Voting rights of citizens in the District of Columbia differ from those of United States citizens in each of the fifty states. District of Columbia residents do not have voting representation in the United States Senate, but D.C. is entitled to three electoral votes for President. In the U.S. House of Representatives, the District is entitled to a delegate, who is not allowed to vote on the floor of the House, but can vote on procedural matters and in House committees.
The United States Constitution grants congressional voting representation to the states, which the District is not. The District is a federal territory ultimately under the complete authority of Congress. The lack of voting representation in Congress for residents of the U.S. capital has been an issue since the foundation of the federal district. Numerous proposals have been introduced to change this situation including legislation and constitutional amendments to grant D.C. residents voting representation, returning the District to the state of Maryland, and making the District of Columbia into a new state. All proposals have been met with political or constitutional challenges; therefore, there has been no change in the District's representation in the Congress.
Friday, December 30, 2011
Tuesday, December 27, 2011
Ptolemaic dynasty
The Ptolemaic dynasty, (Ancient Greek: Πτολεμα?οι, sometimes also known as the Lagids or Lagides, Ancient Greek: Λαγ?δαι, from the name of Ptolemy I's father, Lagus) was a Macedonian Greek[1][2][3][4][5] royal family which ruled the Ptolemaic Empire in Egypt during the Hellenistic period. Their rule lasted for 275 years, from 305 BC to 30 BC. They were the 32nd and last dynasty of ancient Egypt.
Ptolemy, one of the six somatophylakes (bodyguards) who served as Alexander the Great's generals and deputies, was appointed satrap of Egypt after Alexander's death in 323 BC. In 305 BC, he declared himself King Ptolemy I, later known as "Soter" (saviour). The Egyptians soon accepted the Ptolemies as the successors to the pharaohs of independent Egypt. Ptolemy's family ruled Egypt until the Roman conquest of 30 BC.
All the male rulers of the dynasty took the name Ptolemy. Ptolemaic queens, some of whom were the sisters of their husbands, were usually called Cleopatra, Arsinoe or Berenice. The most famous member of the line was the last queen, Cleopatra VII, known for her role in the Roman political battles between Julius Caesar and Pompey, and later between Octavian and Mark Antony. Her apparent suicide at the conquest by Rome marked the end of Ptolemaic rule in Egypt.
Ptolemy, one of the six somatophylakes (bodyguards) who served as Alexander the Great's generals and deputies, was appointed satrap of Egypt after Alexander's death in 323 BC. In 305 BC, he declared himself King Ptolemy I, later known as "Soter" (saviour). The Egyptians soon accepted the Ptolemies as the successors to the pharaohs of independent Egypt. Ptolemy's family ruled Egypt until the Roman conquest of 30 BC.
All the male rulers of the dynasty took the name Ptolemy. Ptolemaic queens, some of whom were the sisters of their husbands, were usually called Cleopatra, Arsinoe or Berenice. The most famous member of the line was the last queen, Cleopatra VII, known for her role in the Roman political battles between Julius Caesar and Pompey, and later between Octavian and Mark Antony. Her apparent suicide at the conquest by Rome marked the end of Ptolemaic rule in Egypt.
Sunday, December 25, 2011
Week News Abstract For SFP Series in 10GTEK: Northern England
Northern England, also known as the North of England, the North or the North Country, is a cultural region of England. It is not an official government region, but rather an informal amalgamation of counties. The southern extent of the region is roughly the River Trent,[4] while the North is bordered by Scotland. The counties of Northern England combined have a population of around 14.5 million covering an area of 37,331 km2 (14,414 sq mi).
