Effects on the Environment of the Abandonment of Agricultural Land
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Johannes Fröhlinger: „The Return of the Deutschland Tour on Roads I Know – It Could Hardly Be Better”
Johannes Fröhlinger: „The return of the Deutschland Tour on roads I know – it could hardly be better” Johannes Fröhlinger is one of the most experienced German pros in the peloton. The 32-year-old with Team Sunweb has just ended his 11th year as a pro cyclist and extended his contract through 2019. The native of Gerolstein is a cornerstone of his team as its road captain. With his cycling roots in the Eifel, Fröhlinger feels especially good on the challenging rolling terrain. Trier is your second home: You grew up barely 500 kilometers away from Trier. Your family lives in Trier and you spend a lot of time in the region. Now the Deutschland Tour is coming to Trier in the first year of its new life. Your first reaction? “That was fantastic news. My first thought was immediately: I have to be there. On the same day I told my team of my wish to include that in the season planning. Hopefully it will work out. Race days for us German riders on our native soil have been drastically reduced over the last decade. At the last Deutschland Tour in 2008, I was at the start. Starting again in the race and then riding on familiar roads, that could hardly be better for me personally.” You know the terrain of the Moselle valley as well as the distinctive climbs in the Eifel and Hunsrück like you know the back of your hand. What can your colleagues in the peloton and especially the fans of the Deutschland Tour look forward to? “The region offers an incredible variety of roads. -
Vom Westerwald Zum Odenwald
IÖ. Dicht] / Wnithnmm, erhalte ihn deinem Revier Vom Westerwald zum Odenwald l" O X (I. B. L E l'ER K t' S Die Stille des Spätsommerabends 1953 liegt über den dun- ein starker Bock mit einem allerdings kiümmerlichen lau- kelgrünen Wäldern des Frankenlandes. Ich sitze an den scherhohen Spießergehörn näher. Schon hatte er den jungen „Waldwiesen“ auf einer hohen Leiter in Erwartung der Sediser eräugt, und mit laut vernehmlichem Keuchen ging Sauen, die hier gern durchwechseln. Da sie aber erst im die Jagd los, quer über die Felder und Hänge hinunter, letzten Dämmerlicht zu Felde ziehen, habe ich Zeit und wieder hinauf durch den Schlag, in den Buschwald hinein Muße, die beiden letzten, der Blattzeit gewidmeten Wochen und wieder ins Feld zurück. Laut fiepend flüchtete der Jüng- im Geiste vorüberziehen zu lassen. ling vor seinem Verfolger her. Nach einiger Zeit kam ein Wieder war ich der Einladung guter Freunde im Westen einzelnes Stück Rehwild im Troll vom Feld zurück. Im Glas und Süden gefolgt. Spät am Abend traf ich, aus dem Siegtal erkannte ich sofort an seinem kräftigen Vorschlag und dem kommend, im W'esterwald ein. Natürlich war ich am ersten dicken Träger den alten Bock. Eilig zog er in den Schlag, Morgen im lieben alten Revier meines Freundes draußen. auf den sich plötzlich ein lichter Nebeldunst legte. Rasch Oben auf der „Alm“ steht eine Kanzel, von der man weit über fiepte ich noch ein-, zweimal. Da verhoffite er, und im Knall die Westerwälder Höhen schauen kann. Dort stieg ich hin- sah ich noch gerade, daß er sich nach hinten überschlug. -
The Real Crisis of Scottish Agriculture
Scottish Government Yearbook 1985 THE REAL CRISIS OF SCOTTISH AGRICULTURE DUNCAN CAMPBELL DEPARTMENT OF SOCIOLOGY UNIVERSITY OF EDINBURGH Scottish and British agriculture has over the past fifty years undergone a transformation so profound that it is barely recognisable from the past. State support, technological innovation, new practices, new products have all transformed the agrarian economy and society of Scotland, and, in many places, the face of the land itself. This article attempts to identify and evaluate the most important economic and political developments bearing upon Scottish agriculture in the Seventies and Eighties. We start, however, with a brief history of agriculture support policies in Britain. The "Great Depression" to 1939 British agriculture reached its zenith of prosperity in the 1860s. Around 1875 