Scotland Great Glen Way Walk & Barge
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Dochgarroch Primary School Handbook 2021-2022
Welcome to our wonderful school nestled near Loch Ness. Dochgarroch Primary School Handbook 2021-2022 At Dochgrroch Primary and Nursery we aim to Dream, Believe, Achieve....together! By providing a stimulating learning environment. All who work and learn in the school understand the value of being Happy, Hard-working, Respectful and Inclusive to all in our school, community and wider world. 1 The current pandemic has affected the normal running of schools in many ways. This Handbook reflects the way the school usually runs but does not cover all of the changes that we have made because of the pandemic. Our arrangements have changed in many ways this session, and may well change again, depending on how the pandemic develops. For the most up-to-date information about any aspect of the work of the school, please make contact and we will be able to tell you about our current arrangements. For the latest information about how the pandemic affects children, young people and families across Scotland, please visit the Scottish Government website, which has helpful information about Coronavirus and its impact on education and children. https://www.gov.scot/coronavirus-covid-19/ 2 CONTENTS 1. OUR VISION, VALUES AND AIMS 2. OUR SCHOOL IMPROVEMENT PLANS 3. GENERAL INFORMATION ABOUT THE SCHOOL Contact details, Staffing, the school facilities, the school atmosphere and ethos, times etc, working in partnerships. 4. EDUCATIONAL POLICY OF THE SCHOOL The curriculum, teaching methods, subjects taught, homework, learning support & special needs, assessment of pupils and reports to parents; 5. SOCIAL EDUCATION Development of spiritual, moral, social and cultural values, school rules, discipline and anti-bullying policy; 6. -
Caol Is in an Area of Flood Risk from the River Lochy and Loch Linnhe
1) Why do we need flood protection? Caol has a long flood history and flooded most recently in Caol is in an area of flood risk from the River Lochy and 2005. Loch Linnhe. Studies have been carried out by professionals that agree there is a clear Flooding within Caol can occur due to four processes; risk of river and coastal flooding in Caol. • extreme sea-levels surging into the Loch, • wind-generated waves breaking over the foreshore, • river flows exceeding the bank level of the River Lochy and inundating the surrounding floodplain and • surface water. Each process may occur in isolation or, during some cases, occur simultaneously to produce extreme flooding. This is likely to get worse as the effects of climate change have an impact on sea levels and increase the rainfall running off the land into the River Lochy. Caol Timeline Scheme Construction (2019/20) Caol Flood Risks Scheme Publication (2018) Scheme Appraisal (& Updated Flood Risk Mapping) JBA Consulting (2014) Feasibility Report Scott Wilson (2007) Flood Risk Mapping Mott MacDonald (2005) Fort William Flood Studies Mott MacDonald (6 reports, 1990 to 1993) High tide with tidal surge and wave 1950 1960 1970 1980 1990 2000 2010 2020 action High river flow with Report / publication Construction tidal surge Flood Event 2 – Flood impacts in Caol and Lochyside What is tidal surge? A tidal or storm surge is a change in sea level that is caused by a storm, predominantly from high winds pushing the sea water towards the coast, causing it to pile up there. The strong winds in the storm generate large waves on top of the surge which can cause damage to sea defences, or spill over the top adding to the flood risk. -
Media 436311 En.Pdf
Contents Where are the Highlands? Where are the islands? Things to do Make an itinerary How to get there Choosing accommodation Food and drink Discounts and saving money Safety tips Where are the Highlands? The Highlands is the area north and west of the Highland Boundary Fault (from Arran and Helensburgh on the west coast stretching across to Stonehaven in the east). It is the uppermost part of Scotland (made up of six smaller regions) and home to famous attractions such as Ben Nevis and Loch Ness, towns (notably Fort William, Nairn and Aviemore) and the “City of the Highlands” - Inverness. Traditionally visitors wishing to experience the beautiful Scottish outdoors will travel to the Highlands to visit the scenic lochs, tall snow capped, mountains, vast glens, ancient monuments as well as the beaches and bays along North Scotland’s iconic coastline. Seals, puffins, whales and dolphins are often spotted on these shores. You may want to try to catch a glimpse of the infamous Aurora Borealis (the Northern Lights), walk amongst the The Highlands varied wildlife and flora or appreciate the breath-taking Scottish landscapes as part of your Highland experience. Or visit historic towns and villages for sightseeing, fine and traditional dining, shopping and a taste of Highland life. (Lowlands) For general information about the history of the Highlands see here! Where are the islands? You can reach the islands as part of your Highlands visit by ferry or air from the mainland. The island groups are: The Shetland The Orkney Islands Islands The -
