Tertiary Age.

See GEOLOGICAL ERAS

(See also: Tertiary Age, Mysticism, Mysticism Dictionary, Body mind and Soul)

See also:

Geology of Hertfordshire, Geology of Hertfordshire - The Cretaceous, Geology of Hertfordshire - The Tertiary, Geology of Hertfordshire - The Ice Age

Read more here: » Geology of Hertfordshire: Encyclopedia II - Geology of Hertfordshire - The Tertiary

On the northern boundary and just inside the county, at the foot of the chalk Chiltern Hills, near Tring and Ashwell, there is a small strip of exposed Cretaceous Gault Clay and Upper Greensand. At 100 million years old, these are the oldest rocks in the county. Rocks get progressively younger as one moves in a south easterly direction through the county. The lowest layer of the chalk is the Chalk Marl, which, with the Totternhoe Clunch Stone above it, lies at the base of the Chiltern Hills escarpment. This is visible as a terra ...

See also:

Geology of Hertfordshire, Geology of Hertfordshire - The Cretaceous, Geology of Hertfordshire - The Tertiary, Geology of Hertfordshire - The Ice Age

Read more here: » Geology of Hertfordshire: Encyclopedia II - Geology of Hertfordshire - The Cretaceous

Saint Catherine of Siena (Siena, Italy, March 25, 1347 – April 29, 1380 in Rome) was a Dominican Tertiary or lay-affiliate of the Dominican Order. Catherine was the 23rd child out of 25 (her twin, the 24th, died at birth); her parents were Giacomo di Benincasa, a cloth-dyer, and his wife, Lapa. At the age of seven she consecrated her virginity to Christ; in her sixteenth year she took the habit of the Dominican Tertiaries. As a tertiary, Catherine lived at home rather than in a convent, and she practiced austerities there which a pr ...

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The Mesozoic is one of three geologic eras of the Phanerozoic eon. The division of time into eras dates back to Giovanni Arduino in the 18th century, although his original name for the era now called the Mesozoic was "Secondary" (see Tertiary.) Mesozoic gets its name from the Greek meso (middle) and zoo (animals) and is often called the "Age of Medieval Life." The Mesozoic includes three geologic periods: from oldest to youngest, they are the Triassic, the Jurassic and the Cretaceous periods. It extended from roug ...

Including:

• Mesozoic - References and further reading

Read more here: » Mesozoic: Encyclopedia - Mesozoic

Christ's College, Canterbury was founded in 1850 as an independent (tertiary) college and a boys' grammar school. Now it is a mixed day and boarding school in Christchurch, New Zealand for boys aged 13 (Form III or Year 9) to 18 (Form VII or Year 13). It is named after Christ's College, Cambridge where the Canterbury provincial superintendent JE Fitzgerald had studied. Its most famous alumnus is Captain Charles Upham who was awarded the Victoria Cross twice. Michael Cullen, Minister for Finance is also an Old Boy. However, his association with the school is minimal. College has produce ...

Including:

• Christ's College Canterbury - Upper department College House University of Canterbury

Read more here: » Christ's College Canterbury: Encyclopedia - Christ's College Canterbury

Classical education as understood and taught in the middle ages of western civilization is roughly based on the ancient Greek concept of Paideia. China had a completely different tradition of classical education, based in large part on Confucian and Taoist traditions. This article concerns the western tradition. Classical education - The overall organization. Classical education developed many of the terms now used to describe modern education. Western classical education has three phases, eac ...

Including:

• Classical education - The overall organization
• Classical education - Primary Education
• Classical education - Secondary Education
• Classical education - Tertiary Education
• Classical education - Modern Interpretations of Classical Education

Read more here: » Classical education: Encyclopedia - Classical education

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

A coal measure (stratigraphic unit) is the name given to any rock sequence that occurs in the upper part of the Carboniferous System in Europe. It is equivalent to the Pennsylvanian of North America. These rocks are typically coal-bearing. The term coal measure is also used to describe a succession of sedimentary rocks comprising of claystones, shales, siltstones, sandstones, conglomerates, and limestones that are interstratified with beds of coal. Such succession occur worldwide and may not necessarily be Carboniferous in age (such as the Permian coal measures of Australia and the late Cretaceous and ...

Including:

• Coal measure - References and further reading

Read more here: » Coal measure: Encyclopedia - Coal measure

Archosaurs (Greek for "ruling reptiles") are a group of diapsid reptiles that first evolved from Archosauriform ancestors during the Olenekian (Lower Triassic). Archosaurs are set apart by having socketed teeth (a feature that inspired the traditional name, "thecodonts", for the Triassic forms) and four-chambered hearts, among other characteristics. Most early forms were carnivores, with narrow serrated meat-tearing teeth. Their "reptilian" metabolism seem to have given them a clear advantage over the mammal-like therapsids that were ...

Read more here: » Archosaur: Encyclopedia - Archosaur

In some educational systems, an undergraduate is a post-secondary student pursuing a Bachelor's degree. Students of higher degrees are known as postgraduates (or often simply graduates). In the United States, most undergraduate education takes place at four-year colleges or universities. Students in their first, second, third, and fourth years of study are often called, respectively, freshmen, sophomores, juniors, and seniors (although some institutions, such as many women's colleges, substitute "first-year" for "freshman" in a ...

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The Cretaceous period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic period, about 146 million years ago (Ma), to the beginning of the Paleocene epoch of the Tertiary period (65.5 Ma). The end of the Cretaceous also defines the boundary between the Mesozoic and Cenozoic eras. Cretaceous - Name and dating. As with other older geologic periods, the rock beds that define the Cretaceous are well identified, but the exact dates of the pe ...

