Physical and Geochemical Characterisation of Canal Sediments in the Black Country, West Midlands
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
PDF995, Job 6
The Wildlife Trust for Birmingham and the Black Country _____________________________________________________________ The Endless Village Revisited Technical Background December 2005 Protecting Wildlife for the Future The Endless Village Revisited Technical Background 2005 The Wildlife Trust for Birmingham and the Black Country gratefully acknowledges support from English Nature, Dudley MBC, Sandwell MBC, Walsall MBC and Wolverhampton City Council. This Report was compiled by: Dr Ellen Pisolkar MSc IEEM The Endless Village Revisited Technical Background 2005 The Endless Village Revisited Technical Background 2005 Contents Page 1. INTRODUCTION 1 2. EXECUTIVE SUMMARY 2 3. SITES 4 3.1 Introduction 4 3.2 Birmingham 3.2.1 Edgbaston Reservoir 5 3.2.2 Moseley Bog 11 3.2.3 Queslett Quarry 17 3.2.4 Spaghetti Junction 22 3.2.5 Swanshurst Park 26 3.3 Dudley 3.3.1 Castle Hill 30 3.3.2 Doulton’s Claypit/Saltwells Wood 34 3.3.3 Fens Pools 44 3.4 Sandwell 3.4.1 Darby’s Hill Rd and Darby’s Hill Quarry 50 3.4.2 Sandwell Valley 54 3.4.3 Sheepwash Urban Park 63 3.5 Walsall 3.5.1 Moorcroft Wood 71 3.5.2 Reedswood Park 76 3.5 3 Rough Wood 81 3.6 Wolverhampton 3.6.1 Northycote Farm 85 3.6.2 Smestow Valley LNR (Valley Park) 90 3.6.3 West Park 97 4. HABITATS 101 The Endless Village Revisited Technical Background 2005 4.1 Introduction 101 4.2 Heathland 103 4.3 Canals 105 4.4 Rivers and Streams 110 4.5 Waterbodies 115 4.6 Grassland 119 4.7 Woodland 123 5. -
Upper Neogene Stratigraphy and Tectonics of Death Valley — a Review
Earth-Science Reviews 73 (2005) 245–270 www.elsevier.com/locate/earscirev Upper Neogene stratigraphy and tectonics of Death Valley — a review J.R. Knott a,*, A.M. Sarna-Wojcicki b, M.N. Machette c, R.E. Klinger d aDepartment of Geological Sciences, California State University Fullerton, Fullerton, CA 92834, United States bU. S. Geological Survey, MS 975, 345 Middlefield Road, Menlo Park, CA 94025, United States cU. S. Geological Survey, MS 966, Box 25046, Denver, CO 80225-0046, United States dTechnical Service Center, U. S. Bureau of Reclamation, P. O. Box 25007, D-8530, Denver, CO 80225-0007, United States Abstract New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from N3.58 Ma to b1.1 ka. These tephra beds and tuffs establish relations among the Upper Pliocene to Middle Pleistocene sedimentary deposits at Furnace Creek basin, Nova basin, Ubehebe–Lake Rogers basin, Copper Canyon, Artists Drive, Kit Fox Hills, and Confidence Hills. New geologic formations have been described in the Confidence Hills and at Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ~3.3 Ma the Furnace Creek basin was a northwest–southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique–normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone. -
Walking and Cycling in the Black Country
in the Black Country Introduction There’s never been a better time to get active for your health and wellbeing. You’ve been advised to start being a bit more active and there’s lot of reasons why this is a good idea. We understand that making those first changes to your lifestyle can often be the hardest ones to take. This booklet will help you make decisions on how and where to be active in the surrounding area. PLEASE NOTE: Please be safe when visiting parks and open spaces. If outdoor gym or play equipment is available for use, please use it responsibly and follow Public Health England guidance on hand washing. Please don’t visit these spaces if you’re suffering with symptoms of coronavirus. Please keep your distance if you’re walking or on a bike, staying at least 2 metres away from other people. Benefits to Activity It also reduces your chances of developing a number of preventable health conditions 50% less chance of developing Type 2 Diabetes 50% less chance of developing high blood pressure 40% less chance of developing coronary heart disease 35% less chance of developing cardiovascular disease 30% less chance of having a stroke 25% less chance of developing certain types of cancer (including breast and colon) 25% less chance of developing joint and back pain 21% less chance of having a fall Love Exploring There are lots of ways to enjoy all of the open spaces that the Black Country has to offer. Active Black Country and local partners have teamed up with Love Exploring to bring a new interactive app to some of our parks and green It’s currently available at spaces. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Deal Hop . Batham's New