it entered a period of sustained depression-of falling product and land prices, lower rents and untenanted farms- which was to continue for almost forty years, ending only with the outbreak of world war. It was in this period that farming finally ceased to be Britain's major industry, unable to compete with imports of cheap grain and meat from Latin America, Australia, New Zealand and the American prairies. The effects of what became known as the "Great Depression" were most marked in the wheat growing areas of England. Scottish farming, being more dependent on stock activities and with only a small-scale involvement in wheat production, survived the shock of the depression better. If Symon is to be believed this was due also in no small measure to the moral sturdiness and resourcefulness of the Scottish farmer, who countered adversity by, " .. -
River Cruises Cover
2 2018 EUROPEAN RIVER CRUISE COLLECTION The relaxing 0 way to cruise r w The Dutch and Belgian Waterways, We are also voyaging to the Channel The Main, Rhine & I Moselle Rivers " " " " " " " " " " " " " " " " " Welcome to the 2018 Hebridean River Cruise Collection Relaxing, informative, sociable and stimulating – just some of the words which can be used to describe a Hebridean river cruise in Europe. A cruise holiday with Hebridean is like no other, with meticulous attention to the finest details and an elegant charm that is simply unique. Travelling effortlessly to some of Europe’s finest towns and cities, every one of our itineraries will allow you to uncover the soul and make up of each destination. In the style of a 1930’s club, Royal Crown is elegant and understated, with its spacious panoramic lounge containing comfortable sofas and armchairs, and a single sitting restaurant which serves a mix of British and continental cuisine. So put your feet up and choose your Hebridean river cruise from this enticing selection and then relax, safe in the knowledge that Hebridean Island Cruises will be looking after you on a journey which is going to transport you back in time to the Golden Age of cruising. We look forward to seeing you in 2018. Ken Charleson Managing Director Contents The Hebridean Difference 2-3 The Hebridean Connection 4 The Faces of Hebridean 5 Life On Board with Hebridean 6-7 Dining and Cuisine with a Hebridean Influence 8-9 Going Ashore with Hebridean 10-11 Hebridean’s Renowned Guest Speakers 12-13 Itineraries 14-21 Grand River Voyages of Europe 22-23 Good Connections 24 Royal Crown Deck Plans 25 Royal Crown Cabins 26-27 General Information 28-29 Conditions of Business 30-34 Booking Form 35 Map of European Rivers 38 Moselle Valley The Hebridean Difference Genuinely fully-inclusive cruises Hebridean river cruises are fully-inclusive; not an empty promise but a Hebridean pledge to ensure that you have a carefree holiday both on board and ashore. -
Status and Population Trend of Corncrake Crex Crex in Germany
VOGELWELT 136: 113 – 119 (2016) 113 Status and population trend of Corncrake Crex crex in Germany Jochen Bellebaum, Christoph Grüneberg & Johanna Karthäuser Bellebaum, J., C. Grüneberg & J. Karthäuser 2016: Status and population trend of Corncrake Crex crex in Germany. Vogelwelt 136: 113 – 119. During the last 20 years our knowledge of the Corncrake breeding distribution and trends in numbers in Germany has greatly improved, despite the difficulties in surveying the species. Data from previous (1974-1995) and recent (2005-2009) breeding bird atlas work show the presence of Corncrakes in all major natural regions as well as an overall increase in atlas grid occupancy. The increase was most obvious in the Northern German Plain, whereas in the Southwest occupancy dropped by a factor of 0.56. Densities of calling males in selected core breeding sites recorded since 1990 showed a signifi- cant trend with an increase before and a decrease after 1998. Influx years in 1998-1999, 2002-2003, 2007-2008, and to a lesser extent 2012 led to a high degree of year-to-year variation. In such years much higher numbers are found outside the core breeding areas, too. These fluctuations were also reflected in estimates of national population size regularly produced in the course of national Red List updates. Key words: Corncrake Crex crex, Germany, breeding population, trend, distribution. 1. Introduction Only 20 years ago, there was considerable uncertainty mately 11 x 11 km) referring to the topographic maps 1:25,000 about occurrence and population trends of the Corn- (Gedeon et al. 2014). Breeding distribution in the eastern crake in Germany (Hashmi 1991, Stiefel 1991). -
