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Devonian

A Wisdom Archive on Devonian

Devonian

A selection of articles related to Devonian

devonian, Devonian, Devonian - Devonian fauna, Devonian - Devonian palaeogeography, Devonian - Devonian subdivisions, Devonian - Naming, Devonian - Lower oldest, Devonian - Marine biota, Devonian - Middle, Devonian - Reefs, Devonian - Terrestrial biota, Devonian - Upper most recent, Geologic timescale, <i>Phacops rana</i>: a Devonian trilobite.


ARTICLES RELATED TO Devonian

Devonian: Encyclopedia II - Insect - Morphology and development

Insects range in size from less than a millimeter to over 18 centimeters (some walkingsticks) in length. Insects possess segmented bodies supported by an exoskeleton, a hard outer covering made mostly of chitin. The body is divided into a head, a thorax, and an abdomen. The head supports a pair of sensory antennae, a pair of compound eyes, and a mouth. The thorax has six legs (one pair per segment) and wings (if present in the species). T ...

See also:

Insect, Insect - Relationship to other arthropods, Insect - Morphology and development, Insect - Behavior, Insect - Roles in the environment and human society, Insect - Fossils and evolution, Insect - Quotes

Read more here: » Insect: Encyclopedia II - Insect - Morphology and development

Devonian: Encyclopedia II - Yosemite National Park - Geography

Yosemite National Park is located in the central Sierra Nevada of California. It takes 3.5 hours to drive to the park from San Francisco and about six hours from Los Angeles. Yosemite is surrounded by wilderness areas: the Ansel Adams Wilderness to the southeast, the Hoover Wilderness to the northeast, and the Emigrant Wilderness to the north. The 1,200-square-mile (3,100 km²) park contains thousands of lakes and ponds, 1,600 miles (2,600 km) of streams, 800 miles (1300 km) of hiking trails, and 350 miles (560 km) of roads. Two feder ...

See also:

Yosemite National Park, Yosemite National Park - Geography, Yosemite National Park - Rocks and erosion, Yosemite National Park - Popular features, Yosemite National Park - Water and ice, Yosemite National Park - Climate, Yosemite National Park - History, Yosemite National Park - The Ahwahnechee and the Mariposa Wars, Yosemite National Park - Early tourists, Yosemite National Park - The Yosemite Grant, Yosemite National Park - Increased protection efforts, Yosemite National Park - Later history, Yosemite National Park - Geology, Yosemite National Park - Tectonic and volcanic activity, Yosemite National Park - Uplift and erosion, Yosemite National Park - Sculpting by glaciers, Yosemite National Park - Biology, Yosemite National Park - Habitats, Yosemite National Park - Management issues, Yosemite National Park - Activities, Yosemite National Park - Hiking, Yosemite National Park - Climbing, Yosemite National Park - Summer activities, Yosemite National Park - Winter activities

Read more here: » Yosemite National Park: Encyclopedia II - Yosemite National Park - Geography

Devonian: Encyclopedia II - Geology of India - Geological Phases

The major geological phases responsible for making of india can be enumerated thus: The first phase is marked by the cooling and solidification of the upper crust of the earth surface in the pre-Cambrian era (prior to 600 million years) represented by the exposure of the Archaean gneisses and granites especially on the Peninsula. Minor igneous activities, subsequent metamorphism and crumpling along with the fol ...

See also:

Geology of India, Geology of India - Geological Phases, Geology of India - Main rock groups, Geology of India - Archaean, Geology of India - Palaeozoic, Geology of India - Mesozoic, Geology of India - Kainozoic, Geology of India - Quaternary, Geology of India - Notes

Read more here: » Geology of India: Encyclopedia II - Geology of India - Geological Phases

Devonian: Encyclopedia II - Global Boundary Stratotype Section and Point - Agreed-upon GSSPs

The Precambrian-Cambrian boundary GSSP at Fortune Head, Newfoundland is a typical GSSP. It is accessible by paved road and is set aside as a nature preserve. A continuous section is available from beds that are clearly Precambrian into beds that are clearly Cambrian. The boundary is set at the first appearance of a complex trace fossil Trichophycus pedum that is found worldwide. The Fortune Head GSSP is unlikely to be washed away or built over. Trichophycus pedum is less than ideal as a marker fossil as it is not found in every Cambrian sequ ...

