On the Way of St. James in Switzerland a -Constance - Einsiedeln („Way of Svabia“) B - Rorschach - Einsiedeln („Way of St
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3470 Interlaken - Brienz (Brienzersee) Stand: 22
FAHRPLANJAHR 2021 3470 Interlaken - Brienz (Brienzersee) Stand: 22. Oktober 2020 vom 2.4.–25.6. 61 65 65 67 71 71 83 85 Spiez ab 09 34 11 34 11 34 12 34 14 34 14 34 15 34 16 34 Interlaken Ost an 09 58 11 58 11 58 12 58 14 58 14 58 15 58 16 58 Interlaken West ab 09 53 11 53 11 53 12 53 14 53 14 53 15 53 16 53 Interlaken Ost an 09 58 11 58 11 58 12 58 14 58 14 58 15 58 16 58 Interlaken Ost (See) 10 07 12 07 12 07 13 07 15 07 15 07 16 10 17 30 Bönigen 10 25 12 25 12 25 13 25 15 25 15 25 Ringgenberg (See) 12 33 12 33 13 33 15 33 15 33 Niederried (See) 13 43 Iseltwald (See) 10 45 12 51 12 51 13 51 15 51 15 51 16 42 18 02 Iseltwald (See) 10 46 12 52 12 52 13 52 15 52 15 52 Oberried am Brienzersee 10 56 Giessbach See 11 09 13 09 13 09 14 09 16 09 16 09 Brienz (See) 11 20 13 20 13 20 14 20 16 20 16 20 Brienz ab 11 25 13 25 13 25 14 25 16 25 16 25 Meiringen an 11 35 13 35 13 35 14 35 16 35 16 35 Brienz BRB ab 11 45 13 58 14 58 16 36 Brienzer Rothorn an 12 45 14 57 15 57 17 31 3470 Brienz - Interlaken (Brienzersee) Stand: 22. -
Eiger Bike Challenge 22 Km Holzmatten – Bort – Unterer Lauchbühl Grosse Scheidegg – First Waldspitz – Aellfluh Einfache Dorfrunde Grindelwald Rules of Conduct
Verhaltensregeln IG Bergvelo Eiger Bike Challenge 55 km Eiger Bike Challenge 22 km Holzmatten – Bort – Unterer Lauchbühl Grosse Scheidegg – First Waldspitz – Aellfluh Einfache Dorfrunde Grindelwald Rules of Conduct Grosse First Holzmatten Bort Holzmatten Grosse Scheidegg First Waldspitz Befahre nur bestehende Wege und respektiere vorhandene Sperrungen. 1690 Unterer Bort Scheidegg 2184 1565 Wetterhorn Terrassenweg Oberhaus Wetterhorn 1690 1964 2184 Oberhaus 1904 Terrassenweg Stählisboden 1964 Holenwang Oberhalb Bort Lauchbühl 1565 Nodhalten Nodhalten Grindelwald Bussalp 1226 Grindelwald Grindelwald 1140 1355 1226 Grindelwald 1548 1644 1355 1675 1675 Grindelwald Anggistalden 1140 1182 Kirche Gletscher- Grindelwald Meide die Trails nach Regenfällen und möglichst das Blockieren der Räder Grindelwald 1455 Grindelwald 2200 1036 1791 Oberhaus 1036 1036 1036 Wetterhorn Grindelwald Grindelwald Grindelwald Holenwang Aellfluh Grindelwald 1036 1038 schlucht 1036 Holenwang 1355 1036 1226 1036 2200 1036 1036 1036 1548 1430 1036 2000 beim Bremsen – dies begünstigt die Erosion. Bergwege sind keine Renn- 1548 Gletscher- 2000 1800 Wetterhorn schlucht 1800 1800 1800 strecken, darum fahre auf Sicht und rechne mit Hindernissen und anderen 1600 1226 Gletscher- schlucht 1600 1600 1600 1400 1400 1400 1400 1400 Nutzern auf den Wegen. Hinterlasse keine Abfälle. 1200 1200 1200 1200 1200 1200 1000 1000 1000 Only ride on existing trails and respect closures. Avoid using the trails after 1000 1000 1000 0202 5 10 152530 35 40 45 50 55 km 0 2 4 6 81810 12 1416 20 22 km 0122 4 6 81810 1416 20 22 24 km 0122 4 6 81810 1416 20 22 26 km 061 2 3 495 7128 1011 1314 15 16 17 19 km 061 2 3 495 7128 1011 13 14.5 km rainfall and wheel blockage when braking (to stop erosion). -
Hike the Swiss Alps 23Nd Annual | September 11-22, 2016
