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The 1934 Pahiatua Earthquake Sequence: Analysis of Observational and Instrumental Data
221 THE 1934 PAHIATUA EARTHQUAKE SEQUENCE: ANALYSIS OF OBSERVATIONAL AND INSTRUMENTAL DATA Gaye Downes1' 2, David Dowrick1' 4, Euan Smith3' 4 and Kelvin Berryman1' 2 ABSTRACT Descriptive accounts and analysis of local seismograms establish that the epicentre of the 1934 March 5 M,7.6 earthquake, known as the Pahiatua earthquake, was nearer to Pongaroa than to Pahiatua. Conspicuous and severe damage (MM8) in the business centre of Pahiatua in the northern Wairarapa led early seismologists to name the earthquake after the town, but it has now been found that the highest intensities (MM9) occurred about 40 km to the east and southeast of Pahiatua, between Pongaroa and Bideford. Uncertainties in the location of the epicentre that have existed for sixty years are now resolved with the epicentre determined in this study lying midway between those calculated in the 1930' s by Hayes and Bullen. Damage and intensity summaries and a new isoseismal map, derived from extensive newspaper reports and from 1934 Dominion Observatory "felt reports", replace previous descriptions and isoseismal maps. A stable solution for the epicentre of the mainshock has been obtained by analysing phase arrivals read from surviving seismograms of the rather small and poorly equipped 1934 New Zealand network of twelve stations (two privately owned). The addition of some teleseismic P arrivals to this solution shifts the location of the epicentre by less than 10 km. It lies within, and to the northern end of, the MM9 isoseismal zone. Using local instrumental data larger aftershocks and other moderate magnitude earthquakes that occurred within 10 days and 50 km of the mainshock have also been located. -
History of Royal Cromer Golf Club Established 1888
History of Royal Cromer Golf Club established 1888 Information obtained from minute books, letters, members records, journals and periodicals. Royal Cromer Golf Club History Established 1888 Royal Cromer Golf Club owes its existence to the enthusiasm and love of the game of a Mr. Henry Broadhurst M.P., a Scot who lived at 19, Buckingham Street, The Strand, London. In the 1880's, whilst holidaying in Cromer, he recognised the potential of land to the seaward of the Lighthouse as a possible site for a Links Course. The popularity of North Norfolk at this time had been noted in the London City Press in a report dated 5th September 1886: "The public are greatly indebted to railway enterprise for the opening up of the East Coast. More bracing air and delightful sands are not to be found in any part of England. The only drawback is that the country is rather flat. This remark, however, does not apply to Cromer, which bids fair to become the most popular watering place, it being entirely free from objectionable features". The site of the proposed golf course was owned by the then Lord Suffield KCB, who kindly consented to the request of Broadhurst and some twenty other enthusiasts to rent the land. The Club was instituted in the Autumn of 1887 with Lord Suffield as President. Doubtless it was his friendship and influence with the Prince of Wales which precipitated the Prince's gracious patronage of the infant club on 25th December 1887. Thus Cromer had a Royal Golf Club even before its official opening the following January. -
Influence of the Spatial Pressure Distribution of Breaking Wave
