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History of geology

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28: 1073: 1261:, published calculations that fixed the age of the Earth at between 20 million and 400 million years. He assumed that the Earth had formed as a completely molten object, and estimated the amount of time it would take for the near-surface to cool to its present temperature. Many geologists contended that Thomson's estimates were inadequate to account for observed thicknesses of sedimentary rock, evolution of life, and the formation of the crystalline basement rocks beneath the sedimentary cover. The discovery of radioactivity in the early twentieth century provided an additional source of heat within the Earth, allowing for an increase in Thomson's calculated age, as well as a means of dating geological events. 3092: 1146: 1024:. Once the term was established to denote the study of the Earth and its history, geology slowly became more generally recognized as a distinct science that could be taught as a field of study at educational institutions. In 1741 the best-known institution in the field of natural history, the National Museum of Natural History in France, created the first teaching position designated specifically for geology. This was an important step in further promoting knowledge of geology as a science and in recognizing the value of widely disseminating such knowledge. 916: 881:. With this enhanced desire for data came an increase in observations of the Earth's composition, which in turn led to the discovery of fossils. Although theories that resulted from the heightened interest in the Earth's composition were often manipulated to support the concept of the Deluge, a genuine outcome was a greater interest in the makeup of the Earth. Due to the strength of Christian beliefs during the 17th century, the theory of the origin of the Earth that was most widely accepted was 2981: 523: 65: 3485: 2993: 2613: 852: 3473: 1303: 3462: 1318:. This theory suggests that the shapes of continents and matching coastline geology between some continents indicates they were joined together in the past and formed a single landmass known as Pangaea; thereafter they separated and drifted like rafts over the ocean floor, currently reaching their present position. Additionally, the theory of continental drift offered a possible explanation as to the formation of mountains; 1158: 3005: 1431:, began supplying satellite images that can be geologically analyzed. These images can be used to map major geological units, recognize and correlate rock types for vast regions and track the movements of Plate Tectonics. A few applications of this data include the ability to produce geologically detailed maps, locate sources of natural energy and predict possible natural disasters caused by plate shifts. 1329:, to cause the continents to move. However, it was not until after the Second World War that new evidence started to accumulate that supported continental drift. There followed a period of 20 years during which the theory of continental drift developed from being believed by a few to being the cornerstone of modern geology. Beginning in 1947 research provided new evidence about the ocean floor, and in 1960 1052:. The Neptunist thesis was the most popular during the late eighteenth century, especially for those who were chemically trained. However, another thesis slowly gained currency from the 1780s forward. Instead of water, some mid-eighteenth-century naturalists such as Buffon had suggested that strata had been formed through heat (or fire). The thesis was modified and expanded by the Scottish naturalist 1250:
vast areas of the countries. Geological mapping provides the location of useful rocks and minerals and such information could be used to benefit the country's mining and quarrying industries. With the government and industrial funding of geological research, more individuals undertook study of geology as technology and techniques improved, leading to the expansion of the field of the science.
903:. Steno was trained in the classical texts on science; however, by 1659 he seriously questioned accepted knowledge of the natural world. Importantly, he questioned the idea that fossils grew in the ground, as well as common explanations of rock formation. His investigations and his subsequent conclusions on these topics have led scholars to consider him one of the founders of modern 1060:: the formation of the Earth through the gradual solidification of a molten mass at a slow rate by the same processes that had occurred throughout history and continued in the present day. This led him to the conclusion that the Earth was immeasurably old and could not possibly be explained within the limits of the chronology inferred from the Bible. Plutonists believed that 1299:
4,500 ± 100 million years, based on measurements of the relative abundance of uranium isotopes established by Alfred O. C. Nier. Theories that did not comply with the scientific evidence that established the age of the Earth could no longer be accepted. The established age of the Earth has been refined since then but has not significantly changed.
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With the application of scientific methods to the investigation of the Earth's history, the study of geology could become a distinct field of science. To begin with, the terminology and definition of what constituted geological study had to be worked out. The term "geology" was first used technically
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Economic motivations for the practical use of geological data motivated some governments to support geological research. During the 19th century several countries, including Canada, Australia, Great Britain and the United States, initiated geological surveying that would produce geological maps of
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Period. The stratigraphic column was significant because it supplied a method to assign a relative age of these rocks by slotting them into different positions in their stratigraphical sequence. This created a global approach to dating the age of the Earth and allowed for further correlations to be
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came to a rough consensus that the age of the Earth was a few billion years and that radiometric dating was credible. Holmes published The Age of the Earth, an Introduction to Geological Ideas in 1927 in which he presented a range of 1.6 to 3.0 billion years increasing the estimate in the 1940s to
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and co-workers showed with a computer calculation how the continents along both sides of the Atlantic would best fit to close the ocean, which became known as the famous "Bullard's Fit". By the late 1960s the weight of the evidence available saw continental drift as the generally accepted theory.
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By the 1770s, chemistry was starting to play a pivotal role in the theoretical foundation of geology and two opposite theories with committed followers emerged. These contrasting theories offered differing explanations of how the rock layers of the Earth's surface had formed. One suggested that a
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which brought him widespread recognition because he presented a detailed system for identifying specific minerals based on external characteristics. The more efficiently productive land for mining could be identified and the semi-precious metals could be found, the more money could be made. This
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realized that the relative ages of fossils could be determined from a geological standpoint; in terms of what layer of rock the fossils are located and the distance these layers of rock are from the surface of the Earth. Through the synthesis of their findings, Brogniart and Cuvier realized that
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necessary to make the mobility of the plates on the globe function. A symposium on continental drift that was held at the Royal Society of London in 1965 must be regarded as the official start of the acceptance of plate tectonics by the scientific community. The abstracts from the symposium are
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methods rather than methods based on geological sedimentation or cooling of the Earth (many people still clung to Lord Kelvin's calculations of less than 100 million years). Holmes estimated the oldest Archean rocks to be 1,600 million years old, but did not speculate about the Earth's age. His
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in 1755. From the works of these respected men, as well as others, it became acceptable by the mid eighteenth century to question the age of the Earth. This questioning represented a turning point in the study of the Earth. It was now possible to study the history of the Earth from a scientific
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which presented a variety of geological evidence from England, France, Italy and Spain to prove Hutton's ideas of gradualism correct. He argued that most geological change had been very gradual in human history. Lyell provided evidence for Uniformitarianism, a geological doctrine holding that
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made critical observations of the slow rate of geological change. He observed the composition of the land and formulated a theory where the Earth changes at a slow rate and that these changes cannot be observed during one person's lifetime. Aristotle developed one of the first evidence-based
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In recent years, geology has continued its tradition as the study of the character and origin of the Earth, its surface features and internal structure. What changed in the later 20th century is the perspective of geological study. Geology was now studied using a more integrative approach,
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Also during the eighteenth century, aspects of the history of the Earth – namely the divergences between the accepted religious concept and factual evidence – once again became a popular topic for discussion in society. In 1749, the French naturalist
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different strata could be identified by fossil contents and thus each stratum could be assigned to a unique position in a sequence. After the publication of Cuvier and Brongniart's book, "Description Geologiques des Environs de Paris" in 1811, which outlined the concept,
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and Adam Sedgwick interpreted "diluvial" deposits as the outcome of Noah's flood, but by the end of the decade they revised their opinions in favour of local inundations. Charles Lyell challenged catastrophism with the publication in 1830 of the first volume of his book
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processes occur at the same rates in the present as they did in the past and account for all of the Earth's geological features. Lyell's works were popular and widely read, and the concept of Uniformitarianism took a strong hold in geological society.