During antiquity most of the area was part of Brigantia — homeland of the Brigantes and the largest Brythonic kingdom of Great Britain. After the Roman conquest of Britain the city of York became capital of the area, called Britannia Inferior then Britannia Secunda. In Sub-Roman Britain new Brythonic kingdoms of the Hen Ogledd emerged. The Angle settlers created Bernicia and Deira from which came Northumbria and a Golden Age in cultural, scholarly and monastic activity, centred around Lindisfarne and aided by Irish monks.[5] Norse and Gaelic Viking raiders gained control of much of the area, creating the Danelaw. During this time there were close relations with Mann and the Isles, Dublin and Norway. Northumbria was unified with the rest of England under Eadred around 952.Much of Northumbria was also shired, the best known of these counties being Hallamshire and Cravenshire. The Normans did not use these divisions, and so they are not generally regarded as ancient counties. The huge county of Yorkshire was a successor to the Viking Kingdom of York, and at the time of the Domesday Book in 1086 it was considered to include what was to become northern Lancashire, as well as parts of Cumberland, and Westmorland. Most of the later Cumberland and Westmorland were under Scottish rule until 1092. After the Norman Conquest in 1066 and the harrying of the North, much of the North of England was left depopulated and was included in the returns for Cheshire and Yorkshire in the Domesday Book.[26] However, there is some disagreement about the status of some of this land. The area in between the River Ribble and the River Mersey, referred to as "Inter Ripam et Mersam" in the Domesday Book,[27] was included in the returns for Cheshire.[28] Whether this meant that this land was actually part of Cheshire is however not clear.[27][29][30][31][32] Additionally, the Domesday book included as part of Cheshire, areas that later became part of Wales, including the two hundreds of Atiscross and Exestan, and the southern part of Duddestan Hundred (as it was known as the time), which later became known as Maelor Saesneg, and (later still) "Flintshire Detached" (see Flintshire (historic)),[33] The Northeast, or Northumbria, land that later became County Durham and Northumberland, was left unrecorded.
During antiquity most of the area was part of Brigantia — homeland of the Brigantes and the largest Brythonic kingdom of Great Britain. After the Roman conquest of Britain the city of York became capital of the area, called Britannia Inferior then Britannia Secunda. In Sub-Roman Britain new Brythonic kingdoms of the Hen Ogledd emerged. The Angle settlers created Bernicia and Deira from which came Northumbria and a Golden Age in cultural, scholarly and monastic activity, centred around Lindisfarne and aided by Irish monks.[5] Norse and Gaelic Viking raiders gained control of much of the area, creating the Danelaw. During this time there were close relations with Mann and the Isles, Dublin and Norway. Northumbria was unified with the rest of England under Eadred around 952.Much of Northumbria was also shired, the best known of these counties being Hallamshire and Cravenshire. The Normans did not use these divisions, and so they are not generally regarded as ancient counties. The huge county of Yorkshire was a successor to the Viking Kingdom of York, and at the time of the Domesday Book in 1086 it was considered to include what was to become northern Lancashire, as well as parts of Cumberland, and Westmorland. Most of the later Cumberland and Westmorland were under Scottish rule until 1092. After the Norman Conquest in 1066 and the harrying of the North, much of the North of England was left depopulated and was included in the returns for Cheshire and Yorkshire in the Domesday Book.[26] However, there is some disagreement about the status of some of this land. The area in between the River Ribble and the River Mersey, referred to as "Inter Ripam et Mersam" in the Domesday Book,[27] was included in the returns for Cheshire.[28] Whether this meant that this land was actually part of Cheshire is however not clear.[27][29][30][31][32] Additionally, the Domesday book included as part of Cheshire, areas that later became part of Wales, including the two hundreds of Atiscross and Exestan, and the southern part of Duddestan Hundred (as it was known as the time), which later became known as Maelor Saesneg, and (later still) "Flintshire Detached" (see Flintshire (historic)),[33] The Northeast, or Northumbria, land that later became County Durham and Northumberland, was left unrecorded.
Thursday, December 22, 2011
Evidence for carbon addition
Clear evidence for massive addition of 13C-depleted carbon at the onset of the PETM comes from two observations. First, a prominent negative excursion in the carbon isotope composition (δ13C) of carbon-bearing phases characterizes the PETM in numerous widespread locations from a range of environments. Second, carbonate dissolution marks the PETM in sections from the deep-sea.
