State of Delaware

Total Page:16

File Type:pdf, Size:1020Kb

State of Delaware .. •-,l:l.JNIVERSITY ,- ' OF . :'?DBLAWA·RE .. --, ~ ' . JOURNAL OF TUE OF THE STATE OF DELAWARE, AT A SESSIQN OF • TIIE GEXEBAli .&SSEMBI.T, CO~MENCED AND HELD AT DOVER, ON TUESDAY THE FIRST DAY OF JANUARY, IN THE YEAlt.JJF OUR LORD Ill' . · .. ONE THOUSAND EIGHT HUNDRED AND THIRTY-NINE, AND OF.THE INDEPENDENCE OF THE UNITED STATES OF AMERICA THE SIXTY-THIRD. ... ' . , r <' • er' " ... ~ .... Cl. .• ( ((' ( c ' . L' .... ..'' ' /s-tod e._ ---oo c "\X. f'::- 'D ,c . ',JgB \ ~3'\ . ..-· .. : .... ... .. ..... ... .~.·. ... ..... .. .. .... ... ....... .. .. .. .. .... : . .: ... .: . .: .... • ... ...,J·. ... .. .. .. , ·.:·~::.. ..... .. : ·.: :.: .: : ,:-.~;,,.•:.:,: i/ • • • • • < •• . ... .. :.: .. .. .. .. .. .. ... : .. .... : : ~'.: ._,. ~--.:-: ... ,' /~· JOURNAL OF THE OF THE STATE OF DELAWARE. At a session ef the General A.~sembly commenced and held at Dover, on Tuesday the first day ef January, in tlie year ef our Lord, one thou­ .~and eight hundred and thirty-nine, and ef the Independence ef the United States ef America, the sixty-third. Messrs. Alexa :der M. Biddle, John D. Dilworth, William H. Rogers, Nathan Boulden, Andrew Kerr, William Hemphill Jones, and Harry Williamson, from New Castle county; Messrs. Presley Spruance, Thomas A. Rees, John Frazer, Robert Frame, Henry Pratt, Samuel B. Cooper and Philip D. Fiddeman, from Kent county; and Messrs. John P. Brinkloe, .Tames Hopkins, Robert Houston, Joseph W. Neal, Aaron Marshall, jr., Richard Jefferson and Robert Hopkins, from Sussex county, appeared. The members all being present, the returns of the election for Repre· sentatives of the several counties of the State, were read. By the returns 0f the officers of New Castle county, appointed by law judges of elections, it appears that on the second Tuesday of November last, at the several and respective places specified by law for holding the elections in and for the said county, the following persons were chosen to represent the said county, in the House of RepresentatiVPs of th€ State of Delaware; viz:-Alexander M. Biddle, John D. Dilworth, William H. Ro­ gers, Nathan Boulden, Andrew Kerr, William Hemphill Jones and Harry Williamson, Esquires. , By the returns of the officers of Kent county, appointed by law,judges of elections, it appears that on the second Tuosday of November last, at ,the several and respective places, specified by law, for holding elections 'in an,d for the said county, the following persons were chosen to represent ,the ~uid cO:tinty, in the House of Representatives of the State of Delaware; viz:-Presley Spruance, Thomas A. Rees, John Frazier, Robert Frame, Henry Pratt, Samuel B. Cooper and Philip D. Fiddeman, Esquires. By the returns of the officers of Sussex county, ~ppointed by law, judges of elections, it appears that on the second Tuesday of November last, at the several and respective places, specified by law, for holding the elec­ tions, in and for the said county, the following persons were chosen to represent the said county, in the House of Representatives of the State of ·Delaware, to wit:-John P. Brinkloe, James Hopkins, Robert Houston, Joseph W. Neal, Aaron Marshall, jr., Richard Jefferson and Robert Hop· kins, Esquires. • On motion of Mr. Dilworth, The House proceeded to elect by ballot, a Speaker, whereupon JOHN P. BRINKLOE, was elected. The Speaker was then qualified, according to the Constitution of the State, and the act of congress entitled "An act to regulate the time and manner of administering certain oaths," and then took his scat in the Speaker's chair. The Speaker then 'lualified, in due form of law, the members present. On motion of Mr. Frame, The House proceeded to ballot for a Clerk, and Henry Todd was duly elected, introduced, sworn, and took his seat at the Clerk's table. On motion of Mr. Rogers, The House proceeded to ballot for aSeargeant-at-arms, and Josiah :Mar­ vel, was duly elected. On motion of