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principles about the geological processes he saw, and even challenging some of Lyell's ideas. He speculated about the Earth expanding to explain uplift, then on the basis of the idea that ocean areas sank as land was uplifted, theorised that
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It was not until the 17th century that geology made great strides in its development. At this time, geology became its own entity in the world of natural science. It was discovered by the Christian world that different translations of the
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became very popular amongst geologists; many hoped to apply this concept to all the rocks of the Earth. During this century various geologists further refined and completed the stratigraphic column. For instance, in 1833 while
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drive for economic gain propelled geology into the limelight and made it a popular subject to pursue. With an increased number of people studying it, came more detailed observations and more information about the Earth.
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considering the Earth in a broader context encompassing the atmosphere, biosphere and hydrosphere. Satellites located in space that take wide scope photographs of the Earth provide such a perspective. In 1972, The
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liquid inundation, perhaps like the biblical deluge, had created all geological strata. The theory extended chemical theories that had been developing since the seventeenth century and was promoted by Scotland's
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and their natural distribution vital. Scholars began to study the makeup of the Earth in a systematic manner, with detailed comparisons and descriptions not only of the land itself, but of the semi-precious
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During the 17th century, both religious and scientific speculation about the Earth's origin further propelled interest in the Earth and brought about more systematic identification techniques of the Earth's
1277:, among the pioneers in the use of radioactive decay as a means of measuring geological time, dated a sample from Ceylon at 1.6 billion years old using lead isotopes. In 1913 Holmes was on the staff of 1325:
Unfortunately, Wegener provided no convincing mechanism for this drift, and his ideas were not generally accepted during his lifetime. Arthur Holmes accepted Wegener's theory and provided a mechanism:
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during the 1780s. He argued against the theory of Neptunism, proposing instead the theory of based on heat. Those who followed this thesis during the early nineteenth century referred to this view as
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and geology (Steno, who became a Catholic as an adult, was eventually made a bishop, and was beatified in 1988 by Pope John Paul II. Therefore, he is also called Blessed Nicolas Steno).
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stimulated the rapid development of the stratigraphic column – "the sequence of rock formations arranged according to their order of formation in time." In England, the mining surveyor
1201:, who had just completed his BA degree and had accompanied Sedgwick on a two-week Welsh mapping expedition after taking his Spring course on geology. Fitzroy gave Darwin Lyell's 3192: 1048:, had formed as a precipitate from an ocean that covered the entire Earth. Werner's system was influential and those who accepted his theory were known as Diluvianists or 1465: 1232:. Darwin's discovery of giant fossils helped to establish his reputation as a geologist, and his theorising about the causes of their extinction led to his theory of 899:. The Earth's strata can be defined as horizontal layers of rock having approximately the same composition throughout. An important pioneer in the science was 990: 777:
personality who dabbled in many fields of study in his age. In terms of geology, Shen Kuo is one of the first naturalists to have formulated a theory of
1295: 984:, but rather 75,000 years. Another individual who described the history of the Earth with reference to neither God nor the Bible was the philosopher 434: 3167: 1228: 891:. Whiston used Christian reasoning to "prove" that the Great Flood had occurred and that the flood had formed the rock strata of the Earth. 3043: 869:
contained different versions of the biblical text. The one entity that remained consistent through all of the interpretations was that the
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England, P; Molnar, P (2007). "John Perry's neglected critique of Kelvin's age for the earth : A missed opportunity in geodynamics".
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Wegener, Alfred (1912). "Die Herausbildung der Grossformen der Erdrinde (Kontinente und Ozeane), auf geophysikalischer Grundlage".
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and so the major stumbling block to the theory was removed. Geophysical evidence suggested lateral motion of continents and that
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suggested the concept of paleomagnetism from his finding that the continents had moved relative to the Earth's magnetic poles.
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described fossil fish and shells found in deposits on mountains. Similar fossils were noted by Herodotus (about 490 BC).
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Blacket, P.M.S.; Bullard, E.; Runcorn, S.K., eds. (1965). "A Symposium on Continental Drift, held on 28 October 1965".
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developed some primary geological concepts concerning the origin of the Earth. Additionally, in the 4th century BC
3379: 1029: 1014:, though "geology" was not well received as a term until it was taken up in the very influential compendium, the 218: 742:" (the Book of Cure, Healing or Remedy from ignorance), in which Part 2, Section 5, contains his commentary on 3417: 3323: 3111: 2334:. Revised and translated by Albert V. Carozzi and Marguerite Carozzi. New Brunswick: Rutgers University Press. 2318: 2265: 809: 228: 976:
in which he attacked the popular Biblical accounts given by Whiston and other ecclesiastical theorists of the
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A portrait of Whiston with a diagram demonstrating his theories of cometary catastrophism best described in
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province. He formulated a hypothesis for the process of land formation: based on his observation of fossil
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From this increased interest in the nature of the Earth and its origin, came a heightened attention to
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Four centuries of geological travel : the search for knowledge on foot, bicycle, sledge and camel
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was adapted with the aim of reconciling geological science with religious traditions of the biblical
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concepts connected to the geological realm regarding the rate at which the Earth physically changes.
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then widely used for practical ends. He was among the first to correctly identify the origin of
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from trees by the observation of insects trapped within some pieces. He also laid the basis of
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proposed that the oceanic crust forms as the seafloor spreads apart along mid-ocean ridges in
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in Europe during the mid to late 18th century made the possession of accurate knowledge about
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promotion of the theory over the next decades earned him the nickname of Father of Modern
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Wilson, J. Tuzo (1965). "A new class of faults and their bearing on continental drift".
