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Geology of Malta

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The rock layers in Malta are relatively flat-lying, with the exception of zones where the rock has been folded close to faults. The faults have two main orientations, with the largest faults being northwest-southeast trending, parallel to the line of islands, although these faults are only locally
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age (~10–7 million years old). Yellow-green in colour, it takes on an orange tint when it comes into contact with the air. It is generally very thin, a few tens of centimetres in most areas, with a maximum thickness of 11 m. It is friable and therefore unsuitable for building purposes. Its
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in age (~15–10 million years old) measuring up to 65 m thick. It shows major thickness variations and is missing completely from most of the eastern parts of the islands. It was deposited in a deepwater environment. It forms an impermeable layer beneath the Greensand and Upper Coralline
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Since prehistoric times, this limestone has constituted the majority of building material used in Malta. Exposed to the air, the stone takes on a rosy colour, which browns with the formation of a protective patina. Lesser quality rocks can erode easily however, and can show
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that give it its name. It is divided into three members, the lower, middle and upper, with the boundaries between them being hardgrounds, representing the effects of further seabed exposure.
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exposed, and a second set that are WSW-ENE trending, with generally small displacements that dominate the topography of the islands. The largest of the second set are the
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age (~28–23 million years old) with a maximum thickness of 162 m. The unit is exposed on the lower parts of cliffs in the south-west of the archipelago such as at
2186: 477:. The Coralline Limestone is a hard, pale-grey limestone. It was used frequently in constructions requiring great strength, and in fortifications in particular. 2235: 504:
Overall, the islands of the archipelago are tilted towards the northeast, with cliffs on the southwest coast and descending gradients towards the northeast.
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Limestone formations. It is most visible in the northwest of Malta and the northeast of Gozo. It allows the capture of rainfall and the creation of
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Courtin, Jean (1995). "Malte préhistorique, une île de Pâques méditerranéenne?". In Villain-Gandossi, Christiane (ed.).
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Fault on northern Malta and the Qala Fault on southern Gozo. The fault is around 18.5 kilometres (11.5 mi) long.
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is generally developed indicating a period during which the seafloor was exposed. It is this formation of which the
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is situated on the mainly shallow water continental platform between Sicily and North Africa that lies beneath the
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permeable nature and its position immediately above the Blue Clay allow for the infiltration of rainwater.
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age (~7–5 million years old) and is around 140 m thick. It is mainly present on the islands of
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age (~23–14 million years old), ranging in thickness from 23 m to 207 m. It contains many
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at the top of the Lower Coralline Limestone Formation with limestone clasts and fossils of the
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The oldest exposed rock layer of Malta is the Lower Coralline Limestone Formation (
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Cliffs of Upper Coralline Limestone Formation on islands at the western end of
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Seismic history of the Maltese islands and considerations on seismic risk
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is made up of an identical structure on the southwest side of this rift.
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Cliffs of Upper Globogerina Limestone Formation at Il-Ħofra l-Kbira near
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by which animals have been able to cross, as evinced by the presence of