The Deal Dover Sandwich & District Branch Magazine Issue 75 Free Spring 20 l ^ j Inside: ♦ DEAL HOP After last year’s success, bigger and better this year? . BATHAM’S NEW PUB The start of a move back to more traditional style pubs? IN THIS ISSUE Local News Page 5 All the latest news from pubs in the Branch area Ramblings & Rumblings Page 14 'Stroller's' observations on his pub visits National News Page 17 Fullers buy Dark Star, National Pub of the Year, Brains to move and more Issue 75 Batham’s New Pub Page 18 Spring 2018 Could this start a return to more traditional pub formats White Cliffs Festival of Winter Ales 2018 Page 21 A review of this year's Festival Channel Draught The Uncryptic Crossword Page 23 is published and Channel View Page 25 ©2018 by the Comment & Opinion Deal Dover Sandwich Deal Hop Farm 2018 Page 27 & District Branch After last year's success, bigger and better in 2018. of the From Across the Water Page 28 Campaign for Real Ale Our 'foreign correspondent' makes a trip back to Kent The Potterers Cycle Club Page 30 www.camra-dds.org.uk Cycling and beer. Spring 2018 update Editorial T eam To the Pub By Bus Page 32 A response to the article in our last issue Editor & Advertising Dodging Downpours on the BCN Page 37 Martin Atkins A look back at the Beery Boaters 1993 trip to the Birmingham canals Editorial Assistants Last Knockings Page 42 Trisha Wells ‘Old W ort's' Musings John Pitcher Design & Format BRANCH DIARY Steve Bell Events shown in blue are not organised by C A M R A Editorial Address Fri 1 - Sun 3 Jun BeerFest & Family Fun Day, D uke of Cumberland, Barham You can write to the Editor Sat 2 Jun Medway CAMRA Beer Festival, Star c/o Beaconsfield House Meadow Sports Club, Gillingham 12 Noon Beaconsfield Road Thur 7 Jun G BG Trail - long walk. -
Display PDF in Separate
NRA Severn-Trent 36 TAME CATCHMENT MANAGEMENT PLAN CONSULTATION REPORT JANUARY 1996 v NRA N at ion a I Rivers Authority Sc v e rn - Trcn t R eg io n Your views We want your views, comments, ideas and criticisms This is the basis for consultation between the NRA and all those with interests in the catchment. Please consider:- o The Vision for the Catchment. o The issues and options identified in the report. o Alternative options for resolving identified issues. o Raising additional issues not identified in the report. o Raising anything else you feel is important. All comments received will be treated as public information unless you explicitly state otherwise in your response. Following the consultation period all comments received will be considered in preparing the next phase, the Action Plan. This Consultation Report will not be rewritten as part of the Action Plan process. We intend that the Plan should influence the policies and action of developers, planning authorities and other as well as assisting in the day to day management of the Catchment. A letter outlining the issues was sent to local authorities, national organisations, other representative bodies and representatives of the NRA Statutory Committees in the summer of 1995. All the comments have been incorporated into this document where possible. A list of organisations that were contacted is given in Appendix 1. We are grateful for the useful suggestions received. Comments on the Consultation Report should be sent to: Tony Stanley National Rivers Authority Upper Trent Area Sentinel House 9 Wellington Crescent Fradley Park Lichfield Staffs WS13 8RR All contributions should be made in writing by: 31 March 1996 If you or your organisation need further information or further copies of this Report, please contact Jonathan Jenkin at the above address or by telephone on (01543) 444141 Ext 4086. -
BCN Moorings Leaflet
FACILITIES GENERAL INFORMATION WATER POINTS he Birmingham Canal Navigations (BCN) is a 100 mile network of narrow Sherborne Wharf (Birmingham) [0121 456 6163] T canals situated at the very heart of the Midlands waterway system. There is, Farmers Bridge Top Lock (Birmingham & Fazeley) Holliday Wharf (just south of Gas Street Basin) arguably, no other inland waterways complex in the world which provides such Tividale Aqueduct (Netherton Tunnel Branch) vivid, sometimes breathtaking, contrasts. It would be difficult to imagine a canal Tividale Aqueduct (Old Main Line) landscape containing more features of interest to such a wide variety of users. Wolverhampton Top Lock Wolverhampton Lock No.15 BW Sneyd Yard (Wyrley & Essington) Unfortunately, the BCN harbours a serious burden – its image. To the uninitiated the Anglesey Bridge Marina (Anglesey Branch) [01543 454994] Longwood Junction (by Boat Club) BCN is still perceived as grimy and unpleasant, but this is simply not true. Perry Barr Top Lock Admittedly, some parts do pass through industrialised areas – but