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Minutes of a Meeting with Bedford Borough Council Highways Department, Borough Cllr. T. Wootton, and Representatives from Staplo
Minutes of a Meeting with Bedford Borough Council Highways Department, Borough Cllr. T. Wootton, and representatives from Staploe, Little Staughton, Colmworth and Bolnhurst and Keysoe Parish Councils on Wednesday 19th February 2020 at 2pm at Keysoe Village Hall, Keysoe Row West, Bedford MK44 2JE Present: Andrew Prigmore (Bedford Borough Council Highways Dept.), Borough Cllr. T. Wootton, Lucy Crawford (Clerk to Staploe Parish Council), Cllr. Veronica Zwetsloot (Staploe Parish Council), Cllr. Kevin Head (Little Staughton Parish Council), Cllr. Gordon Johnstone (Wyboston Parish Council), Cllr. Martina Perry (Bolnhurst and Keysoe Parish Council) and Cllr. Beverley Brightman (Colmworth Parish Council). Apologies: Gareth Turner (Bedford Borough Council Highways Department) 1. Consider the introduction of a 50mph limit on Bushmead Road All the parish councils represented supported the introduction of reduced speed limits on the Bushmead Road to a maximum of 50mph but KH suggested it should be 40mph in places. They recounted witnessing several nasty accidents on the road (one requiring an airlift to hospital). They also recounted many near misses some of which they believed were due to large HGV’s passing at speed when the road is not wide enough and cars being forced into the middle of the road by potholes. They acknowledged that recent repairs had improved the worst areas of the road but were concerned that some areas with failing patches had not been addressed. Andrew Prigmore explained that the worst areas had been repaired at a cost of approximately £70K but they had to choose the worst areas due to their limited budget. He reported that police data showed that none of the accidents on the road had been directly caused by excess speed. -
Free JULY 2021
free JULY 2021 p.2 July’s E vents p.15 The Art of Danielle Barabé-Bussières p.3 Interview with Tony Belcourt p.11 Music at Daisy Dell Farm p.16 Bloomfest: Blooms & Art July’s Events ALL MONTH MUSIC Bittersweet Gallery presents Anne- Sat Night on Daisy Dell Farm, 7-10PM: Jul 237 Borden Road Marie Chagnon’s jewellery <burnstown. 17 Marie-Lynn Hammond; Jul 24, Mississippi Mills ON K7C 3P1 ca/bittersweet> Rick Fines. Outdoor concert. Perth. Phone: (613) 256–5081 Mississippi Valley Textile Museum $30, ticketsplease.ca presents Homage to Canadian Women, Jul 23, 7PM, Heather Rankin. Studio Editor: and Cloth & Consequence <mvtm.ca> Theatre Perth. Tix: harmonyconcerts. [from Jul 17] ca, $20-40 Kris Riendeau S.M.art Gallery presents Abstract + The Cove (Westport, 273-3636): 5-8PM [email protected] Landscape group show <sarahmoffat. unless noted; Wed Rack ‘n Tunes w/ theHumm Who’s Reading com> [to Jul 4] Shawn McCullough, 5:30-8PM; Sun Head Layout and Design: Sivarulrasa Gallery presents Gayle over Heels Kells [to Jul 2] & William Liao [to Jul Jul 2 Shawn McCullough Rob Riendeau 30] <sivarulrasa.com> Jul 3 Chris Murphy & Jon McLurg [email protected] Strévé Design Gallery presents Jul 5, 19 Matt Dickson Canadian Local: paintings, handweaving, Jul 6, 27 Nolan Hubbard Advertising/Promotions: jewellery <strevedesign.com> Jul 8, 22 Jazz Night w/Spencer Evans Trio Kris Riendeau: (613) 256–5081 Whitehouse Perennials presents Jul 9 Brea Lawrenson Bloomfest Garden Art Show & Sale Jul 10 Jason Kent [email protected] [from Jul 21] Jul 12 David James Allen Jul 13 Spencer Scharf Calendar Submissions: Jul 15 Eric Uren Rona Fraser Jul 16 Borgin & Benni FESTIVALS th [email protected] Jul 3-4, Almonte Celtfest online. -