A Guide to Bryologically Interesting Regions in Germany
A GUIDE TO BRYOLOGICALLY INTERESTING REGIONS IN GERMANY with contributions by K. von der Dunk, R. Lotto, R. Lübenau and G. Philippi edited and translated by Jan-Peter Frahm prepared for a bryological fieldtrip during the XIV Botanical Congress, Berlin 1987 THE FICHTEL MOUNTAINS by Klaus von der Dunk 1. General Information 1.1 Location The Fichtelgebirge is situated in the northeastern part of Bavaria and is enclosed to the north and East by the borders of the German Democratic Republic and the CSSR. The name "Fichtel"gebirge probably does not link with the spruce trees (Fichte = Picea abies), which is much abandoned today, but there is a word conjunction with some kind of sprites, called "Wichtel" in German, who are supposed to live in dark woods. The Fichtelgebirge has the shape of a horseshoe open to the east The interior part with the city of Wunsiedel is in about 600 m altitude. The surrounding mountains raise up to 1000m (Schnee-berg, Ochsenkopf). The Fichtelgebirge is part of the main water draining line: three rivers flow to the North Sea (Saale, Eger, Main), while the fourths (Naab) flows (via Danube) to the Black Sea. 1.2. Geology The Fichtelgebirge lies beyond a famous fault, the so-called Fränkische Linie (Fig.1). This fault divides the mesozoic layers of sedimentary rocks in the Southwest from the granitic igneous rocks in the Northeast. The mountain area itself consists of granite, now and then intruded by magma, especially in the southern part. In several places one can see large basalte quarries. The higher elevations of the granitic massif are often eroded to solitary rocks called "Blockmeere". -
National 4/5 Geography Rural Change Summary Notes and Past
National 4/5 Geography Rural Change Summary Notes and Past Paper Questions 1 National 4/5 Geography Rural Change By the end of this unit you will: 1. Be able to explain key terms in farming 2. Be able to describe and explain the main characteristics of a rural landscape in a developed country (extensive commercial farming in East Anglia) 3. Be able to describe and explain changes that have taken place, the reasons and the impact of these, in a rural landscape in a developed country 4. Be able to describe and explain the main characteristics of a rural landscape in a developing country (intensive subsistence farming in India) 5. Be able to describe and explain changes that have taken place, the reasons and the impact of these, in a rural landscape in a developing country Introduction Types of Farming Intensive Farming Intensive farms generally take up a fairly small area of land, but aim to have a very high output, through massive inputs of capital and labour. These farms use machines and new technologies to become as efficient and cost-effective as possible. Extensive Farming Extensive farming is the direct opposite of intensive farming. The farms are large in comparison to the money injected into them or the labour used. The cattle ranches of central Australia area good example of extensive agriculture, where often only a few farm workers are responsible for thousands of acres of farmland. Subsistence Farming Subsistence farmers only produce enough to feed themselves and their family, without having any more to sell for profit. -
Biodiversity of the Hercynian Mountains of Central Europe