HIKE THE SWISS ALPS 23ND ANNUAL | SEPTEMBER 11-22, 2016 Guided by Virginia Van Der Veer & Terry De Wald Experience the Swiss Alps the best way of all – on foot with a small, congenial group of friends! Sponsored by Internationally-known Tanque Verde Ranch. Hiking Director, Virginia Van der Veer, and Terry DeWald, experienced mountaineer, lead the group limited to 15 guests. Having lived in Europe for many years, Virginia has in-depth knowledge of the customs of the people and places visited. She has experience guiding Alpine hiking tours and is fluent in German. Terry has mountaineering experience in the Alps and has guided hikers in Switzerland. INCLUDED IN PACKAGE… • Guided intermediate level day-hikes in spectacular scenery. • Opportunities for easy walks or more advanced hiking daily. • 5 nights hotel in Kandersteg, an alpine village paradise. • 1 day trip to Zermatt with views of the Matterhorn. • 5 nights hotel in Wengen with views of the Eiger and Jungfrau. • 2 nights in 4-star Swissotel, Zurich. • Hearty breakfast buffets daily. • 3 or 4-course dinners daily. • Swiss Rail Pass, allowing unlimited travel on Swiss railroads, lake streamers, PTT buses and city transports. • Day-trip to world-famous Zermatt at the foot of the Matterhorn. Opportunity for day-hike with views of the world’s most photographed mountain. • Visit to Lucerne. TOUR PRICING… Tour price $4,595(single supplement is $325 if required) Tour begins and ends in Zurich. A deposit of $800 is due at booking. Full payment is due at the Ranch by July 15. Early booking is advised due to small group size. -
Different Pockmark Systems and Their Potential Importance for the Hydrological and Biogeochemical Balance of a Perialpine Lake
Different pockmark systems and their potential importance for the hydrological and biogeochemical balance of a perialpine lake Adeline N.Y. Cojean*, Maciej Bartosiewicz**, Jeremy Zimmermann*, Moritz F. Lehmann**, Katrina Kremer*** and Stefanie B. Wirth* * Centre for Hydrogeology and Geothermics, University of Neuchatel, Rue Emile-Argand 11, CH-2000 Neuchâtel ([email protected]) ** Department of Environmental Sciences, University of Basel, Bernoullistrasse 30, CH-4056 Basel ***Swiss Seismological Service (SED), ETH Zürich, Sonneggstrasse 5, CH-8006 Zürich Lacustrine pockmarks Ø Much less investigated than marine pockmark systems Ø Fluid-flow formation Ø CH4 gas ebullition => Lake Constance (Wessel 2010; Bussmann, 2011) Ø Groundwater discharge => Lake Neuchâtel (Reusch 2015; Wirth et al., in prep.) Pockmarks in Lake Thun, Switzerland Thun Lake Thun Tannmoos Fault gypsum carying bedrock Einigen Fault Zone Spiez Fabbri et al., 2017 Beatenberg Interlaken Research questions Thun Ø Are there more pockmarks in Lake Lake Thun Thun? Ø If yes, where are they? Ø What is their mechanism of formation? Spikes in electrical Taanmoos conductivity Ø What is their influence on the lake hydrological and biogeochemical Einigen budget? Fault Zone Beatenberg karst system Spiez Beatenberg Beaten Connected to Daerligen karst system Interlaken Intensive CH4 bubbling Different pockmarks systems in Lake Thun Thun Lake Thun Connection to karst system leads to groundwater discharge? Tannmoos Einigen Fault Zone Beatenberg karst system Spiez Beatenberg Beaten Daerligen -
Climate Change and Tourism in Switzerland : a Survey on Impacts, Vulnerability and Possible Adaptation Measures
