Red Squirrel (Sciurus Vulgaris) Conservation Management Plan
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Dublin/Wicklow
Recreational facilities: a guide to recreational facilities in the East Coast Area Health Board Item Type Report Authors East Coast Area Health Board (ECAHB) Publisher East Coast Area Health Board (ECAHB) Download date 24/09/2021 15:27:28 Link to Item http://hdl.handle.net/10147/251420 Find this and similar works at - http://www.lenus.ie/hse ,«' Recreational Facilities i lly Gap Regular physical activity can This project, funded by the confer benefits throughout Cardiovascular Health Strategy, life. It has been established Building Healthier Hearts, aims i ntaih that regular physical activity to increase awareness of area can play an important role in opportunities where physical reducing stress and improving activity can take place. • well being, reducing the risk of heart attack and stroke, and Getting started is easy. Using v assist in achieving and this resource choose an maintaining a healthy weight. activity that you enjoy and let the fun begin! So you've never really been physically active before? Or Get more active - How much? you did once, but abandoned For a health benefit we need activity efforts years ago? to be physically active for Here's the good news: No "30 minutes or more, most days matter when you start to of the week. The good news become active, making a is this activity can be commitment to physical accumulated or spread over activity can improve your 1,2, or 3 sessions. health and help you feel great! For example, 2 X 15 minute walking sessions. .*.$js 'fa ^¾¾ ' Woodland and Forest Walks Dublin/Wicklow DUBLIN and is 6km long. -
EIS Chapter 4
ECOLOGY 4 CONTENTS INTRODUCTION ........................................................................................................ 1 Background ............................................................................................................. 1 Location and Setting ................................................................................................ 1 Purpose of the Ecological Impact Assessment ........................................................ 1 LEGISLATIVE and POLICY CONTEXT ...................................................................... 2 Legislative Context .................................................................................................. 2 Planning Policies ..................................................................................................... 3 Biodiversity Plans .................................................................................................... 5 METHODOLOGY ........................................................................................................ 5 Area of Study ........................................................................................................... 6 Desk-based Study ................................................................................................... 6 Field Survey ............................................................................................................ 6 Constraints and Uncertainty of Data ........................................................................ 7 Assessment -
Wicklow - County Geological Site Report
WICKLOW - COUNTY GEOLOGICAL SITE REPORT NAME OF SITE Lough Bray Other names used for site IGH THEME IGH7 Quaternary TOWNLAND(S) Powerscourt NEAREST TOWN/VILLAGE Glencree, Enniskerry SIX INCH MAP NUMBER 6 NATIONAL GRID REFERENCE 713405E 715950N (arête between corries) 1:50,000 O.S. SHEET NUMBER 56 GSI Bedrock 1:100,000 Sheet No. 16 Outline Site Description The Lough Bray site consists of two lakes; Lough Bray Upper and Lough Bray Lower, which occupy two of the most accessible corries in Ireland, 2 kilometres south of Glencree Village and just off the Military Road. Geological System/Age and Primary Rock Type The features were formed during the Quaternary (Ice Age), by glacier ice scouring out two deep, armchair-shaped hollows at the northeastern edge of the Wicklow Mountains. The majority of the features therefore