Artículos de revistas: "Devon and Dorset Regiment"

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Todd, Malcolm. "Roman Military Occupation at Hembury (Devon)". Britannia 38 (noviembre de 2007): 107–23. http://dx.doi.org/10.3815/000000007784016511.

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The large hillfort at Hembury, near Honiton (Devon) is one of the most impressive late prehistoric sites in South-West England. Occupied in the Neolithic and Iron Age, it was taken over by a Roman force about or shortly before A.D. 50. Substantial timber buildings were constructed, including a probablefabrica, in which iron from the adjacent Blackdown hills was worked. The Roman site was abandoned by the early Flavian period and not reoccupied. Though not evidently a conventional fort, Hembury joins a list of hillforts in South-West England which were used by the Roman army in the early decades of conquest. These include Hod Hill and possibly Maiden Castle (Dorset), Ham Hill and South Cadbury (Somerset).

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2

Brunsden, Denys. "The Dorset and East Devon Coast World Heritage Site: A Vision". Proceedings of the Geologists' Association 130, n.º 3-4 (junio de 2019): 263–64. http://dx.doi.org/10.1016/j.pgeola.2019.01.003.

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3

Gallois, Ramues y Hugh Owen. "The stratigraphy of the Upper Greensand Formation (Albian, Cretaceous) of the Isle of Purbeck, Dorset, UK". Acta Geologica Polonica 67, n.º 3 (26 de septiembre de 2017): 405–24. http://dx.doi.org/10.1515/agp-2017-0016.

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AbstractAt its maximum development in the type area on the Devon coast, the Upper Greensand Formation comprises up to 55 m of sandstones and calcarenites with laterally and stratigraphically variable amounts of carbonate cement, glauconite and chert that were deposited in fully marine, shallow-water environments. The formation is divided into three members, in ascending order the Foxmould, Whitecliff Chert and Bindon Sandstone, each of which is bounded by a prominent erosion surface that can be recognised throughout the western part of the Wessex Basin. The full thickness of the formation, up to 60 m, was formerly well exposed in cliffs in the Isle of Purbeck in the steeply dipping limb of the Purbeck Monocline. The upper part of the succession is highly condensed in comparison with the Devon succession and exhibits lateral variations over distances of hundreds of metres that are probably related to penecontemporaneous fault movements. Much of the fauna is not age-diagnostic with the result that the ages of parts of the succession are still poorly known. However, the Isle of Purbeck sections contain diverse ammonite faunas at a few stratigraphically well-defined levels that enable the succession to be correlated with that of east Devon and west Dorset.

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May, Vincent. "Coastal cliff conservation and management: the Dorset and East Devon Coast World Heritage Site". Journal of Coastal Conservation 19, n.º 6 (4 de septiembre de 2014): 821–29. http://dx.doi.org/10.1007/s11852-014-0338-8.

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5

Kong, Dal-Yong, Jong-Deock Lim y Min Huh. "Characteristics of the Dorset and East Devon Coast, a UNESCO World Natural Heritage Site, United Kingdom". Journal of Korean Nature 2, n.º 2 (septiembre de 2009): 99–102. http://dx.doi.org/10.1016/s1976-8648(14)60044-x.

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6

Gallois, Ramues. "The stratigraphy of the Permo-Triassic rocks of the Dorset and East Devon Coast World Heritage Site, U.K." Proceedings of the Geologists' Association 130, n.º 3-4 (junio de 2019): 274–93. http://dx.doi.org/10.1016/j.pgeola.2018.01.006.

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7

Jones, Andy M. y Henrietta Quinnell. "Daggers in the West: Early Bronze Age Daggers and Knives in the South-west Peninsula". Proceedings of the Prehistoric Society 79 (14 de mayo de 2013): 165–91. http://dx.doi.org/10.1017/ppr.2013.4.

