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695:. Porphyritic andesite is dark grey with white crystals of plagioclase feldspar embedded. Outcrops occur on the coast at Giffards Bay on the north coast and Vicard Point on the east coast. The volcanoes were to the north east and south. Vicard Tuff contains bombs. The Long Echet Tuff contains large crystals of quartz and feldspar and strands of quartz. Les Rouaux Agglomerate and L' Homme Mort Agglomerate contain fragments of the surrounding rocks including shale and andesite embedded in a feldspar matrix. The Les Rouaux Agglomerate also contains
749:. In this orogeny the rocks were first crushed and folded with East West pressure, then later they were compressed in the north south direction. Gabbro is found at Sorel Point. This rock can be observed to transition into diorite by changes in the mineral content and texture. Layered gabbro has also been changed into diorite at Le Nez point, the southernmost point of the main island. The diorite is emplaced at and near Sorel point, and at several places along the south coast east of
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consist of andesite, rhyolite, granite and shale. The pebbles range from 1 cm to 60 cm, and are quite irregular. The conglomerate bed is above a bed of red sandstone and mudstone which has pits, probably being rain drop marks, and also has polygonal shaped cracks. Apart from the main outcrop, the conglomerate is also found in smaller areas at Les Hurets Valley, west of the Bouley Bay and at La Pierre de FĂ©telle. The conglomerate is estimated to be
Ordovician in age.
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lakes and streams. The Les
Platons Rhyolite contains spherulites. Spherulites are also found at Les Hurets on Bouley Bay. At Bouley Bay there are three units of ignimbrite: the Lower Bouley Ignimbrite, Middle Bouley Ignimbrite and Upper Bouley Ignimbrite. These contain flow banding and spherulites up to 10 cm and eutaxitic and
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which have themselves been eroded to form cliffs from 3 to 12 metres high. At
Belcroute there is a more complex deposit of loess head on a raised beach deposit elevated at 8 metres, that sits on another loess deposit. Head occurs at the foot of cliffs along the north, north east and south west sides,
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The high surface has been eaten into by cliffs dropping down to 8 metres. These have been formed during the
Quaternary when the sea level was around 8 metres above the current sea level. There are also raised beaches at 18 and 30 metres above current sea level. During the glacial periods valleys were
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Le Havre de Fer Beach has an outcrop of columnar rhyolite that has been separated by faulting from the rest of the units. North of
Archirondel Round Tower there are three more flows stacked on top of each other called Archirondel Ignimbrite, Dolmen Ignimbrite and St. Catherine's Ignimbrite. These are
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in the east coast, and La Belle Hougue Point, and Le Mont Mado granite has an occurrence. The shale is more easily eroded, and this has affected the shape of the island by the concave St Ouens's Bay and St Aubin's Bay. The deepest valleys (Valley of St. Peter and St. Lawrence) are cut into this soft
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The land here was uplifted and eroded in the
Cambrian. A coarse conglomerate known as Rozel Conglomerate was washed in by a flash flood flowing from somewhere to the north of the island during the Cambrian to Ordovician time period. This conglomerate is on the north east cape at Rozel. The pebbles
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Ground water is found in rock fractures and to a limited extend in porous rocks, in the upper 40 meters. Ground water is irregular, with some perched aquifers and vertical screens preventing underground flow. The water underground is young (as determined by isotope analysis), replenished from the
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Fine grained rhyolite of Bouley
Rhyolite Formation occurs even further to the north east. This is 430 metres thick. At Giffard Bay are Gifford Rhyolite, Gifford Andesite, Gifford Ignimbrite and Gifford Tuffs. Les Platons Rhyolite top this off. These rocks contain xenoliths and tuff deposits from
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of St. John's
Rhyolite Formation is found to the north east of the centre. It contains banded flows and ignimbrite. Totally it is 950 meters thick. It contains shards of glass and pumice. Different flows exits with sections called Bonne Nuit Ignimbrite followed by Frémont Ignimbrite on the north
636:, termed Association I from the upper parts of the fan, is found in lenticular bodies near St Peter's Valley, at Gargate Mill. The pebbles in the conglomerate are of multiple kinds of rock. The granite intrusions at the boundary of the formation have caused metamorphism and intrusion by dykes.
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There is a known acid dyke of rhyolitic composition on the east side of
Noirmont headland. This is 1 metre wide and coloured light grey to pink. It has an east–west strike. Porhyritic microgranite dykes occur below Le Saut Jeffroi, and south of Le Mont Orgueil. These have a NNE strike.
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Granite quarrying still occurs in three quarries in the north west at Ronez, Gigoulande (by
Granite Products company) and La Saline. The La Saline company produces decorative stone for building. The other two quarries produce aggregate for roads and concrete and a product called
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zone, where the Celtic oceanic plate was converging and descending in the trench. The sediments were carried by rivers from the Le Vast Arc, a strip of land oriented east north east, that lay to the south of Jersey. The sea at this time was termed l' Océan de la Manche.
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with four intrusions. The magma came from a volcanic arc. One of these intrusions contained the gabbro and diorite. The granites are coloured grey-pink and orange, with the gabbro a dark grey, and the diorite speckled grey. The main intrusion is the St. Mary's Granite
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The tidal range is high at 13 meters, exposing a wide rock platform around Jersey. Western Jersey sedimentary rocks are underlain by shallow granite, and in eastern Jersey there is a high in the gravity field near Grande Charriere, which could be due to gabbro.