Climate Change and Tourism in Switzerland : a Survey on Impacts, Vulnerability and Possible Adaptation Measures Cecilia Matasci, Juan‐Carlos Altamirano‐Cabrera 1 Research group on the Economics and Management of the Environment Swiss Federal Institute of Technology Lausanne, CH1015 Lausanne, Switzerland, [email protected] The tourism industry is particularly affected by climate change, being very climate‐ and weather‐ dependent. Moreover, particularly in the Alpine region, it is specially exposed to natural hazards. Nonetheless, this industry is an important pillar of the Swiss economy, providing employment and generating income. Then, it becomes essential to reduce its vulnerability and starting implementing adaptation measures. In order to do so, it is important to define which areas face which problems and to recognize vulnerability hot spots. This motivation comes from the prospect that the largest environmental, social and economic damages are likely to be concentrated in vulnerable areas. This article presents an overview of the current state of the knowledge on the impacts, the vulnerability and the possible adaptation measures of the tourism industry in relation to climate change. Moreover, it presents different methods that could help assessing this vulnerability, referring in particular to the Swiss situation. This is the first step toward the establishment of the vulnerability analysis and the consequent examination of possible adaptation measures. Keywords: climate change, adaptation, vulnerability, tourism, Switzerland Introduction Climate change is a global phenomenon, but its effects occur on a local scale. Moreover, these effects have a clear impact on economic activities. An example of an activity heavily affected is tourism. Tourism is closely interlinked with climate change both as culprit and as victim. -
Swiss: 1,600 Kilometres Long, It Spans Four 4 /XJDQR࣠±࣠=HUPDWW Linguistic Regions, Five Alpine Passes, P
mySwitzerland #INLOVEWITHSWITZERLAND GRAND TOUR The road trip through Switzerland Whether you’re travelling by car or by motorcycle – mountain pass roads like the Tremola are one of the highlights of the Grand Tour of Switzerland. Switzerland in 10 stages Marvel at the sunrise over the 1 =XULFK࣠±࣠$SSHQ]HOO Matterhorn at least once in your lifetime. p. 12 Don’t miss wandering through the vine- yards of the winemaking villages of the 2 $SSHQ]HOO࣠±࣠6W0RULW] Lavaux. Or conquering the cobblestoned p. 15 Tremola on the south side of the Gotthard Pass. The Grand Tour of Switzerland is a 3 6W0RULW]࣠±࣠/XJDQR magnificent holiday and driving experi- p. 20 ence – and a concentration of all things Swiss: 1,600 kilometres long, it spans four 4 /XJDQR࣠±࣠=HUPDWW linguistic regions, five Alpine passes, p. 24 12 UNESCO World Heritage Properties and 22 stunning lakes. MySwitzerland is happy 5 =HUPDWW࣠±࣠/DXVDQQH to present a selection of highlights from p. 30 10 fascinating stages. Have fun exploring! 6 *HQHYD±࣠1HXFKkWHO p. 32 7 Basel 7 ࣠±࣠1HXFKkWHO 1 2 p. 35 10 8 9 8 1HXFKkWHO࣠±࣠%HUQ p. 40 3 9 %HUQ࣠±࣠/XFHUQH 6 5 4 p. 42 10 /XFHUQH±࣠=XULFK You will find a map of the Grand Tour at the back of the magazine. For more information, p. 46 please see MySwitzerland.com/grandtour 3 Grand Tour: people and events JUST LIKE OLD FRIENDS The Grand Tour of Switzerland is a journey of sights and discoveries. You will meet many different people along the tour, and thus enjoy the most enriching of experiences. -
3470 Interlaken - Brienz (Brienzersee) Stand: 28