Journal of Marine Science and Engineering Article Influence of the Spatial Pressure Distribution of Breaking Wave Loading on the Dynamic Response of Wolf Rock Lighthouse Darshana T. Dassanayake 1,2,* , Alessandro Antonini 3 , Athanasios Pappas 4, Alison Raby 2 , James Mark William Brownjohn 5 and Dina D’Ayala 4 1 Department of Civil and Environmental Technology, Faculty of Technology, University of Sri Jayewardenepura, Pitipana 10206, Sri Lanka 2 School of Engineering, Computing and Mathematics, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK; [email protected] 3 Faculty of Civil Engineering and Geosciences, Delft University of Technology, Stevinweg 1, 2628 CN Delft, The Netherlands; [email protected] 4 Department of Civil, Environmental and Geomatic Engineering, Faculty of Engineering Science, University College London, Gower Street, London WC1E 6BT, UK; [email protected] (A.P.); [email protected] (D.D.) 5 College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, UK; [email protected] * Correspondence: [email protected] Abstract: The survivability analysis of offshore rock lighthouses requires several assumptions of the pressure distribution due to the breaking wave loading (Raby et al. (2019), Antonini et al. (2019). Due to the peculiar bathymetries and topographies of rock pinnacles, there is no dedicated formula to properly quantify the loads induced by the breaking waves on offshore rock lighthouses. Wienke’s formula (Wienke and Oumeraci (2005) was used in this study to estimate the loads, even though it was not derived for breaking waves on offshore rock lighthouses, but rather for the breaking wave loading on offshore monopiles. -
Walk 0A# Mortehoe And
Walking on Exmoor and the Quantock Hills saurus’s back. Pick your way carefully down to the point (25mins, [1]), then turn around and exmoorwalker.uk take the coast path on what is now your le -hand (north) side, heading for the lighthouse at Bull Point. You may see seals among the rocks here. Connuing along the coast path ignore Walk 0A. Mortehoe and Lee Bay. the turn to Mortehoe, but follow a short diversion soon a er where the original path is dan- gerously close to crumbling cliffs. Go through a gate, climb upwards, and pass a short secon 7.2 miles, ascents and descents of 550 metres. 3 hours 5 minutes constant walking, next to a sheer drop before heading down again. Through another gate, then another path allow 4-5 hours overall. from Mortehoe comes in from the right; keep le here. The path goes up and down before Terrain: A mix of roads, tracks, and paths, some uneven and potenally slippery. Morte Point is going through a third gate, just a er another Mortehoe path (55mins, [2]), and bearing le . uneven rock. A er the next gate the path diverts briefly inland; the 2014 storms washed away the way Access: Start from the car park in Mortehoe (SS 458 452, EX34 7DR, £). Bus 31 runs roughly down to the beach, leaving wooden steps hanging precariously over the cliff. Take a narrow hourly between Ilfracombe, Mortehoe and Woolacombe on weekdays and Saturdays. The walk path to the le , bringing you to Bull Point lighthouse (1hr10mins, [3]). You can walk all the can also be started from the car park at Lee (SS 480 464, near EX34 8LR). -
Ldu: 578 Lct: 4H, 2C, 4C
LDU: 578 LCT: 4H, 2C, 4C Area of LDU within AONB: 236.5 hectares % of LDU within AONB: 69% Date surveyed: 24 February 2010 Survey points: SS479464, SS478465, SS454447, SS454446, SS456445 Summary of landscape character This LDU comprises the dramatic north-western coastline of the AONB, stretching from the western fringes of Ilfracombe (Torrs Point) to Morte Bay. The majority of the coast is unsettled, with rocky cliffs displaying complex, folded strata backed by coastal heath and rough maritime grassland. The landscape retains high levels of tranquillity and evokes a wild, exposed character, disrupted in the south by tourism-related development around the coastal headland from Woolacombe. All of the landscape falls within the North Devon Heritage Coast and most is owned by the National Trust. LANDSCAPE DESCRIPTION LANDFORM / TOPOGRAPHY Landform description Undulating, rocky coastline punctuated by small coves and bays. Cliffs up to 100 metres high display a complex geology of mainly Upper Devonian sandstones and slates. Cliffs are backed by often steeply sloping land with rounded summits. LAND USE AND PATTERNS Agriculture Main agricultural land use Other agricultural land use(s) Rough grazing Pasture fields, particularly on the north coast. Field patterns and Field patterns and origins Size (note Boundary type / boundaries variations) description The majority of the LDU N/A There are some comprises rough grazing land stone-faced Devon on open cliff slopes and hedges in parts (many in a poor state of summits. repair) Other land uses (e.g. Recreation: walking along the South West Coast Path and Tarka Trail. recreation) The coastline above Morte Point is open access land. -