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primigenius bones have been found at La Cotte de St. Brelade along with deer bones. Mollusk shells are found in the Loess and beach deposits. A submerged forest in St. Ouën's Bay between L'Ouzière slipway and Le Port Slipway has stumps of Birch and Alder
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The Jersey Main Dyke Swarm consists of dolerite dykes intruded into the South East Igneous complex. Some dolerite dykes have a porphyry centre. The strike is north-west, and the direction is vertical. Augite and labradorite are found in these dolerites.
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The south west granites are 550 – 480 mya, and has three intrusions. The intrusions are called Corbière Granite, La Moye Granite, and Beau Port Granite. They are coloured pale to deep red. The north west area was intruded
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The Brioverian rocks were formed between 900 and 700 mya. They were named after Briovère, the native name for St. Lô, in Normandy, which is the first area these rocks were described from. They start with
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There are several sea caves. A notable cave is the Le Creux du Vis. This cave has a tunnel going in from the beach at the base of the cliff, and a crater shaped opening with steep rocky sides above.
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coast. They contain xenoliths of the andesite and shale found in Jersey. Also there are local mudstone and conglomerate deposited on the flows. The conglomerate is called L'Homme Mort Conglomerate.
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and can also be found beneath wind blown sand at the bays of St. Ouen, St. Aubin, St. Clement and the Royal Bay of Grouville. The thickest parts of loess are five metres deep at St Clements and at
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At Le Pulec there is a small deposit of lead and zinc that was mined in the late 19th century, but the venture was unsuccessful. There are also some other small unmined mineral veins, such as
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periods. The kind of rocks go from conglomerate to shale, volcanic, intrusive and plutonic igneous rocks of many compositions, and metamorphic rocks as well, thus including most major types.
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with four intrusions. One of these intrusions contained the gabbro and diorite. These granites are coloured grey-pink and orange, with the gabbro a dark grey, and the diorite speckled grey.
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These sediments were uplifted and are overlaid by volcanic rocks of the Jersey Volcanic Group around 530 Mya. The magma came from the subduction zones below and to the north of the island.
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Earth tremors occur more commonly near Jersey that other areas in the Channel Islands, with magnitudes up to 3. The epicentres are mostly on the sea floor to the west, south and east.
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The Jeffrey's Leap Ignimbrite is overlaid by the Anne Port Ignimbrite named after locations on the east coast. The Trinity Ignimbrite is a purple tuff near Les Grands Vaux, inland.
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left a smaller print on the island, with the intrusion of some dykes, and some folding and jointing that affected the island's rocks including the Rozel Conglomerate. During the
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veins in the igneous complexes up to 5 cm wide. The aplite is the lowest melting remanent of the granite magma, that is poor in volatiles. The aplite minerals include
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lamprophyre (spessarites) contain plagioclase, coloured light brown and are oriented north–south. A hornblende lamprophyre dyke in the Rozel Conglomerate is dated at
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from St. Saviour's Andesite Formation is in the centre and in the north at Les Rouaux. It is coloured grey and includes some basalt and pyroclastic fallout such as
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630:, 2% dark iron containing minerals, with carbon flakes, in a matrix of 10 to 20% clay. The minerals contained are very diverse indicating a broad source area.
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786:. At St Brelade's Bay there are two aplogranites: Beau Port Granite and La Moye Granite. This is coloured yellow brown to pink and contains fine crystals of
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is termed Association IV along with the shale. It is found in the same areas as the shale. In an analysis of the greywacke it has fragments with 70%
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lamprophyres (minettes) are oriented in the north west direction. They are coloured brown, and are up to 1 metre wide. They contain orthoclase.
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Granite intrudes into the north west, south west and south east. The south west granite also includes porphyries and some fine grained sections.
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718:. The Anne Port Rhyolite is the bottom unit on the east coast. This is massive but columnar jointed. It shows flow banding. It resembles the
593:
1097:. There are many other disused or abandoned quarries that have been used for stone to make the buildings, castles, and piers on the island.
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651:. At St. Ouën's Bay the metamorphosis of greywacke has made hornblende-hornfels. Regional metamorphism has converted the shale to a low
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1066:. These are found at La Hougue Bie in St. Saviour and Le Mont Ubé dolmen, St. Clément and La Pouquelaye de Faldouet and Le Couperon.
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was deposited, blown in by wind from the west. The loess has formed thick deposits on the island interior and combined with
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The island was only separated from the continent of Europe by rising sea levels about 5000 BC during the new Stone Age.
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eroded deeply below the sea level These raised beaches are found at Portelet Bay, Giffard Bay, and Belcroute Bay.
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La Société Jersiaise has a geology section that studies, presents talks, and tours of the Geology of the island.
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quarries used to be in what is now Handois reservoirs. Bricks have also been made from clay from St. Saviour. La
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The plutonic rocks are not foliated, showing that the orogeny was near completion at the time they formed.
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During the Eocene limestone was deposited in the sea around Jersey, but none is actually on the island.
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The south east granites moved into the south east about the same time. The components here are called
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Sand mining takes place at St. Ouen's Bay in the west by Simon's Sand and Gravel, and formerly at
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sp) from 1980 BC. Legends record that the sea encroached on the forest in the fifteenth century.