comprise ice-scoured bedrock, which is coarse-grained granite. The granite is part of the Lugnaquillia Pluton which is one of the five plutons that comprise the late-Caledonian (405 Ma) Leinster Granite batholith. Main Geological or Geomorphological Interest These corries have almost-vertical backwalls up to 200m in height. Two tarns (glacial lakes) floor the features and the corries and lakes are bounded on their eastern sides by a series of impressive moraines. These have been dissected by Holocene (post-glacial) streams draining the lakes. The moraines comprise well-drained, bouldery material, and the area around and east of Lough Bray is littered with large erratic boulders up to 10m across. Many of these erratics weigh several hundred tonnes and bear testament to the power of the ice sheet which transported them. -
Listing and Index of Evening Herald Articles 1938 ~ 1975 by J
Listing and Index of Evening Herald Articles 1938 ~ 1975 by J. B. Malone on Walks ~ Cycles ~ Drives compiled by Frank Tracy SOUTH DUBLIN LIBRARIES - OCTOBER 2014 SOUTH DUBLIN LIBRARIES - OCTOBER 2014 Listing and Index of Evening Herald Articles 1938 ~ 1975 by J. B. Malone on Walks ~ Cycles ~ Drives compiled by Frank Tracy SOUTH DUBLIN LIBRARIES - OCTOBER 2014 Copyright 2014 Local Studies Section South Dublin Libraries ISBN 978-0-9575115-5-2 Design and Layout by Sinéad Rafferty Printed in Ireland by GRAPHPRINT LTD Unit A9 Calmount Business Park Dublin 12 Published October 2014 by: Local Studies Section South Dublin Libraries Headquarters Local Studies Section South Dublin Libraries Headquarters County Library Unit 1 County Hall Square Industrial Complex Town Centre Town Centre Tallaght Tallaght Dublin 24 Dublin 24 Phone 353 (0)1 462 0073 Phone 353 (0)1 459 7834 Email: [email protected] Fax 353 (0)1 459 7872 www.southdublin.ie www.southdublinlibraries.ie Contents Page Foreword from Mayor Fintan Warfield ..............................................................................5 Introduction .......................................................................................................................7 Listing of Evening Herald Articles 1938 – 1975 .......................................................9-133 Index - Mountains ..................................................................................................134-137 Index - Some Popular Locations .................................................................................. -
Great Sugar Loaf
WICKLOW - COUNTY GEOLOGICAL SITE REPORT NAME OF SITE Great Sugar Loaf Other names used for site Big Sugar Loaf, Little Sugar Loaf, Ó Cualann IGH THEME IGH4 Cambrian-Silurian, IGH7 Quaternary TOWNLAND(S) Glencap Commons South, Glencap Commons Upper, Glencap Commons North NEAREST TOWN/VILLAGE Kilmacanoge SIX INCH MAP NUMBER 7, 8 ITM CO-ORDINATES 723710E 713110N (summit) 1:50,000 O.S. SHEET NUMBER 56 GSI BEDROCK 1:100,000 SHEET NO. 16 Outline Site Description A prominent, scree covered, quartzite conical mountain peak standing out on the north Wicklow and Dublin skyline. Geological System/Age and Primary Rock Type Cambrian quartzite (Bray Head Formation) bedrock with greywacke/quartzite bedrock on the south/southwest slopes. The scree deposits (of quartzite) are Quaternary in age, having formed from freeze-thaw activity during the last glaciation. Main Geological or Geomorphological Interest Great Sugar Loaf (501m) is a prominent conical peak of pale-pink Cambrian quartzite, around 7km southwest of Bray. The conical shape contrasts with the rounded summits of the granite mountains to the west. The elevated terrain comprising Great Sugar Loaf, Little Sugar Loaf and Bray Head marks the northern margin of a tectonic slide (roughly along the course of the River Dargle) where Cambrian rocks were thrust up onto Ordovician rocks (found between Bray Head and Killiney Hill and southwest beyond Rathdrum). This NW directed thrusting occurred during a great mountain building event (Caledonian Orogeny), 475-400 million years ago, also during which the Late Caledonian Leinster granites were formed. Great Sugar Loaf and Little Sugar Loaf (341m), 3km to the northeast, are separated by Kilmacanoge valley. -
