NKU Academic Exchange in Leon, Spain
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Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2008 Imagining Scotland in Music: Place, Audience, and Attraction Paul F. Moulton Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF MUSIC IMAGINING SCOTLAND IN MUSIC: PLACE, AUDIENCE, AND ATTRACTION By Paul F. Moulton A Dissertation submitted to the College of Music in partial fulfillment of the requirements of the degree of Doctor of Philosophy Degree Awarded: Fall Semester, 2008 The members of the Committee approve the Dissertation of Paul F. Moulton defended on 15 September, 2008. _____________________________ Douglass Seaton Professor Directing Dissertation _____________________________ Eric C. Walker Outside Committee Member _____________________________ Denise Von Glahn Committee Member _____________________________ Michael B. Bakan Committee Member The Office of Graduate Studies has verified and approved the above named committee members. ii To Alison iii ACKNOWLEDGMENTS In working on this project I have greatly benefitted from the valuable criticisms, suggestions, and encouragement of my dissertation committee. Douglass Seaton has served as an amazing advisor, spending many hours thoroughly reading and editing in a way that has shown his genuine desire to improve my skills as a scholar and to improve the final document. Denise Von Glahn, Michael Bakan, and Eric Walker have also asked pointed questions and made comments that have helped shape my thoughts and writing. Less visible in this document has been the constant support of my wife Alison. She has patiently supported me in my work that has taken us across the country. She has also been my best motivator, encouraging me to finish this work in a timely manner, and has been my devoted editor, whose sound judgement I have come to rely on. -
Scotland with the Greenville-Pitt County Chamber of Commerce
DISCOVER & EXPLORE SCOTLAND WITH THE GREENVILLE-PITT COUNTY CHAMBER OF COMMERCE Edinburgh, Scotland EARLY BIRD DISCOUNT BOOK & SAVE Click here to $3,399 PER PERSON $3,399 PER PERSON $3,099 PER PERSON $3,199 PER PERSON BOOK NOW if deposited by December 31st!* if deposited by February 14th!* Departing July 14, 2022 For more information, please contact Jackie Listecki at (252) 752-4101 HIGHLIGHTS: Edinburgh Castle and spend some and personal view of the course, leisure time exploring Calton we’d be happy to show you • Round trip scheduled airfare Hill and its unbeatable view of around following lunch.) Then, • Round trip transfers between Edinburgh before transferring to we’ll travel on to Inverness, the airports and hotels while overseas our hotel in Edinburgh. Few cities capital of the highlands. (B, L) • 6 nights hotel accommodation make such a strong impression Day 5: Inverness • 2 nights Edinburgh on the visitor as Edinburgh. After breakfast, enjoy a full day • 2 night Inverness Scotland’s capital is without a at leisure in Inverness where you • 2 night Glasgow doubt one of the most beautiful may wish to visit the Inverness • 8 meals: breakfast daily, 1 lunch and elegant cities in Europe. Castle and visit the Cathedral Join us for a Welcome Drink at and 1 dinner or meander alongside the loch. the hotel this evening before Or you have the option to join • Tours of: Edinburgh Castle, Rosslyn venturing out for dinner on your Chapel, Edinburgh, Inverness and us for a full day tour to the Isle own. of Skye with a visit to the Eileen Glasgow City Tours Day 3: Edinburgh • Time to visit: Dunfermline Abbey, Donan Castle; explore a 13th After breakfast, delve into Century Castle in the Highlands of Stirling Castle, St. -
English Project: Geography and History of Ireland And