The total mass of carbon injected to the ocean and atmosphere during the PETM remains the source of debate. In theory, it can be estimated from the magnitude of the δ13C excursion, the amount of carbonate dissolution on the seafloor, or ideally both. However, the shift in the δ13C across the PETM depends on the location and the carbon-bearing phase analyzed. In some records of bulk carbonate, it is about 2‰; in some records of terrestrial carbonate or organic matter it exceeds 6‰.[11] Carbonate dissolution also varies throughout different ocean basins. It is extreme in parts of the north and central Atlantic Ocean but far less pronounced in the Pacific Ocean. With available information, estimates of the carbon addition range from about 2500 to over 6800 gigatons [12]
The timing of the PETM δ13C excursion has been calculated in two complementary ways. The iconic core covering this time period is the ODP's Core 690, and the timing is based exclusively on this core's record. The original timing was calculated assuming a constant sedimentation rate.[13] This model was improved using the assumption that 3He flux is constant; this cosmogenic nuclide is produced at a (roughly) constant rate by the sun, and there is little reason to assume large fluctuations in the solar wind across this short time period.[14] Both models have their failings, but agree on a few points. Importantly, they both detect two steps in the drop of δ13C, each lasting about 1,000 years, and separated by about 20,000 years. The models diverge most in their estimate of the recovery time, which ranges from 150,000[13] to 30,000[14] years. There is other evidence to suggest that warming predated the δ13C excursion by some 3,000 years.
The total mass of carbon injected to the ocean and atmosphere during the PETM remains the source of debate. In theory, it can be estimated from the magnitude of the δ13C excursion, the amount of carbonate dissolution on the seafloor, or ideally both. However, the shift in the δ13C across the PETM depends on the location and the carbon-bearing phase analyzed. In some records of bulk carbonate, it is about 2‰; in some records of terrestrial carbonate or organic matter it exceeds 6‰.[11] Carbonate dissolution also varies throughout different ocean basins. It is extreme in parts of the north and central Atlantic Ocean but far less pronounced in the Pacific Ocean. With available information, estimates of the carbon addition range from about 2500 to over 6800 gigatons [12]
The timing of the PETM δ13C excursion has been calculated in two complementary ways. The iconic core covering this time period is the ODP's Core 690, and the timing is based exclusively on this core's record. The original timing was calculated assuming a constant sedimentation rate.[13] This model was improved using the assumption that 3He flux is constant; this cosmogenic nuclide is produced at a (roughly) constant rate by the sun, and there is little reason to assume large fluctuations in the solar wind across this short time period.[14] Both models have their failings, but agree on a few points. Importantly, they both detect two steps in the drop of δ13C, each lasting about 1,000 years, and separated by about 20,000 years. The models diverge most in their estimate of the recovery time, which ranges from 150,000[13] to 30,000[14] years. There is other evidence to suggest that warming predated the δ13C excursion by some 3,000 years.
Tuesday, December 20, 2011
Cultural significance
The exodus from Egypt is the theme of the Jewish holiday of Passover ("pesa?"); the term continues to be used in the Passover Hagadah.[6] At the beginning of the Exodus narrative the Israelites are instructed to prepare unleavened bread as they will be leaving in haste, and to mark their doors with blood of the slaughtered sheep so that the "Angel" or "the destroyer" will "pass over" them while killing the first-born of Egypt. The Hebrew name for the festival, "Pesa?", refers to the "skipping over", "jumping over" or "passing over" by God over the Jewish houses while killing the first born of Egypt. (Despite the biblical story, scholars believe that the passover festival originated in a magic ritual to turn away demons from the household by painting the doorframe with the blood of a slaughtered sheep.)[7]
Jewish tradition has preserved national and personal reminders of this pivotal narrative into daily life. Examples of such reminders include the wearing of 'tefilin' (phylacteries) on the hand and forehead, which some Jews practice daily; the wearing of 'tzitzit' (knotted ritual fringes attached to the four corners of the prayer shawl); the eating of 'matzot' (unleavened bread) during the Pesach (Passover) holiday; the fasting of the firstborn a day before Pesach; the redemption of firstborn children and animals; and even the observance of the Sabbath.
Jewish tradition has preserved national and personal reminders of this pivotal narrative into daily life. Examples of such reminders include the wearing of 'tefilin' (phylacteries) on the hand and forehead, which some Jews practice daily; the wearing of 'tzitzit' (knotted ritual fringes attached to the four corners of the prayer shawl); the eating of 'matzot' (unleavened bread) during the Pesach (Passover) holiday; the fasting of the firstborn a day before Pesach; the redemption of firstborn children and animals; and even the observance of the Sabbath.