Mr. Jones, Resolved, That the Clerk be directed to inform the Senate that the House of Representatives is duly organized and ready to proceed to busi­ ness. On motion of Mr. Rogers, The House adjourned to 10 o'clock to-morrow morning. WEDNESDAY, 10 o'clock A. Jiil. January 2, 1839. The House assembled pursuant to adjournment. Roll called, journal read and found to be correct. A message from the Senate by the Clerk. Mr. Laws, Clerk of the Senate being admitted, informed the House that the following resolution hpd passed the Senate, and that the concurrence of the House was desired in the same, to wit : ~ "IN SENATE, January 1, 1839. Resolved, That a committee of two members be appointed on the part of the Senate, to act jointly with such committee as may be appointed on the part of the House of Representatives, to wait on the Governor and in- ])~:)'/,~?,. J) '?.i~3 \':~ ~9 r tf(J, t .. ~ 5 form him, that a quorum of both houses of the Legislature have now con· ,Vened, and are ready to receive any communication which h3 may wish to make.-Messrs. Polk and Herdman were appointed that committee on the part of the ,Senate. "Extract from tlie Journal." S. G. LA. Vi7S, Clerk. ' 1For concurrence." And he withdrew. On motion of Mr. Jones, Said resolution was read and concurred in by the Honse. On motion of Mr. Frame, Resolved, That a committee to consist of three members on the r:i.rt of the House be appointed, to act jointly with the committee appointed on tho part of the Senate, to wait upon his Excellency the Governor, and inform him that a quorum of both houses of the Legislature have convened, and are ready to receive any communication he may think proper to make. Messrs. Fiddeman, Williamson and Marshall, were appointed that com­ mittee. Ordered, That the Clerk proceed to the Senate, and ask their concur­ rence in the same. The committee then withdrew for a short time, when they returned to the House, and Mr. Fiddeman from said committee, informed the House that the Governor would forthwith make a communication to both Houses of the Legislature. A message from the Governor by the Secretary of State: Charles Marim, Esquire, Secretary of State, being admitted, laid on the fllble a written Message of the Governor of the State, with its accompa­ nying documents, And he withdrew. On motion of Mr. Frame, The clerk read the Message as follows, to wit:- Fellow-Oitizens ef the Senate, and ef the House ef Representatives: In presenting to you my first biennial communication, I cannot forbear to congratulate you on the condition of our beloved State. At no former period, has Delaware exhibited so manX' indications of growing prosperity as at the present. The spirit of enterprise and the ardour of pursuit seem to pervade all classes of her citizens. Agriculture, stimulated by the in­ terest which it has awakened in all directions, is flourishing beyond re­ cent, if not all former example. Every other branch of industry presents a· flattering aspect, and is meeting with encouraging success. Intelligence and morality are progressing under the influence of our benign institutions. Our citizens are strengthened in attachment 1io their native soil. The dis­ content which for a while prevailed and caused so many emigrations to the west has happily subsided; and all appear now satisfied, that our State, though small in extent, combines, within its limits, every essential element to its moral and physical advancement. I have reason also, to congratu­ late you on the peace and tranquility in which you are permitted to as­ semble: The spirit of rebellious violence, however dominant in other di- 11ftions, finds no congenial materials here. The supremacy of the law lll'ld the silent authority of the ballot box retain their legitimate influence. No riotous commotion r,as yet received the sanction of our citizens and blotted the pages of our history. Order still prevails, and a laudable sub­ ql'jssion to the constituted authorities is the distinguished characteristic of ·'tfie people. We have therefore, abundant caus~ for thankfulness to the ~reat Giver of all good for His gracious protection, and our hearts should be inspired with the most humble devotion for a continuance of his mercy. The confidence reposed in you by your fellow-citizens, and the weigh:y responsibilities of the trust committed to your hands will, I have no doubt, excite you to a diligent dnd anxious application to yom·engagements. In entering upon your duties, it will be prudent to consider that, as on the one hand, radical changes in the law are exceedingly unwise and dange­ rous, so on the ,,ther, the .mind of the legislator should not content itself with rr<::judices or authorities which will not stand the test of fair and im­ partial invesl.igation. In a government, such as ours, the habits and man­ ners of the people require that the spirit of inquiry should be fostered, and that all questions which relate to the well being of the community should receive the most anxious deliberation. In studying the interests of the commonwealth, we cannot be too mindful of the respect and veneration which is due to the common law-its general adaptation to the affairs of men, and its intimate connexion with our instirutions an•f system of juris­ prudence. We should beware of the substitution of fanciful theories for those established principles, which have ever been regarded as the land­ marks of right, and for many centuries have received the admiration of the world. Still, on such ~u~jects as, frorh the fluctuating interests of so· ciety the public welfare and sound expediency may require legislative in­ terfercnC'e, it would be manifestly improper to suffer an attachment to for­ mer prejudices to so far operate as to prevent salutary changes. Enter· taining these views, and placing a firm reliance on your discretion, I should hardly deem it necessary to offer you any suggestions, were I not admonish­ ed by the constitution, ofmy duty "to give you information of affairs con­ cerning the State, and recommend to your consideration such measures as I shall judge e::vpedient." In performing this duty, is is almost unnecessary for me to remark, that education is entitled to your first and most vigilant attention.
Recommended publications
  • Bell Bend, BBNPP Plot Plan Change COLA Supplement, Part 3 (ER
    R. R. Sgarro PPL Bell Bend, LLC *-E# Manager-Nuclear Regulatory Affairs 38 Bomboy Lane, Suite 2 Berwick, PA 18603 Tel. 570.802.8102 FAX 570.802.8119 flp1 [email protected] 11V * December 21, 2010 ATTN: Document Control Desk U.S. Nuclear Regulatory Commission Washington, DC 20555-0001 BELL BEND NUCLEAR POWER PLANT BBNPP PLOT PLAN CHANGE COLA SUPPLEMENT, PART 3 (ER); SECTION 2.6 BNP-2010-338 Docket No. 52-039 References: 1) BNP-2010-175, T. L. Harpster (PPL Bell Bend, LLC) to U.S. NRC, "July 2010 BBNPP Schedule Update", dated July 16, 2010 2) BNP-2010-246, R. R. Sgarro (PPL Bell Bend, LLC) to U.S. NRC, "BBNPP Plot Plan Change Supplement Schedule Update," dated September 28, 2010 In Reference 1, PPL Bell Bend, LLC (PPL) provided the NRC with schedule information related to the intended revision of the Bell Bend Nuclear Power Plant (BBNPP) footprint within the existing project boundary which has been characterized as the Plot Plan Change (PPC). As the NRC staff is aware, the plant footprint relocation will result in changes to the Combined License Application (COLA) and potentially to new and previously responded to Requests for Additional Information (RAIs). PPL declassified this docketed schedule information from regulatory commitment status in Reference 2, with an agreement to update the staff via weekly teleconferences as the project moves forward. PPL has committed to provide the NRC with COLA supplements, consisting of revised COLA Sections and associated RAI responses/revisions, as they are developed. These COLA supplements will only include the changes related to that particular section of the COLA and will not include all conforming COLA changes.