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in St. Peter's Valley there is peat dated to 7600 BC which contains pollen from boreal forest.
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During the Tertiary the surface of the island was a plain at 60 to 130 metres above sea level.
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832:. One other intrusion was an aplogranite called Mont Mado granite, or Red Granite solidified
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The only fossils date from the Quaternary, and are found in raised beaches, peat and clay.
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by Eldridge M. Moores, Rhodes Whitmore Fairbridge, Published 1997 by Springer pp 276–277.
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730:. They consist of pumice, quartz crystals and feldspar in a feldspar rich matrix.
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608:. The shale layers have been identified as Association IV in the submarine fan.
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is found amongst the pebbles on these beaches, and this is derived from
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separated from each other by layers of tuff, and are coloured maroon by
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surface from local rain, and not by underground streams from Normandy.
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The interpretation of this area is that is a part of the north facing
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Granophyre, Dicq Granite, Longueville Granite, and La Roque Granite.
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is characterised by the Late Proterozoic Brioverian volcanics, the
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Geological excursion guide 1: Jersey and Guernsey, Channel Islands
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Geological Magazine; March 1959; volume 96; number 2; page 89-98
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rock shelter which was inhabited 200000 years ago by hunters of
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frost shattered rock fragments sliding down the cliffs to form
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In the L'ĂŠtacq area, the metamorphism has produced spotted
753:. It also is found on the south east tidal rock platform.
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The sandstone is Association III of the submarine fan.
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Evolution of the Island Character – Geological History
699:. This was eroded before the next phase of volcanism.
563:
in the west, centre and south of Jersey, including at
896:. The dykes included a swarm of dolerite dykes, also
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with a grey colour. The spots are darker, containing
584:
rock. Other sediments associated with the shale are
1197:
Encyclopedia of European and Asian Regional Geology
575:. This constitutes the Jersey Shale Formation. The
165:
59:. Unsourced material may be challenged and removed.
150:, and only small signs of later deposits from the
802:. Other parts more rich in volatiles have formed
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940:In the north-west there are sills of dolerite.
877:Sinistral tear faults have affected the rock.
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911:The aplite dykes are one to two metres wide.
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1262:
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1355:Channel Islands Occupation Society (CIOS)
892:, Jersey was part the north-west edge of
592:. Various sedimentary structures include
119:Learn how and when to remove this message
2149:
1178:Gravity anomalies in the Channel Islands
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130:
678:
551:Axis scale is in millions of years ago.
161:
14:
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1743:List of members of the States Assembly
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979:and rhinoceros amongst other animals.
596:and bounce castes, ripple lamination,
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1300:German occupation during World War II
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863:
1852:Jersey Financial Services Commission
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57:adding citations to reliable sources
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543:An approximate time-scale of events
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738:Intrusions were formed during the
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817:The north west area was intruded
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968:deposits only found underwater.
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1686:Customs and Immigration Service
1009:Peat occurs in the valleys. At
44:needs additional citations for
1193:Great Britain: Channel Islands
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545:in the Geological history of
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1:
3307:European Cenozoic Rift System
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971:La Cotte de St Brelade has a
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655:, where clay is converted to
1235:Jersey geology photo gallery
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770:There are also pink and red
7:
3497:UNESCO World Heritage Sites
1076:is making a brick archive.
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1847:Jersey Electricity Company
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170:Jersey Geological Timeline
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2186:de Haut du Mont au PrĂŞtre
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1533:Highlands College, Jersey
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1164:www.societe-jersiaise.org
468:Granite in the south west
450:Granite in the north west
3415:Jan Mayen Microcontinent
2546:de la Petite Longueville
2541:de la Grande Longueville
2181:de Bas du Mont au PrĂŞtre
1728:Procureur du Bien Public
1559:St Michael's Preparatory
1513:Jersey College for Girls
1129:
1112:
1088:Ronez Quarry, Saint John
1058:Rocks have been used in
1006:on the eastern plateau.
516:Brioverian Sedimentation
178:−1000 —
175:
3357:Peri-Caspian Depression
3086:Hallandian-Danopolonian
2465:Cueillette de Vinchelez
1549:Beaulieu Convent School
1100:
931: million years ago
844: million years ago
837: million years ago
830: million years ago
268:−100 —
258:−200 —
248:−300 —
238:−400 —
228:−500 —
218:−600 —
208:−700 —
198:−800 —
188:−900 —
3199:Scandinavian Mountains
2717:Bosnia and Herzegovina
2569:de la Ville-à -l'Évêque
2470:Cueillette de LĂ©oville
2083:ITV Channel Television
1608:Places in the islands
1450:Jersey Eastern Railway
1440:La Corbière Lighthouse
1398:La Cotte de St Brelade
1372:Coastal fortifications
1210:volume 1 number 3 1985
1089:
914:There are two sets of
136:
3367:White Sea Rift System
2460:Cueillette de Millais
2455:Cueillette de Grantez
1988:Durrell Wildlife Park
1087:
904:porphyry and aplite.