Sunday, December 18, 2011
Week News Abstract For SFP Series in 10GTEK: Wales
Wales ( listen), Welsh: Cymru; pronounced ( listen)) is a country that is part of the United Kingdom and the island of Great Britain,[4] bordered by England to its east and the Atlantic Ocean and Irish Sea to its west. It has a population of three million, and a total area of 20,779 km2 (8,023 sq mi). Wales has over 1,200 km (746 mi) of coastline, including its offshore islands; the largest, Anglesey (Ynys M?n), is also the largest island in the Irish Sea. Generally mountainous, its highest mountains are in the north and central areas, especially in Snowdonia (Eryri), which contains Snowdon (Yr Wyddfa), its highest peak.
During the Iron Age and early medieval period, Wales was inhabited by the Celtic Britons. A distinct Welsh national identity emerged in the centuries after the Roman withdrawal from Britain in the 5th century, and Wales is regarded as one of the modern Celtic nations today. Gruffydd ap Llywelyn was recognised as king of Wales in 1057. Llywelyn ap Gruffydd's death in 1282 marked the completion of Edward I of England's conquest of Wales. The castles and town walls erected to ensure its permanence are now UNESCO World Heritage Sites. Owain Glynd?r briefly restored independence to what was to become modern Wales, in the early 15th century. Wales was subsequently annexed by England under the Laws in Wales Acts 1535–1542 since when, excluding those matters now devolved to Wales, English law has been the legal system of Wales and England. Distinctive Welsh politics developed in the 19th century. Welsh Liberalism, exemplified in the early 20th century by Lloyd George, was displaced by the growth of socialism and the Labour Party. Welsh national feeling grew over the century; Plaid Cymru was formed in 1925 and Cymdeithas yr Iaith Gymraeg (The Welsh Language Society) in 1962. The National Assembly for Wales, created in 1999 following a referendum, holds responsibility for a range of devolved policy matters.
Wales lies within the north temperate zone, its changeable, maritime climate making it one of the wettest countries in Europe. It was an agricultural society for most of its early history, the country's terrain making arable farming secondary to pastoral farming, the primary source of Wales' wealth. In the 18th century, the introduction of the slate and metallurgical industries, at the dawn of the Industrial Revolution, began to transform the country into an industrial nation; the UNESCO World Heritage Sites Pontcysyllte Aqueduct and the Blaenavon Industrial Landscape date from that period. The south Wales coalfield's exploitation in the Victorian era caused a rapid expansion of the Welsh population. Two-thirds of Wales' three million population live in south Wales, mainly in and around the cities of Cardiff (Caerdydd), Swansea (Abertawe) and Newport (Casnewydd), and in the nearby valleys. Another concentration live in eastern north Wales. Cardiff, Wales' capital, is the country's most populous city, with 317,500 residents, and for a period was the biggest coal port in the world. Today, with the country's traditional heavy industries (coal, steel, copper, tinplate and slate) either gone or in decline, Wales' economy depends on the public sector, light and service industries, and tourism.
Although Wales shares a close political and social history with the rest of Great Britain, it has retained a distinct cultural identity. Wales is officially bilingual, the Welsh and English languages having equal status. The Welsh language is an important element of Welsh culture, and its use is supported by national policy. Over 580,000 Welsh speakers live in Wales, more than 20% of the population. From the late 19th century onwards, Wales acquired its popular image as the "land of song", attributable in part to the revival of the eisteddfod tradition. At international sporting events, such as the FIFA World Cup, Rugby World Cup and the Commonwealth Games, Wales is represented by national teams regulated and organised by over fifty national governing bodies of sports in Wales. At the Olympic Games, Welsh athletes compete as part of a Great Britain team. Although football has traditionally been the more popular sport in north Wales, rugby union is seen as a symbol of Welsh identity and an expression of national consciousness.Iron is a chemical element with the symbol Fe (from Latin: ferrum) and atomic number 26. It is a metal in the first transition series. It is the most common element (by mass) forming the planet Earth as a whole, forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. Iron's very common presence in rocky planets like Earth is due to its abundant production as a result of fusion in high-mass stars, where the production of nickel-56 (which decays to iron) is the last nuclear fusion reaction that is exothermic. This allows radioactive nickel to become the last element to be produced before collapse of a supernova leads to events that scatters this precursor radionuclide of iron into space.
