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Perhaps the best result of the Birming- ham school will hardly be achieved until the formal effe6t of its training is less patent. The ' sixties ' might have been void of art, so far as these designers are concerned, save that in those days Morris and Burne-Jones and Walter Crane, as well as Millais and Houghton and Sandys, were about their work. Far other is the case with artists such as Mr. Byam Shaw, or with the many draughtsmen, including Messrs. P. V. Woodroffe, Henry Ospovat, Philip Connard, and Herbert Cole, whose art derives its form and intention from the sixties. Differing in technical power and fineness of invention, in all that distinguishes good from less good, they have this in common — that the form of their art would have been quite other if the illus- trated books of that period were among things unseen. Mr. Byam Shaw began his work as an illustrator in 1897 with a volume of' Browning's Poems,' edited by Dr. Garnett. He proved himself in these draw- ings, as in his pictures and later illustrations, an artist with a definite memory for the forms, and a genuine sympathy with the aims of pre-Raphaelite art. Evidently, too, he admires the black-and- white of Mr. Abbey. He has the gift of dramatic conception, sees a situation at high pitch, and has a pleasant way of giving side-lights, pi(5torial asides, by means of decorative head and tailpieces. Feneris video er key. His illustrations to the little green and gold volumes of the ' Chiswick Shakespeare ' are more emphatic than his earlier work, and in the decorations his H ENGLISH BOOK-ILLUSTRATION power of summarizing the chief motive is put to good use.

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As for caricature of Nero, the Roman writers don't seem all that fond of him, either. I knew before I watched this how Boudicca died, so I assumed (wrongly perhaps) that they simply didn't show it. However Tacitus says she took poisoned and died.

I watched this on prime-time television with the expectation of seeing a good production. There is nothing that I can write about this poor quality production which would recommend it. The events of this part of our history are not well documented but Boudica did exist so at the very least we should have been treated to a more realistic portrayal of her and her exploits. Alex Kingston acted the part well but she was handicapped by a bad script, poor supporting actors and very unrealistic scenery and props. This was a lost opportunity to show a piece of English history to a generation who probably know little about the past. Even a computer generated Star Wars type film would have been preferable to this production. There is little more to say but please do better next time English history is being screened.


The world turned weird and bright for a second. She was suddenly standing in a rundown, messy room. The walls were coated in graffiti, the ceiling was spotted with mold. The summoning circle was drawn with care, but clearly by a non-professional - or perhaps the uneven wooden floor was to blame for the wonky chalk lines.

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The abbreviated character of this list will be appreciated when it is understood that although the works of Turner, Lobel, Bauhin, and Gerarde, ranging from 1538 to 1641, con- tain several hundred first notices, Cornwall was an unknown land to those authors. Gerarde's Herbal (1633) is the starting point of Cornish botany, but it contains only one reference; even that one, Plantago maritima, belongs to the Scilly Isles. With Merrett's Pinax Rerum Naturalium, Parkinson's Tbeatrum Botanicum, Ray's several works, Hudson's Flora Anglica, and Withering's Arrangement, disappeared the old order. The publication of the Botanist' s Guide (1805) was the beginning of that vast accumulation of facts, scattered it is true, which is now at the disposal of the student of the flora of Cornwall. Jones' Botanical Tour (1820) and Watson's New Botanist's Guide (1835) brought the county more into line with its neighbours. Then in rapid succession followed a number of workers Rev. W. T. Bree, C. C. Babington, W. Borrer, Rev. W. S. Hore, G. S. Gibson, Rev. C. A. Johns, W. Curnow, Dr. Ralfs, F. V. Pascoe, T. R. A. Briggs, I. W. Keys, H. C. Bastian, T. Q. Couch, Rev. W. Moyle Rogers, H. and J. Groves, J. Cunnack, Dr. Hind, J. G. Baker, Miss Warren and others, whose contributions to the Botanical Gazette, the Phytologist, the journal of Botany, and to the Transactions of local scientific societies are of greatest value.


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Celtic-Roman history seems to be beyond film/television writers ken. Maybe they need to read a little.