    [Show full text]
  • Geological Map Extracts
    Geological Map Extracts This part of the report contains extracts of geological maps taken from the 1:50 000 scale BGS Digital Geological Map of Great Britain (DiGMapGB-50). The geological information in DiGMapGB is separated into four themes: artificial ground, landslide deposits, superficial deposits and bedrock, shown here in separate maps. The fifth ‘combined geology’ map superimposes all four of these themes, to show the geological formations that occur at the surface, just beneath the soil. More information about DiGMapGB-50 and how the various geological units are classified can be found on the BGS website (www.bgs.ac.uk). The maps are labelled with two-part computer codes that indicate the name of the geological unit and its composition. Descriptions of the units listed in the map keys may be available in the BGS Lexicon of Named Rock Units, which is also on the BGS website (http://www.bgs.ac.uk/lexicon/). If available, these descriptions can be found by searching against the first part of the computer code used on the maps. Please treat this labelling with caution in areas of complex geology, where some of the labels may overlap occurrences of several geological formations. If in doubt, please contact BGS Enquiries for clarification. In the map keys the geological units are listed in order of their age, as defined in the BGS Lexicon, with the youngest first. However, where units are of the same defined age they are listed alphabetically and this may differ from the actual geological sequence. Date: 26 April 2011 Page: 1 of 6 © NERC, 2011.
    [Show full text]
  • Superficial Deposits
    Mineral Resource Information in Support of National, Regional and Local Planning: North Yorkshire (comprising North Yorkshire, Yorkshire Dales and North York Moors National Parks and City of York) Commissioned Report CR/04/228N BRITISH GEOLOGICAL SURVEY COMMISSIONED REPORT CR/04/228N Mineral Resource Information in Support of National, Regional and Local Planning: North Yorkshire (comprising North Yorkshire, Yorkshire Dales and North York Moors National Parks and City of York) D J Harrison, P J Henney, D Minchin, F M McEvoy, D G Cameron, S F Hobbs, D J Evans, G K Lott, E L Ball and D E Highley The National Grid and other Ordnance Survey data are used with the permission of the This report accompanies the two 1:100 000 scale maps: Controller of Her Majesty’s Stationery Office. North Yorkshire (comprising North Yorkshire, Yorkshire Ordnance Survey licence number GD 272191/2006 Dales and North York Moors National Parks and City of York). Key words North Yorkshire; mineral resources; mineral planning Front cover Coldstones Quarry, Carboniferous limestones, view to southwest. North Yorkshire Bibliographical reference Harrison, D J, Henney, P J, Minchin, D, McEvoy, F M, Cameron, D G, Hobbs, S F, Evans, D J, Lott, G K, Ball, E L, and Highley, D E. 2006. Mineral Resource Information in Support of National, Regional and Local Planning: North Yorkshire (comprising North Yorkshire, Yorkshire Dales and North York Moors National Parks and City of York). British Geological Survey Commissioned Report, CR/04/228N. 24pp © Crown Copyright 2006 Keyworth, Nottingham British Geological Survey 2006 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available Keyworth, Nottingham NG12 5GG from the BGS Sales Desks at Nottingham and Edinburgh; see contact details below or shop online 0115-936 3241 Fax 0115-936 at www.thebgs.co.uk 3488 e-mail: [email protected] The London Information Office maintains a www.bgs.ac.uk reference collection of BGS publications including Shop online at: www.thebgs.co.uk maps for consultation.
