountains.

The waterfalls at the heads of the valleys of Glendalough, and Glendasan also occur approximately at the schist-granite junctions, as does the Carrawaystick waterfall in . The rises in the North Prison of Lugnaquilla mountain and winds through the where it is joined by the Leoh, Knickeen and Little Slaney.

Another of its tributaries, the River Derreen, rises on Lugnaquilla's southern side. Each of the main branches of the – the , the and the rivers – have their origins in smaller tributaries, many of which rise in the Wicklow Mountains. The Glenealo, Glendasan and Annamoe rivers meet to form the Avonmore near .

The Annamoe rises near Sally Gap and is joined by Cloghoge Brook between and and by the River Inchavore in Lough Dan. The Avonbeg rises on and the Three Lakes. The Avonmore and Avonbeg rivers join to form the River Avoca at the Meeting of the Waters in the Vale of , celebrated in the song The Meeting of the Waters by . The Avoca is joined by the River Aughrim at Woodenbridge, sometimes referred to as the "Second Meeting of the Waters".

The Aughrim is formed at the junction of the Derry Water and the River Ow, the latter of which rises on Lugnaquilla. See also: Several of these rivers have been dammed to create reservoirs to provide for the residents of Dublin and its environs.

The first of these was the River Vartry, dammed to create the near in the 1860s. A second dam was added in 1924 to increase capacity. The River Dodder feeds the two Bohernabreena reservoirs in the northern foothills of the Wicklow Mountains at Glenasmole in County Dublin, which were constructed between 1883 and 1887 to supply water to the of .

The , on the River Liffey near Blessington, was constructed between 1938 and 1940. There are also two plants at Poulaphouca, constructed during the 1940s. A plant was constructed at between 1968 and 1974.

Water is pumped up from Lough Nanahangan, a natural corrie lake, into an artificial reservoir on Tomaneena mountain and released at times of peak electricity demand. See also: In common with the rest of Ireland, the Wicklow Mountains experience a with mild, damp summers and cool, wet winters. Annual rainfall reaches 2,000 mm (79 inches) on the highest mountains with the more westerly peaks getting the most rainfall (for example, Djouce mountain, in the east, receives c.

1,630 mm (64 inches) whereas , in the west, receives c. 1,950 mm (77 inches) a year). June and July are generally the driest months and there is an average of four hours of sunshine a day over the entire year. Snow cover in winter can reach an average of 50 days a year on the highest peaks. Strong winds are an important factor in peat erosion on the summits. on the slopes of Mountain The primary of the uplands consists of and .

The mountain formed around 4,000 years ago as a result of a combination of and human activity. Prior to this, the mountains were cloaked with .

A change in the climate to wetter and milder weather left the ground waterlogged and leached nutrients from the soil, leading to the formation of . Mountain blanket bog is found in areas above 200 metres (660 feet) in altitude and where there are more than 175 days rainfall a year. The most important builders of peat are the bog mosses.

such as and are specific to boglands and and are also common. Bog water is important for the reproduction of and and the Wicklow mountain bogs also support insects such as , , and as well as the and the . such as , and feed in the waterlogged bogland. Due to drainage of water from the bogs as a result of human activity, most of Wicklow's peat has dried out too much for Sphagnum mosses to grow and and vegetation has taken over.

Active peat building is still occurring at some sites, most notably the Liffey Head Bog. (or ling) and are the most common moorland plants along with (or fraughan, as it is known in Ireland), , and . Bird species found on the Wicklow moorland include , and .

found in the uplands include , , and . The latter of these are protected species. The uplands are used for sheep and so the moorland is periodically burned to keep the growth of heather in check and encourage growth of grasses. in the Glenealo valley , once native to Wicklow but hunted to extinction, were reintroduced on the in the 18th century. Japanese were also imported by the Powerscourt Estate and have with the red deer.

All deer found in the Wicklow Mountains are descended from the Powerscourt herd and are either sika deer or hybrid red-sika deer. Other mammals occurring include , , , , , , and .

The is an extinct species of deer that lived in the Wicklow Mountains c. 11,000 years ago, remains of which were discovered in great quantities in Ballybetagh Bog near . were also once native to the mountains but were hunted to extinction in Ireland: the last wolf in Wicklow was killed at Glendalough in 1710.

