See also:

• RHAETIC (Fr. Rhetien or Rhcetien; Ger. Rhdt or Rhktisch; It. Retico)

RHAETIC (Fr. Rhetien or Rhcetien; Ger. Rhdt or Rhktisch; It. Retico)  , in See also:

• GEOLOGY (from Gr. yp7, the earth, and Abyor, science)

geology, the assemblage of rocks classed by most See also:

• ENGLISH

English and See also:

• GERMAN
• GERMAN, DUTCH AND SCANDINAVIAN

German authorities in the Triassic See also:

• SYSTEM

system, and by most See also:

• FRENCH
• FRENCH, DANIEL CHESTER (1850– )
• FRENCH, NICHOLAS (1604-1678)

French geologists placed at the See also:

• BASE

base of the See also:

• LIAS

Lias, in the See also:

• JURASSIC

Jurassic system . It has been called the Infra-Lias . This diversity of See also:

• OPINION (Lat. opinio, from opinari, to think)

opinion is due to the fact that the See also:

• RHAETIC (Fr. Rhetien or Rhcetien; Ger. Rhdt or Rhktisch; It. Retico)

Rhaetic formation presents the characters of a See also:

• GROUP

group of passage-beds, uniting certain features of the Trias with others of the Jurassic system; none the less, it has sufficient individuality to be recognized with tolerable certainty over a wide arearin See also:

• EUROPE

Europe and beyond . The name Rhaetic was first applied by C . W . See also:

• GUMBEL, KARL WILHELM VON, BARON (1823-1898)

Gumbel to the strata of this See also:

• HORIZON (Gr. 6pfTwv, dividing)

horizon in the Rhaetic See also:

• ALPS

Alps, where they are thickly See also:

• DEVELOPED

developed and in parts fossiliferous . The labours of E . V . Mojsisovic and E . See also:

• SUESS, EDUARD (1831– )

Suess have demonstrated that in the Alpine Rhaetic several distinct facies may be recognized, viz. a Swabian facies: See also:

• SHORE

shore and See also:

• LAGOON (Fr. lagune, Lat. lacuna, a pool)

lagoon deposits with a pelecypod See also:

• FAUNA

fauna, poor in See also:

• SPECIES

species but See also:

• RICH, BARNABE (c. 1540-1617)
• RICH, CLAUDIUS JAMES (1787-1821)
• RICH, JOHN (1692-1761)
• RICH, PENELOPE, LADY (c. 1562–1607)
• RICH, RICHARD, 1ST BARON RICH (1490?-1567)

rich in individuals; a Carpathian facies with See also:

• CORALS (KoRAis), ADAMANTIOS [in French, DIAMANT CORAY] (1748–1833)

corals, See also:

• ALGAE

algae, Terebratula gregaria and Plicatula intusstriata, exemplified in the upper See also:

• PART

part of the Dachstein See also:

• LIMESTONE

limestone; a Kossener facies: See also:

• BLACK
• BLACK, ADAM (1784-1874)
• BLACK, JEREMIAH SULLIVAN (1810–1883)
• BLACK, WILLIAM (1841-1898)

black limestones and marls, with a brachiopod fauna in which Spirigera oxycolpos is very noticeable; and a See also:

• SALZBURG

Salzburg facies, characterized by pelagic pelecypods and some See also:

• AMMONITES

ammonites (see table in Massie SYSTEM) . The whole of the Rhaetic falls within Mojsisovic's See also:

• ZONE (Gr. 'WV77, a girdle, from 'wvvLvay to gird)

zone of Avicula contorta . This See also:

• EPOCH (Gr. E7roxij, holding in suspense, a pause, from E1rxav, to hold up, to stop)

epoch is marked off from the earlier Triassic See also:

• PERIOD
• PERIOD (Gr. irepioSos, a going or way round, circuit, aepi, round, and &Sis, way, road)

period by a very See also:

• GENERAL
• GENERAL (Lat. generalis, of or relating to a genus, kind or class)

general marine transgression which proceeded with See also:

• MINOR
• MINOR (Lat. for smaller, lesser)
• MINOR, ROBERT CRANNELL (1839-1904)

minor irregularities and retrogressions over the whole See also:

• AREA

area, until at its See also:

• CLOSE
• CLOSE (from Lat. clausum, shut)
• CLOSE, MAXWELL HENRY (1822-1903)

close it was followed by the more decided transgression which indicates the commencement of the Lias .