Pirineos, 151-152: 83 a 99, JACA; 1998 BIODIVERSITY OF THE HERCYNIAN MOUNTAINS OF CENTRAL EUROPE JAN JENÍK Faculty of Science, Charles University, Benátská 2, CZ-12801 Praha 2, Czech Republic SUMMARY.- The vegetation of temperate Central Europe north of the Alps is mainly of low diversity broadleaf and conifer forest. The occurrence of three azonal habitat types: mires with their numerous microhabitats, the georelief of the karst and its deeply-cut river valleys, and ecological islands with a distinct vegetation near the treeline of the middle-mountains causes local areas of high diversity. These high species diversity spots are the result of an interplay between physical, biotic and historical factors. A model of an anemo-orographic system with its underlying factors is described to explain the high plant and animal diversity in the corries (glacial cirques) of the Hercynian mountains. RÉSUMÉ.-La végétation de l'Europe Centrale tempérée au nord des Alpes nous montre surtout des forêts à de feuillues et de connifères à faible diversité. Cependant, la présence de trois types d'habitats azonaux peut produire une haute diversité au niveau local: zones humides avec leur nombreux microhabitats, reliefs karstiques et leur profonds défilés fluviaux, et enfin des îles écologiques avec une végétation par ticulière situées près de la limite supérieure des arbres (treeline). Ces secteurs riches en espèces peuvent s'expliquer par l'interaction des facteurs physiques, biotiques et historiques. Dans ce domaine nous proposons un système anémo-orographique avec ses facteurs inféodés qui pourrait expliquer la haute diversité animale et végétale dans les cirques glaciaires des montagnes hercyniennes. -
Naturräumlich-Ökologische Analyse Der Flechtenflora Von Deutschland
624 Herzogia 28 (2) Teil 2, 2015: 624 – 653 Naturräumlich-ökologische Analyse der Flechtenflora von Deutschland Ulf Schiefelbein*, Florian Jansen, Birgit Litterski & Volkmar Wirth Zusammenfassung: Schiefelbein, U., Jansen, F., Litterski, B. & Wirth, V. 2015. Naturräumlich-ökologische Analyse der Flechtenflora von Deutschland. – Herzogia 28: 624 – 653. Die Flechtenflora von Deutschland wird auf der Grundlage der Angaben von Wirth et al. (2013; Die Flechten Deutschlands) analysiert, wobei Naturräume die geografische Basis für die Analysen bilden. Bewertet werden Artendiversität, Exklusivität des Arteninventars, substratspezifische Eigenschaften (Substratbindung, pH-Werte und Nährstoffgehalt/Eutrophierung der besiedelten Substrate) und klimatische Faktoren (Licht, Luftfeuchte). Die artenreichs- ten Naturräume sind nach den Bayerischen Alpen, dem Schwarzwald und Odenwald-Spessart die ebenfalls sehr nieder- schlagsreichen Naturräume Eifel, Weserbergland, Harz, Fränkische Alb, Sauerland und Bayerisch-Böhmischer Wald. Die artenärmsten Landschaften liegen überwiegend im südlichen Teil des Nordostdeutschen Tieflandes. Die Exklusivität des Arteninventars eines Naturraumes wird als Anzahl der Arten, die in Deutschland nach 1950 nur in einem bis zwei Naturräumen nachgewiesen wurden, definiert. In der gesamten Bundesrepublik sind es 638 Arten, davon kommen die meisten in den Bayerischen Alpen, im Schwarzwald, Bayerischen Wald, Odenwald-Spessart und in der Schwäbischen Alb vor. Im gesamten Deutschland überwiegen die Gesteinsbewohner (47,6 % des Gesamtarteninventars), -
1/1 the Weather in Germany in November 2019
The weather in Germany in November 2019 A mild month that was somewhat too dry with below-normal sunshine Offenbach, 29 November 2019 – Low-pressure areas mostly determined the weather in November 2019. During the first ten days of the month, these areas of low pressure followed a direct course from the west to central Europe, frequently bringing precipitation and mild air. They then skirted Germany so it still remained dry in spite of the low air pressure. During this time, the temperatures were often dependent on the dispersal of the fog and low stratus cloud cover, which then occurred frequently. In summary, November was somewhat too mild and too dry yet with below-normal sunshine. This is what the initial analysis by the Deutscher Wetterdienst (DWD) of data from its around 2,000 weather stations shows. A predominantly mild November At 5.2 degrees Celsius (°C), the average temperature in November was 1.2 degrees higher than the figure for the international reference period for 1961–1990. Compared to the warmer reference period 1981–2010, the temperature was 0.8 degrees higher. Inflows of subtropical air temporarily reached large swathes of Germany at the start of November. These caused the mercury to rise to over 17 °C on 2 November, with Ohlsbach near Offenburg registering the highest November temperature of 20.1 °C. The rest of November was much cooler, but it was still mild. In the second and third ten-day periods, temperatures were frequently determined by the dispersal of fog and low stratus cloud cover as well as the position of low-pressure areas. -