Widespread clearance of forest began in the Bronze Age and continued up until the early 20th century. programmes began in the 1920s and accelerated in the 1950s with the widespread planting of forest, especially in upland moorland areas previously considered unsuitable for planting.

The dominant tree is the , accounting for 58% of forest plantations, with , , , and also planted. is low in the conifer plantations because they are not native tree species.

plantations are rare, accounting for less than 10% of forest. The young rivers in the upper glens are grounds for and . , isolated in the Wicklow lakes following the end of the last ice age, have been recorded in Lough Dan and the lakes of Glendalough but are now believed extinct.

A programme to reintroduce them into the at Glendalough commenced in 2009. The neolithic passage tomb on the summit of Seefin Mountain The earliest evidence of human activity in the interior of Wicklow dates to around 4,300 BCE. , from the period, are the earliest and most prominent feature of prehistoric Irish civilisation in the Wicklow Mountains. These tombs sit on many of the western and northern summits between in Dublin and in Wicklow, such as at and .

Archaeologist Geraldine Stout has suggested they had a territorial marking function, much like modern-day border posts. Other prehistoric monuments to be found in the uplands include , and . The presence of standing stones at altitudes suggests they may have served route-marking purposes.

The largest complex of in Ireland is to be found on the hills near Baltinglass. The earliest known tribes to have controlled the Wicklow Mountains include the , the , the Uí Theig and the . One member of the Dál Messin Corb was , who founded the at in the latter part of the 6th century.

Kevin travelled to Glendalough from , crossing the mountains via the Wicklow Gap. By the 8th century, Glendalough had grown into a substantial settlement of 500–1,000 people and an important site of learning and . Monasteries were often attacked, especially at times of disease or famine, and Glendalough's wealth made it a frequent target for both local tribes and, later, invaders. The monastery declined in importance after the arrival of the in the 12th century and its subsequent annexation to the .

It was burned by the English in 1398, although settlement there continued until the end of the 16th century. There are also important early Irish church sites in the Dublin foothills of the Wicklow Mountains at and Tully.

In 1170, during the , and successfully laid siege to Dublin by following a high route through the Wicklow Mountains, avoiding the defences along the normal route to the west of the mountains. The Norman invasion displaced two important from , the and the , who moved into the Wicklow Mountains, the O'Byrnes in the east and the O'Tooles in the west.

From their mountain strongholds both families conducted a persistent campaign of harassment against the invaders and the Wicklow Mountains became known as the terra guerre (“land of war”), as opposed to the terra pacis (“land of peace”) of the settled lowlands. The valley of provided an almost unassailable refuge for the clans and English forces suffered heavy defeats there, first in 1274 and again in 1580 in the . The latter defeat was at the hands of , who led many attacks against the English and assisted in the escapes of many of the hostages held by the English to guarantee the loyalty of the Irish clans.

One such hostage was , who escaped from on the night of 6 January 1592 in the company of Art O'Neill. The two men crossed the mountains in blizzard conditions, making for Fiach McHugh O'Byrne's stronghold at Glenmalure.

Art O'Neill died from during the journey and Red Hugh had several toes amputated due to . A cross and a plaque to the north of mountain mark the place where Art O'Neill perished and an annual walk is now held following in the two men's footsteps.

The O'Byrnes' and O'Tooles' dominance finally came to an end with the of 1652 when their land was confiscated by the . Glendalough Valley, showing the Monastic City, the Lower Lake and the Upper Lake A prolonged period of peace reigned in the Wicklow Mountains from the end of the until the . Although the main rebellion was quickly defeated, Irish rebels once again used the Wicklow Mountains as a hiding place and stronghold to attack the English for many years afterwards.

Among their number was , a native of the Wicklow Mountains, born in the of Camara in the , and . Both men eventually surrendered and were to Australia. Determined to prevent any future rebel activity, a military road through the mountains, similar to those built in the to quell the , was proposed by the British government to enable troops to be deployed quickly into the region.

The was constructed between 1800 and 1809 and runs from , County Dublin to , County Wicklow via , the Sally Gap and . A series of army barracks and police stations were built along the route, although they were little used and soon fell into disrepair as the Wicklow Mountains soon ceased to be a centre of rebel activity after the road was completed. The census of 1841 recorded a population of 13,000 in the Wicklow uplands out of 126,143 persons in the county as a whole. Following the , the census of 1891 showed that the population of County Wicklow had declined to 62,136 with the proportionate fall in the uplands regions even greater as the populace deserted the marginal lands.