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of the Mediterranean, Malta has been connected to Sicily by a surface
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SW-dipping minor fault on the southwest coast of Malta, near the
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Blue Clay Formation exposed in the cliffs at the northern end of
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cliffs showing stratification in the Lower Coralline Limestone
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overlying yellow-weathering Upper Globigerina Limestone
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of depths of less than 100 m. During different
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most of the earthquakes that affect the archipelago
512:The Maltese archipelago is linked to Sicily by an 180:) dating from between 25 and 5 million years ago. 637: 635: 124:in Sicily may have damaging effects, such as the 642:Dart C.J.; Bosence D.W.J.; McClay K.R. (1993). 453:The top layer, the Upper Coralline Limestone ( 1875: 849: 156:on the edge of the Malta Graben. The isle of 8: 2315: 2254: 2147: 2091: 1882: 1868: 1860: 1227: 856: 842: 834: 347:International Union of Geological Sciences 260:, and also along rifts, particularly near 2182:Ministry for Foreign and European Affairs 540:(fossils of the Maltese Giant Dormouse, 484: 441: 375: 308:) is a soft, gold-coloured limestone of 219: 198: 192:of the Maltese islands consists of five 28: 2510: 580:"Geological Map of the Maltese Islands" 555: 794: 784: 704: 702: 616: 614: 573: 571: 569: 567: 565: 563: 561: 559: 7: 829:. Environment Protection Department. 216:Lower Coralline Limestone Formation 148:, was created through the uplift of 686:IUGS Subcommission: Heritage Stones 438:Upper Coralline Limestone Formation 112:graben, that of Malta, and that of 364:, built from Globigerina Limestone 25: 808:Malta, its Archeology and History 781:. Vol. 50. pp. 725–740. 648:Journal of the Geological Society 120:, although some earthquakes with 2525: 2513: 2076: 1212: 806:Samut Tagliaferro, John (1991). 461:), is the youngest formation of 827:Wildlife of the Maltese Islands 737:"CENNI SUL MEDITERRANEO MARINO" 285:Globigerina Limestone Formation 100:. The platform is crossed by a 825:Sultana, Joe; Falzon, Victor. 578:Continental Shelf Department. 351:Global Heritage Stone Resource 1: 1506:European Cenozoic Rift System 730:. Progress Press Publication. 396:) is a blue-gray mudstone of 2187:Minister for Foreign Affairs 56:age cut through by a set of 1696:UNESCO World Heritage Sites 300:The Globigerina Limestone ( 2564: 530:Maltese dwarf hippopotamus 320:, especially those of the 168:The rocks are exclusively 44:consists of a sequence of 2465: 2318: 2257: 2150: 2094: 2074: 2061:Award of the George Cross 1210: 810:. Casa Editrice Perseus. 508:Recent geological history 1614:Jan Mayen Microcontinent 660:10.1144/gsjgs.150.6.1153 132:Formation of the islands 1556:Peri-Caspian Depression 1285:Hallandian-Danopolonian 775:Galea, Pauline (2007). 620:Samut Tagliaferro, John 293:Limestone wall showing 1398:Scandinavian Mountains 916:Bosnia and Herzegovina 726:Blouet, Brian (1989). 493: 458: 450: 429:-bearing sandstone of 422: 393: 385: 365: 305: 297: 249: 241: 207: 164:Nature of the sub-soil 126:1693 Sicily earthquake 37: 2007:Rising of the Priests 1566:White Sea Rift System 682:"Designation of GHSR" 582:. Government of Malta 536:fossils), as well as 488: 445: 379: 359: 292: 223: 202: 194:geological formations 184:The geological strata 92:boundary between the 32: 2453:World Heritage Sites 2036:British Protectorate 1672:Fennoscandian Craton 1667:East European Craton 758:Le Carrefour Maltais 735:Catalano, Raimondo. 599:Galea, P. pp.725–740 335:honeycomb weathering 295:honeycomb weathering 172:. There is a lot of 1926:Carthaginian Empire 1561:Timan-Pechora Basin 1496:Dnieper–Donets Rift 1413:Western Carpathians 629:Sultana, J., et al. 473:and in the east of 413:Greensand Formation 372:Blue Clay Formation 140:, situated between 138:Maltese archipelago 86:Mediterranean Basin 74:Maltese archipelago 18:Blue Clay Formation 2287:Telecommunications 1963:Byzantine invasion 1916:Megalithic Temples 1714:Calanques de Piana 1468:basins and grabens 728:The Story of Malta 543:Leithia melitensis 518:marine regressions 514:underwater plateau 494: 451: 386: 366: 360:Gardjola Tower at 298: 242: 208: 58:extensional faults 38: 2501: 2500: 2461: 2460: 2305: 2304: 2244: 2243: 2214:Political parties 2177:Foreign relations 2137: 2136: 2046:Language Question 2014:French occupation 1970:Kingdom of Sicily 1958:Aghlabid invasion 1857: 1856: 1794:Monte San Giorgio 1690: 1689: 1647:Armorican terrane 1451:Mediterranean Sea 865:Geology of