ENGLISH PROJECT: GEOGRAPHY AND HISTORY OF IRELAND AND SCOTLAND • Explanation • Exercises on the topics • Group presentations • Evaluation GEOGRAPHY OF IRELAND LOCATION LOCATION • Is in the North Atlantic. It is separated from Great Britain to its east by the North Channel, the Irish Sea, and St George's Channel. • It is separated from the neighbouring island of Great Britain by the Irish Sea and the North Channel. • To the west is the northern Atlantic Ocean and to the south is the Celtic Sea, which lies between Ireland and Brittany, in France. • Is located in the north- west of Europe, between latitudes 51° and 56° N, and longitudes 11° and 5° W. • Ireland has a total area of 84,421 km2 • Ireland is the second- largest island of the British Isles, the third- largest in Europe, and the twentieth- largest on Earth • The region was subjected to glacier and periglacial erosion, for which the U-shaped valleys, the drumlin and the esker, which are characteristic of the periglacial forms, are common. • The limestones are covered by clays and sands from the remains of glacial erosion, forming the gentle hills that characterize the landscape of Irish countryside. • This structure explains the arrangement of mountain ranges, all of them coastal. The main ones are Macgillycuddy's Reeks, Comeragh Hills, Blackstair Mountains, Wicklow Hills, Sperrin Mountains, Bluestack Mountains, Derryveagh Hills, Ox Mountains, Nephinbeg Hills, Mountains Twelve Goods and Maumturks. • In the south there are some mountains a little further from the coast: the Galtee Mountains, the Silvermines Mountains and Slieve Bloom. • A ring of coastal mountains surround low plains at the centre of the island. -
Impacts of Climate Change on Forests in Scotland (11 January 2008) Forest Research
Impacts of climate change on forests and forestry in Scotland Report compiled for Forestry Commission Scotland by: Duncan Ray, Ecology Division, Forest Research, Roslin, EH25 9SY Sections drafted by Duncan Ray, Dave Wainhouse, Joan Webber and Barry Gardiner January 2008 Impacts of climate change on forests in Scotland (11 January 2008) Forest Research Impacts of climate change on forests and forestry in Scotland .........................................1 Executive summary........................................................................................................3 1. Climate change in Scotland ...................................................................................6 1.1. Temperature ...................................................................................................6 1.2. Frost ...............................................................................................................7 1.3. Rainfall...........................................................................................................7 1.4. Summer heat and drought ..............................................................................8 1.5. Wind...............................................................................................................9 1.6. Conclusions..................................................................................................10 2. Managing the impacts of climate on forests and tree species..............................12 2.1. Species and provenance choice....................................................................12 -
In My Defence, God Me Defend-Expression, Saying
IN MY DEFENCE, GOD ME DEFEND-EXPRESSION, SAYING CLIMATE THE CLIMATE OF SCOTLAND IS TEMPERATE AND OCEANIC, AND TENDS TO BE VERY CHANGEABLE. IT HAS MUCH MILDER WINTERS AND COOLER WETTER SUMMERS THAN OTHER AREAS IN THE SAME LATITUDE (MOSCOW REGION IN RUSSIA, SOUTHERN SCANDINAVIA). HOWEVER, TEMPERATURES ARE GENERALLY LOWER THAN IN THE REST OF THE UK. IT HAD THE COLDEST EVER UK TEMPERATURE OF -27,2ºc IN THE GRAMPIAN MOUNTAINS ON 11TH FEBRUARY 1895. HEAVY SNOWFALL IS NOT COMMON IN THE LOWLANDS, BUT IT BECOMES MORE COMMON WITH THE ALTITUDE. BRAEMAR HAS AN AVERAGE OF 59 ANOW DAYS PER YEAR WHILE MANY COASTSAL AREAS AVERAGE FEWER THAN 10 DAYS OF LYING SNOW PER YEAR. THE WEST OF SCOTLAND IS USUALLY WARMER THAN THE EAST, OWING TO THE INFLUENCE OF ATLANTIC OCEAN CURRENTS. TIREE IS ONE OF THE SUNNIEST PLACES IN THE COUNTRY. RAINFALL VARIES WIDELY ACROSS SCOTLAND. THE WESTERN HIGHLANDS OF SCOTLAND ARE THE WETTEST. RAINFALL IN A FEW PLACES EXCEEDS 3,000 MM ANNUALLY. THE LOWLANDS RECIEVE LESS THAN 800 MM ANNUALLY. HISTORY: IT STARTED WHEN THE ROMANS OCCUPIED WHAT IS NOW ENGLAND AND WALES, ADMINISTERING IT AS A PROVINCE CALLED BRITANNIA. ROMAN INVASIONS AND OCCUPATIONS OF SOUTHERN SCOTLAND WERE A SERIES OF BRIEF INTERLUDES. ACCORDING TO THE ROMAN HISTORIAN TACITUS, THE CALEDONIANS ATTACKED ROMAN FORTS AND FOUGHT WITH THER LEGIONS, IN A SURPRISE NIGHT-ATTACK. THEY VERY NEARLY WIPED OUT THE WHOLE 9YH LEGION UNTIL IT WAS SAVED BY AGRICOL’AS CAVALRY. THE ROMANS ERECTED HADRIAN’S WALL TO CONTROL TRIBES ON BOTH SIDES OF THE WALL, AND THAT WAS THE NORTHERN BORDER OF THE ROMAN EMPIRE. -