418:Jersey Volcanic group
134:
3473:Fennoscandian Craton
3468:East European Craton
2356:du Coin Tourgis Nord
1681:Council of Ministers
1671:Government of Jersey
1215:Jersey Geology Trail
820:465 to 426
763:465 to 426
745:700 to 500
679:Brioverian volcanics
162:Brioverian sediments
53:improve this article
18:Brioverian volcanics
3362:Timan-Pechora Basin
3297:Dnieper–Donets Rift
3214:Western Carpathians
2399:du Fief de la Reine
2361:du Coin Tourgis Sud
2089:Jersey Evening Post
2023:Jersey Royal potato
2008:Jèrriais literature
1892:Visite du Branchage
1790:Jersey Legal French
1708:Lieutenant Governor
1554:De La Salle College
722:at La CrĂŞte Point.
588:, and fine grained
532:Sturtian glaciation
68:"Geology of Jersey"
3515:Calanques de Piana
3269:basins and grabens
1904:Telecommunications
1842:Financial services
1703:External relations
1345:Battery Lothringen
1340:War Tunnels Museum
1330:SechsschartentĂĽrme
1219:States of Jersey
1213:Dr Ralph Nichols:
1090:
864:Rozel Conglomerate
653:greenschist facies
137:
3671:Geology of Jersey
3658:
3657:
3595:Monte San Giorgio
3491:
3490:
3448:Armorican terrane
3252:Mediterranean Sea
2666:Geology of Europe
2632:
2631:
2597:
2596:
2531:de Sous la Hougue
2450:Grande Cueillette
2445:Petite Cueillette
2176:du Rouge Bouillon
2140:
2139:
2098:
2097:
2003:Jèrriais language
1973:Battle of Flowers
1951:
1950:
1876:(former currency)
1824:
1823:
1820:
1819:
1785:HM Prison La Moye
1718:Political parties
1632:
1631:
1571:
1570:
1567:
1566:
1468:
1467:
1176:Alan Arthur Day:
1074:Société Jersiaise
822:million years ago
765:million years ago
747:million years ago
664:continental slope
556:
555:
537:
536:
521:
520:
505:
504:
489:
488:
473:
472:
457:
456:
439:
438:
423:
422:
135:Geology of Jersey
129:
128:
121:
103:
16:(Redirected from
3678:
3555:Jungfrau-Aletsch
3540:Giant's Causeway
3478:Sarmatian Craton
3395:Aegean Sea Plate
3292:Central Lowlands
3287:Baltic Sea Basin
3267:Intracontinental
3029:
3028:
3024:Geologic regions
3017:
2968:Northern Ireland
2659:
2652:
2645:
2636:
2635:
2617:
2610:
2551:de Sous l'Église
2285:Grande Vingtaine
2191:du Mont à l'Abbé
2146:
2145:
2116:Beautiful Jersey
2073:BBC Radio Jersey
1966:
1965:
1962:
1961:
1914:Newtel Solutions
1909:JT Group Limited
1877:
1835:
1834:
1693:Duke of Normandy
1647:
1646:
1643:
1642:
1582:
1581:
1528:Victoria College
1488:
1487:
1479:
1478:
1435:Battle of Jersey
1425:Elizabeth Castle
1285:
1284:
1264:
1257:
1250:
1241:
1240:
1181:
1174:
1168:
1167:
1156:
1039:Economic geology
932:
882:Variscan Orogeny
873:Variscan Orogeny
855:Elizabeth Castle
845:
838:
831:
823:
766:
748:
740:Cadomian Orogeny
734:Cadomian Orogeny
528:
523:
512:
507:
500:Cadomian Orogeny
496:
491:
484:Variscan Orogeny
480:
475:
464:
459:
446:
441:
430:
425:
414:
409:
279:
274:
269:
264:
259:
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234:
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194:
189:
184:
179:
166:
148:Cadomian Orogeny
124:
117:
113:
110:
104:
102:
61:
37:
29:
21:
3686:
3685:
3681:
3680:
3679:
3677:
3676:
3675:
3661:
3660:
3659:
3654:
3505:Aeolian Islands
3487:
3434:
3400:Anatolian Plate
3382:microcontinents
3380:
3377:Tectonic plates
3371:
3347:Pannonian Basin
3337:North Sea Basin
3312:Hellenic Trench
3277:Aquitaine Basin
3268:
3261:
3218:
3151:Mountain ranges
3145:
3018:
3009:
2871:North Macedonia
2668:
2663:
2633:
2628:
2620:
2613:
2606:
2593:
2589:de la Croiserie
2555:
2512:
2498:Grand Vingtaine
2474:
2431:
2408:
2365:
2327:
2299:
2271:
2238:
2200:
2157:
2136:
2094:
2059:
1978:Catholic Church
1947:
1924:Airtel-Vodafone
1875:
1816:
1754:
1738:States Assembly
1713:Parish Assembly
1628:
1563:
1537:
1464:
1455:Jersey Heritage
1386:
1274:
1268:
1231:
1189:
1184:
1175:
1171:
1158:
1157:
1153:
1149:
1140:
1132:
1124:
1115:
1103:
1082:
1062:times to build
1041:
957:
946:
927:
875:
866:
840:
833:
826:
818:
761:
743:
736:
720:Giants Causeway
716:fiamme textures
681:
552:
550:
544:
533:
526:
517:
510:
501:
494:
485:
478:
469:
462:
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428:
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405:
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366:
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296:
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125:
114:
108:
105:
62:
60:
50:
38:
23:
22:
15:
12:
11:
5:
3684:
3674:
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3656:
3655:
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3637:
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3612:
3607:
3602:
3597:
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3577:
3572:
3567:
3562:
3560:Jurassic Coast
3557:
3552:
3547:
3542:
3537:
3535:Geirangerfjord
3532:
3527:
3522:
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3507:
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3432:
3427:
3422:
3417:
3412:
3407:
3405:Eurasian Plate
3402:
3397:
3392:
3390:Adriatic Plate
3386:
3384:
3373:
3372:
3370:
3369:
3364:
3359:
3354:
3349:
3344:
3339:
3334:
3329:
3324:
3319:
3317:Limagne Graben
3314:
3309:
3304:
3299:
3294:
3289:
3284:
3279:
3273:
3271:
3263:
3262:
3260:
3259:
3254:
3249:
3244:
3239:
3234:
3232:Atlantic Ocean
3228:
3226:
3224:Oceanic basins
3220:
3219:
3217:
3216:
3211:
3206:
3201:
3196:
3191:
3186:
3184:Massif Central
3181:
3176:
3171:
3166:
3161:
3155:
3153:
3147:
3146:
3144:
3143:
3138:
3133:
3131:Sveconorwegian
3128:
3123:
3118:
3113:
3108:
3103:
3098:
3093:
3088:
3083:
3078:
3073:
3068:
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2985:
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2965:
2958:United Kingdom
2955:
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2935:
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2925:
2920:
2915:
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2900:
2895:
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2783:
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2756:
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2749:
2739:
2737:Czech Republic
2734:
2729:
2724:
2719:
2714:
2709:
2704:
2699:
2694:
2689:
2684:
2678:
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2599:
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2511:
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2505:
2500:
2495:
2493:de St. Nicolas
2490:
2484:
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2476:
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2467:
2462:
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2366:
2364:
2363:
2358:
2353:
2351:du Coin Motier
2348:
2346:du Coin Hâtain
2343:
2337:
2335:
2333:Saint Lawrence
2329:
2328:
2326:
2325:
2320:
2315:
2309:
2307:
2301:
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2298:
2297:
2292:
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2269:
2264:
2262:des Quennevais
2259:
2254:
2248:
2246:
2240:
2239:
2237:
2236:
2231:
2226:
2224:de Longueville
2221:
2216:
2210:
2208:
2202:
2201:
2199:
2198:
2196:du Mont Cochon
2193:
2188:
2183:
2178:
2173:
2167:
2165:
2159:
2158:
2142:
2141:
2138:
2137:
2135:
2134:
2132:Liberation Day
2129:
2124:
2119:
2108:
2106:
2100:
2099:
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2095:
2093:
2092:
2085:
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2061:
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2052:
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2040:
2035:
2025:
2020:
2015:
2010:
2005:
2000:
1995:
1990:
1985:
1980:
1975:
1969:
1959:
1953:
1952:
1949:
1948:
1946:
1945:
1944:
1943:
1933:
1928:
1927:
1926:
1921:
1916:
1911:
1901:
1896:
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1710:
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1695:
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1683:
1678:
1676:Chief Minister
1668:
1663:
1662:
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1650:
1640:
1634:
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1535:
1530:
1525:
1523:Les Quennevais
1520:
1515:
1510:
1505:
1500:
1494:
1492:
1485:
1476:
1470:
1469:
1466:
1465:
1463:
1462:
1460:National Trust
1457:
1452:
1447:
1445:Jersey Railway
1442:
1437:
1432:
1427:
1422:
1420:Grosnez Castle
1417:
1412:
1411:
1410:
1400:
1394:
1392:
1388:
1387:
1385:
1384:
1379:
1374:
1369:
1364:
1359:
1358:
1357:
1352:
1350:Battery Moltke
1347:
1342:
1337:
1335:German tunnels
1332:
1327:
1322:
1317:
1312:
1307:
1297:
1291:
1289:
1282:
1276:
1275:
1273: articles
1267:
1266:
1259:
1252:
1244:
1238:
1237:
1230:
1229:External links
1227:
1226:
1225:
1217:
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1169:
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1131:
1128:
1123:
1120:
1114:
1111:
1102:
1099:
1081:
1078:
1040:
1037:
977:woolly mammoth
956:
953:
945:
942:
874:
871:
865:
862:
798:, coloured by
735:
732:
680:
677:
598:graded bedding
569:St Aubin's Bay
554:
553:
539:
538:
535:
534:
531:
529:
519:
518:
515:
513:
503:
502:
499:
497:
487:
486:
483:
481:
471:
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467:
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455:
454:
452:and north west
449:
447:
437:
436:
434:end of ice age
433:
431:
421:
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406:
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401:
397:
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3:
2:
3683:
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3643:
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3628:
3626:
3623:
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3618:
3616:
3613:
3611:
3608:
3606:
3603:
3601:
3598:
3596:
3593:
3591:
3590:Monte Perdido
3588:
3586:
3583:
3581:
3578:
3576:
3573:
3571:
3568:
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3563:
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3533:
3531:
3528:
3526:
3523:
3521:
3520:Curonian Spit
3518:
3516:
3513:
3511:
3508:
3506:
3503:
3502:
3500:
3498:
3494:
3484:
3481:
3479:
3476:
3474:
3471:
3469:
3466:
3464:
3461:
3459:
3456:
3454:
3451:
3449:
3446:
3445:
3443:
3441:
3437:
3431:
3428:
3426:
3423:
3421:
3420:Moesian Plate
3418:
3416:
3413:
3411:
3410:Iberian Plate
3408:
3406:
3403:
3401:
3398:
3396:
3393:
3391:
3388:
3387:
3385:
3383:
3378:
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3353:
3350:
3348:
3345:
3343:
3340:
3338:
3335:
3333:
3330:
3328:
3327:Molasse Basin
3325:
3323:
3320:
3318:
3315:
3313:
3310:
3308:
3305:
3303:
3300:
3298:
3295:
3293:
3290:
3288:
3285:
3283:
3282:Barents Basin
3280:
3278:
3275:
3274:
3272:
3270:
3264:
3258:
3257:Norwegian Sea
3255:
3253:
3250:
3248:
3245:
3243:
3242:Bay of Biscay
3240:
3238:
3235:
3233:
3230:
3229:
3227:
3225:
3221:
3215:
3212:
3210:
3207:
3205:
3202:
3200:
3197:
3195:
3192:
3190:
3189:Ore Mountains
3187:
3185:
3182:
3180:
3177:
3175:
3172:
3170:
3167:
3165:
3162:
3160:
3157:
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3139:
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3129:
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3119:
3117:
3114:
3112:
3109:
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3102:
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3084:
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3034:
3030:
3027:
3025:
3021:
3016:
3004:
3001:
2999:
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2991:
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2859:
2857:
2854:
2852:
2849:
2847:
2844:
2842:
2839:
2837:
2834:
2832:
2831:Liechtenstein
2829:
2827:
2824:
2822:
2819:
2817:
2814:
2811:
2807:
2804:
2802:
2799:
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2779:
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2769:
2765:
2764:Ă…land Islands
2762:
2761:
2760:
2757:
2755:
2752:
2748:
2747:Faroe Islands
2745:
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2730:
2728:
2725:
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2720:
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2621:
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2609:
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2600:
2590:
2587:
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2577:
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2542:
2539:
2537:
2534:
2532:
2529:
2527:
2524:
2523:
2521:
2519:
2518:Saint Saviour
2515:
2509:
2508:du Coin Varin
2506:
2504:
2501:
2499:
2496:
2494:
2491:
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2400:
2397:
2395:
2392:
2390:
2389:de la Quéruée
2387:
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2377:
2376:
2374:
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2362:
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2308:
2306:
2302:
2296:
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2286:
2283:
2282:
2280:
2278:
2277:Saint Clement
2274:
2268:
2265:
2263:
2260:
2258:
2255:
2253:
2250:
2249:
2247:
2245:
2241:
2235:
2234:Les Minquiers
2232:
2230:
2227:
2225:
2222:
2220:
2217:
2215:
2212:
2211:
2209:
2207:
2203:
2197:
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2189:
2187:
2184:
2182:
2179:
2177:
2174:
2172:
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2168:
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2160:
2156:
2152:
2147:
2143:
2133:
2130:
2128:
2125:
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2120:
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2113:
2110:
2109:
2107:
2105:
2101:
2091:
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2068:
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2062:
2056:
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2046:
2043:
2039:
2036:
2034:
2031:
2030:
2029:
2026:
2024:
2021:
2019:
2018:Jersey people
2016:
2014:
2011:
2009:
2006:
2004:
2001:
1999:
1996:
1994:
1991:
1989:
1986:
1984:
1981:
1979:
1976:
1974:
1971:
1970:
1967:
1963:
1960:
1958:
1954:
1942:
1939:
1938:
1937:
1934:
1932:
1929:
1925:
1922:
1920:
1917:
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1910:
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1905:
1902:
1900:
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1872:
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1865:
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1860:
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1798:
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1788:
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1776:
1773:
1769:
1766:
1765:
1763:
1761:
1757:
1751:
1748:
1744:
1741:
1740:
1739:
1736:
1734:
1733:Royal Militia
1731:
1729:
1726:
1724:
1721:
1719:
1716:
1714:
1711:
1709:
1706:
1704:
1701:
1699:
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1679:
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1623:
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1610:
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1600:
1597:
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1587:
1586:
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1580:
1578:
1574:
1560:
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1531:
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1526:
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1504:
1501:
1499:
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1477:
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1471:
1461:
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1438:
1436:
1433:
1431:
1428:
1426:
1423:
1421:
1418:
1416:
1413:
1409:
1408:La Hougue Bie
1406:
1405:
1404:
1401:
1399:
1396:
1395:
1393:
1389:
1383:
1380:
1378:
1375:
1373:
1370:
1368:
1365:
1363:
1360:
1356:
1353:
1351:
1348:
1346:
1343:
1341:
1338:
1336:
1333:
1331:
1328:
1326:
1323:
1321:
1320:Civilian life
1318:
1316:
1315:Collaboration
1313:
1311:
1308:
1306:
1303:
1302:
1301:
1298:
1296:
1293:
1292:
1290:
1286:
1283:
1281:
1277:
1272:
1265:
1260:
1258:
1253:
1251:
1246:
1245:
1242:
1236:
1233:
1232:
1224:
1223:
1218:
1216:
1212:
1209:
1208:Geology Today
1205:
1202:John Renouf:
1201:
1198:
1194:
1191:
1190:
1179:
1173:
1165:
1161:
1155:
1151:
1144:
1135:
1127:
1119:
1110:
1109:in the east.