Unsettling a Settler Family's History in Aotearoa New Zealand
genealogy Article A Tale of Two Stories: Unsettling a Settler Family’s History in Aotearoa New Zealand Richard Shaw Politics Programme, Massey University, PB 11 222 Palmerston North, New Zealand; [email protected]; Tel.: +64-27609-8603 Abstract: On the morning of the 5 November 1881, my great-grandfather stood alongside 1588 other military men, waiting to commence the invasion of Parihaka pa,¯ home to the great pacifist leaders Te Whiti o Rongomai and Tohu Kakahi¯ and their people. Having contributed to the military campaign against the pa,¯ he returned some years later as part of the agricultural campaign to complete the alienation of Taranaki iwi from their land in Aotearoa New Zealand. None of this detail appears in any of the stories I was raised with. I grew up Pakeh¯ a¯ (i.e., a descendant of people who came to Aotearoa from Europe as part of the process of colonisation) and so my stories tend to conform to orthodox settler narratives of ‘success, inevitability, and rights of belonging’. This article is an attempt to right that wrong. In it, I draw on insights from the critical family history literature to explain the nature, purposes and effects of the (non)narration of my great-grandfather’s participation in the military invasion of Parihaka in late 1881. On the basis of a more historically comprehensive and contextualised account of the acquisition of three family farms, I also explore how the control of land taken from others underpinned the creation of new settler subjectivities and created various forms of privilege that have flowed down through the generations. -
Report and Accounts March 2010
Report and Accounts to 31 March 2011 Table of Contents Directors of the Lighthouse Board 1 Office and Advisers 2 Executive Chairman’s Review 3-5 Directors’ Report and Management Commentary: 6 - Nature, Objectives and Strategy of the Business 6-10 - Current Developments and Performance 10-19 - Resources 20-21 - Risks and Uncertainties 21 - Relationships 22 - Financial Position 22-25 Remuneration Report 26-28 Statement of Accounting Officer’s responsibilities 29 Executive Chairman’s Statement on Internal Control 30-33 Statement of Comprehensive Net Income for the Year Ended 31st March 2011 34 Statement of Financial Position as at 31st March 2011 35-36 Statement of Cash Flows for the Year Ended 31st March 2011 37 Statement of Changes in Reserves for the Year Ended 31st March 2011 38 Notes to the Accounts 39-71 Five Year Summary 72 Appendix A – Letter of Comfort 73 DDirireecctotorrss o of ft hThe eL iLgighhththoouuses eB Booarad rd: ReRaera Ar dAmdimrairl aSl irS iJr MJ Md ed He aHlpaelpret rKt CKVCOV OC BC BFR FIRNI* N* ExEexceuctuivteiv Ce hCahiramiramn an CaCpatpatina inR DH CB aGrklaesrs (retired 21st May 2009)* DiDreircetoctro or fo Nf aNvaigvaigtaiotnioanl aRl eRqeuqirueirmeemnetns ts CoCmapmtoadino rRe HS BJ aSrckoerre (ra*p FpCoMinIted 21st May 2009)* DiDreircetoctro or fo Of pNearvaitgioantisonal Requirements J SC oWmemdgoed,o CreI PSF AJ SMcBoAre Br*A F(CEcMoI n) Hons** DiDreircetoctro or fo Ffi nOapnecrea taionnds Support Services CaJp Sta Wine Nd gRe ,P CryPkFeA, MCBIAT B FAN (IE* con) Hons** DeDpiruetcyt oCrh aoifr mFianna nacned -
Trinity House to Decommission Royal Sovereign Lighthouse End of Serviceable Life