S' Parting ~~~~~~=-=-=:=~~~~~~~Q~~~~~:S~ Page ~ at Galway --- 82 --0-- the Upper Boyne Is Ellsy to Fish - 83 -----0---- I Saw Cork -- 84
Lovers' Parting ~~~~~~=-=-=:=~~~~~~~Q~~~~~:S~ Page ~ at Galway --- 82 --0-- The Upper Boyne is ellsy to Fish - 83 -----0---- I saw Cork -- 84- Curiosities Around Ireland --- 85 --0-- Surprising Number of Poems of Irish Places ----- 87 --00 Through the streets ---- 88 -<> Father was _.always lIke That !- -. 91 Seen from top of Crogbaun =9. VOL. XVIII. No. 6. ma~ch, 1943. THREEPENCE Cumonn Luer IR ISH TNA [/ I~ L March, 1943. DUBLIN * BANK OF IRELAND N FACILITIES FOR TRAVELLERS AT Bead omce: COLLEGE GREEN,DUBLIIf BKLrAIT .. OORK DERRY tt JVhere North meets South" PHONE: DUBLIN 71371 (6 Lines) .TB.Y D••ORIPTION 01' I'OR.ION .XOHANG. IiU8INlI88 TRA.N8A.OT.D ON ARRIVA.L 01' LIN_U BY DA.Y OR NIGHT AT OOBH (QU.IlN8TOWJf) ReStdent Manager . ......• T. O'Sultwan AND OALWAY DOOQ. Everything to satisfy the most exacting connoisseur is provided. Coal fires in all public rooms; after noon tea, 3-6; liberal table; excel lent cooking aId service; a pleasant and informal atmosphere. Centrally situated, with moderate terms. Visit H's of little us(' having your tables aUra liv('Iy Jaid unless the Restaurant next time you're you have equipmrnt in your kitchens which enables your staft to serve npp<'tising courses rapidly. Your guests asS('Ss your lunching in town. service' by the standard of meals you offer and modern equip ment enables you to maintain a high standard. De!=pitc the difficulties attendinR' dt-liveryof equipment wC" can still supply many items which wiiJ moderni.51.' your kitchen and incrcast' efficiency: Electric ookers; turf and wood-hurn in!: ran!'te.; electric dish washers; CH El' ranges; HA~IMONj) Steam Cookers; aluminium utc:lsiJs in large and small size!'. -
List of Irish Mountain Passes
List of Irish Mountain Passes The following document is a list of mountain passes and similar features extracted from the gazetteer, Irish Landscape Names. Please consult the full document (also available at Mountain Views) for the abbreviations of sources, symbols and conventions adopted. The list was compiled during the month of June 2020 and comprises more than eighty Irish passes and cols, including both vehicular passes and pedestrian saddles. There were thousands of features that could have been included, but since I intended this as part of a gazetteer of place-names in the Irish mountain landscape, I had to be selective and decided to focus on those which have names and are of importance to walkers, either as a starting point for a route or as a way of accessing summits. Some heights are approximate due to the lack of a spot height on maps. Certain features have not been categorised as passes, such as Barnesmore Gap, Doo Lough Pass and Ballaghaneary because they did not fulfil geographical criteria for various reasons which are explained under the entry for the individual feature. They have, however, been included in the list as important features in the mountain landscape. Paul Tempan, July 2020 Anglicised Name Irish Name Irish Name, Source and Notes on Feature and Place-Name Range / County Grid Ref. Heig OSI Meaning Region ht Disco very Map Sheet Ballaghbeama Bealach Béime Ir. Bealach Béime Ballaghbeama is one of Ireland’s wildest passes. It is Dunkerron Kerry V754 781 260 78 (pass, motor) [logainm.ie], ‘pass of the extremely steep on both sides, with barely any level Mountains ground to park a car at the summit. -
Killiney Hill Trail