Including:

• Cretaceous - Name and dating
• Cretaceous - Divisions
• Cretaceous - Paleogeography
• Cretaceous - Flora
• Cretaceous - Fauna
• Cretaceous - Land animals
• Cretaceous - Marine animals
• Cretaceous - Extinction
• Cretaceous - References and further reading

Read more here: » Cretaceous: Encyclopedia - Cretaceous

The Quaternary Period is the geologic time period from the end of the Pliocene Epoch roughly 1.8-1.6 million years ago to the present. The Quaternary includes 2 geologic subdivisions -- the Pleistocene and the Holocene Epochs. In a recent revision of the international classification of geological time periods, the Quaternary was subsumed into the Neogene. The move has met with some resistance from geologists. Quaternary - Overview. The term Quaternary ("fourth") was proposed by Jules Desnoyers in 182 ...

Including:

• Quaternary - Overview
• Quaternary - The Quaternary glacial period

Read more here: » Quaternary: Encyclopedia - Quaternary

Vocational education (or Vocational Education and Training (VET)) prepares learners for careers or professions that are traditionally non-academic and directly related to a specific trade, occupation or vocation, hence the term, in which the learner participates. It is sometimes referred to as technical education, as the learner directly specialises in a particular narrow technique of using technology. Vocational education might be contrasted with education in a usually broader scientific field, which might ...

Including:

• Vocational education - VET internationally
• Vocational education - Australia
• Vocational education - Commonwealth of Independent States
• Vocational education - Germany
• Vocational education - Singapore
• Vocational education - United States
• Vocational education - Readings

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A school is most commonly a place designated for learning. The range of institutions covered by the term varies from country to country. In the United Kingdom, the term school refers primarily to pre-university institutions, and these can, for the most part, be divided into primary schools (sometimes further divided into infant school and junior school), and secondary schools. School performance is monitore ...

Including:

• School - Records
• School - Criticism
• School - Bullying

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Conservation status: Fossil A. magniventris Ankylosaurus (ang-KYL-o-sore-us) meaning "stiffened lizard", because of its hard dermal armor (Greek ankylo = stiffen + sauros = lizard) was the last, largest, and most famous of the armored dinosaurs known as the Ankylosaurians. Its back and sides were covered with a stiff shell of armor, but its underbelly was exposed. It also had a great club-like tail that could be used for defense against predators. Ankylosaurus was ...

Including:

• Ankylosaurus - Description
• Ankylosaurus - Environment
• Ankylosaurus - Classification and history

Read more here: » Ankylosaurus: Encyclopedia - Ankylosaurus

Sir Charles Lyell (November 14, 1797 – February 22, 1875), British lawyer, geologist, and popularizer of uniformitarianism. Charles Lyell was born in Kinnordy, Forfarshire, Scotland, the eldest of ten children. Lyell's father, also named Charles, was a botanist of minor repute and first exposed the younger Charles to the study of nature. Having attended Exeter College, Oxford ending in 1816, Lyell encountered geology as a serious profession under the wing of William Buckland. Upon graduation he took a professional detour into ...

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About 500,000 years ago during the ice age period known as the Anglian glaciation, glaciers approached from the North Sea and reached as far south-west as Bricket Wood. Glacial gravels and boulder clays cover a great deal of the whole area to the north east of the county and the Upper Chalk itself has been disturbed at Reed and Barley by glaciation. Prior to the ice ages the River Thames followed a path through the southern part of Hertfordshire, running from the area of modern Staines up the valley of the Colne to Hatfield and then e ...

See also:

Geology of Hertfordshire, Geology of Hertfordshire - The Cretaceous, Geology of Hertfordshire - The Tertiary, Geology of Hertfordshire - The Ice Age

Read more here: » Geology of Hertfordshire: Encyclopedia II - Geology of Hertfordshire - The Ice Age

Deposition resumed in the Cambrian period and continued through the Paleozoic era, creating nine major formations which together are 4000 feet (1200 m) thick (the only geologic period in the Paleozoic not represented is the Silurian). This unit was laid down in a shallow sea and later became a discontinuous mix of dolomite, limestone, sandstones, and shales. The layers of this unit are relatively undeformed for their age even though periodic upwarp exposed them to erosion, creating uncomformities . Fossilized brachiopods, bryozoans, corals, ...

See also:

Geology of the Grand Teton area, Geology of the Grand Teton area - Precambrian deposition metamorphosis and intrusion, Geology of the Grand Teton area - Paleozoic and Mesozoic deposition, Geology of the Grand Teton area - Tertiary uplift and deposition, Geology of the Grand Teton area - Quaternary volcanic deposits and ice ages

Read more here: » Geology of the Grand Teton area: Encyclopedia II - Geology of the Grand Teton area - Paleozoic and Mesozoic deposition

The uplift responsible for erasing the Cretaceous Seaway and fusing the Sierran Arc to the rest of North America was caused by the Laramide orogeny. Starting 70 million years ago and lasting well into the first half of the Cenozoic era, the Laramide was the main mountain-building episode responsible for creating the Rocky Mountains. Compressive forces from this orogeny created north-south-trending thrust faults along with general regional uplift. Erosion of the Targhee uplift north of park borders was driven by steepened stream gradients. Gr ...

See also:

Geology of the Grand Teton area, Geology of the Grand Teton area - Precambrian deposition metamorphosis and intrusion, Geology of the Grand Teton area - Paleozoic and Mesozoic deposition, Geology of the Grand Teton area - Tertiary uplift and deposition, Geology of the Grand Teton area - Quaternary volcanic deposits and ice ages

Read more here: » Geology of the Grand Teton area: Encyclopedia II - Geology of the Grand Teton area - Tertiary uplift and deposition