See also:

Global Boundary Stratotype Section and Point, Global Boundary Stratotype Section and Point - Agreed-upon GSSPs, Global Boundary Stratotype Section and Point - GSSAs, Global Boundary Stratotype Section and Point - External link, Global Boundary Stratotype Section and Point - Reference

Read more here: » Global Boundary Stratotype Section and Point: Encyclopedia II - Global Boundary Stratotype Section and Point - Agreed-upon GSSPs

Devonian: Encyclopedia II - Devon - History

Devon was one of the first areas of England settled following the end of the last ice age. Dartmoor is thought to have been settled by Mesolithic hunter-gatherer peoples from about 6000 BC. The name "Devon" derives from the name given by the Romans to the Celtic people who inhabited the south western peninsula of Britain at the time of the Roman invasion c. 50AD , known as the Dumnonii, thought to mean 'Deep Valley Dwellers'. The Romans held the area under Military Occupation for approx 25 years. Later the area became a frontier between Bryt ...

See also:

Devon, Devon - History, Devon - Economy, Devon - Flag, Devon - Geology landscape and ecology, Devon - Politics and administration, Devon - Cities towns and villages, Devon - Places of interest, Devon - Rivers, Devon - Devon as a descriptor

Read more here: » Devon: Encyclopedia II - Devon - History

Devonian: Encyclopedia II - Cornwall - Culture

Cornwall - Language. Main article: Cornish language The Cornish language is closely related to Welsh and Breton, and less so to Irish, Scots Gaelic and Manx. It continued as a living Celtic language until 1777 and the death of Dolly Pentreath, the last person thought to have used only the Cornish language (although this is disputed on a number of counts). The publication of Henry Jenner's "Handbook of the Cornish Language" in 1904 caused a resurgence of interest in the Cornish language. ...

See also:

Cornwall, Cornwall - History, Cornwall - Physical geography, Cornwall - Politics, Cornwall - Flag, Cornwall - Demographics, Cornwall - Economy, Cornwall - Tourism, Cornwall - Industry, Cornwall - Culture, Cornwall - Language, Cornwall - Cornish studies and literary references, Cornwall - Religion, Cornwall - Music and festivals, Cornwall - Sports and games, Cornwall - Food, Cornwall - Settlements, Cornwall - Transport, Cornwall - Places of interest

Read more here: » Cornwall: Encyclopedia II - Cornwall - Culture

Devonian: Encyclopedia II - Cornwall - Culture

Cornwall - Language. The Cornish language is closely related to Welsh and Breton, and less so to Irish, Scots Gaelic and Manx. It continued as a living Celtic language until 1777 and the death of Dolly Pentreath, the last person thought to have used only the Cornish language (although this is disputed on a number of counts). The publication of Henry Jenner's "Handbook of the Cornish Language" in 1904 caused a resurgence of interest in the Cornish language. The subsequent revival gathered pace during the twentieth ...

See also:

Cornwall, Cornwall - History, Cornwall - Physical geography, Cornwall - Politics, Cornwall - Flag, Cornwall - Demographics, Cornwall - Economy, Cornwall - Tourism, Cornwall - Industry, Cornwall - Culture, Cornwall - Language, Cornwall - Cornish studies and literary references, Cornwall - Religion, Cornwall - Music and festivals, Cornwall - Sports and games, Cornwall - Food, Cornwall - Settlements, Cornwall - Transport, Cornwall - Places of interest

Read more here: » Cornwall: Encyclopedia II - Cornwall - Culture

Devonian: Encyclopedia II - Le Roy town New York - Demographics

As of the census2 of 2000, there are 7,790 people, 3,037 households, and 2,034 families residing in the town. The population density is 71.3/km² (184.7/mi²). There are 3,219 housing units at an average density of 29.5/km² (76.3/mi²). The racial makeup of the town is 96.01% White, 1.87% Black or African American, 0.27% Native American, 0.44% Asian, 0.01% Pacific Islander, 0.21% from other races, and 1.19% from two or more races. 0.78% ...