    [Show full text]
  • A 3D Geological Model of the Superficial Deposits of the Holderness Area Geology and Landscape Programme Commissioned Report CR/09/132N
    A 3D geological model of the superficial deposits of the Holderness area Geology and Landscape Programme Commissioned Report CR/09/132N BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE PROGRAMME COMMISSIONED REPORT CR/09/132 A 3D geological model of the superficial deposits of the Holderness area The National Grid and other Ordnance Survey data are used with the permission of the Controller of H. F. Burke, D. J. Morgan, H. Kessler and A. H. Cooper Her Majesty’s Stationery Office. Licence No: 100017897/ 2015. Keywords Report; Holderness; 3D model; GSI3D; Environment Agency; Quaternary; Chalk. National Grid Reference SW corner 488722,424886 Centre point 506328,448157 NE corner 526348,474973 Map Front cover Cover picture details, delete if no cover picture. Bibliographical reference BURKE, H. F., MORGAN, D. J., KESSLER, H., AND A. H. COOPER. 2015. A 3D geological model of the superficial deposits of the Holderness area. British Geological Survey Commissioned Report, CR/09/132N. 58pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based
    [Show full text]
  • Compartmentalisation and Groundwater
    Durham Research Online Deposited in DRO: 14 July 2020 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Wilson, Miles. P. and Worrall, Fred. and Clancy, Sarah. A. and Ottley, Christopher. J. and Hart, Alwyn. and Davies, Richard. J. (2020) 'Compartmentalisation and groundwatersurface water interactions in a prospective shale gas basin : assessment using variance analysis and multivariate statistics on water quality data.', Hydrological processes., 34 (15). pp. 3271-3294. Further information on publisher's website: https://doi.org/10.1002/hyp.13795 Publisher's copyright statement: c 2020 The Authors. Hydrological Processes published by John Wiley Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Received: 23 January 2020 Accepted: 25 April 2020 DOI: 10.1002/hyp.13795 RESEARCH ARTICLE Compartmentalisation and groundwater–surface water interactions in a prospective shale gas basin: Assessment using variance analysis and multivariate statistics on water quality data Miles P.
    [Show full text]
  • Improved Understanding of Groundwater Flow in Complex
    Hydrogeology Journal (2015) 23: 493–506 DOI 10.1007/s10040-014-1207-0 Improved understanding of groundwater flow in complex superficial deposits using three-dimensional geological-framework and groundwater models: an example from Glasgow, Scotland (UK) R. J. Turner & M. M. Mansour & R. Dearden & B. É. Ó Dochartaigh & A. G. Hughes Abstract Groundwater models are useful in improving central Glasgow. A prototype groundwater-monitoring knowledge of groundwater flow processes, both for testing network for part of Glasgow is an encouraging develop- existing hypotheses of how specific systems behave and ment in this regard. This would allow the development of predicting the response to various environmental stresses. a time-variant groundwater model which could be used to The recent advent of highly detailed three-dimensional study future modelling scenarios. (3D) geological-framework models provides the most accurate representation of the subsurface. This type of Keywords Conceptual modelling . 3D geological modelling has been used to develop conceptual under- modelling . Superficial deposits . Urban standing of groundwater in the complex Quaternary groundwater . UK deposits of Glasgow, Scotland (UK). Delineating the 3D geometry of the lithostratigraphical units has allowed the most detailed conceptualisation of the likely groundwater flow regime yet attempted for these superficial deposits. Introduction Recharge and groundwater flow models have been developed in order to test this conceptual understanding. Urban regeneration in the UK aims to facilitate land Results indicate that the direction of groundwater flow is recycling, sustainable development and effective land and predominantly convergent through the permeable, rela- water resources management to tackle issues associated with industrial decline. In the Clyde corridor, which is tively thick Quaternary deposits of the Clyde valley ’ towards the River Clyde, which runs through Glasgow, Scotland s national regeneration priority, the British with some indication of down-valley flow.
    [Show full text]
  • Geological Mapping in Urban Areas
    3 8 3 勿 R A E llison, S J B ooth and P J Strange G eological m apping in urban areas The B G S exp erience in London B ased on a p ap er p resented at the International C onference on G eoscience in U rban D evelop m ent (L andp lan IV) 11- 15 A ugust 1993, B eijing, C hina The B ritish G eological Survey has established the tively leading to better interpretation of ground conditions and pre- L O C U S (L O ndon C om p uterised U nderground and Sur- diction of potential geological hazards. H ow ever, the potential value of sound geological know ledge in underpinning planning and urban face) geological p roject, w hose aim is to p rovide geo- regeneration issues has been largely underplayed, and the benefits of logical m ap s and interp reted datafor London. The resul- detailed understanding of the relevant geological factors, for the tant high-quality m odel has alrea办 p roved valuable in m ost part, have not been fully realised. C ostly rem edial w ork during con s tr u ction caused by unfore- p rojects rangingf rom the site-specif c to strategic over- seen geological factors is not uncom m on in the L ondon region, and v ie i认 the variability of strata below London has been a source ofe ngineer- T h e p erceived requirem entfor geological inform a- Ing difficulty dating back to the first tunnel under the Tham es, built tion in urban areas is to supp ort land-use p lanning, by B runel in 1825.