Among the marine fossils of the Rhaetic, Avicula contorta, the See also:

• PRINCIPAL

principal zone See also:

• FORM (Lat. forma)

form, is very characteristic and has a wide range; Myophoria inflata, Modiola minuta, Protocardium rhaeticum and Terebratula gregaria are See also:

• COMMON

common species . True belemonites make their first See also:

• APPEARANCE (from Lat. apparere, to appear)

appearance . Corals, Thecosmilia, &c., are common in some districts . Plant remains are abundant in certain areas, and in places give rise to beds of See also:

• LIGNITE (Lat. lignum, wood)

lignite and See also:

• COAL

coal . The See also:

• FLORA

flora is more nearly akin to that of the Trias than to that of the Jurassic rocks . Vertebrate remains are fairly abundant in the form of See also:

• TEETH (O.E. Eel); plural of tooth, O.E. top)

teeth, isolated bones, scales and See also:

• COPROLITES (from Gr. KInrpos, dung, and X10os, stone)

coprolites in what are known as " See also:

• BONE (a word common in various forms to Teutonic languages, in many of which it is confined to the shank of the leg, as in the German Bein)
• BONE, HENRY (1755-1834)

Bone Beds " (q.v.) . These beds are a very characteristic feature; they occur on several horizons in many tracts of the See also:

• EUROPEAN

European Rhaetic, and recur in beds of this See also:

• AGE (Fr. age, through late Lat. aetaticum, from aetas)

age in See also:

• AMERICA

America . In See also:

• ENGLAND
• ENGLAND, THE CHURCH OF

England there is usually a bone See also:

• BED
• BED (a common Teutonic word, cf. German Bett, probably connected with the Indo-European root bhodh, seen in the Lat. fodere, to dig; so " a dug-out place " for safe resting, or in the same sense as a garden " bed ")

bed about the base of the formation; in See also:

• GERMANY
• GERMANY (Ger. Deutschland)

Germany one occupies a similar position; a second occurs less constantly about the See also:

• MIDDLE

middle, and in the See also:

• WURTTEMBERG

Wurttemberg See also:

• DISTRICT

district a third bed separates the Rhaetic and Lias, and constitutes the well-known manure bed of Bebenhausen . In these beds are found the bones of See also:

• ICHTHYOSAURUS

Ichthyosaurus and Pliosaurus, anticipating their See also:

• GREAT

great development in the Lias, while the remains of Belodon and blystriosuchus serve to See also:

• LINK

link this epoch with Triassic stegocephalian See also:

• REPTILES (Lat. Reptilia, creeping things, from reptilis; ref ere, to creep; Gr. Ep7rety, whence the term " herpetology," for the science dealing with them)

reptiles . Several coleopterous See also:

• INSECTS

insects have been found in the same beds, but the most interesting feature of the bone-bed fauna is the first appearance in the See also:

• NORTHERN

northern hemisphere of true mammals: Microlestes in England and Wurttemberg, Triglyphus in Wurttemberg, Dromatherium and Microconodon in America . In England the Rhaetic formation occurs as a thin but See also:

• CONSTANT, BENJAMIN (1845-1902)

constant See also:

• SERIES (a Latin word from serere, to join)

series of beds at the base of the Lias and above the See also:

• KEUPER

Keuper marls . The upper part, often called the " See also:

• WHITE
• WHITE, ANDREW DICKSON (1832– )
• WHITE, GILBERT (1720–1793)
• WHITE, HENRY KIRKE (1785-1806)
• WHITE, HUGH LAWSON (1773-1840)
• WHITE, JOSEPH BLANCO (1775-1841)
• WHITE, RICHARD GRANT (1822-1885)
• WHITE, ROBERT (1645-1704)
• WHITE, SIR GEORGE STUART (1835– )
• WHITE, SIR THOMAS (1492-1567)
• WHITE, SIR WILLIAM ARTHUR (1824--1891)
• WHITE, SIR WILLIAM HENRY (1845– )
• WHITE, THOMAS (1628-1698)
• WHITE, THOMAS (c. 1550-1624)

White Lias," is a series of thin-bedded shales, limestone and marls, t to 25 ft. thick; the See also:

• LOWER

lower portion consists mainly of dark shales, sometimes with very perfect lamination— "See also:

• PAPER
• PAPER (Fr. papier, from Lat. papyrus)

paper shales." Below there are beds of See also:

• GREY, CHARLES GREY, 2ND EARL (1764-1845)
• GREY, HENRY GREY, 3RD EARL (1802-1894)
• GREY, LADY JANE (1537-1554)
• GREY, SIR EDWARD
• GREY, SIR GEORGE (1812–1898)

grey and " See also:

• TEA (Chinese cha, Amoy dialect t€)

tea-See also:

• GREEN, A
• GREEN, ALEXANDER HENRY (1832—1896)
• GREEN, DUFF (1791—1875)
• GREEN, JOHN RICHARD (1837—1883)
• GREEN, MATTHEW (1696-1737)
• GREEN, THOMAS HILL (1836-1882)
• GREEN, VALENTINE (1739–1813)
• GREEN, WILLIAM HENRY (.1825–1900)

green " marls which are now usually regarded as the topmost Keuper beds, but they have often been included in the Rhaetic formation (see KEUPER) .

The best exposures in See also:

• BRITAIN (Gr. Hperavuml vi7vot, Bperravia; Lat. Britannia, rarely Britannia)

Britain are those between See also:

• PENARTH

Penarth See also:

• HEAD (in 0. Eng. heafad; the word is common to Teutonic languages; cf. Dutch hoofd, Ger. Haupt, generally taken to be in origin connected with Lat. caput, Gr. KerbOvi7)
• HEAD, SIR EDMUND WALKER, BART
• HEAD, SIR FRANCIS BOND, BART

Head and Cavernock Point, Aust Cliff and See also:

• GARDEN (from O. Fr. garden, mod. Fr. jardin; this, like our words " garth," a paddock attached to a building, and " yard," comes from a Teutonic word for an enclosure which appears in Gothic as gards and O. H. Ger. gart, cf. Dutch gaarde and Ger. .garten)

Garden Cliff near See also:

• WESTBURY
• WESTBURY, RICHARD BETHELL, 1ST BARON (1800-1873)

Westbury-on-See also:

• SEVERN
• SEVERN, JOSEPH (1793-1879)

Severn, and Wainlode Cliff between See also:

• TEWKESBURY

Tewkesbury and See also:

• GLOUCESTER
• GLOUCESTER (abbreviated as pronounced Glo'ster)
• GLOUCESTER, EARLS AND DUKES OF
• GLOUCESTER, GILBERT DE CLARE, EARL OF (1243-1295)
• GLOUCESTER, RICHARD DE CLARE, EARL OF (1222-1262)
• GLOUCESTER, ROBERT, EARL OF (d. 1147)
• GLOUCESTER, THOMAS OF WOODSTOCK, DUKE

Gloucester . From their excellent development near Penarth the Rhaetic beds have See also:

• LONG, GEORGE (1800-1879)
• LONG, JOHN DAVIS (1838– )

long been known in England as the Penarth Beds (H . W . See also:

• BRISTOW, BENJAMIN HELM (1832-1896)
• BRISTOW, HENRY WILLIAM (1817-2889)

Bristow, 1864) . The more prominent beds in the White Lias of the See also:

• WEST
• WEST, BENJAMIN (1738-1820)
• WEST, NICHOLAS (1461-1533)

west of England and See also:

• GLAMORGANSHIRE (Welsh Morganwg)

Glamorganshire are the Estheria beds and the See also:

• INSECT

insect limestone or Pseudomonotis-bed, and on both of these horizons the limestone may assume the See also:

• PECULIAR

peculiar characters of landscape See also:

• MARBLE (from Lat. marmor, Gr. pApµapos, shining stone)

marble, sometimes called Cotham marble, from Cotham See also:

• HOUSE
• HOUSE (O. Eng. hiss, a word common to Teutonic languages, cf. Dut. huis, Ger. Haus; in Gothic it is only found in gudhiss, a temple; it may be ultimately connected with the root of " hide," conceal)

House near See also:

• BRISTOL
• BRISTOL, EARLS AND MARQUESSES OF
• BRISTOL, GEORGE DIGBY, 2ND EARL OF1 (1612-1677)
• BRISTOL, JOHN DIGBY, 1ST EARL OF 6 (1580-1653)

Bristol . A hard See also:

• FINE

fine-grained limestone, known locally as the See also:

• SUN
• SUN (0. Eng. sonne, Ger. sonne. Fr. soleil, Lat. sol, Gr. ijXior, from which comes helio- in various English compounds)

Sun-bed, occurs at the See also:

• TOP (cf. Dan. top, Ger. Topf, also meaning pot)

top of the series near See also:

• BATH
• BATH, THOMAS THYNNE
• BATH, WILLIAM

Bath and Radstock; at See also:

• STREET
• STREET, GEORGE EDMUND (1824-1881)

Street, See also:

• WEDMORE, FREDERICK (1844— )

Wedmore and See also:

• SOUTH
• SOUTH, ROBERT (1634–1716)

south of the Mendips generally it is called See also:

• JEW, THE WANDERING

Jew See also:

• STONE
• STONE (0. Eng. shin; the word is common to Teutonic languages, cf. Ger. Stein, Du. steen, Dan. and Swed. sten; the root is also seen in Gr. aria, pebble)
• STONE, CHARLES POMEROY (1824-1887)
• STONE, EDWARD JAMES (1831-1897)
• STONE, FRANK (1800-1859)
• STONE, GEORGE (1708—1764)
• STONE, LUCY [BLACKWELL] (1818-1893)
• STONE, MARCUS (184o— )
• STONE, NICHOLAS (1586-1647)

stone . Wedmore stone is a tough, shelly and sandy limestone in the black shales at Wedmore, near See also:

• WELLS
• WELLS, CHARLES JEREMIAH (1798?–1879)
• WELLS, DAVID AMES (1828—1898)
• WELLS, HERBERT GEORGE (1866— )
• WELLS, SIR THOMAS SPENCER, 1ST BART

Wells; it is employed in the neighbourhood as a See also:

• BUILDING

building stone . See also:

• NORTH
• NORTH, BARONS
• NORTH, MARIANNE (1830—1890)
• NORTH, ROGER (1653-1734)
• NORTH, SIR THOMAS (1535?-16o1?)

North of See also:

• SOMERSETSHIRE

Somersetshire the White Lias is poorly represented; in Glamorgan-See also:

• SHIRE

shire it appears between See also:

• CARDIFF

Cardiff and See also:

• PYLE, HOWARD (1853– )

Pyle, west of See also:

• BRIDGEND

Bridgend and at See also:

• SUTTON
• SUTTON, SIR RICHARD (d. c. 1524)
• SUTTON, THOMAS (c. 1532—1611)

Sutton and Southerndown . Rhaetic beds have been traced at See also:

• MARKET (Lat. mercatus, trade or place of trade)

Market See also:

• DRAYTON, MICHAEL (1563-1631)

Drayton, Salop; near Audlem, See also:

• CHESHIRE

Cheshire; See also:

• RUGBY

Rugby and See also:

• STRATFORD
• STRATFORD, JOHN DE (d. 1348)

Stratford-on-See also:

• AVON

Avon in See also:

• WARWICKSHIRE

Warwickshire; Wigston in See also:

• LEICESTERSHIRE

Leicestershire; Needham See also:

• FOREST

Forest in See also:

• STAFFORDSHIRE

Staffordshire, and in See also:

• NOTTINGHAMSHIRE, or NOTTS

Nottinghamshire and See also:

• YORKSHIRE

Yorkshire as far as the See also:

• COAST (from Lat. costa, a rib, side)

coast . They have not yet been proved beneath the Lias of See also:

• CUMBERLAND
• CUMBERLAND, DUKES AND EARLS OF
• CUMBERLAND, RICHARD (1632-1718)
• CUMBERLAND, RICHARD (1732-1811)
• CUMBERLAND, WILLIAM AUGUSTUS

Cumberland . Rhaetic fossils have been found in great See also:

• NUMBERS, BOOK OF
• NUMBERS, PARTITION OF

numbers in fissures in the Carboniferous limestone of the Mendips . On the western See also:

• SIDE
• SIDE (mod. Eski Adalia)

side of See also:

• SCOTLAND
• SCOTLAND, CHURCH OF
• SCOTLAND, EPISCOPAL CHURCH OF

Scotland Rhaetic rocks occur at Applecross, Ardnamurchan, Morven, See also:

• MULL

Mull, Raasay and See also:

• SKYE

Skye .