Besides the differences we have noted these rocks present great variations in their decomposition, being often represented by a soft clay, as their felspars readily decompose into kaolin. On the other hand the durability of certain elvans is such that they provide some of the best building material which the county possesses. Their general distribution is noted on the map, from which it will be seen that the greatest departure from their usual trend, parallel to the longitudinal axis of the county, occurs in the elvan system of St. Austell, which follows a course slightly north of west. The mica traps of Cornwall consist of dyke-like intrusions, the range of which is mainly restricted to a belt of country running north and south between Newquay and Falmouth Bay. This peculiar type of intrusions as related to Cornwall was first described by Mr. J. H. Collins. Their most characteristic feature in the field is a marked readiness to decompose, so that a fresh surface of the rock is seldom visible, and consequently they have been utilized to a trifling extent as building material. They are usually of a rusty brown colour, and occur as dykes and sills within the slates, not usually continuous for more than short distances. They vary in width from a foot to 50 yards, and have effected a very limited amount of contact alteration on the slates which they traverse. They often exhibit spheroidal structure, cores of more solid rock being encircled by concentric outer layers of exfoliating material; and flow structure is not uncommon, more especially in the finer grained marginal portions. Notwithstanding their advanced state of decomposition, the ground-mass of these rocks can generally be seen to consist of a medium-grained admixture of biotite and felspar, while inclusions of quartz and crystalline felspathic rock are character- istic.

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These peculiar zones of metamorphism are sometimes observed where visible granite is absent; Mr. E. Dixon has recorded two such metamorphic areas, one north of Gwinear, the other around Leeds- town, from which we may confidently infer that bodies of granite lie below the surface. Moreover the great elvan region which abuts against the granite at Gwennap contains large areas of spotted slate, but the meta- morphism is more feeble than that found bordering the granite mass. The granite of the Brown Willy district frequently contains large porphyritic crystals of felspar, and is more particularly schorlaceous towards the south. The granite district of Hensborough or St. Austell is far more variable and more schorlaceous. This granite was described by Dr. Boase and in more recent years by Mr. J. H. Collins. The latter observer alludes to the large size of the porphyritic felspars, and calls attention to veins almost entirely composed of that mineral, while others consist almost exclusively of mica. He also records the occurrence of both lithia and fluorine in the micas of this granite, and the relation which the latter element bears to the decomposition of felspar into kaolin, with which the very existence of our china clay industries is linked. As the industries and minerals of Cornwall will be treated in a separate section it will suffice here to state that china clay and china stone are the products of the decomposition of the granite in situ, and that this chemical alteration appears to be mainly brought about by the action of fluoric acid. The relative abundance of fluorine therefore in the original rock mass is probably the determining factor in the production of china clay, and its restriction as regards commercial purity to limited areas. In the Carn Menelez granite for instance the decomposition of its mass rarely yields china stone, and in conjunction with this fact we find an almost entire absence of fluor spar except in association with the mineral veins.

The Victoria history of the county of Cornwall. Edited by William Page

If he had been anyone but himself, he probably would not even have noticed it, but he was and he did. For a fraction of a moment he even considered letting it live, as a tribute to the pure nerve it took to sting him of all people, but no. Stinging bugs did not deserve his mercy.


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An undemanding movie set in historic rural England. Many lovely scenes from the village life, good costumes and sympathetic characters.

If this is going to have a theatrical release in the US this is going to bomb big time. A very dissapointing film, with the occasional good momment, but the worst thing is the typical trates of ITV dramas that have crept in. The tendancy for everyone behind the scenes to try and stand out from the crowd by throwing in their own little bits. As a result what could have been a good film was pretty much destroyed.


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This takes in a long narrow tract of country at no place more than 7 miles wide, and for a considerable distance little above 3 miles wide. As the crow flies its length from Stepper Point, outside Padstow Harbour, to Hayle is about 33 miles. Its boundary is the road from Padstow through St. Columb to Blue Anchor, forming the western limit of the Camel District. From Blue Anchor the line follows the turnpike road through Mitchell, Zelah, and Scorrier to Redruth. At the mining town of Redruth it takes the Helston road across Buller Downs, turning offat Nine Maidens, and at Praze Station joining the railway line to Hayle. Geologically this is an interesting district. From Stepper Point to the northern bank of the Gannel at Newquay the soil is Lower Devonian, and the whole of that district has been brought to a fine state of cultivation. West of the Gannel, coastwards from a line drawn from the head of the creek to Perranporth, the country is Upper Silurian intersected by elvan courses and the well known Perran Iron Lode. A little distance from the south bank of the upper waters of the Gannel there are faint traces of a small deposit of limestone. Inland from the line above indicated Lower Silurian cover portions of the parishes of Cubert, Newlyn East, and Perran, while at St. Enoder the district takes in a small portion of the same rocks which form a belt around Hensbarrow Hill.