    [Show full text]
  • Report on the Geology of Tuscola County Michigan
    REPORT General surface configuration of the county ..................6 OF THE Elevations within the County..........................................7 STATE BOARD OF GEOLOGICAL SURVEY Elevations in Tuscola county..........................................8 OF MICHIGAN Surface drainage systems..............................................8 FOR THE YEAR 1908 The cass river valley ......................................................8 Lapeer river tributaries ...................................................9 GEOLOGY Lakes, Ponds and Swamps............................................9 ALFRED C. LANE Number and size ............................................................9 STATE GEOLOGIST Temporary ponds .........................................................10 MAY 18, 1910 Swamps and Marshes..................................................10 Saginaw Bay and its beaches......................................11 BY AUTHORITY Diagonal Features of the County .................................12 LANSING, MICHIGAN Strike and dip of the rock formations ...........................12 WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS 1909 Surface slopes and drainage .......................................12 The soils of the county .................................................13 REPORT CHAPTER III. THE GLACIAL PERIOD IN TUSCOLA ON THE COUNTY..........................................................................13 GEOLOGY OF TUSCOLA COUNTY MICHIGAN Introductory ..................................................................13 Pre-Wisconsin
    [Show full text]
  • Clyde Superficial Deposits and Bedrock Models Released to the ASK Network 2014: a Guide for Users. Version 3
    Clyde superficial deposits and bedrock models released to the ASK Network 2014 : a guide for users Version 3 Geology and Regional Geophysics Programme Open Report OR/14/013 BRITISH GEOLOGICAL SURVEY GEOLOGY AND REGIONAL GEOPHYSICS PROGRAMME OPEN REPORT OR/14/013 Clyde superficial deposits and bedrock models released to the ASK Network 2014 : a guide for users Version 3 A A Monaghan, S L B Arkley, K Whitbread, M McCormac Contributor D J Lawrence The National Grid and other Ordnance Survey data © Crown Copyright and database rights 2014. Ordnance Survey Licence No. 100021290. Bibliographical reference MONAGHAN A A, ARKLEY S L B, WHITBREAD K, MCCORMAC M. 2014.Clyde superficial deposits and bedrock models released to the ASK Network 2014 : a guide for users Version 3. British Geological Survey Open Report, OR/14/013.35pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NERC 2014. All rights reserved Keyworth, Nottingham British Geological Survey 2014 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation.