Middle and Upper Pleistocene Fluvial Evolution of the Meurthe and Moselle Valleys in the Paris Basin and the Rhenish Massif ⅲ
Quaternaire, 16, (3), 2005, p. 201-215 MIDDLE AND UPPER PLEISTOCENE FLUVIAL EVOLUTION OF THE MEURTHE AND MOSELLE VALLEYS IN THE PARIS BASIN AND THE RHENISH MASSIF Ⅲ Stéphane CORDIER*, Manfred FRECHEN**, Dominique HARMAND*** and Monique BEINER**** ABSTRACT The terrace systems of the River Meurthe (Me), and the River Moselle (M) downstream from the present Moselle-Meurthe confluence are composed of eight stepped alluvial terraces (Me8-M8 to Me1-M1), situated at less than 90 m above the modern floodplain Me0-M0. Morphological, mineralogical and petrographical studies evidence that the oldest five terraces (Me8-M8 to Me4-M4) were formed by the “Palaeo-Meurthe”, while the Upper Moselle flowed towards the Meuse valley. Downstream from the confluence, the three youngest alluvial terraces (Me3-M3 to Me1-M1) contain crystalline sediments from the Upper Moselle basin; they have been formed since the Upper Moselle capture, dated about 250-270 ka before present. IRSL and radiocarbon datings provide independent absolute age control for these post-capture terraces, which respectively correlate with the end of the Saalian (Me3-M3) and the Weichselian (Me2-M2 and Me1-M1). The constant relative height of the terraces between France, Luxemburg and Germany gives evidences that there was no differenciated tec- tonic movements along the valley since at least the capture. A cyclic evolution scheme for the formation of the terraces is presented. The main gravel sedimentation occurred during cold periods (pleniglacial and late glacial phases), with a minor erosive period at the beginning of late glacial periods. Major incision occurs at the warm-to-cold transition. Key-words: Meurthe and Moselle valleys, alluvial terraces, alluvial sequences, IRSL datings, heavy minerals, Upper and Middle Pleistocene. -
2.14 Mean Annual Climatic Water Balance
2.14 Mean Annual Climatic Water Balance The climatic water balance (CWB) is defined as the difference between precipitation depth Baltic Sea. The whole lowland regions of Mecklenburg-Vorpommern (Mecklenburg-Western and the depth of potential evapotranspiration at a given site during a certain time period. Pomerania), Brandenburg, Sachsen-Anhalt (Saxony-Anhalt), and Sachsen (Saxony) have negative summer half-year balances, with average values sometimes drastically below In general climatology, climate classifications are usually based on the weather elements “air - 100 mm. The highest deficits in the summer half-year show values below -300 mm. In sum- temperature” and “precipitation depth”, from which e. g. the description of the aridity of the mers with abundant rainfall, positive half-year balances may be recorded too, what was the climate is derived, the so-called aridity index. However, in the context of water-resources case in about one third of the years in the series 1961–1990. management and hydrology, the climatic water balance is better suitable for the hydroclimatic characterisation of sites, areas or periods, because the (hydro-)climatic conditions are The period with mean negative monthly balances in the inland lowlands lasts from April to described directly by means of the water-balance effective elements “precipitation” or “poten- September/October. The highest monthly balance deficits below -100 mm are recorded in the tial evapotranspiration” in the dimension “mm”. Dependent on whether precipitation depth or months from May to July. Negative monthly balances may occur throughout the year, potential evapotranspiration depth prevails in the considered period, the climatic water provided dry weather prevails.