FAHRPLANJAHR 2020 3470 Interlaken - Brienz (Brienzersee) Stand: 28. Oktober 2019 vom 4.4.–26.6. 61 65 65 67 71 71 83 85 Spiez ab 9 33 11 33 11 33 12 33 14 33 14 33 15 33 16 33 Interlaken West ab 9 52 11 53 11 53 12 52 14 53 14 53 15 53 16 52 Interlaken Ost (See) 10 07 12 07 12 07 13 07 15 07 15 07 16 10 17 30 Bönigen 10 25 12 25 12 25 13 25 15 25 15 25 Ringgenberg (See) 12 33 12 33 13 33 15 33 15 33 Niederried (See) 13 43 Iseltwald (See) 10 45 12 51 12 51 13 51 15 51 15 51 16 42 18 02 Iseltwald (See) 10 46 12 52 12 52 13 52 15 52 15 52 Oberried am Brienzersee (See) 10 56 Giessbach See 11 09 13 09 13 09 14 09 16 09 16 09 Brienz (See) 11 20 13 20 13 20 14 20 16 20 16 20 Meiringen an 11 35 13 35 13 35 14 35 16 35 16 35 Planalp an 12 15 14 30 14 27 15 27 17 03 14 30 Brienzer Rothorn an 12 45 14 57 15 57 17 31 3470 Brienz - Interlaken (Brienzersee) Stand: 28. Oktober 2019 vom 4.4.–26.6. 62 66 66 68 84 72 72 86 Brienzer Rothorn ab 12 20 13 28 15 28 Planalp ab 10 45 12 58 13 00 14 02 16 02 13 00 Meiringen ab 11 22 13 22 13 22 14 22 16 22 16 22 Brienz (See) 11 40 13 40 13 40 14 40 16 40 16 40 Giessbach See 11 51 13 51 13 51 14 51 16 51 16 51 Oberried am Brienzersee (See) 15 06 Iseltwald (See) 12 07 14 07 14 07 15 16 17 07 17 07 Iseltwald (See) 12 08 14 08 14 08 15 17 16 44 17 08 17 08 18 04 Niederried (See) 12 17 Ringgenberg (See) 12 28 14 28 14 28 17 28 17 28 Bönigen 12 35 14 35 14 35 15 35 17 35 17 35 Interlaken Ost (See) 12 53 14 53 14 53 15 53 17 18 17 53 17 53 18 38 Interlaken West an 13 03 15 03 15 03 16 03 17 32 18 03 18 03 19 03 Spiez an 13 21 15 21 15 21 16 21 17 50 18 21 18 21 19 21 1 / 5 FAHRPLANJAHR 2020 3470 Interlaken - Brienz (Brienzersee) Stand: 28. -
The 1996 AD Delta Collapse and Large Turbidite in Lake Brienz ⁎ Stéphanie Girardclos A, , Oliver T
Marine Geology 241 (2007) 137–154 www.elsevier.com/locate/margeo The 1996 AD delta collapse and large turbidite in Lake Brienz ⁎ Stéphanie Girardclos a, , Oliver T. Schmidt b, Mike Sturm b, Daniel Ariztegui c, André Pugin c,1, Flavio S. Anselmetti a a Geological Institute-ETH Zurich, Universitätsstr. 16, CH-8092 Zürich, Switzerland b EAWAG, Überlandstrasse 133, CH-8600 Dübendorf, Switzerland c Section of Earth Sciences, Université de Genève, 13 rue des Maraîchers, CH-1205 Geneva, Switzerland Received 13 July 2006; received in revised form 15 March 2007; accepted 22 March 2007 Abstract In spring 1996 AD, the occurrence of a large mass-transport was detected by a series of events, which happened in Lake Brienz, Switzerland: turbidity increase and oxygen depletion in deep waters, release of an old corpse into surface waters and occurrence of a small tsunami-like wave. This mass-transport generated a large turbidite deposit, which is studied here by combining high- resolution seismic and sedimentary cores. This turbidite deposit correlates to a prominent onlapping unit in the seismic record. Attaining a maximum of 90 cm in thickness, it is longitudinally graded and thins out towards the end of the lake basin. Thickness distribution map shows that the turbidite extends over ∼8.5 km2 and has a total volume of 2.72⁎106 m3, which amounts to ∼8.7 yr of the lake's annual sediment input. It consists of normally graded sand to silt-sized sediment containing clasts of hemipelagic sediments, topped by a thin, white, clay-sized layer. The source area, the exact dating and the possible trigger of this turbidite deposit, as well as its flow mechanism and ecological impact are presented along with environmental data (river inflow, wind and lake-level measurements). -
Stauverminderung Reichenbach Im Kandertal Bericht Zur Mitwirkung