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This paper describes the results from a project to date Early Bronze Age daggers and knives from barrows in south-west England. Copper alloy daggers are found in the earliest Beaker associated graves and continue to accompany human remains until the end of the Early Bronze Age. They have been identified as key markers of Early Bronze Age graves since the earliest antiquarian excavations and typological sequences have been suggested to provide dating for the graves in which they are found. However, comparatively few southern British daggers are associated with radiocarbon determinations. To help address this problem, five sites in south-west England sites were identified which had daggers and knives, four of copper alloy and one of flint, and associated cremated bone for radiocarbon dating. Three sites were identified in Cornwall (Fore Down, Rosecliston, Pelynt) and two in Devon (Upton Pyne and Huntshaw). Ten samples from these sites were submitted for radiocarbon dating. All but one (Upton Pyne) are associated with two or more dates. The resulting radiocarbon determinations revealed that daggers/knives were occasionally deposited in barrow-associated contexts in the south-west from c. 1900 to 1500 calbc.The dagger at Huntshaw, Devon, was of Camerton-Snowshill type and the dates were earlier than those generally proposed but similar to that obtained from cremated bone found with another dagger of this type from Cowleaze in Dorset: these dates may necessitate reconsideration of the chronology of these daggers

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8

Pinn, Eunice H. y Michelle Rodgers. "The influence of visitors on intertidal biodiversity". Journal of the Marine Biological Association of the United Kingdom 85, n.º 2 (31 de marzo de 2005): 263–68. http://dx.doi.org/10.1017/s0025315405011148h.

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The Purbeck Marine Wildlife Reserve lies within the boundary of the Dorset and East Devon World Heritage Site on the south coast. This study investigated the influence of visitors on intertidal biodiversity at Kimmeridge Bay, the only accessible part of the reserve. The assemblages present on two rock ledges were compared: Washing Ledge, which is regularly visited and utilized by people, and Yellow Ledge, which is more isolated and visited much less regularly. At each ledge, three habitat types were investigated: open rock, rockpools and the fucoid zone. Multivariate statistical analysis revealed significant differences in assemblages between ledges and among habitat types. The differences observed in the communities of the two ledges can be explained to some extent by natural ecological processes, but human impacts were also detected. The most obvious contrast associated with trampling was a reduction in the larger, branching species of algae and an increase in ephemeral and crustose species in the more heavily utilized areas.

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Mortimore, Rory N. "Late Cretaceous stratigraphy, sediments and structure: Gems of the Dorset and East Devon Coast World Heritage Site (Jurassic Coast), England". Proceedings of the Geologists' Association 130, n.º 3-4 (junio de 2019): 406–50. http://dx.doi.org/10.1016/j.pgeola.2018.05.008.

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Brereton, Tom, Duncan Jones, Keith Leeves, Kate Lewis, Rachel Davies y Trudy Russel. "Population structure, mobility and conservation of common bottlenose dolphin off south-west England from photo-identification studies". Journal of the Marine Biological Association of the United Kingdom 98, n.º 5 (27 de febrero de 2017): 1055–63. http://dx.doi.org/10.1017/s0025315417000121.

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In this study photo-identification data were used to better understand movements, population structure and abundance of common bottlenose dolphin (Tursiops truncatus) in south-west England and surrounding waters, to inform conservation efforts. A catalogue of 485 photographic sightings of 113 individuals was compiled from ~150 common bottlenose dolphin encounters made on 87 dates between March 2007 and January 2014. From these and other data, three likely sub-populations were identified in the western English Channel, demarcated by bathymetry and distance to land: (1) south-west England – inshore Cornwall to Devon, (2) offshore English/French waters and (3) inshore France from Brittany to Normandy. Maximum abundance estimates for south-west England coastal waters, using two methods, ranged between 102 and 113 (range 87–142, 95% CL) over the period 2008–2013, likely qualifying the region as nationally important, whilst the yearly maximum was 58 in 2013. The population was centred on Cornwall, where 19 well-marked animals were considered ‘probable’ residents. There were no ‘probable’ resident well-marked individuals found to be restricted to either Devon or Dorset, with animals moving freely within coastal areas across the three counties. Movements were also detected within offshore English waters and French waters (from other studies) of the western English Channel, but no interchange has as yet been detected between the three regions, highlighting the possible separation of the populations, though sample sizes are insufficient to confirm this. Given the findings, south-west England waters should be considered as a separate management unit requiring targeted conservation efforts.

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11

Kennedy, C. R. "Colonization and establishment of Pomphorhynchus laevis (Acanthocephala) in an isolated English river". Journal of Helminthology 70, n.º 1 (marzo de 1996): 27–31. http://dx.doi.org/10.1017/s0022149x00015091.