During the Iron Age and early medieval period, Wales was inhabited by the Celtic Britons. A distinct Welsh national identity emerged in the centuries after the Roman withdrawal from Britain in the 5th century, and Wales is regarded as one of the modern Celtic nations today. Gruffydd ap Llywelyn was recognised as king of Wales in 1057. Llywelyn ap Gruffydd's death in 1282 marked the completion of Edward I of England's conquest of Wales. The castles and town walls erected to ensure its permanence are now UNESCO World Heritage Sites. Owain Glynd?r briefly restored independence to what was to become modern Wales, in the early 15th century. Wales was subsequently annexed by England under the Laws in Wales Acts 1535–1542 since when, excluding those matters now devolved to Wales, English law has been the legal system of Wales and England. Distinctive Welsh politics developed in the 19th century. Welsh Liberalism, exemplified in the early 20th century by Lloyd George, was displaced by the growth of socialism and the Labour Party. Welsh national feeling grew over the century; Plaid Cymru was formed in 1925 and Cymdeithas yr Iaith Gymraeg (The Welsh Language Society) in 1962. The National Assembly for Wales, created in 1999 following a referendum, holds responsibility for a range of devolved policy matters.
Wales lies within the north temperate zone, its changeable, maritime climate making it one of the wettest countries in Europe. It was an agricultural society for most of its early history, the country's terrain making arable farming secondary to pastoral farming, the primary source of Wales' wealth. In the 18th century, the introduction of the slate and metallurgical industries, at the dawn of the Industrial Revolution, began to transform the country into an industrial nation; the UNESCO World Heritage Sites Pontcysyllte Aqueduct and the Blaenavon Industrial Landscape date from that period. The south Wales coalfield's exploitation in the Victorian era caused a rapid expansion of the Welsh population. Two-thirds of Wales' three million population live in south Wales, mainly in and around the cities of Cardiff (Caerdydd), Swansea (Abertawe) and Newport (Casnewydd), and in the nearby valleys. Another concentration live in eastern north Wales. Cardiff, Wales' capital, is the country's most populous city, with 317,500 residents, and for a period was the biggest coal port in the world. Today, with the country's traditional heavy industries (coal, steel, copper, tinplate and slate) either gone or in decline, Wales' economy depends on the public sector, light and service industries, and tourism.
Although Wales shares a close political and social history with the rest of Great Britain, it has retained a distinct cultural identity. Wales is officially bilingual, the Welsh and English languages having equal status. The Welsh language is an important element of Welsh culture, and its use is supported by national policy. Over 580,000 Welsh speakers live in Wales, more than 20% of the population. From the late 19th century onwards, Wales acquired its popular image as the "land of song", attributable in part to the revival of the eisteddfod tradition. At international sporting events, such as the FIFA World Cup, Rugby World Cup and the Commonwealth Games, Wales is represented by national teams regulated and organised by over fifty national governing bodies of sports in Wales. At the Olympic Games, Welsh athletes compete as part of a Great Britain team. Although football has traditionally been the more popular sport in north Wales, rugby union is seen as a symbol of Welsh identity and an expression of national consciousness.Iron is a chemical element with the symbol Fe (from Latin: ferrum) and atomic number 26. It is a metal in the first transition series. It is the most common element (by mass) forming the planet Earth as a whole, forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. Iron's very common presence in rocky planets like Earth is due to its abundant production as a result of fusion in high-mass stars, where the production of nickel-56 (which decays to iron) is the last nuclear fusion reaction that is exothermic. This allows radioactive nickel to become the last element to be produced before collapse of a supernova leads to events that scatters this precursor radionuclide of iron into space.
Thursday, December 15, 2011
The "Fourth Party"
It was not until 1878 that he came to public notice as the exponent of a species of independent Conservatism. He made a series of furious attacks on Sir Stafford Northcote, R. A. Cross, and other prominent members of the "old gang". George Sclater-Booth (afterwards 1st Baron Basing), President of the Local Government Board, was a specific target, and the minister's County Government Bill was fiercely denounced as the "crowning dishonour to Tory principles", and the "supreme violation of political honesty". Lord Randolph's attitude, and the vituperative fluency of his invective, made him a parliamentary figure of some importance before the dissolution of the 1874 parliament, though he was not yet taken quite seriously.