In See also:

• SUTHERLANDSHIRE

Sutherlandshire See also:

• SANDSTONE

sandstone and See also:

• CONGLOMERATE (from the Lat. conglomerare, to form into a ball, glomus, glomeris; so also the general term " conglomeration " for a miscellaneous collection of things, gathered together in a mass)

conglomerate and large transported masses occur; one of them, at Linksfield, carries a bone bed . Here the black shales of the English type fail; sandstones with coaly layers and yellowish-grey crystalline and oolitic limestones take their See also:

• PLACE (through Fr. from Lat. platea, street; Gr. IrAar6s, wide)

place . In See also:

• ANTRIM
• ANTRIM, RANDAL MACDONNELL, 1ST EARL OF (d. 1636)
• ANTRIM, RANDAL MACDONNELL, 1ST MARQUESS OF (1609-1683)

Antrim a small outcrop of black shales with Avicula contorta occurs near See also:

• PORT

Port See also:

• RUSH
• RUSH, BENJAMIN (1745–1813)
• RUSH, RICHARD (1780–1859)

Rush . On the European See also:

• CONTINENT (from Lat. continere, "to hold together "; hence " connected," " continuous ")

continent the Rhaetic rocks are most thickly developed in the Alpine regions; and, as in the See also:

• CASE
• CASE, JOHN (d. 1600)

case of the older Triassic formations, calcareous and dolomitic strata predominate here and in the Mediterranean See also:

• PROVINCE
• PROVINCE (Lat. provincia; perhaps a contraction of providentia)

province . In the Alpine district the See also:

• MAIN (from the Aryan root which appears in " may " and " might," and Lat. magnus, great)
• MAIN (Lat. Moenus)

main divisions are the Rhaetic Dachstein limestone and the Kossener beds; shales, marls and limestones . In the northern See also:

• TRACT (from Lat. tractare, to treat of a matter, through Provencal tractat and Ital. trattato)

tract the following subdivisions have been recognized in descending See also:

• ORDER
• ORDER (through Fr. ordre, for earlier ordene, from Lat. ordo, ordinis, rank, service, arrangement; the ultimate source is generally taken to be the root seen in Lat. oriri, rise, arise, begin; cf. " origin ")
• ORDER, HOLY

order: beds with Choristeceros Marschi; Starhem passage beds; Rhynchonella fissicostata beds; Lithodendron limestone; beds with Terebratula gregaria; beds with Avicula contorta; " Platten See also:

• KALK

Kalk with Rhynchonella alpina . In the See also:

• SOUTHERN

southern tract the subdivisions are: Conchodus See also:

• DOLOMITE

dolomite (Conchodus infraliassicus=Lycodius See also:

• COR

cor.); Lithodendron limestone, Azzarola beds, Contorta marls, Plattenkalk." Much limestone is of the " See also:

• REEF (1)

reef " type . In Germany the rocks are mainly fine, clean yellow sands, suggesting littoral or dune conditions, with bituminous See also:

• CLAYS, PAUL JEAN (1819-1900)

clays and marls . The formation is often missing in south-west Germany . Similar beds occur in See also:

• LORRAINE

Lorraine and Luxembourg (gres de Vic, gres de Kedange, gres de Mortinsart) . In Cotentin are dolomitic sandstones and See also:

• MARL (from O. Fr. marle, Late Lat. margila, dim. of marga; cf. Du. and Ger. Mergel)

marl; See also:

• ROUND (O. Fr. rond, Lat. rotundus, the Fr. is the source also of Du. rond; Ger., Swed., Dan. and Nor. rond)

round the central See also:

• PLATEAU (a French term, older platel, for a flat piece of wood, metal, &c., from plat, flat)
• PLATEAU, JOSEPH ANTOINE FERDINAND (1801-1883)

plateau of See also:

• FRANCE
• FRANCE, ANATOLE (1844– )

France the rocks are coarse sands, arkoses, and conglomerates; while in the south of France the sandy and calcareous facies occur intermixed . In See also:

• SPAIN
• SPAIN (Espana)

Spain limestones and See also:

• DOLOMITES, THE

dolomites occur up to too metres in thickness; in See also:

• PORTUGAL

Portugal sandy beds recur .