2-DAY TOUR to EILEAN DONAN CASTLE, LOCH NESS & the WEST
2-DAY TOUR to EILEAN DONAN CASTLE, LOCH NESS & the WEST HIGHLANDS DAY 1 We leave Edinburgh and head west on a motorway that links the capital to Glasgow, the largest city in Scotland and its industrial heartland. From Glasgow, we pass Stirling on the right, the site of the Battle of Bannockburn where, in 1314, a Scottish army under King Robert the Bruce won a crucial victory against the English. Dominating the town is Stirling Castle which sits high on a large volcanic rock. Prominently sited on a hill close to Stirling is the Wallace Monument, our first stop of the day. It is 67 metres high and was built in the 1860’s to commemorate our great freedom fighter, William Wallace, who led an army against the English and defeated them at the Battle of Stirling Bridge in 1297. He was immortalised in the 1995 film ‘Braveheart’. You will have the chance to visit the monument* and the museum inside which has Wallace’s massive sword (1.7 metres long) on display. There are excellent views from the top. At Stirling we head west. Soon we cross over the river Teith and as we do so, on the right, is the very imposing Doune Castle. Next we drive through Callander, and in the area where the Clan MacGregor reigned in the Middle Ages : the clans were extremely powerful at that time and the best known MacGregor was Rob Roy who was born in 1671. At the next village, Tyndrum, the road divides and we head north into a very sparsely populated area. -
Quaternary of Scotland the GEOLOGICAL CONSERVATION REVIEW SERIES
Quaternary of Scotland THE GEOLOGICAL CONSERVATION REVIEW SERIES The comparatively small land area of Great Britain contains an unrivalled sequence of rocks, mineral and fossil deposits, and a variety of landforms that span much of the earth's long history. Well-documented ancient volcanic episodes, famous fossil sites, and sedimentary rock sections used internationally as comparative standards, have given these islands an importance out of all proportion to their size. These long sequences of strata and their organic and inorganic contents, have been studied by generations of leading geologists thus giving Britain a unique status in the development of the science. Many of the divisions of geological time used throughout the world are named after British sites or areas, for instance the Cambrian, Ordovician and Devonian systems, the Ludlow Series and the Kimmeridgian and Portlandian stages. The Geological Conservation Review (GCR) was initiated by the Nature Conservancy Council in 1977 to assess, document, and ultimately publish accounts of the most important parts of this rich heritage. The GCR reviews the current state of knowledge of the key earth-science sites in Great Britain and provides a firm basis on which site conservation can be founded in years to come. Each GCR volume describes and assesses networks of sites of national or international importance in the context of a portion of the geological column, or a geological, palaeontological, or mineralogical topic. The full series of approximately 50 volumes will be published by the year 2000. Within each individual volume, every GCR locality is described in detail in a self- contained account, consisting of highlights (a precis of the special interest of the site), an introduction (with a concise history of previous work), a description, an interpretation (assessing the fundamentals of the site's scientific interest and importance), and a conclusion (written in simpler terms for the non-specialist). -
Ness News Turns One
Community News & Events September 2019 Ness News Turns One Nessnewspaper News Ness News Community News & Events September 2018 Community News & Events November 2018 Cruise Loch Ness Celebrate Remembering the Fallen 50 Years in Business One Hundred Years On London to Paris Class of 72 Reunion Shinty Development Day Cill Chuimein Ness News Ness News Heritage Group Community News & Events February 2019 Community News & Events June 2019 Local Crews on Exercise Sustainability at the core BAFTA for Screen Shaun on 14 Kilchuimen 50th Cruise Loch Ness Caps for Scotland 1 Machine 1 1 Golden Gala Day Named UK Small Business 2019 Safeguarding the Safeguarding the Future of the Maddie Changing future of the Caledonian Canal Lives in Inverness Caledonian Canal Sustainability at the core Sustainability at the core Ness News Febuary issue.indd 1 23/02/2019 18:42:31 Sustainability at the core Ness News September issue.indd 1 10/09/2019 22:02:02 Welcome to this edition of Ness News which is slightly late due to work commitments, wedding preparations and illness. It has been another busy summer with lots of tourists, but parking is still a massive issue and was not helped by the car park extension not going ahead as had been promised (hopefully, it will be in place next year). Unfortunately, there were also eight commercial break-ins in Fort Augustus during July and August which is very concerning but the police have stressed that local residential properties are not at risk as this group are targeting commercial premises who have been advised as in the CC Minutes. -