The in the 19th century led to the development of tourism in the Wicklow Mountains. Visitors were taken by horse-drawn transport into the mountains from the railway station at . Glendalough quickly established itself as the most popular tourist destination and a train service there was considered in 1897 but the proposals came to nothing. The tourism potential of the Military Road was spotted soon after its completion and G.

N. Wright's Tours in Ireland (1822) is one of the earliest guides to the sights along the route. The information office in Glendalough The principal farming activity in the uplands is sheep , using mainly the Wicklow breed. Land is also used for and . Tourism and recreation are also major activities in the uplands.

Glendalough remains the most popular destination, receiving around one million visitors each year. Recreational activities in the mountains include walking, ,winter climbing, fishing and cycling.

in the Wicklow Mountains was first popularised by through a weekly column he wrote in the newspaper. Malone was later instrumental in the creation of the , Ireland's first , which opened in 1980 and crosses the Wicklow Mountains. The Wicklow Way has been joined by the and the pilgrim path, both of which also traverse parts of the mountains.

On foot of concerns about environmental degradation and undesirable development of the Wicklow Uplands, the Government announced the creation of the in 1990 to conserve the area's biodiversity and landscape. The park was officially established in 1991 and now encompasses an area of over 20,000 hectares (200 square kilometres; 77 square miles).

In addition, the Wicklow Mountains (including areas outside the National Park) are classed as a under the EU and as a under the EU . The Dublin foothills of the Wicklow Mountains are managed by the Dublin Mountains Partnership (DMP), a group established in May 2008 with the aim of improving the recreational experience of users of the Dublin Mountains. Its members include representatives of state agencies, local authorities and recreational users.

The DMP has restored paths and developed walking trails, courses and a course. • ^ . Placenames Database of Ireland. . Retrieved 5 July 2011. • ^ . • , p. 32. • , p. 154. • , p. 34. • Tempan, Paul (February 2012). (PDF). mountaineering.ie . Retrieved 17 September 2018. • , p. 253. • , p. 11. • ^ . • . MountainViews.ie . Retrieved 5 July 2011. • . MountainViews.ie . Retrieved 5 July 2011. • . MountainViews.ie . Retrieved 5 July 2011. • . MountainViews.ie . Retrieved 5 July 2011. • ^ , p. 268.

• , p. 22. • , p. 142. • , pp. 18–22. • ^ , p. 271. • , pp. 23–28. • , p. 23. • , p. 252. • ^ , p. 27. • , p. 29. • , §2. • , p. 29. • ^ , p. 30. • , p. 28. • . . . Retrieved 6 July 2011. • , p. 261. • , p. 10. • , p. 10-11. • , pp. 3–4. • , p. 11. • , p. 24. • , pp. 36–37.

• , p. 25. • , p. 32. • ^ . • , p. 64. • , p. 315. • , p. 321. • ^ , p. 85. • , p. 15. • , p. 15. • . Powerscourt House & Gardens . Retrieved 5 July 2011. • , pp. 89–90. • , p. 265. • , §3. • , p. 19. • , p. 23. • ^ , p. 93. • , p. 45. • , p. 94. • , pp. 57–59. • . History of ESB. . Retrieved 14 July 2011.

• , p. 111. • . MountainViews.ie . Retrieved 14 July 2011. • , p. 20-21. • ^ , p. 21. • ^ . . . Retrieved 6 July 2011. • ^ , p. 20. • ^ .

. . Retrieved 12 July 2011. • , p. 44. • , p. 44-46, 50. • ^ . . . Retrieved 12 July 2011. • ^ , p. 47. • , p. 50. • (PDF). . 13 October 2010 . Retrieved 17 July 2011. • , p. 84. • ^ , p. 48. • , p. 39. • . . . Retrieved 12 July 2011. • , pp. 5–6. • , p. 164. • , p. 61. • , p. 62. • . • , p. 82. • , p. 82. • , p. 83. • ^ . . . Retrieved 12 July 2011. • , p. 92. • . . . Retrieved 12 July 2011. • , p. 5.

• , p. 6. • , p. 6-7. • , p. 10. • , p. 10. • ^ , p. 11. • ^ , p. 35. • , p. 14. • . . . Retrieved 16 July 2011. • , p. 20. • ^ , p. 22. • , pp. 141–145. • , p. 151.