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in a mountain hundreds of miles from the ocean, he inferred that the land was formed by
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drawn from similarities found in the makeup of the Earth's crust in various countries.
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Rocchio, Laura. "The Landsat Program." National Aeronautics and Space Administration.
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The Age of Achievement: A.D. 750 to the End of the Fifteenth Century: The Achievements
750:, The advantages of mountains in the formation of clouds; Sources of water; Origin of 3472: 3177: 3009: 2903: 2497: 2471: 2450: 2431: 2425: 2401: 2380: 2354: 2335: 2329: 2314: 2283: 2261: 2078: 1912: 1868: 1595: 1544: 1503: 1358: 1350: 1326: 1315: 1237: 801: 699: 506: 496: 427: 379: 3298: 2997: 2918: 2888: 2814: 2799: 2709: 2550: 2186: 2174: 2143: 2131: 2066: 1900: 1773:
The Language of Mineralogy: John Walker, Chemistry and the Edinburgh Medical School
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processes were the chief agent in rock formation, not water from a Great Flood.
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Engraving from William Smith's 1815 monograph on identifying strata by fossils
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from a different direction, was assigning the upper parts of Sedgwick's
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The Role of Women in the History of Geology: Special Publication no 281
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Charles Darwin's zoology notes & specimen lists from H.M.S. Beagle
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took the study of the Moon away from Lunar astronomers and gave it to
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By the early 20th Century radiogenic isotopes had been discovered and
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it contained, which had great commercial value. For example, in 1774
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is the scientific study of the origin, history, and structure of the
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is concerned with the development of the natural science of geology.
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The earth encompassed : a history of the environmental sciences
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De doodskunstenaar – de anatomische lessen van Frederik Ruysch
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By applying sound stratigraphic principles to the distribution of
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round sinking volcanic islands. This idea was confirmed when the
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Controversy in Victorian Geology: The Cambrian-Silurian Dispute
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and many others. Ibn Sina wrote an encyclopedic work entitled "
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produced a very extensive discussion of many more minerals and
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issued as Blacket, Bullard, Runcorn; 1965. In this symposium,
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scientific evidence that the Great Flood had in fact occurred
866: 794: 746:'s Mineralogy and Meteorology, in six chapters: Formation of 672: 665: 661: 575: 2114:
Wilson, J.T. (1963). "Hypothesis on the earth's behaviour".
2099:. In A. E. J. Engel; Harold L. James; B. F. Leonard (eds.). 1683: 819:
found in a preserved state underground near Yanzhou (modern
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Timeline of the development of tectonophysics (before 1954)
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Program, a series of satellite missions jointly managed by
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Time matters : geology's legacy to scientific thought
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In the 19th century, geological inquiry had estimated the
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Petrologic studies: a volume in honor of A. F. Buddington
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was mapping rocks that he had established were from the
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Jardine, N.; Secord, J. A.; Spary, E. C., eds. (1996).
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in terms of millions of years. In 1862, the physicist
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Some of the first geological thoughts were about the
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The Birth and Development of the Geological Sciences
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Time Matters: Geology's Legacy to Scientific Thought
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recorded in magnetic minerals. British geophysicist
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in which he argued strongly in favour of the use of
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Universal Natural History and Theory of the Heavens