2018 Celebrity Birthday Book!
2 Contents 1 2018 17 1.1 January ............................................... 17 January 1 - Verne Troyer gets the start of a project (2018-01-01 00:02) . 17 January 2 - Jack Hanna gets animal considerations (2018-01-02 09:00) . 18 January 3 - Dan Harmon gets pestered (2018-01-03 09:00) . 18 January 4 - Dave Foley gets an outdoor slumber (2018-01-04 09:00) . 18 January 5 - deadmau5 gets a restructured week (2018-01-05 09:00) . 19 January 6 - Julie Chen gets variations on a dining invitation (2018-01-06 09:00) . 19 January 7 - Katie Couric gets a baristo’s indolence (2018-01-07 09:00) . 20 January 8 - Jenny Lewis gets a young Peter Pan (2018-01-08 09:00) . 20 January 9 - Joan Baez gets Mickey Brennan’d (2018-01-09 09:00) . 20 January 10 - Jemaine Clement gets incremental name dropping (2018-01-10 09:00) . 21 January 11 - Mary J. Blige gets transferable Bop-It skills (2018-01-11 09:00) . 22 January 12 - Raekwon gets world leader factoids (2018-01-12 09:00) . 22 January 13 - Julia Louis-Dreyfus gets a painful hallumination (2018-01-13 09:00) . 22 January 14 - Jason Bateman gets a squirrel’s revenge (2018-01-14 09:00) . 23 January 15 - Charo gets an avian alarm (2018-01-15 09:00) . 24 January 16 – Lin-Manuel Miranda gets an alternate path to a coveted award (2018-01-16 09:00) .................................... 24 January 17 - Joshua Malina gets a Baader-Meinhof’d rice pudding (2018-01-17 09:00) . 25 January 18 - Jason Segel gets a body donation (2018-01-18 09:00) . -
The Untapped Potential of Scenic Routes for Geotourism: Case Studies of Lasocki Grzbiet and Pasmo Lesistej (Western and Central Sudeten Mountains, SW Poland)
J. Mt. Sci. (2021) 18(4): 1062-1092 e-mail: [email protected] http://jms.imde.ac.cn https://doi.org/10.1007/s11629-020-6630-1 Original Article The untapped potential of scenic routes for geotourism: case studies of Lasocki Grzbiet and Pasmo Lesistej (Western and Central Sudeten Mountains, SW Poland) Dagmara CHYLIŃSKA https://orcid.org/0000-0003-2517-2856; e-mail: [email protected] Krzysztof KOŁODZIEJCZYK* https://orcid.org/0000-0002-3262-311X; e-mail: [email protected] * Corresponding author Department of Regional Geography and Tourism, Institute of Geography and Regional Development, Faculty of Earth Sciences and Environmental Management, University of Wroclaw, No.1, Uniwersytecki Square, 50–137 Wroclaw, Poland Citation: Chylińska D, Kołodziejczyk K (2021) The untapped potential of scenic routes for geotourism: case studies of Lasocki Grzbiet and Pasmo Lesistej (Western and Central Sudeten Mountains, SW Poland). Journal of Mountain Science 18(4). https://doi.org/10.1007/s11629-020-6630-1 © The Author(s) 2021. Abstract: A view is often more than just a piece of of GIS visibility analyses (conducted in the QGIS landscape, framed by the gaze and evoking emotion. program). Without diminishing these obvious ‘tourism- important’ advantages of a view, it is noteworthy that Keywords: Scenic tourist trails; Scenic drives; View- in itself it might play the role of an interpretative tool, towers; Viewpoints; Geotourism; Sudeten Mountains especially for large-scale phenomena, the knowledge and understanding of which is the goal of geotourism. In this paper, we analyze the importance of scenic 1 Introduction drives and trails for tourism, particularly geotourism, focusing on their ability to create conditions for Landscape, although variously defined (Daniels experiencing the dynamically changing landscapes in 1993; Frydryczak 2013; Hose 2010; Robertson and which lies knowledge of the natural processes shaping the Earth’s surface and the methods and degree of its Richards 2003), is a ‘whole’ and a value in itself resource exploitation. -
Application Form for a Modification to the Definitive Map and Statement Wildlife and Countryside Act 1981 Central Bedfordshire