• , p. 153. • , p. 152. • , pp. 157, 159. • ^ , p. 30. • , pp. 29–31. • , p. 31. • . Simon Stewart's Hillwalking in Ireland . Retrieved 16 July 2011. • , p. 35.

• , p. 68. • , p. 69. • ^ , pp. 46–48. • , p. 23. • ^ , passim. • , p. 71. • , p. 72. • ^ , p. 72. • , pp. 72, 74. • , p. 202. • , p. 16. • , pp. 168–9, 179. • , p. 18. • , p. 17.

• ^ , p. 10. • . IrishTrails.ie. . Retrieved 17 July 2011. • . IrishTrails.ie. . Retrieved 17 July 2011. • (4 April 1990). "Wicklow to get national park". . Dublin.

p. 5. • . . . Retrieved 17 July 2011. • , p. 9. • ^ . Dublin Mountains Partnership . Retrieved 17 July 2011. • . Dublin Mountains Partnership . Retrieved 17 July 2011. Bibliography • Boyle, Ken; Bourke, Orla (1990). The Wicklow Way: A Natural History Field Guide. Dublin: Cospoir. . • ; (1997). The Wicklow Way. An Exploration of its Rocks and Landscape. Dublin: . • Corlett, Christiaan (1999). Antiquities of Old Rathdown. : Wordwell. . • Dalby, Barry (2009) [1st pub.

1993]. The Wicklow Way Map Guide. Clonegal, Ireland: EastWest Mapping. . • Duffy, John (2006). River Slaney from Source to Sea. : John Duffy. . • ; (July 2009). (PDF). (pdf). Dublin: . . Retrieved 11 July 2011. • Fewer, Michael (2007). The Wicklow Military Road: History and Topography. Dublin: Ashfield Press. . • Flynn, Arthur (2003). A History of County Wicklow. Dublin: Gill & Macmillan. . • Gurrin, Brian F.

(2006). A Social History of the Wicklow Uplands. Dublin: . . • (2007). (pdf). Heritage Council. : Wicklow Heritage Office . Retrieved 10 July 2011. • (2003). The Irish Landscape: A Scenery to Celebrate. Edinburgh: Dunedin Academic Press. . • Jackson, Patrick N. Wyse; Parkes, Matthew; Simms, Mike (2010).

Geology of Ireland: County by County. Dublin: Department of Geology, . . • (1900). . . Part I. Atlas . Retrieved 8 July 2011. • (1837). . . Retrieved 10 July 2011. • Lydon, J. F. (1994). "Medieval Wicklow – A Land of War". In Hannigan, Ken; Nolan, William. Wicklow: History & Society. Dublin: Geography Publications. pp. 151–190. . • Moriarty, Christopher (1988a). "The Liffey of the Wilderness". In Healy, Elizabeth. The Book of the Liffey: From Source to Sea. Dublin: Wolfhound Press.

pp. 15–30. . • Moriarty, Christopher (1988b). "The Bounty of Anna Liffey". In Healy, Elizabeth. The Book of the Liffey: From Source to Sea. Dublin: Wolfhound Press. pp. 53–72. . • Moriarty, Christopher (1991). Down the Dodder. Dublin: Wolfhound Press. . • Nairn, Richard; Crowley, Miriam (1998). Wild Wicklow: Nature in the Garden of Ireland.

Dublin: Townhouse. . • (2005). (pdf). Dublin: Department of the Environment, Heritage and Local Government. . Retrieved 14 July 2011. • Pearson, Peter (1998). Between the Mountains and the Sea: Dun-Laoghaire Rathdown County. Dublin: The O'Brien Press. . • Stout, Geraldine (1994). "Wicklow's Prehistoric Landscape". In Hannigan, Ken; Nolan, William.

Wicklow: History & Society. Dublin: Geography Publications. pp. 1–40. . • Vines, Gail (27 January 2007). "The Hunt for Wicklow Gold". . 193 (2588): 48–49. :. • Warren, William P.

(1993). Wicklow in the Ice Age. Dublin: . . • Whittow, J. B. (1975). Geology and Scenery in Ireland. London: Penguin. . • Williams, Michael; (1999). The Making of Ireland: Landscapes in Geology. London: Immel Publishing. .


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