The Rhaetic of Scania, south See also:

• SWEDEN
• SWEDEN [Sverige]
• SWEDEN, NORWAY AND

Sweden, consists mainly of sandstone and shales with beds of coal up to one See also:

• METRE ((terpuc?, sc. rFxvf, from Gr. Or poi', measure)

metre thick . Only the upper beds contain marine fossils; the bulk of the formation is of lacustrine or estuarine origin, with plant remains and insects . In See also:

• ITALY
• ITALY (Italia)

Italy the formation is well developed in the north and at Rotzo, Spezzia and See also:

• CARRARA
• CARRARA, or CARRARESI

Carrara; and yields the famous statuary marble and the black variety known as portor . Rhaetic beds have been re-cognized in See also:

• SARDINIA (Gr. 'IXs'o"uva, from a fancied resemblance to a footprint in its shape, Ital. Sardegna)

Sardinia, See also:

• CORSICA (Fr. Corse)

Corsica, See also:

• SICILY (Ital. Sicilia)

Sicily, in the See also:

• BALKAN

Balkan See also:

• PENINSULA
• PENINSULA (Lat. paeninsula, from paene, almost, and insula, an island)

Peninsula and See also:

• GREECE

Greece; in See also:

• ASIA

Asia Minor, See also:

• AFGHANISTAN

Afghanistan, Turkistan, See also:

• PERSIA

Persia, See also:

• SIBERIA

Siberia and See also:

• INDIA
• INDIA, FRENCH

India (limestones and dolomites of Niti and the Mahaveda beds, sandstones and conglomerates, nearly 10,000 feet thick in See also:

• SATPURA

Satpura) ; in See also:

• CHINA

China, See also:

• JAPAN

Japan and See also:

• TONGKING

Tongking (with coal beds) . In See also:

• AUSTRALASIA

Australasia the Wianamatta beds of New South See also:

• WALES (Cymru, Gwalia, Cambria)

Wales, the Bellarine beds of See also:

• VICTORIA
• VICTORIA (or VITTORIA), TOMMASSO LUDOVICO DA (C. I540-C. 1613)
• VICTORIA [ALEXANDRINA VICTORIA]

Victoria, the See also:

• IPSWICH

Ipswich and See also:

• TIVOLI (anc. Tibur, q.v.)

Tivoli beds of See also:

• QUEENSLAND

Queensland, and the See also:

• JERUSALEM (Heb. ^S0-r, Yerushalaim, pronounced as a dual)
• JERUSALEM, SYNOD OF (1672)

Jerusalem beds of See also:

• TASMANIA

Tasmania, and beds on a similar horizon in New See also:

• ZEALAND (also SEALAND Or SEELAND; Danish Sjaelland)

Zealand, have been regarded as equivalents of the Rhaetic . In See also:

• AFRICA
• AFRICA, ROMAN

Africa the Stormberg beds of the Karoo series and. thg Molten beds of the Cape have been assigned to this epoch . In America Rhaetic rocks are recognized in N . Carolina, See also:

• CONNECTICUT

Connecticut, See also:

• CALIFORNIA
• CALIFORNIA, LOWER (Baja California)
• CALIFORNIA, UNIVERSITY OF

California, See also:

• MEXICO
• MEXICO (Span. Mejico, or Mexico,)
• MEXICO, FEDERAL DISTRICT OF
• MEXICO, GULF OF

Mexico, See also:

• BOLIVIA

Bolivia and See also:

• CHILE, or CHILI (derived, it is said, from the Quichua chin , cold, or tchili, snow)

Chile; the formation is also recorded from Spitzbergen, See also:

• FRANZ, ROBERT (1815-1892)

Franz See also:

• JOSEPH
• JOSEPH, COMTE DE (1785-1870)
• JOSEPH, FATHER (FRANCOIS LECLERC DU TREMBLAY) (1577-1638)

Joseph See also:

• LAND

Land and elsewhere in the See also:

• ARCTIC (Gr. "ApKroc, the Bear, the northern constellation of Ursa Major)

Arctic regions . For the English Rhaetic see L . See also:

• RICHARDSON, GEORGE
• RICHARDSON, HENRY HOBSON (1838-1886)
• RICHARDSON, SAMUEL (1689-1761)
• RICHARDSON, SIR JOHN (1787-1865)

Richardson, " The Rhaetic Rocks of North-west See also:

• GLOUCESTERSHIRE

Gloucestershire," Proc . Cotteswold See also:

• CLUB (connected with " clump ")

Club, xiv. p . 127 (Glos .

1901-1903) . (J . A .