Architecture KITTY LAI SHU YIN S1617644 UNIT 5 TRANS
UNIVERSITY OF EDINBURGH ARCHITECTURAL DESIGN: TECTONICS UNIT 5 TRANSFORMING SCOTLAND’S TOWNS KITTY LAI SHU YIN MA (Hons) Architecture 2019 - 20 Re-Thinking The High Street s1617644 FALKIRK COMMUNITY LIBRARY Unit 5 Transforming Scotland’s Towns Re-Thinking The High Street Located in the central lowlands of Scotland, Falkirk was histor- ically a crucial town for agriculture and manufacturing, which also connects to larger cities such as Edinburgh and Glasgow. Due to changes in retail and commercial patterns, the closure of retail shops caused a lack of variety and mobility in Falkirk’s high street. This addresses the need to reintroduce new and diverse energies in the high street. Falkirk is also the social and economic centre to 20 nearby dependent towns. Hence, the revitalisation of the Falkirk High Street is crucial not only for the local community but for the wider region. In a broader sense, the study of Falkirk town centre demonstrates the need for new purpose and vibrancy in many other high streets in Scotland today as they struggle to survive. With desert- ed town centres and automobile-dependent residential neigh- bourhoods, the call for the return of high-density living become more immediate. 02 According to USP figures, Falkirk has a significant number of res- idents who travel over 30 km to work and to study; these figures are much higher than other towns with more further education opportunities. The past of Falkirk has informed us of the momen- tous history of Technical institutes since the 1940s. It was until the 1960s when all of the four original trade training centres merged into a single Technical College, now known as the Forth Valley College. -
Science in Scottish Archaeology: Scarf Panel Report
Science in Scottish Archaeology: ScARF Panel Report Images © as noted in the text ScARF Summary Science Panel Document June 2012 ScARF Science in Scottish Archaeology Panel Karen Milek and Richard Jones (eds) With contributions from: Richard Bates, Paul Bishop, Kate Britton, Graeme Cavers, Ruby Ceron-Carrasco, Matthew Collins, Gordon Cook, Dave Cowley, Anne Crone, Alastair Dawson, Sue Dawson, Ian J. Fairchild, Oliver Craig, Andy Dugmore, Richard Jones, Peter Langdon, Roderick McCullagh, Kathleen McSweeney, Ingrid Mainland, Karen Milek, Anthony Newton, Sue Ovenden, Eva Panagiotakopulu, Ed Schofield, Marian Scott, Finlay Stuart, Scott Timpany, Richard Tipping, Lyn Wilson, Rob Wilson Abbreviations ED-XRF Energy-dispersive XRF FT IR Fourier Transform Infra Red spectrometry ICP-ES (MS) Inductively coupled emission spectrometry (mass spectrometry) NAA Neutron activation analysis ORA Organic residue analysis SAGES Scottish Alliance for Geosciences and Society SEM Scanning electron microscope SEM-EDAX SEM with energy-dispersive X-ray analysis XRD X-ray diffraction XRF X-ray fluorescence spectrometry Science in Scottish Archaeology Contents Executive Summary Introduction .................................................................................................................................i 1. Chronology ........................................................................................................................ 1 1.1 Introduction .............................................................................................................. -
Scotland's Landscape: Physical Features