See also:

Le Roy town New York, Le Roy town New York - History, Le Roy town New York - Geography, Le Roy town New York - Demographics, Le Roy town New York - Communities and locations in the Town of Le Roy

Read more here: » Le Roy town New York: Encyclopedia II - Le Roy town New York - Demographics

Devonian: Encyclopedia II - London-Brabant Island - The Carboniferous

The period from which the island has exercised most influence on modern Europe was the Carboniferous. As the continent was drifting past the Equator, on the island's shores, there grew a rich tropical forest swamp. On the island's southern shore, it left the Dinantian, Namurian and Westphalian coal fields of France and Belgium. To its north-west, it left those of Leicestershire and Nottinghamshire. These extend further east but at ever greater depth. At the modern east Yorkshire and north Lincolnshire coast for example, their upper su ...

See also:

London-Brabant Island, London-Brabant Island - Formation, London-Brabant Island - The Carboniferous, London-Brabant Island - The Permian and Triassic, London-Brabant Island - Rhaetic Transgression, London-Brabant Island - Cretaceous, London-Brabant Island - Modern existence, London-Brabant Island - Footnote

Read more here: » London-Brabant Island: Encyclopedia II - London-Brabant Island - The Carboniferous

Devonian: Encyclopedia II - Genesee River - History

The Genesee River Valley westward to Lake Erie and the Niagara River was the homeland of the Seneca Nation of the Iroquois Confederacy, also known as The Keepers of the Western Door, as they were the westernmost nation. The Senecas were gradually divested of their homelands and now have just three small reservations left. The falls at present day Rochester were likely the main reason for the city's existence, as they provided water power for mills. When the Erie Canal opened in 1825 the mills could ship their products cheaply to New York City, and business boomed. Roc ...

See also:

Genesee River, Genesee River - Geology, Genesee River - History, Genesee River - List of Communities on the Genesee River north to south

Read more here: » Genesee River: Encyclopedia II - Genesee River - History

Devonian: Encyclopedia II - Sea urchin - Geological history

The earliest known echinoids are found in the rocks of the upper part of the Ordovician period, and they have survived to the present day where they are a successful and diverse group of organisms. In well preserved specimens the spines may be present, but usually only the test is found. Sometimes isolated spines are common as fossils. Some echinoids (such as Tylocidaris clavigera which is found in the Cretaceous period Chalk Formation of England) had very heavy club-shaped spines that would be difficult for an attacking predator to break through and make the echinoid awkward to handle. Such spines ...

See also:

Sea urchin, Sea urchin - Geological history, Sea urchin - References and further reading

Read more here: » Sea urchin: Encyclopedia II - Sea urchin - Geological history

Devonian: Encyclopedia II - Allegany County New York - History

When counties were established in New York State in 1683, the present Allegany County was part of Albany County. This was an enormous county, including the northern part of New York State as well as all of the present State of Vermont and, in theory, extending westward to the Pacific Ocean. This county was reduced in size on July 3, 1766 by the creation of Cumberland County, and further on March 16, 1770 by the creation of Gloucest ...

See also:

Allegany County New York, Allegany County New York - History, Allegany County New York - Geography, Allegany County New York - Demographics, Allegany County New York - Towns and Villages, Allegany County New York - Indian reservations, Allegany County New York - Information about Allegany County, Allegany County New York - Educational institutions, Allegany County New York - Adjacent Counties and areas

Read more here: » Allegany County New York: Encyclopedia II - Allegany County New York - History

Devonian: Encyclopedia II - Irreducible complexity - Criticisms of irreducible complexity

There has been much scientific opposition to the irreducible complexity, with one science writer calling it a "full-blown intellectual surrender strategy." [11] It may be that irreducible complexity does not actually exist in nature: that the examples given by Behe and others are not in fact irreducibly complex, but can be explained in terms of simpler precursors. Thus they would either be merely very complex, or they would be misunderstood or misrepresented. The precursors of complex systems, when they are not useful in themse ...