The 'killas' of Corn- wall, in spite of superinduced structures which largely mask its original condition, is seen to contain alternating layers of gravel, sand and mud similar to those which are observed in our recent deposits. Moreover, preserved within the strata are the fossil remains of the marine life that flourished in those ancient seas, but of types essentially different from our modern fauna; while beds of limestone charged with fossils are the result of organic accumulations in clear water free from the inva- sion of sediment. In other words the rocks which enter so largely into the geological architecture of Cornwall belong to an early chapter in the history of that marine plain or great littoral fringe when its boundaries differed widely from those of to-day. Commingled however with the sediments we find the products of volcanic action in the remains of lava streams and ashes, which having been emitted on the sea-floor have been sealed beneath the overlying accumulation. Under the influence of crustal movements the Palaeozoic deposits with their volcanic beds have gradually subsided, and have been buried beneath a deep pile of overlying strata. So great has been their downward movement that they have been brought within the influence of the great laboratory that lies 16 GEOLOGY beneath the crust. In those subterranean regions they have not only had to support a pile of superincumbent strata, but have been sub- jected to a vast amount of mechanical deformation by the operation of powerful earth stresses. Under the influence of pressure the incoherent particles which enter into the composition of the sediments have been compacted into solid rock. On these rocks the earth movements have produced structural modifications which have not only affected the indi- vidual beds, but also the material of which they are composed. In response to lateral pressure the strata have been bent and doubled back one over another and thrown into a set of folds closely packed together; and finally have obtained relief from the strains by actual disruption.

Anyway, the fighting was well done, but teh ending was too abrupt and left the viewer wanting to know what happened after the battle. All in all, the show was about 90 minutes.


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I actually liked the main player, Alex Kingston. I didn't watch ER, so I have no preconceptions about her.

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It was also about an empire which ran over indigenous people, a practice which continues into the present time. There are many lines in the movie which might just remind you of current day statements. And listen closely to Nero, does he remind you of anyone? The actors are all great in my opinion, they do not falter or miss a beat. Yes, it is a bit violent, and if that is a concern, you should not allow small children (under 8 or 10) to view this. Since we rarely see things about the Celts, I was happy to have an idea of how they dressed and some of their customs. Women definitely had equality, and that is rare to see even in these modern times.


OK, no one expects 100% accuracy. There are 100% accurate productions - they are called documentries. A film/programne can be historically inaccurate and be a darn good spectacle (Gladiator, Braveheart) but it is a different kettle of fish to insult the viewing public with a cheap, badly written and produced item like this.

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The granites vary considerably in texture, but their mineral composition is so closely allied that we are driven to the conclusion that the various individual bosses derived their material from a common source of supply. Mining operations have demonstrated the underground connection of the granites of Carnbrea and Carn Menelez. Similarly the smaller patches which occasionally flank the larger bosses are in all probability united below ground with the main mass. From this reasoning it might be in- ferred that if we could strip off the overlying killas the larger granite masses would be similarly connected; but in spite of their close petro- logical relationship these larger bosses have acquired a marked individu- ality both as regards their texture and the distribution of their chemical contents. It would appear therefore that each of these bosses marks the site of individual eruptive centres, the materials of which have been derived from a common magma at lower depths. Moreover, although 24 GEOLOGY their upper surfaces appear to be domes, it is by no means unlikely that they are huge laccolites, which have been forced laterally between the strata under somewhat similar conditions to the smaller injections which constitute the greenstone sills. Further, although derived from the same magma basin they may differ widely in geological age. Of these five larger bosses the Cam Menelez granite occupies the central position. As it is also the chief seat of the Cornish granite industry, as well as our most important mining centre, its composition and structure will be more particularly described, and the remaining granite masses will be touched upon later in so far as they depart from this type. In the Carn Menelez granite we shall include the two ad- jacent patches of Carnbrea and Carnmarth which are in such close con- tiguity as to lie within the same eruptive centre.