Killiney Hill Trail • This trail will take approximately two hours. • It could be divided into two halves (Stopes 1-3 and Stops 4-7). • It is designed for senior classes. • One booklet per group, with extra paper for activities. • One adult is required with each group of 4-6. • We recommend that the teacher should complete the trail in advance . Pencil and eraser A4 white paper Compass 1. Make sure you have Measuring tape everything you need. String One camera per group. 2. Write your name and the date on your sheet. 3. Remember the rules. Stay with your group. 4. Remember to use all your senses at every station and to have fun! 1 Killiney Hill Trail Do not go down steep steps. Continue up to tower. To get to Stop 4 follow signs 3 for tea rooms. 1 Look out for a little lane on 7 2 your left! Go up that. Toilets/ 4 Off the beaten coffee shop track into the 6 forest. 5 Created July 2017 by: Paula Murphy, Tania Daly, Paul Twomey, Ann-Marie Kenrick, Ann-Marie Greene and Ciara McCarrick The Memory Stone Stop 1 Killiney Hill mark is a combination of Dalkey Hill, Killiney Hill and Roches Image Hill. It was opened to the public as related Victoria Hill in 1887, and re-named to info as Killiney Hill in 1920. Enjoy lgkndfl;fthe woodlands, the magnificent 1830 2017 Enjoy the woodlands, the magnificent seascapes and learn some fascinating local history. Your task, as you move from stop to stop, is to locate the Follow the path monuments, statues and in a south-east objects photographed on direction to Stop page 2, and tick them off. -
Wicklow - County Geological Site Report
WICKLOW - COUNTY GEOLOGICAL SITE REPORT NAME OF SITE Kippure Other names used for site Cipiúr IGH THEME IGH7 Quaternary TOWNLAND(S) Powerscourt Mountain, Kippure, Castlekelly NEAREST TOWN/VILLAGE Enniskerry SIX INCH MAP NUMBER 2, 6 ITM CO-ORDINATES 711500E 715490N (summit) 1:50,000 O.S. SHEET NUMBER 56 GSI BEDROCK 1:100,000 SHEET NO. 16 Outline Site Description A landmark mountain on the South Dublin-Wicklow county boundary, capped with a prominent transmission tower. The upper mountain hosts extensively eroded peat, exposed granite sands, and granite blocks. Geological System/Age and Primary Rock Type Erosion of the peat has been ongoing for the past 3,000 years on this granite mountain. The granites (fine to coarse-grained, with microcline phenocrysts) are part of the Late Caledonian Leinster granites that were emplaced around 405 million years ago (Devonian). Main Geological or Geomorphological Interest Above heights of c. 740m, the near-flat summit of Kippure is devoid of significant peat accumulations. The summit hosts a blockfield of rounded granite boulders that lie embedded in grus (crumbled sandy granite). Below the 740m contour, areas of blanket peat are extensively eroded. Deep peat gullies, sub-peat pipes, solitary peat hags (haggs), and collapsing peat banks characterize much of the upper mountain slopes. Where peat has eroded fully, granite bedrock is exposed, with thick accumulations of grus, or granite sand (quartz, feldspar, mica) overlying the bedrock Peat erosion has been a continual process in Wicklow for over 3,000 years, and is not considered to be attributed solely to recent human disturbance. Peat erosion is considered to be a natural consequence of the accumulation of peat on sloping ground. -
DALKEY COASTAL ZONE & KILLINEY HILL Pnha(002106
NOTE: CONFIDENTIAL, NO THIRD PARTY DISCLOSURE ALLOWED. All rights reserved. © J.B.Barry and Partners T.J O'Connor and Associates Royal Haskoning DHV 2014 N 1. All levels are in metres and relate to O.S. Datum MALIN. 2. This drawing is reproduced from digital maps: O.S. MAPS - Scale 1:2,500 O.S. MAPS - Scale 1:1,000 Discovery Series - Scale 1:50,000 3. All Maps are referenced to IRISH NATIONAL GRID (I.T.M.) 4. Reproduced from the Ordnance Survey Of Ireland by Permission of the Government. License No. 3-3-34. © CROWN COPYRIGHT AND/OR DATABASE RIGHTS. PRODUCTS LICENCE NUMBER 18197. REPRODUCED BY PERMISSION OF THE CONTROLLER OF HER MAJESTY'S STATIIONERY OFFICE AND UK HYDROGRAPHIC OFFICE (www.ukho.gov.uk) "NOT TO BE USED FOR NAVIGATION". LEGEND: PROPOSED NATURAL HERITAGE AREA DUBLIN PORT LIMITS DUN LAOGHAIRE HARBOUR LIMITS HOWTH HEAD pNHA(000202) ROYAL CANAL pNHA(002103) NORTH DUBLIN BAY pNHA(000206) RINGSEND WASTEWATER GRAND CANAL TREATMENT pNHA(002104) PLANT 0 JUNE 2018 LA MH MH PLANNING APPLICATION Rev.: Date: Drawn: Checked: Approved: Description: Client: SOUTH DUBLIN BAY pNHA(000210) Scheme: RINGSEND WASTEWATER TREATMENT PLANT UPGRADE PROJECT Component:RINGSEND WASTEWATER TREATMENT PLANT TJ O'Connor & Associates Corrig House Corrig Road, Tel:+353-1-2952321 Sandyford email:[email protected] Dublin 18, Ireland