Oberingenieurkreis I Ier arrondissement d'Ingénieur en chef Tiefbauamt Office des ponts et des Kantons Bern chaussées du canton de Berne Vorprojekt Strassen-Nr. 223 Revidiert Strassenzug Spiez - Frutigen - Kandersteg Projekt-Nr. 20023 / 14.014 Gemeinde Reichenbach im Kandertal Projekt vom 15.02.201220.12.2017 60 x 147 Bericht zur Mitwirkung Stauverminderung Reichenbach im Kandertal Projektverfassende LP Ingeneure AG B+S AG Laubeggstrasse 70 Weltpoststrasse 5 3000 Bern 31 3000 Bern 15 Tel. 031 359 40 40 Tel. 031 356 80 80 Gemeinde Reichenbach Stauverminderung Reichenbach im Kandertal– Mitwirkungsprojekt / Bericht zur Mitwirkung Verfasser, Impressum und Dokumentenverwaltung Verfasser Impressum Erstelldatum: 28.10.2017 letzte Änderung: 20.12.2017 Autoren: Marino Sansoni Auftragsnummer: B.14.014.02. Datei: H:\DAT\b_reiver\31_Vorproj\11_Mitwirkung\05_MW-Bericht - def. abgegeben\Be_2017_12_20_Mitwirkungbericht_DEF.doc Seitenzahl: 18 (ohne Beilagen) Dokumentenverwaltung Version Datum Autor Bemerkungen 02.11.17 SAM Entwurf an OIK I 09.11.17 SAM Vorabzug an Lenkungsausschuss, Freigabe durch LA 20.12.17 SAM Definitive Version an OIK I LP Ingenieure AG Seite I Bau Verkehr Projektmanagement 20.12.2017 Gemeinde Reichenbach Stauverminderung Reichenbach im Kandertal– Mitwirkungsprojekt / Bericht zur Mitwirkung Inhaltsverzeichnis Inhaltsverzeichnis 1 Problemstellung / Ausgangslage 1 2 Aufbau / Inhalt Bericht zur Mitwirkung 1 3 Die Mitwirkung 2 4 Auswertung der Fragebogen 3 5 Beurteilung der heutigen Situation 3 5.1 Vorbemerkungen zur Funktionsweise -
Human Impact on the Transport of Terrigenous and Anthropogenic Elements to Peri-Alpine Lakes (Switzerland) Over the Last Decades
Aquat Sci (2013) 75:413–424 DOI 10.1007/s00027-013-0287-6 Aquatic Sciences RESEARCH ARTICLE Human impact on the transport of terrigenous and anthropogenic elements to peri-alpine lakes (Switzerland) over the last decades Florian Thevenon • Stefanie B. Wirth • Marian Fujak • John Pote´ • Ste´phanie Girardclos Received: 22 August 2012 / Accepted: 6 February 2013 / Published online: 22 February 2013 Ó The Author(s) 2013. This article is published with open access at Springerlink.com Abstract Terrigenous (Sc, Fe, K, Mg, Al, Ti) and suspended sediment load at a regional scale. In fact, the anthropogenic (Pb and Cu) element fluxes were measured extensive river damming that occurred in the upstream in a new sediment core from Lake Biel (Switzerland) and watershed catchment (between ca. 1930 and 1950 and up to in previously well-documented cores from two upstream 2,300 m a.s.l.) and that significantly modified seasonal lakes (Lake Brienz and Lake Thun). These three large peri- suspended sediment loads and riverine water discharge alpine lakes are connected by the Aare River, which is the patterns to downstream lakes noticeably diminished the main tributary to the High Rhine River. Major and trace long-range transport of (fine) terrigenous particles by the element analysis of the sediment cores by inductively Aare River. Concerning the transport of anthropogenic coupled plasma mass spectrometry (ICP-MS) shows that pollutants, the lowest lead enrichment factors (EFs Pb) the site of Lake Brienz receives three times more terrige- were measured in the upstream course of the Aare River at nous elements than the two other studied sites, given by the the site of Lake Brienz, whereas the metal pollution was role of Lake Brienz as the first major sediment sink located highest in downstream Lake Biel, with the maximum val- in the foothills of the Alps. -
Constitution of an Automized Processing Chain to Analyse a Meris Time Series of Swiss Lakes