APPLICATION FORM FOR A MODIFICATION TO THE DEFINITIVE MAP AND STATEMENT WILDLIFE AND COUNTRYSIDE ACT 1981 CENTRAL BEDFORDSHIRE DEFINITIVE MAP AND STATEMENT FOR PUBLIC RIGHTS OF WAY To: Bedford Borough Council Public Rights of Way, Definitive Map Team, Bedford Borough Council, 4th Floor Borough Hall, Cauldwell Street, Bedford, MK42 9AP I, Charlotte Ditchburn, for and on behalf of the British Horse Society, of Abbey Park, Stareton, Kenilworth, Warwickshire. CV8 2XZ. hereby apply for an order under Section 53(2) of the Wildlife and Countryside Act 1981 modifying the Definitive Map and Statement for the area by:- a) Adding the public bridleway which runs from Point A on the application map (OSGR TL 07156 58556) the southern junction with Thurleigh Road, to Point B (OSGR TL 07699 59511) the junction with Bolnhurst and Keysoe Footpath 16. b) Upgrading part of Bolnhurst and Keysoe Footpath 16 to public bridleway which runs from Point B on the application map (OSGR TL 07699 59511), the junction with Bolnhurst and Keysoe Footpath 16, to Point C (OSGR TL 07783 59727) the junction of Bolhurst and Keysoe Footpath 10, Footpath 16 and Bridleway 15. c) Upgrading Bolnhurst and Keysoe Footpath 10 to public bridleway which runs from Point C on the application map (OSGR TL 07783 59727), the junction of Bolhurst and Keysoe Footpath 10, Footpath 16 and Bridleway 15, to Point D (OSGR TL 07420 60141) the junction of Bolhurst and Keysoe Footpath 10 and Hatch Lane. and shown on the map accompanying this application. I attach copies of the following documentary evidence in support of this application, namely extracts of:- I. -
New Insights Into the Glacial History of Southwestern
Annales Societatis Geologorum Poloniae (2018), vol. 88: 341–359 doi: https://doi.org/10.14241/asgp.2018.022 NEW INSIGHTS INTO THE GLACIAL HISTORY OF SOUTHWESTERN POLAND BASED ON LARGE-SCALE GLACIOTECTONIC DEFORMATIONs – A CASE STUDY FROM THE CZAPLE II GRAVEL PIT (WESTERN SUDETES) Aleksander KOWALSKI1, 2, Małgorzata MAKOŚ1 & Mateusz PITURA1 1Department of Structural Geology and Geological Mapping, Institute of Geological Sciences, University of Wrocław, pl. M. Borna 9, 50-204 Wrocław, Poland; e-mails: [email protected], [email protected] [email protected] 2Polish Geological Institute – National Research Institute, Lower Silesian Branch, al. Jaworowa 19, 50-122 Wrocław, Poland Kowalski, A., Makoś, M. & Pitura, M., 2018. New insights into the glacial history of southwestern Poland based on large-scale glaciotectonic deformations – a case study from the Czaple II Gravel Pit (Western Sudetes). Annales Societatis Geologorum Poloniae, 88: 341 – 359. Abstract: This paper presents the results of structural and sedimentological studies carried out in the outcrops of Quaternary (Middle Pleistocene) deposits near the village of Czaple in Lower Silesia, Western Sudetes. Fluvial sands, gravels and glacial tills traditionally assigned to the Middle Polish Pleistocene Glaciations (Odranian Glaci- ation) crop out in the active gravel pit Czaple II. In these deposits, the authors have recognised and documented nu- merous mesoscale glaciotectonic deformation structures that were previously undescribed from the mountainous part of the Sudetes. These structures represent effects of sediment deformation in both proglacial and subglacial settings, and include such features as asymmetrical and disharmonic folds, thrusts, steeply inclined reverse faults, normal faults and conjugate sets of fractures. -
Cainozoic Evolution of Lower Silesia, Sw Poland: a New Interpretation in the Light of Sub-Cainozoic and Sub-Quaternary Topography
Acta Geodyn. Geomater.Vol.1, No.3 (135), 7-29, 2004 CAINOZOIC EVOLUTION OF LOWER SILESIA, SW POLAND: A NEW INTERPRETATION IN THE LIGHT OF SUB-CAINOZOIC AND SUB-QUATERNARY TOPOGRAPHY Janusz BADURA 1) *, Bogusław PRZYBYLSKI 1) and Witold ZUCHIEWICZ 2) 1) Lower Silesian Branch, Polish Geological Institute, al. Jaworowa 19, 50-122 Wrocław, Poland 2) Institute of Geological Sciences, Jagiellonian University, ul. Oleandry 2A, 30-063 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received March 2004, accepted June 2004) ABSTRACT An analysis of the youngest tectonic movements by the use of either morphometric or instrumental techniques should take into account both exposed and buried fault zones. The sub-Cainozoic and sub-Quaternary surface maps presented in this study display buried palaeotopography whose interpretation proves helpful in identification of tectonic dislocations. Such a kind of analysis has been conducted for the area of Lower Silesia, including the Sudetes, Fore-Sudetic Block, and Fore-Sudetic Monocline. The maps have been constructed on the basis of well-bore data, vertical geoelectrical soundings, and detailed mapping of exposures of pre-Quaternary rocks. Well-bore data have been reinterpreted with a view to reconstruct the original depth to the top of the crystalline basement. Many archival borehole descriptions place the boundary between Tertiary strata and the Proterozoic-Palaeozoic substratum at the top of poorly weathered rocks, including regoliths of the crystalline substratum into the Tertiary cover. The presented maps portray for the first time the actual morphology of the sub-Cainozoic surface. A comparison between the sub-Cainozoic and sub-Quaternary surface maps enables us to document changes in tectonic mobility throughout Cainozoic times. -