Web:www.tjoc.ie J. B. Barry and Partners Classon House Dundrum Business Park Tel: +353-1-485 1400 Dundrum Road email: [email protected] Dublin 14 Web: www.jbbarry.ie Royal HaskoningDHV PO Box 1132 3800 BC Amersfoort Tel:+31-88-3482000 The Netherlands email:[email protected] Web:www.royalhaskoningdhv.com DALKEY COASTAL ZONE Drawn By: Checked By: Approved By: Date: & KILLINEY HILL LHA MH MH JAN.2018 pNHA(002106 Client Project Ref: Project Stage: IW-RGD/10000308 Internal Project Ref: Ring01/JBB-Y14701/TJOC-14040/RHDHV-BB4342 @A1 Drawing Title: DUBLIN BAY CONSERVATION DESIGNATIONS PROPOSED NATURAL HERITAGE AREAS NOTE : DATA OF SHAPE FILES OBTAINED FROM THE WWW.EPA.IE WEBSITE Meters 1000 0 1000 2000 Scales: 1:30,000@A1 1:60,000@A3 Drawing. -
Dún Laoghaire Rathdown
DUN LAOGHAIRE - RATHDOWN – COUNTY GEOLOGICAL SITE REPORT NAME OF SITE Three Rock Mountain Other names used for site Two Rock Mountain, Fairy Castle IGH THEME IGH7 Quaternary TOWNLAND(S) Ticknock, Barnacullin, Ballyedmonduff, Ballybrack, NEAREST TOWN/VILLAGE Glencullen, Kiltiernan SIX INCH MAP NUMBER 25, 26 ITM CO-ORDINATES 717750E 723300N (centre of feature) 1:50,000 O.S. SHEET NUMBER 50 GSI BEDROCK 1:100,000 SHEET NO. 16 Outline Site Description A landmark mountain to the southwest of Dublin City, on which craggy stumps of granite stand proud of a mainly peat-covered granite mountain top. Geological System/Age and Primary Rock Type Devonian granite (porphyritic granite with large muscovite crystals ~80mm), severely weathered during Quaternary (Pleistocene) ice ages forming stumps/crags known as tors. Main Geological or Geomorphological Interest On the summit of Three Rock and Two Rock mountains, deeply etched and conspicuous crags of granite rock stand proud of the surrounding mainly peat covered mountain top. These protruding crags give the two mountains their names. From a distance, the rocky features resemble man-made structures. However, the granite outcrops are natural, formed by differential weathering of granite bedrock, and mass wasting and removal of the weathered material. Weathering along horizontal and near-vertical joints has created the characteristic granite tor shape, and these are the best examples in the Dublin and Wicklow Mountains. Studies of the tors of the Cairngorms (Scotland) conclude that the survival of tors with deeply etched surfaces and no, or limited, block removal requires a cover of largely non-erosive ice during each of the cold stages of the Pleistocene. -
JA0/Rja0040a.Pdf, .PDF Format 497KB
Inspector’s Addendum Report 06S.JA0040. Development Dublin Mountain Visitor Centre and all associated works. Location Townlands of Montpelier, Killakee and Jamestown, South Dublin. Planning Authority South Dublin County Council. Applicant South Dublin County Council. Type of Application Section 175(3), Planning and Development Act 2000 (as amended). Submissions/Observations See Appendix. Inspector Ciara Kellett. 06S.JA0040 Inspector’s Addendum Report Page 1 of 57 Contents 1.0 Introduction .......................................................................................................... 3 2.0 Request for Further Information under S.175(5)(c) of the Act .............................. 3 3.0 Submissions ........................................................................................................ 4 4.0 Further Assessment ............................................................................................. 5 5.0 Environmental Impact Assessment ...................................................................... 6 6.0 Appropriate Assessment .................................................................................... 29 7.0 New issues raised .............................................................................................. 41 8.0 Overall Conclusion ............................................................................................. 41 9.0 Recommendation ............................................................................................... 42 10.0 Reasons and Considerations .....................................................................