2375:How the Catholic Church built Western civilization 2372: 2348: 1730: 1694: 1296:British Association for the Advancement of Science 1294:. In 1921, attendees at the yearly meeting of the 1173:. In the early 1820s English geologists including 996:Allgemeine Naturgeschichte und Theorie des Himmels 937:. Moreover, the increasing economic importance of 2515:. Cambridge, England: Cambridge University Press. 2449:. London, England: Geological Society of London. 2202:Philosophical Transactions of the Royal Society A 2055:Transactions of the Geological Society of Glasgow 1590:Asimov, M. S.; Bosworth, Clifford Edmund (eds.). 1525:"Evolution and Paleontology in the Ancient World" 925:is considered to be the father of modern geology. 3502: 2306:. Baltimore: The Williams & Wilkins Company. 732:) along with other natural philosophers such as 435:Lists of geological features of the Solar System 2254:. San Francisco: Freeman, Cooper & Company. 1121:was elsewhere suggesting a subdivision of the 1002:perspective without religious preconceptions. 957:Von den äusserlichen Kennzeichen der Fossilien 765:In medieval China, one of the most intriguing 3037: 2558: 1965: 1229:The Structure and Distribution of Coral Reefs 547: 2393: 1665: 1522: 1006:in publications by two Genevan naturalists, 994: 955: 2220:http://www.bgs.ac.uk/vacancies/studying.htm 1078:Oxford University Museum of Natural History 3461: 3044: 3030: 2565: 2551: 2510: 2444: 1893:British Journal for the History of Science 1882: 1880: 1589: 1407:, it can be argued that almost overnight, 1322:built on the theory of continental drift. 554: 540: 2463: 2274: 2249: 1996: 1984: 1827: 1798: 1741: 1739: 1653: 1226:, and in 1842 he published his theory on 808:. He also formulated a theory of gradual 2430:(1st Amer. ed.). New York: Norton. 2225: 1567:. New York: Alfred A. Knopf, 1956. p. 13 1381:to the model, completing the classes of 1301: 1156: 1144: 1071: 914: 850: 781:. This was based on his observations of 224:Principle of cross-cutting relationships 26: 2023: 1886: 1877: 1543:. John Wiley & Sons. 9 April 2010. 1365:, the record of the orientation of the 629:both from local mines such as those at 3503: 3051: 2491: 2423: 2394:Wyse Jackson, Patrick N., ed. (2007). 2156: 2113: 2042: 2008: 1839: 1736: 970:Georges-Louis Leclerc, Comte de Buffon 961:(On the External Features of Fossils), 698:(AD 973–1048) was one of the earliest 234:Principle of inclusions and components 3025: 2546: 2445:Burek, C.V.; Higgs, B., eds. (2007). 2367: 2327: 2308: 2296: 2026:Petermanns Geographische Mitteilungen 1937: 1925: 1851: 1810: 1786: 1757: 1745: 1718: 1706: 1677: 1671: 1641: 1629: 1614: 1484: 1165:In early nineteenth-century Britain, 804:, located hundreds of miles from the 609:However, it was his successor at the 2470:(in Dutch). Amsterdam: Bert Bakker. 2091: 1953:, Cambridge University Press, 2000. 1867:Princeton University Press, 301 pp. 1769: 1281:, when he published his famous book 933:and other components of the Earth's 440:Geology of solar terrestrial planets 31:Illustration from a 1767 account by 3004: 2048:"Radioactivity and Earth Movements" 1349:. This was seen as confirmation of 873:had formed the world's geology and 812:, after his observation of ancient 720:(Avicenna, AD 981–1037), a Persian 209:Principle of original horizontality 13: 2416: 2400:. London: The Geological Society. 2379:. Washington, D.C.: Regnery Publ. 823:), in the dry northern climate of 14: 3527: 3082:History and philosophy of science 2521: 1394: 1259:William Thomson, 1st Baron Kelvin 1020:, published beginning in 1751 by 3484: 3483: 3471: 3460: 3090: 3003: 2992: 2991: 2979: 2611: 2208:(1088). Royal Society of London. 1731:Jardine, Secord & Spary 1996 1695:Jardine, Secord & Spary 1996 1153:by William Smith, published 1815 521: 63: 2212: 2193: 2150: 2107: 2092:Hess, H. H. (1 November 1962). 2085: 2036: 2017: 2002: 1990: 1978: 1959: 1943: 1919: 1857: 1845: 1833: 1804: 1792: 1780: 1763: 1751: 1724: 1712: 1700: 1659: 1647: 1635: 1264: 1067: 910: 846: 758:; The diversity of the Earth's 219:Principle of lateral continuity 1608: 1583: 1570: 1557: 1531: 1516: 1490: 1478: 1190:, given charge of the coastal 1137:to the lower parts of his own 1076:Bust of William Smith, in the 690: 229:Principle of faunal succession 1: 2282:. Stanford University Press. 2250:Albritton, Claude C. (1980). 2063:Geological Society of Glasgow 2013:. London: Harper. p. 18. 1770:Eddy, Matthew Daniel (2008). 1471: 2309:Adams, Frank Dawson (1954). 2233:http://landsat.gsfc.nasa.gov 2032:: 185–195, 253–256, 305–309. 1523:Ben Waggoner (9 June 1996). 1273:had been developed. In 1911 641:and building materials like 581: 7: 3433:Neurology and neurosurgery 2636:Geological history of Earth 2572: 2351:Cultures of natural history 2222:, accessed 29 November 2006 1499:Chambers Science Factfinder 1434: 1306:Alfred Wegener, around 1925 1012:Horace-Bénédict de Saussure 339:Geological history of Earth 10: 3532: 2609: 2513:A Brief History of Geology 2511:O'Hara, Kieran D. (2018). 2242: 2235:, accessed 4 December 2006 2071:10.1144/transglas.18.3.559 1915:– via Darwin Online. 