This varying soil cap, due to the form of the ground, produces marked divergence in the agricultural value of the land, apart from the nature of the parent rock from which the soil has been derived. While the richness of the soil depends upon the ever-varying nature of the rock, the quantity of soil dependent upon physical situation is a factor of equal importance in its bearing on the fertility of the county. The perpetual creep of the soil to lower levels is well illustrated in some of our upland valleys, where alluvial basins have been so encroached upon by the downward creep that their ancient margins have been completely obliterated. The stream-tin valley of Porkellis in the parish of Wendron_is fringed with gentle slopes in which the granite is completely hidden by a soil-cap made up of its own dis- integration, and corresponding precisely with the granite alluvium which floors the valley; and the one shades imperceptibly into the other. The high ground in Cornwall occupied by the granite presents frequent in- stances of basins in which the original flat is gradually being obliterated by the soil creep from the slopes. Some of the moors which so frequently occur at the head of our valleys have thus been formed. Largely composed of clay, the want of fall renders drainage difficult, and their bottoms are frequently lined with marshes. Being on this account unsuitable for cultivation they are given over to scrub and gorse and afford coverts for game, just as many of the rocky slopes in the granite districts consist of moorland stretches, clothed with gorse and bracken, the recesses of which form the congenial haunts of the fox. Large tracts on the seaboard of Cornwall owe their existence to the 5 A HISTORY OF CORNWALL direct action of wind, and form extensive sand dunes and towans. These aeolian deposits are most strongly developed on the northern coast, where large areas are permanently cut off from the operations of the plough.

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I don't think the Britons grew cabbages either, maybe mushrooms though I don't know. Their diet consisted mainly of meat, cheese, bread, cakes and apples and berries, maybe some leaves were used as vegetable garnish. Herbs were used in medicine rather than cooking.


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It's got some great sets and costumes, a fantastic, frankly groundbreaking soundtrack of calling vocals, and spectacular deeply theatric moments, basically any time the characters aren't actually speaking is OK. The dialogue is fundamentally awful, Romans are one-dimensionally bad, absurdly condescending and arrogant, and barbarians good. Obviously the writer wanted to make this a commentary about current politics, referring to Icenians as "terrorists", a concept which did not exist at the time.

There's an air of Icelandic saga simmering over the movie all the time with unnerving background music. Women have the central stage here and the movie will talk to many both girls and boys, although it is somewhat bloody at times.


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The faults often occur every few yards, both parallel to the strike (or trend of the beds) and in oblique directions, with the result that the whole rock-mass when seen in ground plan presents the appearance of a huge mosaic. On that part of the coast with which we are now dealing neither large faults nor large folds are common. It would appear that at an early stage of the folding process the resistance to the strains was so feeble that fractures were readily produced. In many districts reversed faults are as numerous as those of normal type. Although the rocks are everywhere cleaved we can in most cases on the south coast distinguish between the cleavage and bedding. The alternations from argillaceous to arenaceous material are so numerous that there is little difficulty in distinguishing these structures. The cleavage which is usually oblique to the bedding varies with the nature of the 21 A HISTORY OF CORNWALL material it traverses, and is always deflected in crossing from an argilla- ceous to an arenaceous bed, and vice versa. The slates on this part of the south coast have a prevailing south- easterly hade, both in bedding and cleavage. By bedding should be understood the lithological alternations due to original stratification, which in most cases along the coast section represent the limbs of folds. Where these are regular in their hade, and the cleavage is uniform, the section may present such an undisturbed appearance that the folding might easily be overlooked.


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Another painter, known for his work in black and white, is Mr. John Fulleylove, whose ' Pictures of Classic Greek Landscape,' and drawings of ' Ox- ford,' show him to be one of the few men who see architecture steadily and whole, and who draw beautiful buildings as part of the earth which they help to beautify. Compare the Greek drawings with ordinary archaeological renderings of pillared temples, and the difference in beauty and interest is apparent. In Mr. Fulleylove's drawings, the relation between landscape and architecture is never forgotten, and he draws both with the struc- tural knowledge of a landscape painter, who is also by training an archited. In aim, his work is in accord with classical traditions; he discerns the classical spirit that built temples and carved statues in the beautiful places of the open-air, a spirit which has nothing of the museum setting about it. The ' Oxford ' drawings show that Mr. Fulleylove can draw Gothic. Though not a painter, Mr. William Hyde works ' to colour ' in his illustrations, and is generally successful in rendering both colour and atmosphere. He has done little with the pen, and it is in wash drawings, reproduced by photogravure, that he is best to be studied. Of his early training as an en- graver there is little to be seen in his work, though his appreciation of the range of tone existing between black and white may have developed from working within restrictions of monotone, when the colour 40 ENGLISH BOOK-ILLUSTRATION sense was growing strong in him. At all events he can gradate from black to white with remarkable minuteness and ease. His earliest work of any im- portance after giving up engraving, was in illustra- tion of ' L'Allegro ' and 'II Penseroso,' 1895, and shows his talent already well controlled. There are thirteen illustrations, and the opportunities for rendering aspe6ts of light, from the moment of the lark's morning flight against the dappled skies of dawn, to the passing of whispering night-winds over the darkened country, given in the verse of a poet sensitive as none before him to the gradations of lightness and dark, are realized.