1108:
1098:
1096:
1086:
1077:
1075:
1071:
1067:
1065:
1061:
1056:
1054:
1050:
1046:
1036:
1034:
1030:
1025:
1020:
1017:
1014:
1012:
1011:Quetivel Mill
1007:
1005:
1004:La Hougue Bie
1000:
996:
992:
988:
985:
980:
978:
974:
969:
967:
963:
952:
949:
941:
938:
934:
930:
925:
921:
917:
912:
909:
905:
903:
899:
895:
891:
887:
883:
878:
870:
861:
858:
856:
852:
847:
843:
836:
829:
821:
815:
813:
809:
805:
801:
797:
793:
789:
785:
781:
777:
773:
768:
764:
757:
754:
752:
746:
741:
731:
729:
723:
721:
717:
711:
708:
705:
700:
698:
694:
690:
686:
676:
673:
669:
665:
660:
658:
654:
650:
646:
642:
637:
635:
631:
629:
626:
622:
619:, 10% to 15%
618:
614:
609:
607:
603:
602:cross bedding
599:
595:
591:
587:
582:
581:Gorey Harbour
578:
574:
573:submarine fan
570:
566:
562:
548:
540:
530:
525:
524:
514:
509:
508:
498:
493:
492:
482:
477:
476:
466:
461:
460:
448:
443:
442:
432:
427:
426:
416:
411:
410:
378:
371:
364:
357:
350:
343:
336:
335:Carboniferous
329:
322:
315:
308:
301:
294:
287:
174:
167:
159:
157:
153:
149:
145:
144:
133:
123:
120:
112:
101:
98:
94:
91:
87:
84:
80:
77:
73:
70: –
69:
65:
64:Find sources:
58:
54:
48:
47:
42:This article
40:
36:
31:
30:
27:
19:
3640:Stevns Klint
3483:Volgo–Uralia
3332:Moscow Basin
3237:Arctic Ocean
3174:Dinaric Alps
3126:Svecofennian
2997:
2615:Bibliography
2536:des Pigneaux
2404:Les Écréhous
2371:Saint Martin
2341:de la Vallée
2229:de la Rocque
2122:Coat of arms
2087:
1862:Jersey pound
1777:
1666:Constitution
1593:
1503:Haute Valleé
1415:Mont Orgueil
1325:Deportations
1221:
1207:
1203:
1196:
1192:
1177:
1172:
1163:
1154:
1141:
1133:
1125:
1116:
1104:
1091:
1068:
1057:
1042:
1021:
1018:
1015:
1008:
998:
989:glaciation,
981:
970:
958:
950:
947:
939:
935:
913:
910:
906:
879:
876:
867:
859:
848:
816:
808:milky quartz
769:
758:
755:
751:Saint Helier
737:
724:
712:
709:
702:Porphoritic
701:
682:
661:
638:
634:Conglomerate
632:
610:
579:is found at
565:St Ouens Bay
557:
140:
138:
115:
106:
96:
89:
82:
75:
63:
51:Please help
46:verification
43:
26:
3650:Thingvellir
3620:Rhine Gorge
3430:Tisza Plate
3425:Pelso Plate
3352:Paris Basin
3322:Mezen Basin
3071:Dalslandian
3003:Isle of Man
2943:Switzerland
2866:Netherlands
2503:des Augerez
2480:Saint Peter
2394:de l'Église
2384:de Faldouet
2290:du Rocquier
2252:de Noirmont
2171:de la Ville
2078:Channel 103
2038:Opera House
2033:Jersey Live
1857:Jersey Post
1617:Saint Aubin
1542:Independent
1518:Le Rocquier
1295:Archaeology
1122:Earthquakes
1049:molybdenite
995:periglacial
982:During the
973:Neanderthal
916:lamprophyre
898:lamprophyre
851:Fort Regent
693:agglomerate
621:plagioclase
141:geology of
3605:Nærøyfjord
3600:Mount Etna
3580:Messel Pit
3550:High Coast
3302:Ebro Basin
3096:Laxfordian
3066:Carpathian
3061:Caledonian
3051:Belomorian
2913:San Marino
2861:Montenegro
2841:Luxembourg
2816:Kazakhstan
2702:Azerbaijan
2584:des Augrès
2526:de Maufant
2437:Saint Ouen
2414:Saint Mary
2305:Saint John
2295:de Samarès
2267:de la Moye
2244:St Brelade
2214:des Marais
2151:Vingtaines
2013:Jersey cow
1998:Eisteddfod
1983:Demography
1723:Connétable
1604:Reservoirs
1498:Grainville
1491:Government
1430:Corn Riots
1310:Resistance
1305:Evacuation
1147:References
1138:Geophysics
1070:China clay
984:Quaternary
955:Quaternary
924:Hornblende
812:orthoclase
806:featuring
804:pegmatites
792:oligoclase
776:tourmaline
672:subduction
645:cordierite
625:microcline
561:turbidites
377:Quaternary
363:Cretaceous
314:Ordovician
293:Cryogenian
156:Quaternary
79:newspapers
3525:Dolomites
3342:Oslo Rift
3247:Black Sea
3164:Apennines