Scotland's Landscape: Physical Features I can describe the major characteristic features of Scotland’s landscape and explain how these were formed. SOC 2-07a What are the physical features of a landscape? Can you list some of the physical features of Scotland’s landscape? Circle the words in the table below that are physical features of Scotland’s landscape: bridges mountains football stadiums rivers glens hills motorways islands coastline lochs Choose one of the physical features of Scotland’s landscape; what facts can you find out about it? Write your facts in the space below. Something extra… Think about how you could present these facts to the rest of the class! twinkl.co.uk Page 1 of 7 Scotland's Landscape: Physical Features I can describe the major characteristic features of Scotland’s landscape and explain how these were formed. SOC 2-07a On this map of Scotland, identify, colour and label these areas: the Highlands and Islands, the Central Lowlands and the Southern Uplands. Complete the key for your map. Legend Highlands and Islands Central Lowlands Southern Uplands twinkl.co.uk Page 2 of 7 Scotland's Landscape: Physical Features I can describe the major characteristic features of Scotland’s landscape and explain how these were formed. SOC 2-07a On this map of Scotland, identify and mark these mountain ranges: Grampians, Cairngorms, and the Cuillin mountains. Top Ten Highest Mountains in Height in Top Ten Highest Mountains in Height in Scotland Metres Scotland Metres 1. Ben Nevis 6. Cairn Gorm 2. Ben Macdui 7. Aonach Beag 3. -
Making of the Irish Landscape Pangaea • About 300 Million Years Ago the Earth Didn’T Have 7 Continents but One Supercontinent Called Pangaea
Making of the Irish Landscape Pangaea • About 300 million years ago the earth didn’t have 7 continents but one SUPERcontinent called Pangaea • Present-day Ireland was connected to Newfoundland • Pangaea split apart 200 million years ago • Ireland is on the Eurasian plate which drifted to its current position https://www.youtube.com/watch?v=vohv-kVfFAs Bedrock Geology of Ireland Igneous rocks are formed by the cooling and hardening of molten material called magma. Sedimentary rocks are formed by sediment that is deposited over time. Metamorphic rocks are formed when the appearance, texture and chemical composition of igneous or sedimentary rocks are changed by great heat, pressure or a combination of the two. Lowlands Most widely-distributed sedimentary rock is Carboniferous (365 -325 MYBP) limestone, the main rock across much of the central lowlands. It is generally light-grey in colour, and is hard. It was formed in warm, shallow tropical seas teeming with life. The rock is made up of the shells and hard parts of millions of sea creatures. Limestone covers over 50% of Ireland The Burren “There isn’t a tree to hang a man, water to drown a man nor soil to bury a man” Cork Red limestone The red colour comes from iron oxides eroded from the underlying Old Red Ringaskiddy Fota Sandstone. Coastal The coastal mountains vary greatly in geological structure. North and West: metamorphic rocks and granite. Metamorphic: Marble and quartzite Limestone changes into marble e.g. Connemara Marble Sandstone changes into quartzite e.g. Sugarloaf Mountain, Croagh Patrick Igneous: Granite is formed within the crust of the Earth when magma cools down without reaching the surface e.g Bloody Foreland & Mt Errigal in Donegal South - West Composed of Old Red Sandstone with limestone river valleys from the Devonian (415 MYBP) period. -
Natural Heritage Zones: a National Assessment of Scotland's
NATURAL HERITAGE ZONES: A NATIONAL ASSESSMENT OF SCOTLAND’S LANDSCAPES Contents Purpose of document 6 An introduction to landscape 7 The role of SNH 7 Landscape assessment 8 PART 1 OVERVIEW OF SCOTLAND'S LANDSCAPE 9 1 Scotland’s landscape: a descriptive overview 10 Highlands 10 Northern and western coastline 13 Eastern coastline 13 Central lowlands 13 Lowlands 13 2 Nationally significant landscape characteristics 18 Openness 18 Intervisibility 18 Naturalness 19 Natural processes 19 Remoteness 19 Infrastructure 20 3 Forces for change in the landscape 21 Changes in landuse (1950–2000) 21 Current landuse trends 25 Changes in development pattern 1950–2001 25 Changes in perception (1950–2001) 32 Managing landscape change 34 4 Landscape character: threats and opportunities 36 References 40 PART 2 LANDSCAPE PROFILES: A WORKING GUIDE 42 ZONE 1 SHETLAND 43 1 Nature of the landscape resource 43 2 Importance and