Alex Kingston does a good job playing the difficult role of the Warrior Queen and as a bonus; she is actually British. Claudius and Nero make brief appearances. Jack Shepherd successfully duplicates the charming interpretation of Claudius that Derek Jocobi performed in the mini-series `I, Caudius'. Although Nero is a strange, stylised performance with use of some very modern phrases which do jar somewhat.


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Moreover these differences in metamorphism are accompanied by the most marked divergence in the preservation of organic remains; while the eastern area has yielded fossils in tolerable abundance, albeit in a poor state of preservation, the western district is characterized by their extreme rarity. The unravelling of the stratigraphical sequence therefore is attended with serious difficulties. For not only have the ancient stratigraphical boundaries been masked by the extensive deformation to which the rocks have been subjected, but their included fossils to which we might other- wise appeal as chronological landmarks have shared in these processes. The better preservation of the fossils in the eastern area has permitted the historical succession of the formations to be more accurately defined than in the west. An inspection of the map will show the southern boundary of the Culm Measures as extending from the vicinity of Boscastle to Horsebridge, which spans the Tamar near the horizon of Tavistock. The Devonian formation which occurs below the Culm Measures, although tolerably defined in its upper limits by that undulatory boun- dary, does not admit of such precise definition as regards its base. A zone that traverses the county from St. Austell Bay to Holywell Bay, approximately defines the limits of the lowest Devonian beds which have yielded reliable zonal fossils. South of that zone the killas is singularly barren of fossil remains 36 GEOLOGY excepting the narrow strip which forms its eastern margin, where be- tween Mevagissey Bay and Gerrans Bay the grey quartzites yielded to the late Mr. C. W. Peach fossils of Caradoc or Bala age. In the south- westerly prolongation of that zone, which traverses the Meneage peninsula and contains similar lithological types, the quartzites have yielded fossils to Mr. J. H. Collins, while the limestones of both areas enclose frag- mental remains of crinoids. It will be seen therefore that the succession from the Culm Measures (Carboniferous) to the Caradoc (Ordovician) is broken by the geological chapters which separate the latter epoch from the Lower Devonian.

Lolonja admitted that the hooves she were walking on were not very human-like, but at least her eyes had pupils. Incandescence, who after an incident a few weeks after she joined the Flock would never again take a human-like form, walked beside the small group as a large, neon, rainbow-coloured poodle.


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These quartz crystals have often rounded angles which in extreme cases result in their appearance as bleb-like patches without crystalline form. Not only are there all degrees in the texture of the matrix, but the variation is equally wide in the porphyritic constituents both as regards individual size, number, and the nature of the mineral which is porphy- ritic. In some cases the porphyritic felspars are of large size and have been formed in the plutonic magmas from which the elvans have been derived; and there is necessarily every gradation between crystallization of the dyke and plutonic phase, the growth of many crystals having been continuous in both of these conditions. Although identical minerals occur in both elvan and granite, mica A HISTORY OF CORNWALL is more distinctly predominant, in proportion to the other constituents, in granite than in elvan. A characteristic feature of the elvans is the tendency for the white mica to assume a radiating or plumose habit, and in the matrix of the rock to combine with the felspar in forming a pegmatitic structure. The granophyric habit is not confined to this type, but pseudo-spheru- litic structures have also been noted. In width the elvans range from a few feet to many yards; a dyke however of abnormal dimensions has been traced following an east and west course through Gwennap, and attaining a width of 150 to 200 yards. Although the elvans are usually very steeply inclined, they exhibit much variation in this respect, and sometimes lie nearly flat. They occur in greatest abundance in districts invaded by granite, although the number that pierce that rock is far inferior to those enclosed by the killas. Occasionally they are found penetrating green- stone, as at Burntcoose in the parish of Gwennap.