Europe 339:government palace 150:sedimentary rocks 84:from the western 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1325:Svecofennian 1044: 826: 807: 777: 757: 745:. Retrieved 743:(in Italian) 740: 727: 713: 689:. Retrieved 685: 676: 651: 647: 625: 608:Catalano, R. 604: 595: 584:. Retrieved 541: 511: 503: 495: 452: 416: 387: 367: 331: 324: 322:foraminifera 299: 274:Azure Window 243: 231: 190:stratigraphy 187: 167: 154:tilted block 135: 82:Ionian Basin 71: 54:late Miocene 41: 39: 26: 2343:Immigration 2199:LGBT rights 2002:Great Siege 1953:Arab Period 1921:Phoenicians 1849:Thingvellir 1819:Rhine Gorge 1629:Tisza Plate 1624:Pelso Plate 1551:Paris Basin 1521:Mezen Basin 1270:Dalslandian 1202:Isle of Man 1142:Switzerland 1065:Netherlands 717:Courtin, J. 691:24 February 491:Blue Grotto 326:Globigerina 170:sedimentary 110:Pantelleria 2438:Philosophy 2423:Literature 2338:Healthcare 2333:Emigration 2209:Parliament 2124:Localities 1804:Nærøyfjord 1799:Mount Etna 1779:Messel Pit 1749:High Coast 1501:Ebro Basin 1295:Laxfordian 1265:Carpathian 1260:Caledonian 1250:Belomorian 1112:San Marino 1060:Montenegro 1040:Luxembourg 1015:Kazakhstan 901:Azerbaijan 760:. Edisud. 747:26 January 708:Blouet, B. 586:2018-02-22 550:References 427:glauconite 382:Ä nejna Bay 310:Aquitanian 270:hardground 235:subrotunda 225:Hardground 122:epicentres 90:subduction 35:Marsaxlokk 2348:Languages 2328:Education 2297:Transport 2219:President 2172:Elections 2160:Commander 2087:Geography 1724:Dolomites 1541:Oslo Rift 1446:Black Sea 1363:Apennines 1182:Gibraltar 1080:Jan Mayen 1035:Lithuania 873:Countries 797:ignored ( 787:cite book 668:131447222 463:Messinian 431:Tortonian 402:Tortonian 211:Oligocene 174:limestone 158:Lampedusa 102:rift zone 68:Tectonics 50:Oligocene 2542:Category 2488:Category 2418:Folklore 2381:Carnival 2358:Religion 2282:Taxation 2267:Currency 2143:Politics 2024:Blockade 2019:Invasion 1936:Invasion 1911:Timeline 1895:articles 1834:St Kilda 1824:Scandola 1814:Plitvice 1729:Durmitor 1709:Aggtelek 1662:Cimmeria 1652:Avalonia 1639:Terranes 1393:Pyrenees 1368:Caucasus 1340:Variscan 1320:Timanide 1315:Scourian 1310:Scandian 1290:Hellenic 1280:Grampian 1255:Cadomian 1192:Guernsey 1187:Alderney 1172:Scotland 1127:Slovenia 1122:Slovakia 1097:Portugal 1085:Svalbard 921:Bulgaria 407:aquifers 398:Langhian 314:Langhian 254:Chattian 239:bivalves 233:Scutella 229:echinoid 96:and the 62:Pliocene 48:of late 2520:Geology 2506:Portals 2472:Outline 2401:Cuisine 2368:Culture 2311:Society 2250:Economy 2119:Islands 2114:Geology 2104:Climate 1903:History 1844:Surtsey 1829:Ĺ kocjan 1784:Meteora 1774:Laponia 1769:Kvarken 1657:Baltica 1403:Sudetes 1335:Uralian 1305:Saamian 1275:Gothian 1240:Acadian 1232:Orogens 1162:England 1152:Ukraine 1102:Romania 1050:Moldova 1000:Ireland 995:Iceland 990:Hungary 980:Germany 975:Georgia 958:Finland 953:Estonia 941:Denmark 926:Croatia 911:Belgium 906:Belarus 896:Austria 891:Armenia 886:Andorra 881:Albania 741:Siripro 522:isthmus 455:Maltese 425:) is a 419:Maltese 390:Maltese 362:Senglea 318:fossils 302:Maltese 280:Miocene 246:Maltese 178:lagoons 146:Tunisia 106:grabens 2493:Portal 2386:Cinema 2353:People 2272:Energy 2051:Exiles 1893:  1744:Glarus 1300:Lopian 1245:Alpine 1197:Jersey 1147:Turkey 1137:Sweden 1117:Serbia 1107:Russia 1092:Poland 1075:Norway 1055:Monaco 1025:Latvia 1020:Kosovo 1009:Sicily 985:Greece 970:France 931:Cyprus 814:  764:  666:  481:Faults 471:Comino 448:Comino 306:Franka 266:Naxxar 258:Dingli 250:Ĺ»onqor 204:Dingli 142:Sicily 114:Linosa 108:: the 2532:Malta 2479:Index 2448:Sport 2428:Music 2099:Caves 1891:Malta 1809:Pirin 1408:Urals 1177:Wales 1132:Spain 1045:Malta 1005:Italy 664:S2CID 467:Malta 394:Tafal 349:as a 343:Corfu 262:Mosta 64:age. 2413:Flag 2406:Wine 2229:List 2129:Maps 1764:Komi 1378:Harz 1358:Alps 812:ISBN 799:help 762:ISBN 749:2015 693:2019 532:and 475:Gozo 264:and 237:and 188:The 144:and 136:The 72:The 40:The 1578:and 656:doi 652:150 546:). 400:to 341:of 312:to 60:of 52:to 2544:: 791:: 789:}} 785:{{ 739:. 701:^ 684:. 662:. 650:. 646:. 634:^ 613:^ 558:^ 469:, 457:: 421:: 392:: 368:. 353:. 304:: 248:: 128:. 2508:: 1883:e 1876:t 1869:v 1011:) 1007:( 857:e 850:t 843:v 820:. 801:) 770:. 751:. 695:. 670:. 658:: 589:. 528:( 20:)

Index

Blue Clay Formation

Marsaxlokk
sedimentary rocks
Oligocene
late Miocene
extensional faults
Pliocene
Maltese archipelago
Sicily Channel
Ionian Basin
Mediterranean Basin
subduction
African Plate
Eurasian Plate
rift zone
grabens
Pantelleria
Linosa
most of the earthquakes that affect the archipelago
epicentres
1693 Sicily earthquake
Maltese archipelago
Sicily
Tunisia
sedimentary rocks
tilted block
Lampedusa
sedimentary
limestone

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