1095:assisted by his colleague 1034:Johan Gottschalk Wallerius 191:Laws, principles, theories 70:Science of the solid Earth 35:of a volcanic eruption of 17: 3456: 3403: 3370: 3322: 3269: 3231: 3155: 3099: 3088: 3059: 2973: 2947: 2876: 2838: 2785: 2759: 2723: 2690: 2650:Composition and structure 2649: 2621: 2603:Index of geology articles 2580: 2424:Bowler, Peter J. (2000). 2094:"History of Ocean Basins" 1905:10.1017/S0007087400027060 1333:published the concept of 1192:survey expedition of HMS 884:A New Theory of the Earth 858:A New Theory of the Earth 706:, hypothesizing that the 2492:Leddra, Michael (2010). 2464:Kooijmans, Luuc (2004). 1887:Herbert, Sandra (1991). 1451:Outline of Earth science 1243:On the Origin of Species 1101:École des Mines de Paris 839:of the mountains and by 199:Stratigraphic principles 18:Not to be confused with 3147:20th century in science 3142:19th century in science 2328:Gohau, Gabriel (1990). 2009:Holmes, Arthur (1913). 1446:History of paleontology 1441:History of geomagnetism 1314:proposed the theory of 1224:Cocos (Keeling) Islands 982:inferred from the Bible 696:Abu al-Rayhan al-Biruni 3067:Theories and sociology 1680:, pp. 4 & 96. 1429:U.S. Geological Survey 1367:Earth's magnetic field 1307: 1162: 1154: 1080: 995: 956: 952:Abraham Gottlob Werner 926: 887:published in 1696, by 861: 39: 3127:Scientific Revolution 2899:Environmental geology 2496:. Chichester: Wiley. 1949:Keynes, Richard ed.. 1305: 1203:Principles of Geology 1180:Principles of Geology 1160: 1148: 1085:Industrial Revolution 1075: 918: 854: 30: 3380:Agricultural science 3132:Age of Enlightenment 2858:Planetary geophysics 2331:A history of geology 2280:The Age of the Earth 2011:The Age of the Earth 1987:, pp. 14–17, 38 1565:The Earth We Live On 1283:The Age of the Earth 988:, who published his 978:history of the Earth 621:. He described many 586:In the year 540 BC, 214:Law of superposition 3418:Veterinary medicine 3112:Classical Antiquity 2960:Petroleum geologist 2924:Forensic geophysics 2894:Engineering geology 2641:Timeline of geology 2593:Glossary of geology 2298:Adams, Frank Dawson 2276:Dalrymple, G. Brent 2171:1965Natur.207..343W 2128:1963Natur.198..849H 1461:Timeline of geology 1456:Humboldtian science 1337:. Soon after this, 1214:grew from fringing 1097:Alexandre Brogniart 974:Histoire Naturelle, 954:published the book 708:Indian subcontinent 679:by recognising the 595:origin of the Earth 358:Branches of geology 297:Landform structures 178:Geologic time scale 3511:History of geology 3053:History of science 2986:Geology portal 2914:Geologic modelling 2853:Geophysical survey 2805:Geodetic astronomy 2731:Structural geology 2692:Historical geology 2623:History of geology 2598:History of geology 2588:Outline of geology 2311:1990 Dover reprint 1863:Second J A (1986) 1830:, pp. 104–107 1502:. Chambers. 2006. 1347:seafloor spreading 1308: 1287:radiometric dating 1271:radiometric dating 1163: 1155: 1149:Geological map of 1127:Roderick Murchison 1081: 927: 862: 652:Much later in the 613:, the philosopher 568:history of geology 528:Geology portal 448:By planet and body 316:Structural Geology 288:Structure of Earth 40: 20:Historical geology 3498: 3497: 3390:Materials science 3352:Political science 3117:Medieval European 3019: 3018: 2904:Planetary geology 2820:Planetary geodesy 2503:978-1-4051-9908-7 2477:978-90-351-2673-2 2437:978-0-393-32080-0 2407:978-1-86239-234-2 2360:978-0-521-55894-5 2341:978-0-8135-1666-0 2252:The Abyss of Time 1801:, pp. 95–96. 1697:, pp. 212–4. 1666:Wyse Jackson 2007 1601:978-92-3-102719-2 1580:. Book 1, Part 14 1359:continental crust 1351:mantle convection 1327:mantle convection 1316:continental drift 1238:natural selection 802:Taihang Mountains 728:(which he called 700:Muslim geologists 564: 563: 428:Planetary geology 380:Geological survey 3523: 3491: 3487: 3486: 3479: 3475: 3464: 3463: 3385:Computer science 3233:Natural sciences 3198:Medieval Islamic 3094: 3046: 3039: 3032: 3023: 3022: 3007: 3006: 2995: 2994: 2984: 2983: 2919:Forensic geology 2889:Economic geology 2815:Gravity of Earth 2710:Paleoclimatology 2615: 2567: 2560: 2553: 2544: 2543: 2516: 2507: 2488: 2486: 2484: 2460: 2441: 2411: 2390: 2378: 2369:Woods, Thomas E. 2364: 2345: 2324: 2307: 2293: 2271: 2255: 2236: 2229: 2223: 2216: 2210: 2209: 2197: 2191: 2190: 2179:10.1038/207343a0 2165:(4995): 343–47. 2154: 2148: 2147: 2136:10.1038/198849a0 2122:(4884): 849–65. 2111: 2105: 2104: 2098: 2089: 2083: 2082: 2052: 2040: 2034: 2033: 2021: 2015: 2014: 2006: 2000: 1994: 1988: 1982: 1976: 1975: 1963: 1957: 1947: 1941: 1935: 1929: 1923: 1917: 1916: 1884: 1875: 1861: 1855: 1849: 1843: 1837: 1831: 1825: 1814: 1808: 1802: 1796: 1790: 1784: 1778: 1777: 1767: 1761: 1755: 1749: 1743: 1734: 1728: 1722: 1716: 1710: 1704: 1698: 1692: 1681: 1675: 1669: 1663: 1657: 1651: 1645: 1639: 1633: 1627: 1618: 1612: 1606: 1605: 1587: 1581: 1574: 1568: 1561: 1555: 1554: 1535: 1529: 1528: 1520: 1514: 1513: 1494: 1488: 1482: 1413:Lunar geologists 1379:transform faults 1357:is younger than 1335:mid-ocean ridges 1279:Imperial College 1255:age of the Earth 1186:In 1831 Captain 1175:William Buckland 1008:Jean-André Deluc 998: 959: 831:in a geological 789:, deposition of 