remember – that is Walsall Top Lock the reason they were built in the first place! There are many others which remain Parkhead Junction (next to pump house) Aldridge Marina (Daw End Branch) [01922 53397] amazingly rural and completely unspoilt. Nowhere is this more apparent than the Hawne Basin (Dudley No.2) delightful areas of the Northern BCN, providing many miles of tranquil, trouble-free Malthouse Stables, Tipton (Old Main Line) cruising. Cuckoo Wharf (Aston Locks) Canal Transport Services (Cannock Extension) [01543 374370] Grove Colliery Basin (Cannock Extension) Fortunately British Waterways, in conjunction with local canal societies and Black Country Museum Coronation Gardens, Tipton (Old Main Line) councils, has done much in recent years to enhance the waterside, to improve NEW – Windmill End (Dudley No.2) [next to new visitor centre]. -
Death Valley National Monument
DEATH VALLEY NATIONAL MONUMENT D/ETT H VALLEY NATIONAL 2 OPEN ALL YEAR o ^^uJv^/nsurty 2! c! Contents 2 w Scenic Attractions 2 2! Suggested Trips in Death Valley 4 H History 7 Indians 8 Wildlife 9 Plants 12 Geology 18 How To Reach Death Valley 23 By Automobile 23 By Airplane, Bus, or Railroad 24 Administration 25 Naturalist Service 25 Free Public Campground 25 Accommodations 25 References 27 UNITED STATES DEPARTMENT OF THE INTERIOR- Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON EATH VALLEY National Monument was created by Presidential proclamation on 2February 11), 1933, and enlarged to its present dimensions on March 26, 1937. Embracing 2,981 square miles, or nearly 2 million acres of primitive, unspoiled desert country, it is the second largest area administered by the National Park Service in the United States proper. Famed as the scene of a tragic episode in the gold-rush drama of '49, Death Valley has long been known to scientist and layman alike as a region rich in scientific and human interest. Its distinctive types of scenery, its geological phenomena, its flora, and climate are not duplicated by any other area open to general travel. In all ways it is different and unique. The monument is situated in the rugged desert region lying east of the High Sierra in eastern California and southwestern Nevada. The valley itself is about 140 miles in length, with the forbidding Panamint Range forming the western wall, and the precipitous slopes of the Funeral Range bounding it on the east. -
Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California
DISTRIBUTION AS A FUNCTIONAL FACTOR OF ROCK ALIGNMENTS IN THE MOJAVE DESERT Jay Von Werlhof Imperial Valley College Desert Museum El Centro, California ABSTRACT This paper suggests that the distribution, setting, content, and form of early rock alignments in the Mojave Desert are directly related to the function of these features. Each of these factors will be described and discussed in turn, leading to an interpretive synthesis. Why a reliable model cannot be developed for locating rock alignment sites is also suggested. I am pleased to have been invited to present a paper in this noted also that a few isolated sites are uniquely present, which session honoring Dee Simpson. I have admired her life-long is another concern of research. Such sites, for example, might devotion to archaeology and the tenacity with which she works have been in the process of being developed into larger and toward goal completions. I am also indebted to her, along more complex sites but were never completed, as possibly that with Arda Haenzel, her co-worker at the San Bernardino at Lavic Lake (MacDonald 1993). Also, in complex sites con County Museum, for interesting me in earthen art back in taining numerous designs it is not clear whether the diverse el 1975 when few others thought that path worth treading. Since ements are even temporally related, or if each design exists as then, I have worked to advance the study of geogylphs and rock an entity from a different era. However, this type of earthen art alignments, and the paper I am presenting today is drawn appears to have been the earliest, and its association with the around a small sector of that study: distribution as a functional Lake Hill Pleistocene site (Davis 1978) focuses the Panamint factor of rock alignments in the Mojave Desert. -
Dover Gets a New Brewery Brewery