In the new parliament of 1880 he speedily began to play a more notable role. Along with Sir Henry Drummond-Wolff, Sir John Gorst and occasionally Arthur Balfour, he made himself known as the audacious opponent of the Liberal administration and the unsparing critic of the Conservative front bench. The "fourth party", as it was nicknamed, at first did little damage to the government, but awakened the opposition from its apathy; Churchill roused the Conservatives by leading resistance to Charles Bradlaugh, the member for Northampton, who, though an avowed atheist or agnostic, was prepared to take the parliamentary oath. Sir Stafford Northcote, the Conservative leader in the Lower House, was forced to take a strong line on this difficult question by the energy of the fourth party. The long controversy over Bradlaugh's seat, showed that Lord Randolph Churchill was a parliamentary champion who added to his audacity much tactical skill and shrewdness. He continued to play a conspicuous part throughout the parliament of 1880 to 1885, targeting William Ewart Gladstone as well as the Conservative front bench, some of whose members, particularly Sir Richard Cross and William Henry Smith, he singled out for attack.
From the beginning of the Egyptian imbroglio Lord Randolph was emphatically opposed to almost every step taken by the government. He declared that the suppression of Urabi Pasha's rebellion was an error, and the restoration of the khedive's authority a crime. He called Gladstone the "Moloch of Midlothian", for whom torrents of blood had been shed in Africa. He was equally severe on the domestic policy of the administration, and was particularly bitter in his criticism of the Kilmainham Treaty and the rapprochement between the Gladstonians and the Parnellites.
continue efforts
In the new parliament of 1880 he speedily began to play a more notable role. Along with Sir Henry Drummond-Wolff, Sir John Gorst and occasionally Arthur Balfour, he made himself known as the audacious opponent of the Liberal administration and the unsparing critic of the Conservative front bench. The "fourth party", as it was nicknamed, at first did little damage to the government, but awakened the opposition from its apathy; Churchill roused the Conservatives by leading resistance to Charles Bradlaugh, the member for Northampton, who, though an avowed atheist or agnostic, was prepared to take the parliamentary oath. Sir Stafford Northcote, the Conservative leader in the Lower House, was forced to take a strong line on this difficult question by the energy of the fourth party. The long controversy over Bradlaugh's seat, showed that Lord Randolph Churchill was a parliamentary champion who added to his audacity much tactical skill and shrewdness. He continued to play a conspicuous part throughout the parliament of 1880 to 1885, targeting William Ewart Gladstone as well as the Conservative front bench, some of whose members, particularly Sir Richard Cross and William Henry Smith, he singled out for attack.
From the beginning of the Egyptian imbroglio Lord Randolph was emphatically opposed to almost every step taken by the government. He declared that the suppression of Urabi Pasha's rebellion was an error, and the restoration of the khedive's authority a crime. He called Gladstone the "Moloch of Midlothian", for whom torrents of blood had been shed in Africa. He was equally severe on the domestic policy of the administration, and was particularly bitter in his criticism of the Kilmainham Treaty and the rapprochement between the Gladstonians and the Parnellites.
continue efforts
Tuesday, December 13, 2011
Roman Catholicism and Eastern Orthodoxy
According to Christian theology the only transcendent, almighty, and holy God, who cannot be approached or seen in essence or being, becomes immanent primarily in the God-man Jesus the Christ, who is the incarnate Second Person of the Trinity. In Eastern Orthodox theology the immanence of God is expressed as the hypostases or energies of God, who in his essence is incomprehensible and transcendent. In Catholic theology, Christ and the Holy Spirit immanently reveal themselves; God the Father only reveals himself immanently vicariously through the Son and Spirit, and the Divine Nature, the Godhead is wholly transcendent and unable to be comprehended.