CONSTITUTION OF AN AUTOMIZED PROCESSING CHAIN TO ANALYSE A MERIS TIME SERIES OF SWISS LAKES Daniel Odermatt a, *, Thomas Heege b, Jens Nieke a, Mathias Kneubühler a and Klaus Itten a a Remote Sensing Laboratories (RSL), Dept. of Geography, University of Zurich, Winterthurerstrasse 190, CH-8050 Zurich, Switzerland - (dodermat, nieke, kneub, itten)@geo.unizh.ch b EOMAP GmbH & Co. KG, Sonderflughafen Oberpfaffenhofen, D-82205 Gilching, Germany - [email protected] KEY WORDS: Inland water, Case II water, lakes, MERIS, water constituents ABSTRACT: The physically based Modular Inversion & Processing System (MIP) is used in an automized processing chain for inland water constituent retrieval from MERIS level 1B data. Preprocessing routines are used to automatically convert the ESA generic data products into MIP input data format. Water/land masking, atmospheric correction and water constituent retrieval are accomplished by simple batch executables from MIP. The accuracy of the constituent retrieval mainly depends on the spectral fit between the image input data and the radiative transfer model results extracted from a database. Therefore, thresholds and initial values for model fitting have to account for all occurring lake specific temporal variations and need careful adjustment. 1. INTRODUCTION Heege, 2000), using the Modular Inversion & Processing System (MIP) (Heege and Fischer, 2004). Monitoring of water quality in lakes is required as an integral part of water resource management, in order to guarantee the In this work, a processing chain to automatically derive water sustainable use of water and to track the effects of constituents from MERIS level 1B data for Swiss lakes is built anthropogenic influences. Simultaneously, adequate monitoring around MIP. -
Verwaltungskreis Frutigen-Niedersimmental in Der Verwaltungsregion Oberland
VERWALTUNGSKREIS FRUTIGEN-NIEDERSIMMENTAL IN DER VERWALTUNGSREGION OBERLAND Der Verwaltungskreis Frutigen-Niedersimmental besteht seit dem 1. Januar 2010 und gehört zur Verwaltungsregion Oberland. Er umfasst eine Fläche von 785 km² und rund 40’000 ständige Einwohner innen und Einwohner verteilt auf 13 Gemeinden mit rund 40 öffentlich-rechtlichen Körperschaften (Burgergemeinden und -bäuerten, Schwellengemeinden, Kirchgemeinden). FREUNDLICH LÖSUNGSORIENTIERT BÜRGERNAH EFFIZIENT WOHLWOLLEND RATGEBEND Aufsichtsbehörde KOMPETENT • Gemeinden und öffentlich- VERTRAUT rechtliche Körperschaften Bewilligungsbehörde • Vormundschaftsrecht • Baubewilligungsverfahren • Koordination in ausserordentlichen • Gastgewerbe Lagen • Bodenrecht / • Aufsichtsrechtliche Anzeigen Grundstückverkäufe an Ausländer DIE BEREICHE UND Verwaltungsjustiz Ombudsfunktion AUFGABEN DER • Beschwerdeverfahren • Ansprechpartner für alle Fragen VERANTWORTLICHEN • Verständigung der Zentralverwaltung DES REGIERUNGS- STATTHALTERAMTES DIE ORGANISATION SEIT 2010 Regierungsstatthalter • Führung / Koordination • Entscheide / Einspracheverhandlungen • Ombudsperson • Bäuerliches Bodenrecht / ausserordentliche Lagen Stabsdienste • Bäuerliches Bodenrecht • Grundstückverkäufe an Ausländer • Stabsarbeit Stellvertretung des Regierungsstatthalters Bauen / Finanzen • Rechtsauskünfte • Baubewilligungsverfahren • Koordination Beschwerdeverfahren • Finanzen • Gemeindenaufsicht • Abstimmungen und Wahlen Kanzlei • Gastgewerbe • Inventar • Archiv • Vormundschaft ÜBERSICHT ÜBER DIE GEMEINDEN DES VERWALTUNGSKREISES