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In sum, a very engaging film that I'm adding to my collection. Already watched it several times since first seeing it a few weeks ago. Yes, I like and enjoy it - led me to look more closely into the history and that's not a bad thing.

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I'm aware there are historical inaccuracies (not at all clear the spelling of the titular name is one of them - Boudicca and Boadicea are both recognized alternatives), but when did that become unusual for non-documentary? My impression is the purpose was to engage and entertain, and as far as I'm concerned, it accomplished that. Alex did a superb job with her character and the other Celtic characters also worked for me.

She had never personally seen a static worm before, and she suspected neither had the surgeon, but they had both seen the pictures. They were white, shapeless worms with sharp spines sticking out of them, varying in size depending on the host. They should not get much bigger than her pinkie finger. This one was as thick around as her wrist, and almost as long as her forearm. It curled around his uppermost rib and had its spines deeply embedded in the bone.


He looked up, just as the princess of the movie gave the hero a slap. He didn't say anything, just lifted a brow.

All my life I have had a special interest in ancient Celtic culture and lifestyle and a particular fascination for 1st century Britain. Therefore i have done a great lot of research over the years and read and watch anything I can find on the subject.


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One of the major flaws is the casting of Alex Kingston as Boudica. All through the puzzling battle scenes, I kept thinking: " 'Dr.


Full text of The Victoria history of the county of Cornwall. Edited by William Page

At the end, we heard Boudicca announce in voice-over that `we (the Celts, Iceni, etc) don't write stories down, we live them'. There was no story here, just a collection of blindingly obvious landmarks, the links between which were unnecessarily reinforced by truly awful dialogue that demeaned an otherwise fine cast. Aside from making me want to laugh & cry in all the wrong places, it was utterly unemotive, with the exception of Boudicca's public humiliation.

Fenris Film & Multimedia

I loved Alex Kingston (of ER and numerous British period pieces) as the fierce, yet human Queen Boudica (also spelled Boadicea)! She was believably tough, yet believably naive in her struggles with the overwhelming forces of Rome. The whole plot boils down to a clash of two cultures: one ancient and decentralized and one a "modern" empire which butchers with ruthless efficiency. An inspiring tribute to the human spirit!


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On its eastern and southern sides this district is coterminous with the Upper Tamar and Fowey Districts. Its coast line lies between Tintagel Head and Padstow, but does not include any portion of the northern side of the Camel estuary outside of Padstow town. The road from Padstow to Winnard's Perch, through St. Columb Major to Blue Anchor, is the western boundary, and the Mitchell-Bodmin road from Blue Anchor to the north-western corner of the Fowey District completes the southern line. By far the greater portion of this district is occupied by Devonian rocks. From Padstow towards Port Isaac the lowermost of the series prevail. Upper Devonian overlie these as Camelford is neared. At Blisland Lower Silurian abut on the granite of the western side of the Bodmin Moors and narrow away to Wadebridge on one side, and to Bodmin on the other. From the Lower Devonian between Padstow and Fraddon two bosses of granite arise at Castle- an-Dinas; another outcrop is exposed at St. Columb. If for botanical purposes river-basins are to be accepted as the most satisfactory of county divisions, this district of the eight into which Cornwall has been marked off for the purpose of this paper is least open to criticism. East and west it is drained by the Camel and its tribu- taries and has no other river or stream of any consequence within its boundary.

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I liked that they had the Britons lime their hair and paint up with woad, but costuming needed to be brighter and jewelry needed to be richer. However, this seems to be a general trend among costumers in film/television; they think that ancient peoples dressed dully. In fact, most ancient peoples dressed in brilliant colors. Positively garish by our standards. They did have Boudicca & her husband dress a little better when they meet Emperor Claudius. In fact, they look like a color drawing straight out of a costume book I have. However, a king and queen of a people would be far better dressed in this.


They finally got him wheeled into surgery and onto the table. They started cutting off his clothes and he complained about losing his favourite shirt. One of the students joked that if he could complain about that, he was doing fine.