2983:Gibraltar
2881:Jan Mayen
2836:Lithuania
2674:Countries
2579:du Rondin
2318:de HĂ©rupe
2219:de la Rue
2206:Grouville
2163:St Helier
1993:Education
1936:Transport
1887:Committee
1795:Judiciary
1750:Viscounts
1698:Elections
1612:St Helier
1589:Geography
1577:Geography
1474:Education
1391:Specifics
1382:Perquages
1367:Windmills
1288:Overviews
1107:Grouville
1080:Quarrying
1060:Neolithic
1053:haematite
1024:Mammuthus
987:Devensian
810:and pink
670:facing a
613:Greywacke
606:boudinage
590:sandstone
300:Ediacaran
109:July 2018
3665:Category
3635:St Kilda
3625:Scandola
3615:Plitvice
3530:Durmitor
3510:Aggtelek
3463:Cimmeria
3453:Avalonia
3440:Terranes
3194:Pyrenees
3169:Caucasus
3141:Variscan
3121:Timanide
3116:Scourian
3111:Scandian
3091:Hellenic
3081:Grampian
3056:Cadomian
2993:Guernsey
2988:Alderney
2973:Scotland
2928:Slovenia
2923:Slovakia
2898:Portugal
2886:Svalbard
2722:Bulgaria
2624:Category
2574:de Rozel
2488:du Douet
2379:de Rozel
2323:du Douet
2045:Religion
1899:Taxation
1810:Honorary
1779:Greffier
1638:Politics
1599:Parishes
1508:Hautlieu
1377:Maritime
1362:COVID-19
1045:ankerite
944:Tertiary
918:dykes.
902:feldspar
894:Armorica
890:Tertiary
886:Mesozoic
800:limonite
788:perthite
784:fluorite
728:hematite
704:rhyolite
685:Andesite
668:Armorica
657:chlorite
641:hornfels
628:feldspar
586:mudstone
370:Tertiary
356:Jurassic
342:Triassic
328:Devonian
321:Silurian
307:Cambrian
152:Cambrian
3645:Surtsey
3630:Ĺ kocjan
3585:Meteora
3575:Laponia
3570:Kvarken
3458:Baltica
3204:Sudetes
3136:Uralian
3106:Saamian
3076:Gothian
3041:Acadian
3033:Orogens
2963:England
2953:Ukraine
2903:Romania
2851:Moldova
2801:Ireland
2796:Iceland
2791:Hungary
2781:Germany
2776:Georgia
2759:Finland
2754:Estonia
2742:Denmark
2727:Croatia
2712:Belgium
2707:Belarus
2697:Austria
2692:Armenia
2687:Andorra
2682:Albania
2608:Outline
2561:Trinity
2427:du Nord
2313:du Nord
2257:du Coin
2104:Symbols
2055:Theatre
1957:Culture
1941:airport
1931:Tourism
1830:Economy
1654:Bailiff
1594:Geology
1483:Schools
1403:Dolmens
1280:History
1187:Sources
1064:dolmens
1031:sp and
920:Biotite
742:around
649:biotite
527:←
511:←
495:←
479:←
463:←
445:←
429:←
413:←
349:Permian
273:–
263:–
253:–
243:–
233:–
223:–
213:–
203:–
193:–
183:–
93:scholar
3545:Glarus
3101:Lopian
3046:Alpine
2998:Jersey
2948:Turkey
2938:Sweden
2918:Serbia
2908:Russia
2893:Poland
2876:Norway
2856:Monaco
2826:Latvia
2821:Kosovo
2810:Sicily
2786:Greece
2771:France
2732:Cyprus
2422:du Sud
2155:parish
2112:Anthem
1874:Livre
1805:Police
1768:Courts
1271:Jersey
1095:hoggin
1029:Betula
796:quartz
790:, and
772:aplite
697:pumice
617:quartz
604:, and
567:, and
547:Jersey
403:
398:
393:
388:
383:
286:Tonian
143:Jersey
95:
88:
81:
74:
66:
3610:Pirin
3209:Urals
2978:Wales
2933:Spain
2846:Malta
2806:Italy
2065:Media
2050:Sport
2028:Music
1882:Roads
1867:coins
1800:Jurat
1772:Royal
1622:Gorey
1130:Study
1113:Water
1033:Alnus
991:loess
966:chalk
962:Flint
780:topaz
594:flute
577:shale
100:JSTOR
86:books
3565:Komi
3179:Harz
3159:Alps
2127:Flag
1919:Sure
1659:list
1101:Sand
1051:and
999:head
888:and
880:The
794:and
782:and
691:and
689:tuff
647:and
623:and
154:and
139:The
72:news
3379:and
2153:by
1760:Law
1206:in
1195:in
929:435
842:465
835:426
828:438
666:of
55:by
3667::
1162:.
1055:.
1047:,
933:.
900:,
846:.
814:.
778:,
659:.
600:,
549:.
2812:)
2808:(
2658:e
2651:t
2644:v
2118:)
2114:(
1774:)
1770:(
1263:e
1256:t
1249:v
1166:.
1027:(
853:/
122:)
116:(
111:)
107:(
97:·
90:·
83:·
76:·
49:.
20:)
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