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AbstractThe successful colonization, establishment and spread of Pomphorhynchus laevis in a small, isolated, Devon river 128 km from the parasite's nearest focus in Dorset was followed over 11 years from 1985. The parasite was first detected in Anguilla anguilla and Platichthys flesus in 1988: by 1995 it had attained prevalence levels of 22.6% in A. anguilla and 43.6% in P. flesus and also occurred in 100% Salmo trutta, 50% Cottus gobio and Noemacheilus barbatulus. As judged by prevalence, abundance, proportion of females gravid and weight of gravid females, S. trutta was the preferred definitive host although C. gobio was a suitable host and may play a role in cycling the parasite: the other three species were unsuitable hosts. The intermediate host was the freshwater Gammarus pulex: the euryhaline G. zaddachi was not infected. On biological grounds, the P. laevis could be assigned to the English freshwater strain and was almost certainly introduced to the river by anthropochore stocking of S. trutta from a Dorset hatchery. The findings demonstrate conclusively that the English strain of P. laevis can colonize and establish in a new locality from which Leuciscus cephalus and Barbus barbus, its normal preferred hosts, are absent and use S. trutta instead. The results also confirm that P. laevis is a poor natural colonizer and appears always to be introduced to new localities by anthropochore transfers of fish. The implications of these conclusions for understanding the present distribution of P. laevis are discussed and it is considered that they provide direct evidence in support of the hypothesis that P. laevis was introduced to Ireland from England and subsequently adapted to use of S. trutta and G. duebeni there.

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12

Kelley, D. F. "Food of bass in U.K. waters". Journal of the Marine Biological Association of the United Kingdom 67, n.º 2 (mayo de 1987): 275–86. http://dx.doi.org/10.1017/s002531540002659x.

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Published information on the diet of bass in U.K. waters is limited. The very young fish, mainly 0- and 1-groups, have been investigated in the Fleet (Dorset) by Bass et al. (1983), in the Severn Estuary by Aprahamian & Barr (1985), and at the Kingsnorth power-station outfall in Kent by Langford (in preparation). Limited data for older fish have been given by Sant (1978) for the central Welsh coast and by Hester (1980) for the Cornish coast. An early report by the present author reviewed the feeding habits of 250 bass aged 3–16 years caught in 1946–52 in Devon and Cornwall (Kelley, 1953). Data for southern Irish waters have been given by Kennedy & Fitzmaurice (1972), and for west Brittany waters by Boulineau-Coatanea (1969). Other reports from mainland Europe are concerned chiefly with young bass reared in the etangs of the south and west coasts of France and in similar habitats on the coasts of Spain and Italy. There are similar reports from Tunis and Israel. These more specialised studies are listed by Barnabe (1980).

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13

Wilson, Ian Richard. "The constitution, evaluation and ceramic properties of ball clays". Cerâmica 44, n.º 287-288 (agosto de 1998): 88–117. http://dx.doi.org/10.1590/s0366-69131998000400002.

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Ball clay is a fine-grained highly plastic, mainly kaolinitic, sedimentary clay, the higher grades of which fire to a white or near white colour. The paper will review the origin of the term "Ball Clay" and the location and origins of several deposits with particular emphasis on the mineralogical, physical and rheological properties which make the clays so important in ceramics bodies. Particular attention will be paid to the well known bay clay deposits of Devon and Dorset in southwest England, which are mined by ECC International Europe and Watts Blake Bearne & Company PLC, and brief descriptions from elsewhere in the world of ball clays from the United States, Germany, Czech Republic, Thailand, Indonesia, Argentina and China. The evaluation of deposits will be covered along with a description of the main types of ball clay for ceramics with details of the mining, processing and blending techniques which are necessary to ensure long term consistency of products. A brief description in given of the ceramic properties of some Brazilian ball clays. The location of some ball clay deposits is shown in Fig. 1.

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14

Gallois, Ramues W. y Hugh G. Owen. "The stratigraphy of the Gault and Upper Greensand Formations (Albian stage, Cretaceous) of the Dorset and East Devon Coast World Heritage Site, U.K." Proceedings of the Geologists' Association 130, n.º 3-4 (junio de 2019): 390–405. http://dx.doi.org/10.1016/j.pgeola.2018.03.006.

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15

Weedon, Graham P., Kevin N. Page y Hugh C. Jenkyns. "Cyclostratigraphy, stratigraphic gaps and the duration of the Hettangian Stage (Jurassic): insights from the Blue Lias Formation of southern Britain". Geological Magazine 156, n.º 9 (17 de diciembre de 2018): 1469–509. http://dx.doi.org/10.1017/s0016756818000808.

