There is a lot of information found both in prophecies and in recent writings and articles talking about Earth Changes, usually defined as catastrophic geological events such as earthquakes, volcanoes, polar shifts, flooding, and global warming. Many point to the shifting times and the moving into the Golden Age and to 2012 being a turning point in the history of mankind. The research and sometimes channeled material presented, probably with the best of intentions, often still carries elements of our own subconscious fears but is it only fear based material or is there something to this predictions of Earth Changes?

Read more here: » Earth Changes - Will there be dramatic Geological and Political changes the coming years until 2012?

Including:

• Triassic - Triassic naming
• Triassic - Triassic dating and subdivisions
• Triassic - Triassic paleogeography
• Triassic - Triassic climate
• Triassic - Triassic lifeforms
• Triassic - Triassic Lagerstätten
• Triassic - Late Triassic extinction event
• Triassic - Sources

Read more here: » Triassic: Encyclopedia - Triassic

Geology of the British Isles - Proterozoic Era. The Gneisses, the oldest rocks in Britain or Ireland, date from at least 2,700 Ma (Ma = millions of years ago) in the Archean period of this era, the Earth itself being only about 4,600 Ma old. They are found in the far north west of Scotland and in the Hebrides, with a few small outcrops elsewhere. Formed from rock originally deposited at the surface of the planet, the rocks were later buried d ...

See also:

Geology of the British Isles, Geology of the British Isles - Geological history, Geology of the British Isles - Proterozoic Era, Geology of the British Isles - Paleozoic Era, Geology of the British Isles - Mesozoic Era, Geology of the British Isles - Cenozoic Era, Geology of the British Isles - Geological features, Geology of the British Isles - Geological resources, Geology of the British Isles - Events, Geology of the British Isles - Institutions, Geology of the British Isles - People, Geology of the British Isles - Awards

Read more here: » Geology of the British Isles: Encyclopedia II - Geology of the British Isles - Geological history

The Brunhes-Matuyama Reversal was a geologic event approximately 780,000 years ago when the Earth's magnetic field last underwent reversal. The event is useful in dating ocean sediment cores. Other related archivesEarth's, geologic, magnetic field

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Cataclysmic geology is the study of the unusual and rare geologic events that have profound effects on the planet and often happen very rapidly or instantaneously. Most geological processes follow James Hutton's theory of uniformity of causes, which has historically led to skepticism about cataclysmic events. Recent research has shown that while most processes are uniform, time has been punctuated by very rapid, very destructive events. Some examples of cataclysmic geological events are: Caldera eruptions Glacial lake releases Impact events Large-ma ...

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The Capitanian is a stage on the geologic time scale occurring from 265.8 ± 0.7 Ma to 260.4 ± 0.7 Ma (million years ago). It is the last stage of the Guadalupian epoch. A significant mass extinction event occurred at the end of this stage which may be related to the much larger Permian-Triassic extinction event that followed about 10 million years later. ...

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The Permian is a geologic period that extends from about 299.0 Ma to 248.0 Ma (million years before the present; ICS 2004). It is the last period of the Palaeozoic Era. As with most older geologic periods, the strata that define the Permian are well identified, but the exact date of the period's start is uncertain by a few million years. The Permian follows the Carboniferous (Pennsylvanian in North America) and is followed by the Triassic. The end of the period is marked by a major extinction event, called the Permian-Triassic extinct ...

Including:

• Permian - Subdivisions
• Permian - Oceans
• Permian - Permian-Triassic extinction event
• Permian - Life
• Permian - Paleogeography

Read more here: » Permian: Encyclopedia - Permian

Mundane Astrology is the application of astrology to world affairs and world events, taking its name from the Roman word Mundus, meaning "the World". Mundane astrology is branch of Judicial astrology and is widely believed by astrological historians to be the most ancient branch of astrology. Many modern and ancient mundane astrologers believe correlations exist between geological phenomena (such as earthquakes, volcanic eruptions, etc.) and astronomical phenomena (the ...

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The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443.7 Ma (million years ago), to the beginning of the Devonian period, about 416.0 Ma (ICS 2004). As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by 5-10 million years. The base of the Silurian is set at a major extinction event where 60% of marine species were wiped out. See Ordov ...

Including:

• Silurian - Historiography
• Silurian - Silurian subdivisions
• Silurian - Silurian paleogeography
• Silurian - Silurian biota
• Silurian - Source

Read more here: » Silurian: Encyclopedia - Silurian

Catastrophism is the theory that Earth has been affected by sudden, short-lived, violent events that were sometimes worldwide in scope. The dominant paradigm of geology has been gradualism, but a more inclusive and integrated view of geologic events has developed. Before gradualism, the dominant belief in many cultures of the creation and development of the world was essentially catastrophism. The biblical story of the Great Flood is a prime example of these beliefs. Earth's history was viewed as the result of an accumulation o ...

Including:

• Catastrophism - Reference

Read more here: » Catastrophism: Encyclopedia - Catastrophism

The Cenozoic Era (sen-oh-ZOH-ik; sometimes Caenozoic Era in the United Kingdom) meaning "new life" (Greek kaino = new + zoikos = life) is the most recent of the four classic geological eras. It covers the 65.5 million years since the Cretaceous-Tertiary extinction event at the end of the Cretaceous that marked the demise of the last dinosaurs and the end of the Mesozoic Era. The Cenozoic era is ongoing. The Cenozoic is divided into two periods, the Palaeogene and Neogene, and they are in turn divided into e ...