Trinity House to decommission Royal Sovereign Lighthouse End of serviceable life Trinity House London* has begun preparatory work on a project to decommission Royal Sovereign Lighthouse** (English Channel, South coast of England, 50°43′24″N 0°26′08″E). It is the intention that the now-deteriorating lighthouse will be completely removed clear to the seabed. This has necessitated that Beachy Head Lighthouse be upgraded to ensure the safety of the mariner in those waters. Trinity House aims to commence work in 2020. Royal Sovereign Lighthouse was built in 1971 with a design life of 50 years. Having monitored the fabric of the lighthouse over the last decade and observing the expected signs of deterioration, Trinity House concluded that the ongoing safety of the mariner requires that the structure be fully decommissioned. Royal Sovereign Lighthouse has provided nearly 50 years of reliable service as an aid to navigation, one of over 600 that Trinity House operates for the benefit and safety of the mariner. In anticipation of its intention to remove Royal Sovereign Lighthouse, Trinity House upgraded Beachy Head Lighthouse; it will also increase the capability of the offshore CS2 buoy and will retain the nearby Royal Sovereign buoy. The upgrade to Beachy Head Lighthouse has increased the number of solar panels around the base of its lantern gallery and installed a longer-range LED light source; the CS2 lighted buoy will also benefit from an increase in range. The upgrade to Beachy Head Lighthouse will come as good news to mariners and the local community alike. Once Trinity House decommissions Royal Sovereign Lighthouse as proposed, Beachy Head Lighthouse’s future is secured as the principal aid to navigation in the area. -
Fire Island Light Station
Form No. 10-306 (Rev. 10-74) UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM FOR FEDERAL PROPERTIES SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS TYPE ALL ENTRIES--COMPLETE APPLICABLE SECTIONS NAME HISTORIC Fire Island Light Station _NOT FOR PUBLICATION CITY. TOWN Bay Shore 0.1. STATE CODE COUNTY CODE New York 36 Suffolk HCLASSIFICATION CATEGORY OWNERSHIP STATUS PRESENT USE _ DISTRICT -XPUBLIC OCCUPIED —AGRICULTURE —MUSEUM _ BUILDING(S) ^.PRIVATE X.UNOCCUPIED —COMMERCIAL XPARK _XSTRUCTURE —BOTH —WORK IN PROGRESS —EDUCATIONAL —PRIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT _ IN PROCESS iLYES: RESTRICTED —GOVERNMENT —SCIENTIFIC —BEING CONSIDERED —YES: UNRESTRICTED —INDUSTRIAL —TRANSPORTATION —NO —MILITARY —OTHER: AGENCY REGIONAL HEADQUARTERS: (If applicable) National Park Service, Morth Atlantic Region STREET & NUMBER 15 State Street CITY. TOWN STATE VICINITY OF Massachusetts COURTHOUSE, REGISTRY OF DEEDSETC. Land Acquisition Division, National Park Service, North Atlantic CITY. TOWN STATE Boston, Massachusetts TITLE U.S. Coast Guard, 3d Dist., "Fire Island Station Annex" Civil Plot Plan 03-5523 DATE 18 June 1975, revised 8-7-80 .^FEDERAL —STATE —COUNTY —LOCAL DEPOSITORY FOR SURVEY RECORDS- Nationa-| park Service, North Atlantic Regional Office CITY, TOWN CONDITION CHECK ONE CHECK ONE —EXCELLENT _DETERIORATED —UNALTERED X-ORIGINAL SITE —GOOD _RUINS . X-ALTERED —MOVED DATE_____ X.FAIR _UNEXPOSED DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE The Fire Island Light Station is situated 5 miles east of the western end of Fire Island, a barrier island off the southern coast of Long Island. It consists of a lighthouse and an adjacent keeper's quarters sitting on a raised terrace. -
Landslides at Beachy Head, Sussex
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Landslides at Beachy Head, Sussex Beachy Head (Figures 1 and 2) is a famous natural and historic site and tourist attraction on the south coast. The cliff top area is part of the Downland Country Park managed by Eastbourne District Council. The section of cliff surveyed at Beachy Head is situated to the east of the modern lighthouse. The survey spans a 400 m south-facing stretch of beach with a cliff height of between 120 and 160 m. Figure 1 Cliffs and lighthouse at Beachy Head Figure 2 Field sketch at Beachy Head As part of a programme of work monitoring coastal erosion and landsliding at several sites around the coast of Great Britain, BGS has surveyed the cliffs at