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AbstractThe lithostratigraphic characteristics of the iconic Blue Lias Formation of southern Britain are influenced by sedimentation rates and stratigraphic gaps. Evidence for regular sedimentary cycles is reassessed using logs of magnetic susceptibility from four sites as an inverse proxy for carbonate content. Standard spectral analysis, including allowing for false discovery rates, demonstrates several scales of regular cyclicity in depth. Bayesian probability spectra provide independent confirmation of at least one scale of regular cyclicity at all sites. The frequency ratios between the different scales of cyclicity are consistent with astronomical forcing of climate at the periods of the short eccentricity, obliquity and precession cycles. Using local tuned time scales, 62 ammonite biohorizons have minimum durations of 0.7 to 276 ka, with 94% of them <41 ka. The duration of the Hettangian Stage is ≥2.9 Ma according to data from the West Somerset and Devon/Dorset coasts individually, increasing to ≥3.7 Ma when combined with data from Glamorgan and Warwickshire. A composite time scale, constructed using the tuned time scales plus correlated biohorizon limits treated as time lines, allows for the integration of local stratigraphic gaps. This approach yields an improved duration for the Hettangian Stage of ≥4.1 Ma, a figure that is about twice that suggested in recent time scales.

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16

Paul, C. R. C., Peter A. Allison y Carlton E. Brett. "The occurrence and preservation of ammonites in the Blue Lias Formation (lower Jurassic) of Devon and Dorset, England and their palaeoecological, sedimentological and diagenetic significance". Palaeogeography, Palaeoclimatology, Palaeoecology 270, n.º 3-4 (diciembre de 2008): 258–72. http://dx.doi.org/10.1016/j.palaeo.2008.07.013.

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17

Luxford, Julian. "Luxury and locality in a late medieval book of hours from south-west England". Antiquaries Journal 93 (6 de junio de 2013): 225–47. http://dx.doi.org/10.1017/s0003581512001345.

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This paper describes and analyses a previously unrecorded Sarum book of hours of considerable artistic and textual interest. Seven of its pages have bar-frame borders illuminated in a distinctive and remarkable style. Four of these pages also have initials with figure-subjects, some of which are contextually unusual or unique. There is also an initial with a coat of arms displaying a black engrailed cross on a gold field (the arms of Mohun of Dunster in west Somerset). While the manuscript cannot be linked to a member of the Mohun family, the occurrence of a Somerset toponym in an obit dated 1429 in the calendar and the early addition to the litany of St Urith of Chittlehampton show that it was owned by someone who lived in Somerset or Devon in the early fifteenth century. Indeed, the book may also have been made in this region. Several features of its border illumination are paralleled in the Sherborne Missal (London, British Library, Additional ms 74236), produced in north Dorset or Somerset in the decade c 1398–c 1408. The parallels suggest a relationship (not necessarily direct) between the two manuscripts. Certainly, the book of hours discussed here is closer in style to the missal than it is to manuscripts made in or around London in the same period.

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18

Saul, Nigel. "Medieval Pilgrimage: with a survey of Cornwall, Devon, Dorset, Somerset and Bristol. By Nicholas Orme. Pp xiii + 191, 46 col figs. 230mm. Impress Books, London, 2018. isbn9781911293354. £14.99 (pbk)." Antiquaries Journal 99 (septiembre de 2019): 457–58. http://dx.doi.org/10.1017/s0003581519000428.

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19

Neil, Samantha, Jane Evans, Janet Montgomery y Chris Scarre. "Isotopic Evidence for Landscape use and the Role of Causewayed Enclosures During the Earlier Neolithic in Southern Britain". Proceedings of the Prehistoric Society 84 (6 de agosto de 2018): 185–205. http://dx.doi.org/10.1017/ppr.2018.6.

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The nature of landscape use and residence patterns during the British earlier Neolithic has often been debated. Here we use strontium and oxygen isotope analysis of tooth enamel, from individuals buried at the Hambledon Hill causewayed enclosure monument complex in Dorset, England to evaluate patterns of landscape use during the earlier Neolithic. Previous analysis suggests that a significant proportion of the artefacts found at the site may originate from lithology of Eocene and Upper to Middle Jurassic age that the enclosures overlook to the immediate west and south. The excavators therefore argued that the sector of landscape visible from Hambledon Hill provides an approximate index for the catchment occupied by the communities that it served. Most of the burial population exhibit isotope ratios that could be consistent with this argument. Connections between Hambledon Hill and regions much further afield are also hypothesised, based on the presence of artefacts within the assemblage that could have been sourced from lithology in Somerset, Devon, and Cornwall in south-west England. However, few of the sampled individuals have strontium isotope ratios consistent with having obtained the majority of their diet from such areas during childhood. The individuals who exhibit the highest strontium isotope ratios are all adult males, whom the excavators suggest to have died during one or more episodes of conflict, following the burning and destruction of surrounding defensive outworks built during the 36th centurybc. At least one of these individuals, who was found with an arrowhead amongst his ribs, did not obtain his childhood diet locally and has87Sr/86Sr values that could be comparable to those bioavailable in the south-west peninsula.