Including:

• Cenozoic - References and further reading

Read more here: » Cenozoic: Encyclopedia - Cenozoic

The Eocene epoch (56-34 Ma) is a major division of the geologic timescale and the second epoch of the Palaeogene period in the Cenozoic era. The Eocene spans the time from the end of the Paleocene epoch to the beginning of the Oligocene epoch. The start of the Eocene is marked by the emergence of the first modern mammals. The end is set at a major extinction event that may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. Still, as with other other geologic periods, the strata that define the start and end of the epoch are well identified, ...

Including:

• Eocene - Eocene subdivisions
• Eocene - Eocene climate
• Eocene - Eocene paleogeography
• Eocene - Eocene flora
• Eocene - Eocene fauna
• Eocene - Eocene oceans

Read more here: » Eocene: Encyclopedia - Eocene

The Paleocene epoch (65-56 MYA) ("early dawn of the recent") is the first geologic epoch of the Palaeogene period in the modern Cenozoic era. As with most other older geologic periods, the strata that define the epoch's beginning and end are well identified, but the exact date of the end is uncertain. The Paleocene epoch immediately followed the mass extinction event at the end of the Cretaceous, known as the K-T boundary (Cretaceous - Tertiary), which marks the demise of the dinosaurs. The die-off of the dinosaurs left unfille ...

Including:

• Paleocene - Paleocene subdivisions
• Paleocene - Paleocene climate
• Paleocene - Paleocene paleogeography
• Paleocene - Paleocene flora
• Paleocene - Paleocene fauna
• Paleocene - Mammals
• Paleocene - Reptiles
• Paleocene - Birds
• Paleocene - Paleocene oceans

Read more here: » Paleocene: Encyclopedia - Paleocene

These pages contain the trends of millennia and centuries. The individual century pages contain lists of decades and years. See history for different organizations of historical events. See calendar and list of calendars for other groupings of years. For earlier time periods, see cosmological timeline, geologic timescale, evolutionary timeline, pleistocene, and logarithmic timeline. Paleolithic 10th millennium BC | 9th millennium BC | 8th millennium BC 7th millennium BC ...

Read more here: » Centuries: Encyclopedia - Centuries

The Pleistocene Epoch is part of the geologic timescale. The name of the pleistocene is derived from the Greek pleistos (most) and ceno (new). The Pleistocene follows the Pliocene epoch and is followed by the Holocene epoch. The Pleistocene is the third epoch of the Neogene period or 6th epoch of the Cenozoic era. The end of the Pleistocene corresponds with the end of the ...

Including:

• Pleistocene - Pleistocene dating
• Pleistocene - Pleistocene paleogeography and climate
• Pleistocene - Glacial features
• Pleistocene - Major events
• Pleistocene - Palaeocycles
• Pleistocene - Pleistocene fauna
• Pleistocene - Pleistocene deposits

Read more here: » Pleistocene: Encyclopedia - Pleistocene

The cataclysm is the Greek expression for the Biblical Great Flood of Noah, from the Greek kataklysmos, to "wash down." Erudite Bible studies drew it into the English language in 1633. A cataclysm is merely one kind of catastrophe, best used when confined to a geological phenomenon of planetary significance. As with many words of apocalyptic Biblical resonance, the adoption of cataclysm for featur ...

Including:

• Cataclysm - Uses in modern-era creative works

Read more here: » Cataclysm: Encyclopedia - Cataclysm

Cosmogenic isotopes are rare radioactive isotopes created when cosmic radiation interacts with an atomic nucleus. These isotopes are produced on Earth, in Earth's atmosphere, and in extraterrestrial items such as meteorites. Some cosmogenic isotopes include: helium-3 beryllium-10 carbon-14 neon-21 aluminum-26 chlorine-36 calcium-41 iodine-129 Cosmogenic isotope - Applications. Because cosmogenic isotopes have l ...

Including:

• Cosmogenic isotope - Applications

Read more here: » Cosmogenic isotope: Encyclopedia - Cosmogenic isotope

Within scientific philosophy, uniformitarianism is the principle in which one assumes that the same processes that shaped the Universe occurred then as they do now, unless there is good evidence otherwise. Or in other words, certain natural laws are unchangeable. Although most synonymous with geology, other sciences on a similar timescale also employ this principle, such as astronomy or evolutionary biology. Uniformitarianism science - Geology. Uniformitarianism is one of the most basic principles o ...

Including:

• Uniformitarianism science - Geology

Read more here: » Uniformitarianism science: Encyclopedia - Uniformitarianism science

The Miocene epoch is a period of time that extends from about 23 to 5.3 million years before the present. As with other older geologic periods, the rock beds that define the start and end are well identified, but the exact dates of the start and end of the period are uncertain. The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words meion (less) and ceno (new) and means "less recent" because it has 18% (less than the Pliocene) of modern sea invertebrates. The Miocene follows the Oligocene Epoch and is followed by the Pliocene Epoch. The Mio ...

Including:

• Miocene - Miocene Subdivisions
• Miocene - Miocene Climate
• Miocene - Miocene Paleogeography
• Miocene - Miocene Flora
• Miocene - Miocene Fauna
• Miocene - Mammals
• Miocene - Birds
• Miocene - Miocene Oceans
• Miocene - External References

Read more here: » Miocene: Encyclopedia - Miocene

The beginning of the Holocene corresponds with the beginning of the Mesolithic age in most of Europe; but in regions such as the Middle East and Anatolia with a very early neolithisation, Epipaleolithic is preferred in place of Mesolithic. Cultures in this period include: Hamburgian, Federmesser, and the Natufian culture. Both are followed by the aceramic Neolithic (Pre-Pottery Neolithic A and Pre- ...

See also:

Holocene, Holocene - Geology, Holocene - Climate, Holocene - Human developments

Read more here: » Holocene: Encyclopedia II - Holocene - Human developments