726:natural sciences 704:geology of India 556: 549: 542: 526: 525: 330:Geologic history 67: 42: 41: 33:William Hamilton 3531: 3530: 3526: 3525: 3524: 3522: 3521: 3520: 3501: 3500: 3499: 3494: 3482: 3470: 3452: 3399: 3366: 3324:Social sciences 3318: 3265: 3227: 3151: 3095: 3086: 3055: 3050: 3020: 3015: 2978: 2969: 2943: 2939:Mineral physics 2872: 2834: 2781: 2755: 2741:Plate tectonics 2719: 2715:Palaeogeography 2686: 2662:Crystallography 2645: 2617: 2616: 2607: 2576: 2571: 2524: 2519: 2504: 2482: 2480: 2478: 2457: 2438: 2419: 2417:Further reading 2414: 2408: 2387: 2361: 2342: 2321: 2290: 2268: 2256: 2245: 2240: 2239: 2230: 2226: 2217: 2213: 2198: 2194: 2155: 2151: 2112: 2108: 2096: 2090: 2086: 2050: 2041: 2037: 2022: 2018: 2007: 2003: 1995: 1991: 1983: 1979: 1964: 1960: 1948: 1944: 1936: 1932: 1924: 1920: 1885: 1878: 1862: 1858: 1850: 1846: 1838: 1834: 1826: 1817: 1809: 1805: 1797: 1793: 1785: 1781: 1768: 1764: 1756: 1752: 1744: 1737: 1729: 1725: 1717: 1713: 1705: 1701: 1693: 1684: 1676: 1672: 1664: 1660: 1652: 1648: 1640: 1636: 1628: 1621: 1613: 1609: 1602: 1588: 1584: 1575: 1571: 1562: 1558: 1551: 1537: 1536: 1532: 1521: 1517: 1510: 1496: 1495: 1491: 1483: 1479: 1474: 1437: 1397: 1339:Robert S. Dietz 1331:Bruce C. Heezen 1320:plate tectonics 1267: 1129:, mapping into 1125:Period; whilst 1070: 913: 889:William Whiston 849: 773:(1031–1095), a 754:; Formation of 693: 677:crystallography 658:Pliny the Elder 584: 560: 520: 513: 512: 511: 452: 444: 430: 420: 419: 418: 393: 385: 384: 371: 353: 345: 344: 343: 334: 326: 325: 301: 293: 292: 263: 255: 253: 245: 244: 243: 204: 194: 192: 184: 183: 182: 158:Plate tectonics 153: 118: 110: 72: 23: 12: 11: 5: 3529: 3519: 3518: 3513: 3496: 3495: 3493: 3492: 3480: 3468: 3457: 3454: 3453: 3451: 3450: 3445: 3440: 3435: 3430: 3425: 3420: 3415: 3413:Human medicine 3409: 3407: 3401: 3400: 3398: 3397: 3392: 3387: 3382: 3376: 3374: 3368: 3367: 3365: 3364: 3359: 3354: 3349: 3344: 3339: 3334: 3328: 3326: 3320: 3319: 3317: 3316: 3311: 3306: 3301: 3296: 3291: 3286: 3281: 3275: 3273: 3267: 3266: 3264: 3263: 3258: 3253: 3248: 3243: 3237: 3235: 3229: 3228: 3226: 3225: 3220: 3215: 3210: 3205: 3200: 3195: 3190: 3185: 3180: 3175: 3170: 3165: 3159: 3157: 3153: 3152: 3150: 3149: 3144: 3139: 3134: 3129: 3124: 3119: 3114: 3109: 3103: 3101: 3097: 3096: 3089: 3087: 3085: 3084: 3079: 3074: 3072:Historiography 3069: 3063: 3061: 3057: 3056: 3049: 3048: 3041: 3034: 3026: 3017: 3016: 3014: 3013: 3001: 2989: 2974: 2971: 2970: 2968: 2967: 2962: 2957: 2951: 2949: 2945: 2944: 2942: 2941: 2936: 2934:Mining geology 2931: 2926: 2921: 2916: 2911: 2906: 2901: 2896: 2891: 2886: 2880: 2878: 2874: 2873: 2871: 2870: 2868:Tectonophysics 2865: 2860: 2855: 2850: 2844: 2842: 2836: 2835: 2833: 2832: 2830:Geopositioning 2827: 2825:Remote sensing 2822: 2817: 2812: 2807: 2802: 2797: 2791: 2789: 2783: 2782: 2780: 2779: 2777:Marine geology 2774: 2769: 2763: 2761: 2757: 2756: 2754: 2753: 2748: 2743: 2738: 2733: 2727: 2725: 2721: 2720: 2718: 2717: 2712: 2707: 2702: 2696: 2694: 2688: 2687: 2685: 2684: 2679: 2674: 2669: 2664: 2659: 2657:Cosmochemistry 2653: 2651: 2647: 2646: 2644: 2643: 2638: 2633: 2627: 2625: 2619: 2618: 2610: 2608: 2606: 2605: 2600: 2595: 2590: 2584: 2582: 2578: 2577: 2570: 2569: 2562: 2555: 2547: 2541: 2540: 2523: 2522:External links 2520: 2518: 2517: 2508: 2502: 2489: 2476: 2461: 2456:978-1862392274 2455: 2442: 2436: 2420: 2418: 2415: 2413: 2412: 2406: 2391: 2385: 2365: 2359: 2346: 2340: 2325: 2319: 2294: 2288: 2272: 2266: 2246: 2244: 2241: 2238: 2237: 2224: 2211: 2192: 2149: 2106: 2084: 2044:Holmes, Arthur 2035: 2016: 2001: 1997:Dalrymple 1994 1989: 1985:Dalrymple 1994 1977: 1958: 1942: 1930: 1918: 1899:(2): 159–192. 1876: 1856: 1844: 1832: 1828:Albritton 1980 1815: 1803: 1799:Albritton 1980 1791: 1789:, p. 209. 1779: 1762: 1760:, p. 219. 1750: 1735: 1733:, p. 232. 1723: 1711: 1699: 1682: 1670: 1658: 1654:Kooijmans 2004 1646: 1644:, p. 114. 1634: 1632:, p. 118. 1619: 1607: 1600: 1582: 1569: 1556: 1549: 1530: 1515: 1508: 1489: 1476: 1475: 1473: 1470: 1469: 1468: 1463: 1458: 1453: 1448: 1443: 1436: 1433: 1409:Gene Shoemaker 1396: 1395:Modern geology 1393: 1388:Edward Bullard 1363:paleomagnetism 1312:Alfred Wegener 1266: 1263: 1207:uniformitarian 1199:Charles Darwin 1188:Robert FitzRoy 1093:Georges Cuvier 1069: 1066: 1038:Abraham Werner 1036:and Germany's 972:published his 912: 909: 848: 845: 810:climate change 739:Kitab al-Shifa 734:Ikhwan AI-Safa 692: 689: 599:Ancient Greece 583: 580: 562: 561: 559: 558: 551: 544: 536: 533: 532: 531: 530: 515: 514: 510: 509: 504: 499: 494: 489: 484: 479: 474: 469: 464: 459: 453: 451: 450: 443: 442: 437: 431: 426: 425: 422: 421: 417: 416: 411: 406: 401: 395: 394: 391: 390: 387: 386: 383: 382: 377: 370: 369: 360: 354: 351: 350: 347: 346: 342: 341: 335: 333: 332: 324: 323: 318: 313: 308: 302: 300: 299: 291: 290: 285: 280: 275: 270: 264: 262: 261: 254: 251: 250: 247: 246: 242: 241: 236: 231: 226: 221: 216: 211: 205: 203: 202: 193: 190: 189: 186: 185: 181: 180: 175: 170: 165: 160: 154: 152: 151: 146: 140: 135: 126: 120: 119: 117:Key components 116: 115: 112: 111: 109: 108: 98: 93: 88: 83: 77: 74: 73: 68: 60: 59: 51: 50: 