FREE The newsletter of the Deal Dover Sandwich & District PLEASE TAKE A COPY Branch of the Campaign for Real Ale Issue 51 Spring 2012 INSIDE DOVER GETS A NEW THE RISE OF BREWERY PORTER Tír Dhá Ghlas Brewery at Cullin’s Yard is Dover’s Part Two of the First Brewery for 85 Years --- See Page 42 history of this distinctive beer style See Page 45 Getting to Know THE RIPPLE STEAM BREWERY Sutton See Page 34 Page 1 Channel Draught is published and ISSUE 51 ©2012 by the Deal Dover Spring 2012 Sandwich & District Branch of the hether or not spring has actually arrived, and at Campaign for Real Ale W the time of writing there seems serious doubt, www.camra-dds.org.uk here is the 2012 spring edition of Channel Draught . Editorial Team New to our branch this year, at least for recent times, is Editor & a Real Ale Trail – Deal, Dover, Sandwich and District's Advertising contribution to CAMRA's Community Pubs Month. It Martin Atkins takes the form of a treasure hunt, and features twenty Editorial Assistants seven of our best real ale pubs. The competition does Trisha Wells not finish until the end of May, so if you are reading this John Pitcher before then there is still time to take part. See page 29 for details. Design & Format Steve Bell Branch pub of the year, for the fifth year running, is the Berry in Walmer, and once again we congratulate Chris Editorial Address and his staff on doing such a great job. However, there is plenty of good real ale elsewhere, the latest recruit You can write to the being the newly opened Just Reproach in King St. -
Is There Any Evidence of Mega-Lake Manly in the Eastern Mojave Desert During Oxygen Isotope Stage 5E/6?
Quaternary Research 57, 177–179 (2002) doi:10.1006/qres.2001.2299, available online at http://www.idealibrary.com on REPLY Is There Any Evidence of Mega-Lake Manly in the Eastern Mojave Desert during Oxygen Isotope Stage 5e/6? I am pleased to have the opportunity to defend and clarify the implication that Ku’s dates are more reliable than those of my hypothesis regarding the extent of the Blackwelder stand of Hooke and Lively (see Hooke and Dorn, 1992) is debatable, Lake Manly during marine oxygen isotope stage 6 (OS6). Let given that both use the -counting technique and thus may suffer me start by addressing a couple of general points. from problems with U migration. First, with reference to the pejorative prefix “mega” in Enzel Salt Spring Hills shoreline. Enzel et al. maintain that this et al.’s comment, let me put the size of the lake under discussion shoreline is cut into colluvium and, at its southeastern end, into in perspective. If water were to fill Death Valley to the 90-m alluvial fan deposits. I agree with the former. On the other hand, level today, the surface area would be 1600 km2 (Meek, 1997), air photos, a map in Anderson and Wells (1997), and my own whereas the area Hale proposed, based on overflow at Ash Hill observations do not support the interpretation that it is cut into an pass, would have been 8000 km2 (Hale, 1985). The surface alluvial fan at its southeastern end. Even if further study shows area of the OS6 lake proposed in my paper is 2800 km2, less that it is, however, Enzel et al.’s statements about the age of than half the size of Hale’s lake and less than twice the size a the fan unit are misleading (1) because they are based on dates 90-m lake would have were it to occupy the valley today. -
The Formation of Badwater Basin and the Death Valley Salt Flats S
The Formation of Badwater Basin and the Death Valley Salt Flats S. G. Minton-Morgan 12 June 2013 ABSTRACT The iconic landscape of Badwater Basin, located in Death Valley National Park, rests 282 ft (86 m) below sea level; the lowest point in North America. It is home to a varied collection of landforms and features – many of them ephemeral - including salt flats, saline springs, ephemeral lakes, and their resultant muddy deposits. The unique landscape is a result of ancient volcanism, climate, and flooding combined with modern weather patterns and underground hydrothermal activity. Of these factors, flooding and hydrothermal activity are perhaps the most dramatic, as they visibly alter the terrain in ways directly observable on timescales of a few years. Similarly, two most notable features of Badwater Basin – its sprawling salt flats and its namesake Badwater Spring – are inextricably linked together in that the minute spring-fed lake provides the hydrological activity necessary to give the salt flats their unique geometric character as distinct from other salt deposits around the Valley. INTRODUCTION What mysteries lay at the lowest point in North America? Death Valley is a site unique among the basins in the Basin and Range region; not only is it home to the lowest, hottest point in North America, it also rests in the rain shadow of the 11049 ft. Telescope Peak, giving it a dry, desert climate found nowhere else in the region. Badwater Basin, the lowest point in Death Valley is a forbidding landscape to human beings, yet is simultaneously home to some of the most fascinating geological and hydrological features in the Northern Hemisphere.