value of the zone landscape 51 3 Landscape and trends in the zone 51 4 Building a sustainable future 53 ZONE 2 NORTH CAITHNESS AND ORKNEY 54 Page 2 11 January, 2002 1 Nature of the landscape resource 54 2 Importance and value of the zone landscape 72 3 Landscape and trends in the zone 72 4 Building a sustainable future 75 ZONE 3 WESTERN ISLES 76 1 Nature of the landscape resource 76 2 Importance and value of the zone landscape 88 3 Landscape and trends in the zone 89 4 Building a sustainable future 92 ZONE 4 NORTH WEST SEABOARD 93 1 Nature of the landscape resource 93 2 Importance and value of the zone landscape 107 3 Landscape and trends -
Sokrates USA A4 2
SCOTLAND Scotland is located in the north of Great Britain and it is one of the countries of the United Kingdom. The capital of Scotland is Edinburgh, and Glasgow is the largest Scottish city. English is the main language spoken in Scotland today. The country has two other official languages that include Scots and Scotland Scottish-Gaelic. The English spoken in Scotland is called Scottish English, United and the Scottish accent is very different from standard English. Kingdom Edinburgh The country can be divided into three parts – the Lowlands, the Northern Ireland Highlands and islands. There are over 700 islands in Scotland! There are also many deep lakes that are called lochs. The most famous lake is Loch Ness and people believe that a monster called ‘Nessie’ lives there. Nessie is often described as a England dinosaur-like creature, with a long neck, two humps and a tail. Many people Wales claim to have seen the monster, but there is no proof that Nessie really exists. Whether real or not, Nessie is famous all over the world! ST ANDREW’S CROSS The national flag of Scotland is called St Andrew’s Cross and it is the oldest flag in Europe. St Andrew is the patron saint of Scotland. There is an old legend that explains the origin of the Scottish flag. Saint Andrew was a fisherman from Galilee in the 1st century AD, and he became one of the twelve apostles – the disciples of Jesus Christ. The apostle was crucified by the Romans on an X-shaped cross and this is represented on the Scottish flag as the white cross in a blue sky. -
Climate Change and Changing Snowfall Patterns in Scotland John
Climate change and changing snowfall patterns in Scotland John Harrison1, Sandy Winterbottom2 and Richard Johnson3 University of Stirling, Scotland1, 2 Mountain Environments, Callander, Scotland3 2001 [email protected] Keywords: snow, snowfall, climate change, models, mountains, Scotland. Executive Summary Introduction The principal objective of the Report was to examine how snowfall patterns are expected to change in the light of climatic change scenarios and to review the possible socio-economic and environmental implications of such changes. An overview has been provided of the effects of changes in the duration of winter snow-lie on key activities within the socio-economic sector, and on key mountain habitats. The changes are such that adaptation strategies are required. The study was undertaken between March 2000 and April 2001 by Dr John Harrison and Dr Sandy Winterbottom of the Department of Environmental Science at Stirling University, and Dr Richard Johnson of Mountain Environments Consultancy in Callander, Perthshire. The study comprised four parts: An analysis of changes in Scottish snowfall patterns over the latter part of the 20th Century Obtaining, by questionnaire survey, expert opinion from key stakeholders on how the Scottish economy and environment have already responded to changes in snowfall Prediction of future changes in snowfall patterns driven by Greenhouse Effect enhancement over the course of the 21st Century Identification of key issues and adaptation strategies for dealing with such changes Climate change The IPCC Report (1996) indicated a reduction in the spatial extent of snow cover in the Northern Hemisphere of approximately 10% between 1973 and 1994. Although there is considerable regional and inter-annual variation in snow cover, there has been a significant trend towards reduced snow depth and cover duration since the 1970's.