37:Mount Vesuvius 9: 6: 4: 3: 2: 3528: 3517: 3514: 3512: 3509: 3508: 3506: 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2628: 2626: 2624: 2620: 2614: 2604: 2601: 2599: 2596: 2594: 2591: 2589: 2586: 2585: 2583: 2579: 2575: 2568: 2563: 2561: 2556: 2554: 2549: 2548: 2545: 2539: 2535: 2534: 2529: 2528:Early Geology 2526: 2525: 2514: 2509: 2505: 2499: 2495: 2490: 2479: 2473: 2469: 2468: 2462: 2458: 2452: 2448: 2443: 2439: 2433: 2429: 2428: 2422: 2421: 2409: 2403: 2399: 2398: 2392: 2388: 2386:0-89526-038-7 2382: 2377: 2376: 2370: 2366: 2362: 2356: 2352: 2347: 2343: 2337: 2333: 2332: 2326: 2322: 2316: 2312: 2305: 2304: 2299: 2295: 2291: 2289:0-8047-2331-1 2285: 2281: 2277: 2273: 2269: 2263: 2259: 2253: 2248: 2247: 2234: 2228: 2221: 2215: 2207: 2203: 2196: 2188: 2184: 2180: 2176: 2172: 2168: 2164: 2160: 2153: 2145: 2141: 2137: 2133: 2129: 2125: 2121: 2117: 2110: 2102: 2095: 2088: 2080: 2076: 2072: 2068: 2064: 2060: 2056: 2049: 2045: 2039: 2031: 2027: 2020: 2012: 2005: 1998: 1993: 1986: 1981: 1973: 1969: 1962: 1956: 1952: 1946: 1940:, p. 226 1939: 1934: 1928:, p. 145 1927: 1922: 1914: 1910: 1906: 1902: 1898: 1894: 1890: 1883: 1881: 1874: 1873:0-691-02441-3 1870: 1866: 1860: 1854:, p. 144 1853: 1848: 1842:, p. 216 1841: 1836: 1829: 1824: 1822: 1820: 1813:, p. 239 1812: 1807: 1800: 1795: 1788: 1783: 1775: 1774: 1766: 1759: 1754: 1747: 1742: 1740: 1732: 1727: 1721:, p. 92. 1720: 1715: 1709:, p. 88. 1708: 1703: 1696: 1691: 1689: 1687: 1679: 1674: 1667: 1662: 1655: 1650: 1643: 1638: 1631: 1626: 1624: 1617:, p. 96. 1616: 1611: 1603: 1597: 1593: 1586: 1579: 1573: 1566: 1563:Moore, Ruth. 1560: 1552: 1550:9781444323269 1546: 1542: 1541: 1534: 1526: 1519: 1511: 1509:9780550101488 1505: 1501: 1500: 1493: 1486: 1481: 1477: 1467: 1464: 1462: 1459: 1457: 1454: 1452: 1449: 1447: 1444: 1442: 1439: 1438: 1432: 1430: 1426: 1422: 1416: 1414: 1410: 1406: 1402: 1392: 1389: 1384: 1380: 1376: 1372: 1371:S. K. Runcorn 1368: 1364: 1360: 1356: 1355:oceanic crust 1352: 1348: 1344: 1343:Harry H. Hess 1340: 1336: 1332: 1328: 1323: 1321: 1317: 1313: 1304: 1300: 1297: 1293: 1292:Geochronology 1288: 1284: 1280: 1276: 1275:Arthur Holmes 1272: 1262: 1260: 1256: 1251: 1247: 1245: 1244: 1240:published in 1239: 1235: 1231: 1230: 1225: 1222:surveyed the 1221: 1217: 1213: 1208: 1204: 1200: 1196: 1195: 1189: 1184: 1181: 1176: 1172: 1168: 1167:catastrophism 1159: 1152: 1151:Great Britain 1147: 1143: 1140: 1136: 1132: 1128: 1124: 1120: 1119:Charles Lyell 1116: 1112: 1111:Adam Sedgwick 1107: 1102: 1098: 1094: 1090: 1089:William Smith 1086: 1079: 1074: 1065: 1063: 1059: 1055: 1051: 1047: 1043: 1039: 1035: 1031: 1025: 1023: 1022:Denis Diderot 1019: 1018: 1013: 1009: 1003: 1000: 997: 992: 987: 986:Immanuel Kant 983: 979: 975: 971: 965: 962: 958: 953: 949: 944: 940: 936: 932: 924: 921: 917: 908: 906: 902: 901:Nicolas Steno 898: 892: 890: 886: 885: 880: 876: 872: 868: 860: 859: 853: 844: 842: 838: 834: 830: 826: 822: 818: 815: 811: 807: 806:Pacific Ocean 803: 800:found in the 799: 796: 792: 788: 784: 780: 779:geomorphology 776: 772: 768: 763: 761: 757: 753: 749: 745: 741: 740: 735: 731: 727: 723: 719: 715: 713: 709: 705: 701: 697: 688: 686: 682: 678: 674: 671: 667: 663: 659: 655: 650: 648: 644: 640: 636: 632: 628: 624: 620: 616: 612: 607: 604: 600: 596: 591: 589: 579: 577: 573: 569: 557: 552: 550: 545: 543: 538: 537: 535: 534: 529: 524: 519: 518: 517: 516: 508: 505: 503: 500: 498: 495: 493: 490: 488: 485: 483: 480: 478: 475: 473: 470: 468: 465: 463: 460: 458: 455: 454: 449: 446: 445: 441: 438: 436: 433: 432: 429: 424: 423: 415: 412: 410: 407: 405: 402: 400: 397: 396: 389: 388: 381: 378: 376: 373: 372: 368: 364: 361: 359: 356: 355: 349: 348: 340: 337: 336: 331: 328: 327: 322: 319: 317: 314: 312: 309: 307: 306:Geomorphology 304: 303: 298: 295: 294: 289: 286: 284: 281: 279: 278:Sedimentology 276: 274: 271: 269: 266: 265: 260: 257: 256: 249: 248: 240: 239:Walther's law 237: 235: 232: 230: 227: 225: 222: 220: 217: 215: 212: 210: 207: 206: 201: 200: 196: 195: 188: 187: 179: 176: 174: 171: 169: 166: 164: 161: 159: 156: 155: 150: 147: 144: 141: 139: 136: 134: 130: 127: 125: 122: 121: 114: 113: 106: 102: 99: 97: 94: 92: 89: 87: 84: 82: 79: 78: 76: 75: 71: 66: 62: 61: 58: 57: 53: 52: 48: 44: 43: 38: 34: 29: 25: 21: 16: 3428:Neuroscience 3332:Anthropology 3314:Trigonometry 3008: 2996: 2977: 2877:Applications 2848:Geomagnetism 2772:Hydrogeology 2705:Paleontology 2700:Stratigraphy 2667:Geochemistry 2622: 2597: 2532: 2512: 2493: 2481:. Retrieved 2466: 2446: 2426: 2396: 2374: 2350: 2330: 2310: 2302: 2279: 2258:1986 reprint 2257: 2251: 2227: 2214: 2205: 2201: 2195: 2162: 2158: 2152: 2119: 2115: 2109: 2100: 2087: 2058: 2054: 2038: 2029: 2025: 2019: 2010: 2004: 1999:, p. 74 1992: 1980: 1971: 1967: 1961: 1950: 1945: 1933: 1921: 1896: 1892: 1864: 1859: 1847: 1835: 1806: 1794: 1782: 1772: 1765: 1753: 1748:, p. 8. 