See also:

Irreducible complexity, Irreducible complexity - Irreducible complexity IC, Irreducible complexity - Criticism, Irreducible complexity - Definitions, Irreducible complexity - Stated examples, Irreducible complexity - Flagella, Irreducible complexity - Blood clotting cascade, Irreducible complexity - Forerunners, Irreducible complexity - Criticisms of irreducible complexity, Irreducible complexity - Gradual replacement, Irreducible complexity - Handicaps and sexual selection, Irreducible complexity - Falsifiability and experimental evidence, Irreducible complexity - Behe's own Criticisms, Irreducible complexity - God and Irreducible Complexity, Irreducible complexity - Claimed significance

Read more here: » Irreducible complexity: Encyclopedia II - Irreducible complexity - Criticisms of irreducible complexity

Devonian: Encyclopedia II - Renewable energy - Modern sources of renewable energy

Renewable energy - Wind energy. Main articles: Wind power, and [[{{{2}}}]], and [[{{{3}}}]], and [[{{{4}}}]]< ...

See also:

Renewable energy, Renewable energy - Modern sources of renewable energy, Renewable energy - Wind energy, Renewable energy - Water power, Renewable energy - Solar energy, Renewable energy - Geothermal energy, Renewable energy - Biomass, Renewable energy - Small scale energy sources, Renewable energy - Issues, Renewable energy - Aesthetics habitat hazards and land use, Renewable energy - Concentration, Renewable energy - Proximity to demand, Renewable energy - Availability, Renewable energy - Fossil fuels, Renewable energy - Transmission, Renewable energy - Historical usage of renewable energy

Read more here: » Renewable energy: Encyclopedia II - Renewable energy - Modern sources of renewable energy

Devonian: Encyclopedia II - Sponge - Anatomy

Sponges comprise only four types of cells: Choanocytes (also known as "collar cells"), which line the spongocoel and function as the sponge's digestive system, are remarkably similar to the protistan choanoflagellates. Porocytes are tubular cells that make up the pores. Flat epidermal cells line the outside of the sponge and form its skin. Amoebocytes live between the choanocytes and the epidermis. They carry out many of the sponge's functions, such as transport of nutrients, secretion of the spicules, ...

See also:

Sponge, Sponge - Anatomy, Sponge - Taxonomy, Sponge - Reproduction, Sponge - Ecology, Sponge - Skeleton as absorbent, Sponge - Geological history

Read more here: » Sponge: Encyclopedia II - Sponge - Anatomy

Devonian: Encyclopedia II - Frog - Characteristics

Because of the great diversity of frogs (over 4000 species), many characteristics are not shared throughout all of the species. However, there are some characteristics which distinguish them from other amphibians. Frogs are generally well suited to jumping, and have long hind legs, with elongated ankle bones. They have a short vertebral column, with no more than ten free vertebrae, followed by a fused tail bone, usually resulting in a frog without a tail. Frogs range in size from 10mm (Psyllophryne didactyla of Brazil and Eleut ...

See also:

Frog, Frog - Characteristics, Frog - Call, Frog - Poison, Frog - Distribution and status, Frog - Life cycle, Frog - Diversity of reproductive behaviours, Frog - Diet and Predators, Frog - Taxonomy, Frog - Distinction of frogs and toads, Frog - Hybridisation, Frog - Evolution, Frog - Uses

Read more here: » Frog: Encyclopedia II - Frog - Characteristics

Devonian: Encyclopedia II - Hemer - History

Hemer was first mentioned in 1072 with its old name Hademare in a document from the bishop Anno II. of Cologne. Among the lands given to the newly founded Benedictine monastery Grafschaft were the St. Vitus church and two farms (the later Haus Hemer and the Hedhof). In 1124 the parish of St. Vitus was split from parish Menden. Hemer stayed an unimportant settlement without market rights, also when count of the Mark liberated themselves from the bishopric state of Cologne in the 13th century and Hemer was at the bo ...

See also:

Hemer, Hemer - History, Hemer - Creation of Amt Hemer, Hemer - Communal reform of 1929, Hemer - Military, Hemer - Communal reform of 1975, Hemer - Municipalities as of 1904, Hemer - List of mayors, Hemer - Points of interest, Hemer - Coat of arms, Hemer - Economics, Hemer - Traffic, Hemer - Twin towns and city friendships, Hemer - Famous people from Hemer, Hemer - Literature

Read more here: » Hemer: Encyclopedia II - Hemer - History

Devonian: Encyclopedia II - Pineal gland - Structure and composition

The pineal gland consists mainly of pinealocytes, but four other cell types have been identified: interstitial cells, perivascular phagocyte, pineal neurons and peptidergic neuron-like cells. The pineal body has nervous tissue, and consists of follicles lined by epithelium and enveloped by connective tissue. These follicles contain a variable quantity of gritty material, called brain sand, acervuli, or corpora arenacea, which is composed of calcium phosphate, calci ...