Waterway Dimensions
Generated by waterscape.com Dimension Data The data published in this documentis British Waterways’ estimate of the dimensions of our waterways based upon local knowledge and expertise. Whilst British Waterways anticipates that this data is reasonably accurate, we cannot guarantee its precision. Therefore, this data should only be used as a helpful guide and you should always use your own judgement taking into account local circumstances at any particular time. Aire & Calder Navigation Goole to Leeds Lock tail - Bulholme Lock Length Beam Draught Headroom - 6.3m 2.74m - - 20.67ft 8.99ft - Castleford Lock is limiting due to the curvature of the lock chamber. Goole to Leeds Lock tail - Castleford Lock Length Beam Draught Headroom 61m - - - 200.13ft - - - Heck Road Bridge is now lower than Stubbs Bridge (investigations underway), which was previously limiting. A height of 3.6m at Heck should be seen as maximum at the crown during normal water level. Goole to Leeds Lock tail - Heck Road Bridge Length Beam Draught Headroom - - - 3.71m - - - 12.17ft - 1 - Generated by waterscape.com Leeds Lock tail to River Lock tail - Leeds Lock Length Beam Draught Headroom - 5.5m 2.68m - - 18.04ft 8.79ft - Pleasure craft dimensions showing small lock being limiting unless by prior arrangement to access full lock giving an extra 43m. Leeds Lock tail to River Lock tail - Crown Point Bridge Length Beam Draught Headroom - - - 3.62m - - - 11.88ft Crown Point Bridge at summer levels Wakefield Branch - Broadreach Lock Length Beam Draught Headroom - 5.55m 2.7m - - 18.21ft 8.86ft - Pleasure craft dimensions showing small lock being limiting unless by prior arrangement to access full lock giving an extra 43m. -
Control of Erosion on Construction Sites
624 RAN:c COf'<-\ I A LIBRARY PLANNING AND EP CONTROL OF EROSION ON CONSTRUCTION SITES By Michael J. Ransom CONTENTS INTRODUCTION 7 1 CONTROL OF EROSION ON CONSTRUCTION SITES 9 1.1 General 9 1 .2 How Does Erosion Occur? 9 2. BENEFITS OF EROSION CONTROL ON CONSTRUCTION SITES 11 3. PRINCIPLES OF EROSION CONTROL ON CONSTRUCTION SITES 12 3.1 Planning Phase Controls 12 3.2 Design and Construction Phase Controls 13 3.3 Maintenance Phase Controls 14 4. CONSTRUCTION SITE PRACTICE 15 4.1 Initial Clearing and Site Preparation 15 4.2 Access Around the Site 16 4.3 Drainage 19 4.4 Stockpiles and Spoil Dumps 30 4.5 Vegetation and Reclamation 31 4.6 Batters 34 4.7 SedimentTrapping 37 APPENDIX 1. Construction Supervisor's Check List 46 APPENDIX 2. Conservation, Forestsand Lands 47 Regional Offices REFERENCES 48 f l � t. tf.· . ' f•-':·.· . · . I . ACKNOWLEDGMENTS (First Edition) A number of people have assisted in the preparation of this booklet, both in technical advice and in reviewing the text. Particular thanks are due to a number of officers of the Soil Conservation Authority, particularly Mr. Graydon Findlay, the Authority's Chief Engineer. Also, the assistance of the following is greatly appreciated: Mr. John Mapson, State Rivers and Water Supply Commission, Messrs. Cliff Lawton and Peter Nash of the Road Construction Authority, and Mr. Don Thomson and his staff of the Dandenong Valley Authority who assisted greatly in providing technical input and advice on the presentation of the booklet. INTRODUCTION Each year, an increasing area of agricultural and open land is converted to urban use for houses, shopping centres, factories, roads, schools and other facilities. -
Lands Than the Roads That Were Constructed by General Wade
I. MILITARY ROADS AND FORTIFICATIONS IN THE HIGHLANDS, WITH BRIDGE MILESTONESD SAN THOMAY B . S WALLACE, F.S.A. SCOT. Nothing contributed peace mor prosperitth d o ean t Highe th f y-o lands tha roade nth s that were constructe Generay db ls Wadhi d ean successors ways,d "e ol Th ". accordin Burto gt , consiste stonf o d y moors, bogs, rugged, rapid fords, declivities of hills, entangling woods, giddd an y precipices. Although Wad responsibls ewa comparaa r efo - tively small portion of the work, yet he was undoubtedly the originator scheme oth f e whic completes h wa s successorshi y db . These roads, which followed pretty much the old tracks (which have been continued railways)e th y b , were commence dn 172i carried 5an tiln o dl 1814. widte firse thes th a Th tfeetf 6 yhd o road1 weran s , militarr swa e fo y purposes they proceede straighs a dn i lina t possibles ea shorteo t , e nth journey. On account of the peculiar circumstances which followed the Dis- arming Act after 1715, and after representations made by Lord Lovat and others, General Wad commandes ewa Georgy db proceeo t . eI do t the Highlands in 1724 and report upon the state of affairs as he found them, and to suggest remedies for the same. A copy of his instructions will be found in the Record Office, vol. xiv. p. 60. Among other things keeo t roade s pth goon wa si e dh repair communicating betweee nth barracks already established, and to build a galley to be employed in conveying troops, etc. -