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WEEDON, GRAHAM P., HUGH C. JENKYNS y KEVIN N. PAGE. "Combined sea-level and climate controls on limestone formation, hiatuses and ammonite preservation in the Blue Lias Formation, South Britain (uppermost Triassic – Lower Jurassic)". Geological Magazine 155, n.º 5 (30 de enero de 2017): 1117–49. http://dx.doi.org/10.1017/s001675681600128x.

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AbstractLithostratigraphic and magnetic-susceptibility logs for four sections in the Blue Lias Formation are combined with a re-assessment of the ammonite biostratigraphy. A Shaw plot correlating the West Somerset coast with the Devon/Dorset coast at Lyme Regis, based on 63 common biohorizon picks, together with field evidence, demonstrate that intra-formational hiatuses are common. Compared to laminated shale deposition, the climate associated with light marl is interpreted as both drier and stormier. Storm-related non-deposition favoured initiation of limestone formation near the sediment–water interface. Areas and time intervals with reduced water depths had lower net accumulation rates and developed a greater proportion of limestone. Many homogeneous limestone beds have no ammonites preserved, whereas others contain abundant fossils. Non-deposition encouraged shallow sub-sea-floor cementation which, if occurring after aragonite dissolution, generated limestones lacking ammonites. Abundant ammonite preservation in limestones required both rapid burial by light marl during storms as well as later storm-related non-deposition and near-surface carbonate cementation that occurred prior to aragonite dissolution. The limestones are dominated by a mixture of early framework-supporting cement that minimized compaction of fossils, plus a later micrograde cement infill. At Lyme Regis, the relatively low net accumulation rate ensured that final cementation of the limestones took place at relatively shallow burial depths. On the West Somerset coast, however, much higher accumulation rates led to deeper burial before final limestone cementation. Consequently, the oxygen-isotope ratios of the limestones on the West Somerset coast, recording precipitation of the later diagenetic calcite at higher temperatures, are lower than those at Lyme Regis.

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21

Hosfield, Robert y Jennifer Chambers. "Genuine Diversity? The Broom Biface Assemblage". Proceedings of the Prehistoric Society 75 (2009): 65–100. http://dx.doi.org/10.1017/s0079497x0000030x.

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The Broom Lower Palaeolithic locality, on the river Axe at the Devon/Dorset border in south-western Britain, yielded an assemblage of at least 1800 Acheulean artefacts between the 1870s and 1940s through gravel quarrying and antiquarian collection. The bifacial material, predominantly produced in chert but including a small flint component, is characterised by considerable typological diversity and a distinctive asymmetrical element. While aspects of the assemblage have been reported before, this paper presents new work on the artefacts of the C.E. Bean collection and the sample from Exeter Museum. The Bean archive indicates that the artefact patterning is not due to fluvial mixing of separate, typologically-discrete, assemblages. Analysis of the artefacts suggests that hominin knapping strategies were not notably constrained by variations in raw material granular quality, but that the typological variability strongly reflects blank form and shape. However, while the influences of blank form and resharpening, including the use of tranchet flaking, partially explain the assemblage's asymmetrical component, a significant proportion of those artefacts cannot be understood in these terms. The existence of local, short-lived manufacturing traditions, perhaps reflecting the idiosyncratic approaches of individual knappers, is argued to best explain the distinctive asymmetrical element of the Broom assemblage. This interpretation is further supported by (i) the geoarchaeological model of assemblage formation, which assigns the majority of the artefacts to a single phase of occupation, and (ii) the OSL ages of the Broom fluvial deposits (predominantly MIS-9 and 8) and the atypical character of the assemblage in relation to other British late Lower Palaeolithic material, which oppose the notion of longer-lived, locally, or regionally-maintained, traditions.

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22

Ambler, Richard P. y Kenneth Murray. "Martin Rivers Pollock. 10 December 1914 – 21 December 1999". Biographical Memoirs of Fellows of the Royal Society 48 (enero de 2002): 357–73. http://dx.doi.org/10.1098/rsbm.2002.0021.