A large mass of gabbro forms the cliffs between Coverack and Manacle Point, and extends inland for about 4 miles as an ovate mass occupying an area of 6 or 7 square miles, including the districts of St. Keverne and Crousa Downs. A smaller mass mile in width extends inland from the headland of Karakclews to Gwinter. Another considerable exposure occurs on the shore near Landewednack. According to Mr. Teall the principal constituents of the Lizard gabbro are plagioclase, augite or diallage, hornblende, olivine and saussurite, while original iron ores are rare or altogether absent. The dioritic rocks that occur in this region appear as veins in the gabbro, and as part of a banded series consisting mainly of diorite and a fine grained granite. In places the two latter types vein each other, while they sometimes occur together as parallel bands. Mr. Teall describes the constituents of the dioritic rocks as felspar, biotite, green hornblende, sphene, iron ores and apatite. The granite of the Lizard peninsula occurs as veins in the serpen- tine, gabbro and dioritic rocks, and is of different character from the Cornish granite already described from beyond that region. That of the Lizard has been deformed into schist. It veins the serpentine at Kynance, a dioritic rock at Pen Voose, and occurs in a gabbro north of the last-named locality, and also veins a diorite at Kennack Cove.


It made things much easier when they wouldn’t have to worry about killing anyone on the table as long as they succeeded in getting the worm out. Honestly, for being a critical case with an unknown species, the situation was almost ideal. At least the patient was awake, cooperative, and had some knowledge of his own anatomy.

I have found "Boudica" aka "Warrior Queen" to be quite entertaining and very much worth watching. Although I had glimpsed Alex Kingston on ER, she had never really come up on my radar in a significant way. However, now that she's Boudica the Warrior Queen, I'm quite impressed with her (and maybe a little in love). In general, all of the casting was very good and the actors all made the most of their roles.


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The transition between the respec- tive rock types is sudden, and the line of demarcation appears also to be a line of dislocation. The precise relations therefore of the killas and the Lizard rocks have not been determined. The dominant rock in the Lizard peninsula is undoubtedly ser- pentine, which covers an area of about 20 square miles, while asso- ciated with it are considerable masses of gabbro and hornblende schist. Granite and greenstone (epidiorite) are of subordinate occurrence; while the extreme south of the peninsula is occupied by schists and gneisses. The serpentine extends from Lizard Town on the south to Polwin in the north. It is seen along the east coast from Coverack Cove to the bay below the village of Landewednack; and on the west coast between Pentreath Beach and George's Cove, and further north at Mullion Cove. Smaller masses occur in the vicinity of Porthalla. The variety of the Lizard serpentine constitutes one of its most striking characteristics. This is largely due to the fact that the rock is a product of alteration of pre-existing rock masses; not only did the latter differ in mineral constitution, but the extent of their decomposition, which has given rise to the serpentine, has not been uniform. While in some instances the metamorphism has been complete, in others the original rock is still represented by portions that have been undestroyed.


I've been looking at the comments on this site, and it looks like almost everyone who posted is very familiar with Boudica and very upset by what are apparently myriad inaccuracies. It makes me wonder if anyone saw this show who wasn't a history freak. So let me begin by saying I know absolutely nothing whatsoever about the real story. But from the vantage point of someone who isn't horrified by incorrect costumes and hairstyles, I thought this was an excellent movie with many striking scenes. Also, as someone who doesn't watch ER I have not pigeonholed the excellent actress Alex Kingston into whatever character she plays in the show. I am only familiar with her from her first rate performance in Moll Flanders. It's very silly to object to a performance not based on the quality of the performance but on what you're used to seeing the actress in.

Sina High School goes through about a dozen different sports attempting to find a single one in which they can score a win against their arch-rivals, the Titans. Will they stop being abject failures before their school's funding gets butchered?

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Alcor was lounging in the armchair. He'd ditched his tailored suit for a cosy, oversized and extremely fluffy sweater. His eyes were glued to the movie, black and golden and demonic.


Having glanced at a few of the other user comments, I saw some criticism of the historical accuracy of the film. Those kinds of critiques are unfounded because they are based on naive and unanalytical readings of the source material. In other words, the critic believes everything he or she reads in old books, and criticizes films if they don't match the books point for point. Good historians know that a film like "Boudica" is a valid alternative interpretation of the sources and, at the very least, an excellent heuristic tool.