Inverness Local Plan Public Local Inquiry Report- Volume 3
TOWN AND COUNTRY PLANNING (SCOTLAND) ACT 1997 REPORT OF PUBLIC LOCAL INQUIRY INTO OBJECTIONS TO THE INVERNESS LOCAL PLAN VOLUME 3 THE HINTERLAND AND THE RURAL DEVELOPMENT AREA Reporter: Janet M McNair MA(Hons) MPhil MRTPI File reference: IQD/2/270/7 Dates of the Inquiry: 14 April 2004 to 20 July 2004 CONTENTS VOLUME 3 Abbreviations The A96 Corridor Chapter 24 Land north and east of Balloch 24.1 Land between Balloch and Balmachree 24.2 Land at Lower Cullernie Farm Chapter 25 Inverness Airport and Dalcross Industrial Estate 25.1 Inverness Airport Economic Development Initiative 25.2 Airport Safeguarding 25.3 Extension to Dalcross Industrial Estate Chapter 26 Former fabrication yard at Ardersier Chapter 27 Morayhill Chapter 28 Lochside The Hinterland Chapter 29 Housing in the Countryside in the Hinterland 29.1 Background and context 29.2 objections to the local plan’s approach to individual and dispersed houses in the countryside in the Hinterland Objections relating to locations listed in Policy 6:1 29.3 Upper Myrtlefield 29.4 Cabrich 29.5 Easter Clunes 29.6 Culburnie 29.7 Ardendrain 29.8 Balnafoich 29.9 Daviot East 29.10 Leanach 29.11 Lentran House 29.12 Nairnside 29.13 Scaniport Objections relating to locations not listed in Policy 6.1 29.14 Blackpark Farm 29.15 Beauly Barnyards 29.16 Achmony, Balchraggan, Balmacaan, Bunloit, Drumbuie and Strone Chapter 30 Objections Regarding Settlement Expansion Rate in the Hinterland Chapter 31 Local centres in the Hinterland 31.1 Beauly 31.2 Drumnadrochit Chapter 32 Key Villages in the Hinterland -
Earth As a Whole and Geographic Coordinates
NAME:____________________________________________________________ 1 GO THERE—MYSTERIES OF LOCH NESS, SCOTLAND Use FLY TO and enter Loch Ness, Scotland as the destination. The view will settle in at about 15 miles EYE ALTITUDE, centered about midshore on the northeast coast of the Loch. Note how the cursor (cross-hairs) is labeled Loch Ness, United Kingdom in the VIEW WINDOW. Describe the shape and orientation of Loch Ness based on this view in the box below. Does the shape of the Loch remind you of other bodies of land-based bodies of surface water, and if so what kind? Based on this observation and comparison, describe whether or not the water in the lake is predominantly stationary or rapidly flowing, and give reasons for your arguments in the box below. Without using the ZOOM feature, use the HAND CURSOR and sweep across the lake and along its axis and to determine the average elevation of the lake. Remember that Google Earth® uses an averaging mechanism of regularly spaced coordinates to generate elevations, and that the apparent elevation of the lake is affected by elevations along its shoreline. Record and interpret your findings below. Go to the LAYERS WINDOW, and make sure that the WATER BODIES LAYER is checked in the folder of Geographic Features. In the box below, what do you suppose, based on the other labeled water bodies in the area, the word Loch means? Turn off the WATER BODIES LAYER. The outlines of the WATER BODIES LAYER does not directly overlie the images used as the base for GOOGLE EARTH® in the VIEW WINDOW. -
Watershed Science
Watershed Science This lesson is part of an ongoing monthly series that encourages young adults to learn about the environment through hands-on activities. These activities are recommended for ages 8+ and are designed using materials that most households have on-hand. Where does water come from? Why is it important? What is a watershed? This month, we will explore how water moves on Earth, what a watershed is and why it’s important, and find out what watershed area we live in! Did you know that the water we use today is the same water the dinosaurs used! So how does it move around the earth? Let's find out by making our own model of the water cycle! Model Water Cycle Materials: ❏ 1-quart sized freezer bag ❏ 1 permanent marker ❏ 1 cup of water ❏ Tape *recommend using clear packing tape ❏ Blue Food Coloring *recommended but not necessary ❏ Nature Journal (Click here for activity sheet) Directions: 1. Using a permanent marker, draw a water scene on the outside of the bag including water/waves at the bottom of the bag and clouds and the sun at the top of the bag. 2. Fill the measuring cup with 1 cup of water and add 2 drops of blue food coloring. Carefully stir in food coloring. 3. Slowly pour the water into the freezer bag and seal the bag completely. 4. Tape bag to a sunny window using tape. Choose a window that gets the most sunlight during the day. 5. Check on the bag during the day/several times a day and observe the changes.