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Martin Rivers Pollock was born in Liverpool on 10 December 1914. He came from an old legal family, being the great-great-grandson of Sir Jonathan Frederick Pollock, Bt. (1783–1870), a Fellow of Trinity College, Cambridge, barrister, MP for Huntingdon, Attorney General in Peel's first administration and Chief Baron of the Exchequer from 1844 to 1866. His father, Hamilton Rivers Pollock, also went to Trinity College, qualified as a barrister but never practised, and in 1914 was with the Cunard Steam Ship Company, before spending World War I with the Liverpool Regiment and the Royal Air Force. His mother was Eveline Morton Bell, daughter of Thomas Bell, of Newcastle-upon-Tyne. After the war his father inherited a fortune from an uncle, and the family moved to Wessex, where they lived first at splendid Anderson Manor, Dorset, and then Urchfont Manor, Wiltshire, his father living as a country squire and JP. Pollock had a conventional upper-class education, beginning with a nanny, followed by West Downs School (1923–28) and then Winchester College (1928–33). His first scientific enthusiasm was for astronomy, but he decided he was insufficiently mathematical to pursue it further (his mathematics master was Clement Durrell, author of some famous texts including Advanced algebra), so he then decided to study medicine. His Wessex schooldays were influenced by the nearby Powys brothers, the youngest (Llewelyn1) having been a Cambridge friend and contemporary of his father. Through Sylvia Townsend Warner2 he met her cousin Janet, daughter of Arthur Llewelyn Machen3, who eventually, in 1979, became his second wife. He went up to Trinity College, Cambridge, in 1933, having done his first MB and the first part of his second MB while still at school, and opting to do the two new half-subjects (Pathology and Biochemistry) that had just been instituted—he remembered thinking at the time that biochemistry was going to be the key subject for medicine in the future. Already while at school he had become a theoretical Communist, and as an undergraduate worked very hard, both at his medical studies and in political activity (such as selling the Daily Worker) for the Party—and knew most of the soon-to-be notorious Cambridge Communists of the time, including Guy Burgess4 and Donald Maclean5. He was now a Senior Scholar, and graduated BA first class in 1936; he started to spend a fourth year reading Part II Biochemistry. He decided in April 1937 that he had spent too long at Cambridge, so moved on to his clinical studies at University College Hospital. He also felt he should try to become qualified before what he saw as the inevitable war started, although he was nearly distracted into joining the International Brigade and going off to Spain—he had been a friend of John Cornford6, who did go to Spain and wrote and died there, and of Norman John (but widely known as James) Klugmann.

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Gale, A. "Review of Shipwreck index of the British Isles: Volume 1 Isles of Scilly, Cornwall, Devon, Dorset, by R. Larn and B. Larn; Old Ironsides The Rise, Decline & Resurrection of the USS Constitution, by T. C. Gillmer; The Sailing Navy List: all the Ships of the Royal Navy Built, Purchased and Captured, 1688 1860, by D. Lyon; Captain Cook's Endeavour (Conway's Anatomy of the Ship series), by K. H. Marquardt; Navies and Nations: Warships, Navies and State Building in Europe and America, 1500 1860, by J. Glete; Österjons Sjunkna Skepp. En Marinarkeologisk Tidsresa, by J. Rönnby and J. Adams; Building Plank-on-Frame Ship Models, by R. McCarthy; The Foundry: Excavations on Poole Waterfront 1986/7, by D. R. Watkins and Versunken in der Ostsee Schiffe und Schätze auf dem Meeresgrund, by G. Lanitzki." International Journal of Nautical Archaeology 24, n.º 3 (agosto de 1995): 237–46. http://dx.doi.org/10.1006/ijna.1995.1031.

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Jenkins, John. "Medieval Pilgrimage: With a Survey of Cornwall, Devon, Dorset, Somerset and Bristol, by Nicholas Orme". English Historical Review, 17 de noviembre de 2020. http://dx.doi.org/10.1093/ehr/ceaa201.

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"Corrigendum to “The stratigraphy of the Permo-Triassic rocks of the Dorset and East Devon Coast World Heritage Site, U.K.” [Proceedings of the Geologists' Association 130 (2019) 274–293]". Proceedings of the Geologists' Association 130, n.º 6 (diciembre de 2019): 799. http://dx.doi.org/10.1016/j.pgeola.2019.09.002.

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