Beachy Head in Sussex using terrestrial LiDAR — see Terrestrial LiDAR Survey Techniques Geology The geology of the cliffs at Beachy Head consist of Cretaceous chalk comprising the Seaford Chalk and Lewes Nodular Chalk formations (formerly called the Upper Chalk Formation) overlying the New Pit Chalk Formation (formerly part of the Middle Chalk). The New Pit Chalk Formation (Turonian) in the lower part of the cliff is largely obscured by chalk debris. This is principally blocky, white firm to moderately hard chalk with numerous marls. Flint occurs sporadically or in seams in different part of the formation. Overlying the New Pit Chalk Formation is the Lewes Nodular Chalk Formation, which is Turonian to Coniacian in age. This consists of hard nodular chalk and chalkstone, which is locally porcellaneous. -
Black's Guide to Devonshire
$PI|c>y » ^ EXETt R : STOI Lundrvl.^ I y. fCamelford x Ho Town 24j Tfe<n i/ lisbeard-- 9 5 =553 v 'Suuiland,ntjuUffl " < t,,, w;, #j A~ 15 g -- - •$3*^:y&« . Pui l,i<fkl-W>«? uoi- "'"/;< errtland I . V. ',,, {BabburomheBay 109 f ^Torquaylll • 4 TorBa,, x L > \ * Vj I N DEX MAP TO ACCOMPANY BLACKS GriDE T'i c Q V\ kk&et, ii £FC Sote . 77f/? numbers after the names refer to the page in GuidcBook where die- description is to be found.. Hack Edinburgh. BEQUEST OF REV. CANON SCADDING. D. D. TORONTO. 1901. BLACK'S GUIDE TO DEVONSHIRE. Digitized by the Internet Archive in 2010 with funding from University of Toronto http://www.archive.org/details/blacksguidetodevOOedin *&,* BLACK'S GUIDE TO DEVONSHIRE TENTH EDITION miti) fffaps an* Hlustrations ^ . P, EDINBURGH ADAM AND CHARLES BLACK 1879 CLUE INDEX TO THE CHIEF PLACES IN DEVONSHIRE. For General Index see Page 285. Axniinster, 160. Hfracombe, 152. Babbicombe, 109. Kent Hole, 113. Barnstaple, 209. Kingswear, 119. Berry Pomeroy, 269. Lydford, 226. Bideford, 147. Lynmouth, 155. Bridge-water, 277. Lynton, 156. Brixham, 115. Moreton Hampstead, 250. Buckfastleigh, 263. Xewton Abbot, 270. Bude Haven, 223. Okehampton, 203. Budleigh-Salterton, 170. Paignton, 114. Chudleigh, 268. Plymouth, 121. Cock's Tor, 248. Plympton, 143. Dartmoor, 242. Saltash, 142. Dartmouth, 117. Sidmouth, 99. Dart River, 116. Tamar, River, 273. ' Dawlish, 106. Taunton, 277. Devonport, 133. Tavistock, 230. Eddystone Lighthouse, 138. Tavy, 238. Exe, The, 190. Teignmouth, 107. Exeter, 173. Tiverton, 195. Exmoor Forest, 159. Torquay, 111. Exmouth, 101. Totnes, 260. Harewood House, 233. Ugbrooke, 10P. -
Transactions 1885
93 jun ' so TRANSACTIONS OK THE iim'tulh ami Harwich NATURALISTS' SOCIETY; PRESENTED TO THE MEMBERS FOR 188S—86 . VOL. IV.— Part ii. NORWICH: PRINTED BY FLETCHER AND SON. 1880 . Norfolk anti Remind) naturalists' sorictu OFFICERS FOR 1886-87. yrrsitmt. SIR PETER EADE, M.D. C5x=|3rcstlirnt. MAJOR FEILDEN, F.G.S. Ftre=$restoents. THE RIGHT HON. THE EARL OF LEICESTER, K.G. THE RIGHT HON. THE EARL OF KIMBERLEY, K.G. THE RIGHT HON. LORD WALSINGHAM. SIR F. G. M. BOILEAU, Bart. MICHAEL BEVERLEY, M.D. W. A. TYSSEN AMHERST, M.P. HERBERT D. GELDART. HENRY STEVENSON, F.L.S. JOHN B. BRIDGMAN, F.L.S. •Treasurer. MR. H. D. GELDART. $on. Secretarg. MR. W. H. BIDWELL. (Tominittee. REV. J. A. LAURENCE. MR. T. R. BINDER. REV. E. F. LINTON. MR. T. SOUTHWELL. MR. G. C. EATON. MR. 0. CORDER. MR. J. B. FORRESTER. MR. A. W. PRESTON. DR. S. T. TAYLOR. Journal Committee. PROFESSOR NEWTON. MR. A. W. PRESTON. MR. JAMES REEVE. REV. J. A. LAURENCE. MR T. SOUTHWELL. auditor. MR. S. W. UTTING. TRANSACTIONS OF THE NORFOLK & NORWICH N A T U R ALISTS’ SOCIETY. The Norfolk and Norwich Naturalists’ Society has for its objects:— 1. The Practical study of Natural Science. 2. The protection, by its influence with landowners and others, of indigenous species requiring protection, aiul the circulation of information which may dispel prejudices leading to their destruction. 3. The discouragement of the practice of destroying the rarer species of birds that occasionally visit the County, and of exterminating rare plants in their native localities.