Microscopic examination leaves no doubt that the coarser masses are altered gabbros, while those of finer texture were for the most part originally basalts. At Bellevue near Penryn the massive amphibolite still retains its original felspar, whereas the augite has been replaced by a mat of actinolite (horn- blende), and iron ore is in process of alteration to granular sphene. Near Ponsanooth the rock shows a little foliation, the felspar which is less abundant is mostly in a granulitized condition, and besides some magne- tite the rock contains pale brown flakes of mica, probably the direct re- sult of the contact alteration by the granite. The sill between Pengreep and Treviskey is more variable in texture; while portions are as coarse as that just described, the greater part of the rock is of fine grain. Moreover, as at Devis, the mass has undergone considerable mechanical movement, the finer, more compact zones and those of coarser crystal- line condition having been so packed and squeezed together that the coarser portions exhibit shearing. This rock strongly approaches the type of greenstone seen near St. Ives, which has been so profoundly metamorphosed by the granite of that region, and some of its structures recall the banded hornblendic rocks of the Lizard area. These greenstones may be taken as typical of this class of basic intrusion of Cornwall. While their principal constituents are felspar and hornblende considerable variation is seen in the relative proportions of those constituents. Moreover in the crushed varieties the secondary products may be so widely diffused that the original character of the rock is entirely destroyed. The intrusive greenstones however are not confined to the basic phase, but rocks of intermediate composition find their place within that group.


Finally the beds have been studied by Mr. Clement Reid, who discovered another outlier of these Pliocene deposits on the ridge north of Cannon's Town, at an elevation of 150 feet, in which the fos- siliferous clays of St. Erth are missing. Mr. Reid considers that the 13 A HISTORY OF CORNWALL fossiliferous clays were formed in a depth of water extending to 40 or 50 fathoms, an estimate confirmed by his recent discovery of the ancient shore line of the Pliocene sea at a height of about 420 feet above the present sea level. Another outlier, which has been referred by Sir Henry De la Beche to the Tertiary period, had been previously described in 1832 by Mr. John Hawkins and Dr. Boase. This deposit, which occurs at St. Agnes Beacon, and reaches, according to the latter writer, a height of 375 feet, consists of sands and clays which up to the present have not yielded determinable fossil remains. Like the St. Erth beds they exhibit rapid variation, and it is probable that they may also be the products of the Pliocene sea which Mr. Reid has shown to have exceeded even that elevation. Mr. Thomas Clark of Truro has recently found a shell frag- ment in the clay of this deposit, but too imperfect for identification. On Crousa Downs an isolated patch of gravel, consisting of rounded quartz pebbles, occupies, according to Sir H. De la Beche, an area of about half a square mile, at a height of about 360 feet above the level of the sea. The origin of this deposit is wrapped in obscurity, but its corres- pondence in elevation to the sands and gravels of St. Agnes Beacon suggests that it may also be of corresponding age. Notwithstanding the paucity of those Pliocene deposits which have survived the denudation of the subsequent ages, sufficient have remained to enable us to restore in imagination the physical features of the period to which they relate. The seas then covered large portions of the present land surface of Cornwall, and if we could restore the geography of the Pliocene period we should see an archipelago where Cornwall now stands, while the Isles of Scilly would lie beneath the waves.

Brassica Cheiranthus simply abounds at Par and Pentewan, and stretches away in scattered patches and single plants several miles from the two centres. Since it was first noticed at Pentewan more than fifty years ago as a straggler, it has seized on hedge-banks, waste-heaps, blown sand and pasture land to an astonishing extent. Between Par Sation and Fowey Point Silene Armeria occupies the hedges and sandhills at intervals over fifteen miles of country. This announcement was made thirty years and more ago, and like many another species which has immigrated to that part of the coast from the continent, the plant has settled on the soil. Two localities are known for Eryngium campestre, each having two thriving colonies of plants. Near the Looe locality (Enanthe silaifolia grows in tolerable quantity, and here only in the whole county. Twenty-four years ago Lobelia urens was accidentally discovered between Polperro and Fowey, the find bringing Cornwall into touch with Devon. To the remoteness from the track of the average plant grabber of the two damp places where it grows must be attributed the power of the plant to hold its own and even to increase its numbers. Hayle at one time shared with St. Blazey Bay the honour of being the only bits of Cornish soil where Linaria supina grew. While disappearing from the western town many years ago, it is busy extending its borders in the district now under notice.