    [Show full text]
  • Geological Maps for ALV Alluvium Clay, Silt, Sand Not Supplied - the Area Around the Site
    Geology 1:50,000 Maps Legends Superficial Geology Geology 1:50,000 Maps Map Lex Code Rock Name Rock Type Min and Max Age This report contains geological map extracts taken from the BGS Digital Colour Geological map of Great Britain at 1:50,000 scale and is designed for users carrying out preliminary site assessments who require geological maps for ALV Alluvium Clay, Silt, Sand Not Supplied - the area around the site. This mapping may be more up to date than and Gravel Holocene previously published paper maps. The various geological layers - artificial and landslip deposits, superficial TILMP Till, Mid Pleistocene Diamicton, Sand Not Supplied - geology and solid (bedrock) geology are displayed in separate maps, but and Gravel Cromerian superimposed on the final 'Combined Surface Geology' map. All map TILMP Till, Mid Pleistocene Diamicton Not Supplied - legends feature on this page. Not all layers have complete nationwide Cromerian coverage, so availability of data for relevant map sheets is indicated below. HEAD Head Clay, Silt, Sand Not Supplied - Geology 1:50,000 Maps Coverage and Gravel Quaternary Map ID: 1 Map Sheet No: 101 Map Name: East Retford Map Date: 1967 Bedrock and Faults Bedrock Geology: Available Superficial Geology: Available Artificial Geology: Not Available Map Lex Code Rock Name Rock Type Min and Max Age Faults: Not Supplied Colour Landslip: Not Available Rock Segments: Not Supplied CHES Chester Formation Sandstone, Pebbly Not Supplied - (Gravelly) Olenekian EDT Edlington Formation Mudstone and Not Supplied - Sandstone
    [Show full text]
  • APPENDIX B Geology Maps
    APPENDIX B Geology Maps Geology 1:50,000 Maps Legends Artificial Ground and Landslip Geology 1:50,000 Maps Map Lex Code Rock Name Rock Type Min and Max Age Map Lex Code Rock Name Rock Type Min and Max Age This report contains geological map extracts taken from the BGS Digital Colour Colour Geological map of Great Britain at 1:50,000 scale and is designed for users carrying out preliminary site assessments who require geological maps for WMGR Infilled Ground Artificial Deposit Cenozoic - Faults the area around the site. This mapping may be more up to date than Cenozoic previously published paper maps. The various geological layers - artificial and landslip deposits, superficial WGR Worked Ground Void Holocene - Rock Segments geology and solid (bedrock) geology are displayed in separate maps, but (Undivided) Holocene superimposed on the final 'Combined Surface Geology' map. All map SLIP Landslide Deposit Unknown/Unclassif Quaternary - legends feature on this page. Not all layers have complete nationwide ied Entry Quaternary coverage, so availability of data for relevant map sheets is indicated below. Geology 1:50,000 Maps Coverage Map ID: 2 Map ID: 1 Superficial Geology Map Sheet No: 076 Map Sheet No: 068 Map Name: Rochdale Map Name: Clitheroe Map Lex Code Rock Name Rock Type Min and Max Age Map Date: 2008 Map Date: 1975 Bedrock Geology: Available Bedrock Geology: Available Colour Superficial Geology: Available Superficial Geology: Available Artificial Geology: Available Artificial Geology: Not Available Faults: Not Supplied Faults: Not
    [Show full text]
  • Mineral Resources Map for Surrey
    60 70 80 905 00000 10 20 30 40 50 60 FULLER’S EARTH BRICK CLAY BUILDING STONE CHALK BGS publications covering Surrey and the London Boroughs of Croydon, Hounslow, Kingston upon Thames, Richmond upon Thames and Sutton The term 'fuller's earth' is used to describe clays composed essentially of the clay mineral The term 'Brick clay' is used to describe clay used predominantly in the manufacture of bricks Rocks of Lower Cretaceous age have been important source of building stone in Surrey. Chalk is a relatively soft, fine-grained, white limestone, consisting mostly of the debris of calcium-smectite, which exhibits a unique combination of properties on which its industrial and, to a lesser extent, roof tiles and clay pipes. These clays may sometimes be used in cement Sandstones from the Lower Greensand Group were quarried for local use around Godalming, at planktonic algae. In Surrey, it forms the prominent natural feature of the North Downs. Almost the applications are based. Calcium-smectite can be easily converted into sodium-smectite manufacture, as a source of construction fill and for lining and sealing landfill sites. The suitability Hurtmore (working material known as 'Bargate Stone'), and at Witley and Hurtwood. Ironstone entire outcrop of the chalk is within the Surrey Hills AONB. The Chalk is divided into the Grey 285 1:63 360 and 1:50 000 (bentonite) by a simple sodium-exchange process and most fuller's earth is used in this form in of a clay for the manufacture of bricks depends principally on its behaviour during shaping, drying beds within the Lower Greensand (known as 'carstone') were also once a source of local building Chalk Sub-Group, and the White Chalk Sub-Group and is up to 320 m thick in this part of South 269 HOUNSLOW 270 271 map published papermaking and foundry bonding applications.
    [Show full text]