See also:

Pineal gland, Pineal gland - Location, Pineal gland - Structure and composition, Pineal gland - Function, Pineal gland - Mythology

Read more here: » Pineal gland: Encyclopedia II - Pineal gland - Structure and composition

Devonian: Encyclopedia II - Geology of the Alps - Historical Views of Alpine Geology

The Alps form but a small portion of a great zone of crumpling mountain ranges that stretch in a series of curves from the Atlas Mountains to the Himalayas. Within this zone the crust of the earth has been ridged up into a complex system of creases or folds out of which the great mountain chains of southern Europe and Asia have been carved by atmospheric agencies. Superficially, the continuity of the zone is broken at intervals by gaps of greater or lesser extent, but these are due, in part at least, to the subsidence of portions of the fold ...

See also:

Geology of the Alps, Geology of the Alps - Geological History, Geology of the Alps - Current view, Geology of the Alps - Historical Views of Alpine Geology

Read more here: » Geology of the Alps: Encyclopedia II - Geology of the Alps - Historical Views of Alpine Geology

Devonian: Encyclopedia II - Mammal - Classification

Main article: Mammal classification George Gaylord Simpson's classic "Principles of Classification and a Classification of Mammals" (AMNH Bulletin v. 85, 1945) was the original source for the taxonomy listed here. Simpson laid out a systematics of mammal origins and relationships that was universally taught until the end of the 20th century. Since Simpson's 1945 classification, the paleontological record has been recalibrated, and the intervening years have seen much debate and progress concerning the theoretical underpi ...

See also:

Mammal, Mammal - Characteristics, Mammal - Origins, Mammal - In the Mesozoic, Mammal - In the Paleocene, Mammal - Classification, Mammal - Standardized textbook classification, Mammal - McKenna/Bell classification, Mammal - Molecular classification of placentals, Mammal - Classification system used in related articles

Read more here: » Mammal: Encyclopedia II - Mammal - Classification

Devonian: Encyclopedia II - Northumberland - History

Once part of the Roman Empire and the scene of many wars between England and Scotland, Northumberland has a long and complicated history. This explains the many castles in Northumberland, including among the better-known those at Bamburgh, Dunstanburgh, Warkworth and Alnwick. The region of present-day Northumberland once formed the core of the Anglian kingdom of Northumbria. Northumberland is called the "cradle of Christianity" in England because it was on Lindisfarne, a tidal island north of Bamburgh, also called Holy Island, ...

See also:

Northumberland, Northumberland - History, Northumberland - Physical geography, Northumberland - Economy and industry, Northumberland - Demographics, Northumberland - Politics, Northumberland - Culture, Northumberland - Media, Northumberland - People, Northumberland - Settlements, Northumberland - Notes and references, Northumberland - Bibliography

Read more here: » Northumberland: Encyclopedia II - Northumberland - History

Devonian: Encyclopedia II - Mnemonic - Examples of simple mnemonics

One common mnemonic device for remembering lists consists of an easily remembered word, phrase, or rhyme whose initials or other characteristics are associated with the list items. The idea lends itself well to memorizing hard-to-break passwords as well. Mnemonic - Science and technology. Stellar classification uses a peculiar group of letters, easily remembered using the phrase, "Oh Be A Fine Girl, Kiss Me." With two new categories L an ...

See also:

Mnemonic, Mnemonic - Examples of simple mnemonics, Mnemonic - Science and technology, Mnemonic - General knowledge, Mnemonic - Anamonics Scrabble, Mnemonic - Techniques, Mnemonic - Number rhyme system, Mnemonic - Egg and spear or number shape system, Mnemonic - Visual mnemonics, Mnemonic - Other mnemonic systems, Mnemonic - Arbitrariness of mnemonics, Mnemonic - Assembly mnemonics, Mnemonic - History of mnemonics

Read more here: » Mnemonic: Encyclopedia II - Mnemonic - Examples of simple mnemonics






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