1726: 1714: 1702: 1673: 1661: 1649: 1637: 1610: 1591: 1585: 1577: 1572: 1564: 1559: 1539: 1533: 1518: 1498: 1492: 1480: 1417: 1398: 1324: 1309: 1282: 1268: 1265:20th century 1252: 1248: 1241: 1227: 1219: 1212:coral atolls 1202: 1193: 1185: 1179: 1164: 1134: 1106:stratigraphy 1082: 1068:19th century 1054:James Hutton 1026: 1017:Encyclopédie 1015: 1004: 989: 973: 966: 960: 928: 923:James Hutton 911:18th century 905:stratigraphy 893: 882: 863: 856: 847:17th century 787:soil erosion 764: 737: 729: 716: 694: 651: 618: 615:Theophrastus 608: 592: 585: 567: 565: 447: 392:Applications 374: 329: 296: 268:Geochemistry 258: 197: 100: 69: 54: 24: 15: 3395:Engineering 3337:Archaeology 3304:Probability 3271:Mathematics 3137:Romanticism 3122:Renaissance 2948:Occupations 2929:Meteoritics 2795:Cartography 2751:Volcanology 2736:Geodynamics 2533:In Our Time 2065:: 559–606. 1840:Bowler 2000 1578:Meteorology 1576:Aristotle. 1487:, p. 7 1383:fault types 1375:Tuzo Wilson 1216:coral reefs 1171:Great Flood 1032:, Sweden's 1030:John Walker 783:sedimentary 767:naturalists 752:earthquakes 710:was once a 691:Middle Ages 399:Engineering 321:Volcanology 259:Composition 143:Metamorphic 138:Sedimentary 3516:Geologists 3505:Categories 3372:Technology 3357:Psychology 3309:Statistics 3156:By culture 3060:Background 2909:Geobiology 2884:Biogeology 2863:Seismology 2840:Geophysics 2767:Glaciology 2672:Mineralogy 2483:10 January 2320:048626372X 2267:087477389X 1938:Adams 1938 1926:Gohau 1990 1852:Gohau 1990 1811:Adams 1938 1787:Adams 1938 1776:. Ashgate. 1758:Gohau 1990 1746:Gohau 1990 1719:Gohau 1990 1707:Gohau 1990 1678:Woods 2005 1642:Gohau 1990 1630:Gohau 1990 1615:Adams 1938 1485:Gohau 1990 1472:References 1050:Neptunists 841:deposition 730:Attabieyat 681:octahedral 670:fossilized 643:limestones 588:Xenophanes 311:Glaciology 273:Mineralogy 168:Weathering 3466:Timelines 3443:Pathology 3438:Nutrition 3362:Sociology 3342:Economics 3251:Chemistry 3241:Astronomy 3178:Byzantine 3173:Brazilian 3168:Argentine 2955:Geologist 2810:Geomatics 2677:Petrology 2581:Overviews 2079:122872384 1968:GSA Today 1913:143748414 1246:in 1859. 1234:evolution 1058:Plutonism 875:geography 843:of silt. 814:petrified 748:mountains 744:Aristotle 683:habit of 619:On Stones 603:Aristotle 582:Antiquity 409:Forensics 363:Geologist 283:Petrology 3489:Category 3448:Pharmacy 3405:Medicine 3294:Geometry 3284:Calculus 3203:Japanese 2371:(2005). 2300:(1938). 2278:(1994). 2046:(1931). 1435:See also 1427:and the 1310:In 1912 1139:Silurian 1135:Cambrian 1123:Tertiary 1117:Period, 1115:Cambrian 1062:volcanic 931:minerals 920:Scotsman 785:uplift, 775:polymath 771:Shen Kuo 756:minerals 722:polymath 718:Ibn Sina 656:period, 647:hardness 623:minerals 414:Military 352:Research 149:Sediment 124:Minerals 105:Timeline 96:Glossary 91:Category 47:a series 45:Part of 3423:Anatomy 3347:History 3279:Algebra 3261:Physics 3246:Biology 3223:Spanish 3218:Russian 3213:Mexican 3188:Chinese 3163:African 3010:Geology 2998:Geology 2787:Geodesy 2574:Geology 2536:at the 2243:Sources 2187:4294401 2167:Bibcode 2144:4209203 2124:Bibcode 1421:Landsat 1403:on the 1401:craters 1099:at the 1046:granite 837:erosion 833:stratum 825:Shaanxi 817:bamboos 798:fossils 760:terrain 685:diamond 631:Laurium 572:Geology 457:Mercury 375:Methods 173:Erosion 133:Igneous 101:History 86:Outline 56:Geology 3477:Portal 3208:Korean 3193:Indian 3183:French 3100:By era 2500:  2474:  2453:  2434:  2404:  2383:  2357:  2338:  2317:  2286:  2264:  2185:  2159:Nature 2142:  2116:Nature 2077:  1911:  1871:  1598:  1547:  1506:  1220:Beagle 1194:Beagle 1042:basalt 948:metals 939:mining 897:strata 871:Deluge 829:shells 821:Yan'an 795:marine 793:, and 662:metals 639:marble 635:Athens 611:Lyceum 507:Charon 497:Triton 404:Mining 252:Topics 163:Strata 3299:Logic 2760:Water 2183:S2CID 2140:S2CID 2097:(PDF) 2075:S2CID 2061:(3). 2051:(PDF) 1955:p. ix 1909:S2CID 1131:Wales 935:crust 867:Bible 673:resin 668:as a 666:amber 654:Roman 633:near 576:Earth 502:Pluto 492:Titan 482:Ceres 477:Vesta 462:Venus 367:List) 81:Index 2498:ISBN 2485:2012 2472:ISBN 2451:ISBN 2432:ISBN 2402:ISBN 2381:ISBN 2355:ISBN 2336:ISBN 2315:ISBN 2284:ISBN 2262:ISBN 1974:(1). 1869:ISBN 1596:ISBN 1545:ISBN 1504:ISBN 1425:NASA 1405:Moon 1341:and 1044:and 1010:and 943:ores 791:silt 769:was 627:ores 625:and 566:The 472:Mars 467:Moon 129:Rock 2538:BBC 2530:on 2206:258 2175:doi 2163:207 2132:doi 2120:198 2067:doi 1901:doi 1236:by 712:sea 3507:: 2313:. 2260:. 2204:. 2181:. 2173:. 2161:. 2138:. 2130:. 2118:. 2073:. 2059:18 2057:. 2053:. 2030:63 2028:. 1972:17 1970:. 1907:. 1897:24 1895:. 1891:. 1879:^ 1818:^ 1738:^ 1685:^ 1622:^ 1415:. 762:. 714:. 687:. 649:. 597:. 578:. 487:Io 49:on 3045:e 3038:t 3031:v 2566:e 2559:t 2552:v 2506:. 2487:. 2459:. 2440:. 2410:. 2389:. 2363:. 2344:. 2323:. 2292:. 2270:. 2189:. 2177:: 2169:: 2146:. 2134:: 2126:: 2081:. 2069:: 1903:: 1668:. 1656:. 1604:. 1553:. 1527:. 1512:. 999:) 993:( 555:e 548:t 541:v 365:( 145:) 131:( 107:) 103:( 22:.

Index

Historical geology

William Hamilton
Mount Vesuvius
a series
Geology

Index
Outline
Category
Glossary
History
Timeline
Minerals
Rock
Igneous
Sedimentary
Metamorphic
Sediment
Plate tectonics
Strata
Weathering
Erosion
Geologic time scale
Stratigraphic principles
Principle of original horizontality
Law of superposition
Principle of lateral continuity
Principle of cross-cutting relationships
Principle of faunal succession

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