How Do I Set up an Event with Event Planner? (District) How Do I Set up an Event with Event Planner? (District)
Help Articles > District Help > District - Administration Guide > Events & Calendar > How do I set up an event with Event Planner? (District) How do I set up an event with Event Planner? (District) Zach W. - 2021-03-02 - Events & Calendar Event Planner will let you plan and schedule events for your District. You can invite members and non- members to attend, arrange online payment, and much more. Events can be created by event chairs, executives, and site administrators. 1. To access the Event Planner feature, you must go to your district homepage and log in. Then, click on Member Area on the top right, under the homepage banner. 2. Along the top of the screen you will see several tabs. Click on the Events tab. 3. In the grey bar, just below click on Event Planner. 4. You are now on the Events page. To start setting up your new event, click on the Create a New Event button on the right side of the screen. 5. You are now on the Create New Event screen, where you can write a description of your event and set up the time and place of the event. First, enter a name for your event in the Event Name field. You also have the option to set the Status of event as Active or as a Draft. An Active event will allow registrations if registrations have been configured. A Draft event will not allow registrations, even if registrations have been configured. 6. Now, if you wish you can enter a unique Event Code. This makes it much easier for you to track member payments for events from within your Sage or Bambora merchant account. -
“Advanced Features of Qualtrics”(Updated)
1 “Advanced Features of Qualtrics” (updated) K-State Surveys (powered by Qualtrics®): http://survey.ksu.edu or http://survey.k-state.edu Demo Survey: https://kstate.qualtrics.com/SE/?SID=SV_5gTuBG8ZWa94tMx Training Handout: http://www.k-state.edu/ID/ExploringAdvancedQualtricsHandout.pdf Table of Contents “Advanced Features of Qualtrics” (updated) ................................................................................................ 1 Current Notices: ........................................................................................................................................ 2 Some New-ish Features ............................................................................................................................ 2 1. Some Changes with the Qualtrics Innovation Suite / Qualtrics (“quality” + “metrics” as a blended term) Research Suite: ............................................................................................................................ 2 2. New Navigation: ............................................................................................................................... 4 3. Capturing Survey Statistics (on the New Insight Platform): ............................................................. 5 4. Data and Databases: ........................................................................................................................ 5 5. Text Analysis on Qualtrics: .............................................................................................................. -
Burial and Thermal History of the Intra-Sudetic Basin (SW Poland) Constrained by 1-D Maturity Modelling – Implications for Coalification and Natural Gas Generation
Burial and thermal history of the Intra-Sudetic Basin (SW Poland) constrained by 1-D maturity modelling – implications for coalification and natural gas generation Dariusz Botor Kinetic maturity modelling was performed using publicly available vitrinite reflectance data, for nine well sections in the Intra-Sudetic Basin (NE part of the Bohemian Massif) in order to reconstruct its burial and thermal history. The modelling results indicate that the Carboniferous strata reached maximum palaeotemperatures of c. 100–260 °C in the latest Carboniferous to early Permian. The Carboniferous–Permian magmatic activity must have contributed to high heat flow (c. 90–150 mW/m2 during the late Palaeozoic), adding to the effect of sedimentary burial (to a total depth c. 3–6 km in the early Permian), and caused the coalification of organic matter (c. 0.6–4.5% of vitrinite reflectance), and finally natural gas generation. Major hydrocarbon products were dominated by methane. The second phase of temperature rise occurred due to mainly Late Cretaceous sedimentary burial, but it had no effect on the maturation of the Carboniferous organic matter. • Key words: Variscides, Bohemian Massif, Carboniferous, maturity modelling, coalification, vitrinite reflectance. BOTOR, D. 2020. Burial and thermal history of the Intra-Sudetic Basin (SW Poland) constrained by 1-D maturity modelling – implications for coalification and natural gas generation. Bulletin of Geosciences 95(4), 497–514 (11 figures, 1 table). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received January 30, 2020; accepted in revised form July 28, 2020; published online October 18, 2020; issued November 15, 2020. Dariusz Botor, AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, al. -
Relief Evolution of Landslide Slopes in the Kamienne Mts (Central Sudetes, Poland) – Analysis of a High-Resolution DEM from Airborne Lidar
Contemp.Trends.Geosci., 7(1),2018,1-20 DOI: 10.2478/ctg-2018-0001 Relief evolution of landslide slopes in the Kamienne Mts (Central Sudetes, Poland) – analysis of a high-resolution DEM from airborne LiDAR Aleksandra Osika*, Małgorzata Wistuba, Ireneusz Malik Faculty of Earth Sciences, University of Silesia in Katowice, Bedzinska 60, 41-200 Sosnowiec, Poland * corresponding author: [email protected] Received: 5th November, 2017 Accepted: 9th January, 2018 Abstract The aim of the study is to reconstruct the development of landslide relief in the Kamienne Mountains (Central Sudetes, SW Poland) based on a DEM from LiDAR data. Analyses of relief and geological maps in ArcGIS 10.5 and of slope cross-sections in Surfer 14 allowed to distinguish different types of landslide relief, developed in latites and trachybasalts lying above claystones and mudstones. The types vary from small, poorly visible landslides to vast landslides with complex relief. They were interpreted as consecutive stages of geomorphic evolution of hillslope-valley topography of the study area. Two main schemes have been established which explain the development of landslide slopes in the Kamienne Mts: (1) upslope, from the base of the slope towards the mountain ridge and (2) downslope, beginning on the top of the mountain ridge. The direction of landslide development depends on the thickness of volcanic rocks in relation to underlying sedimentary rocks. When the latter appear only in the lowest part of the slope, landslides develop upslope. If sedimentary rocks dominate on the slope and volcanic rocks form only its uppermost part, landslides develop downslope. The results show that landsliding leads to significant modifications of relief of the study area, including complete degradation of mountain ridges. -
Exhumation of the Orlica-Snieznik Dome
EXHUMATION OF THE ORLICA-SNIEZNIK DOME, NORTHEASTERN BOHEMIAN MASSIF (POLAND AND CZECH REPUBLIC) A thesis presented to the faculty of the College of Arts and Sciences of Ohio University In partial fulfillment of the requirements for the degree Masters of Science Jacob M. Glascock November 2004 This thesis entitled EXHUMATION OF THE ORLICA-SNIEZNIK DOME, NORTHEASTERN BOHEMIAN MASSIF (POLAND AND CZECH REPUBLIC) BY Jacob M. Glascock has been approved for the Department of Geological Sciences and the College of Arts and Sciences by David Schneider Assistant Professor of Geological Sciences Leslie A. Flemming Dean, College of Arts and Sciences Glascock, Jacob M. M.S. November 2004. Geological Sciences Exhumation History of the Orlica Snieznik Dome, Northeastern Bohemian Massif (Poland and Czech Republic) (80 p.) Director of Thesis: David Schneider The Orlica-Snieznik Dome (OSD), located in the northeastern Bohemian massif (Czech Republic and Poland), represents a Variscan massif consisting of widespread amphibolite-facies gneisses and migmatites enclosing eclogite and granulite crustal-scale lenses. 40Ar/39Ar thermochronology yielded cooling ages for white mica and biotite between 341 ± 1 Ma to 337 ± 0.6 Ma and 342 ± 1 Ma to 334 ± 0.6 Ma from the Snieznik mountains. One amphibolite-derived hornblende yielded an integrated Ar-Ar age of ca. 400 Ma. The Orlica mountains yielded cooling ages between 338 ± 0.9 Ma to 335 ± 0.5 Ma. U-Th-total Pb monazite geochronology confirms two thermal events, likely commencing at ca. 400 Ma with granulite facies metamorphism. The cooling ages of the gneisses and schists are consistent across the dome and represent rapid wholesale cooling of the OSD, on an order of 50 oC/m.y.