This is most famously expressed in St. Paul's letter to the Philippians, where he writes:
Who, being in the form of God, thought it not robbery to be equal with God: But made himself of no reputation, and took upon him the form of a servant, and was made in the likeness of men: And being found in fashion as a man, he humbled himself, and became obedient unto death, even the death of the cross.[1]
The Holy Spirit is also expressed as an immanence of God.
and the Holy Spirit descended on him in bodily form like a dove. And a voice came from heaven: "You are my Son, whom I love; with you I am well pleased."[2]
The immanence of the triune God is celebrated in Roman Catholic and Eastern Orthodoxy during the liturgical calendar feast as the Theophany of God (see Feast of Theophany).
Pope Pius X wrote at length about philosophical-theological controversies over immanence in his encyclical Pascendi Dominici Gregis.
Also "immanentism." Immanentism is a theory which teaches that God is "an abstract mind or spirit which pervades the world."
In the theology of Karl Rahner, it is said that "the economic Trinity is the immanent Trinity, and the immanent Trinity is the economic Trinity." That is to say, God communicates Himself to humanity ("economic" Trinity) as He really is in the divine Life ("immanent" Trinity).
continue efforts
This is most famously expressed in St. Paul's letter to the Philippians, where he writes:
Who, being in the form of God, thought it not robbery to be equal with God: But made himself of no reputation, and took upon him the form of a servant, and was made in the likeness of men: And being found in fashion as a man, he humbled himself, and became obedient unto death, even the death of the cross.[1]
The Holy Spirit is also expressed as an immanence of God.
and the Holy Spirit descended on him in bodily form like a dove. And a voice came from heaven: "You are my Son, whom I love; with you I am well pleased."[2]
The immanence of the triune God is celebrated in Roman Catholic and Eastern Orthodoxy during the liturgical calendar feast as the Theophany of God (see Feast of Theophany).
Pope Pius X wrote at length about philosophical-theological controversies over immanence in his encyclical Pascendi Dominici Gregis.
Also "immanentism." Immanentism is a theory which teaches that God is "an abstract mind or spirit which pervades the world."
In the theology of Karl Rahner, it is said that "the economic Trinity is the immanent Trinity, and the immanent Trinity is the economic Trinity." That is to say, God communicates Himself to humanity ("economic" Trinity) as He really is in the divine Life ("immanent" Trinity).
continue efforts
Monday, December 12, 2011
Week News Abstract For SFP Series in 10GTEK: Cropping (animal)
Cropping is the removal of part or all of the pinnae or auricles, the external visible flap of the ear, of an animal. Most commonly performed on dogs, it is an ancient practice that was once done for perceived health, practical or cosmetic reasons. In modern times, it is banned in many nations, but where legal, it is usually performed for cosmetic reasons, usually related to show grooming. It is seen only certain breeds of dog such as the Pit bull, Doberman Pinscher, Schnauzer, Great Dane and Boxer.
The veterinary procedure is known as cosmetic otoplasty. Current veterinary science provides no medical, physical, environmental or cosmetic advantage to the animal from the procedure,leading to concerns over animal cruelty related to performing unnecessary surgery on the animals. In addition to the bans in place in countries around the world, it is described in some veterinary texts as "no longer considered ethical."
Cropping of large portions of the pinnae of other animals is rare, although the clipping of identifying shapes in the pinnae of livestock, called earmarks, were common prior to the introduction of compulsory ear tags.The practice of cropping for cosmetic purposes is rare in non-canines, although some selectively bred animals have naturally small ears which can be mistaken for cropping.
The Football League has been associated with a title sponsor since 1983. As this sponsor has changed over the years the league has been known in turn as the Canon League, the Today League, the Barclays League, the Endsleigh League, the Nationwide Football League and the Coca-Cola Football League, until the present sponsor npower was adopted in 2010, contracted until 2013.
continue efforts
The veterinary procedure is known as cosmetic otoplasty. Current veterinary science provides no medical, physical, environmental or cosmetic advantage to the animal from the procedure,leading to concerns over animal cruelty related to performing unnecessary surgery on the animals. In addition to the bans in place in countries around the world, it is described in some veterinary texts as "no longer considered ethical."
Cropping of large portions of the pinnae of other animals is rare, although the clipping of identifying shapes in the pinnae of livestock, called earmarks, were common prior to the introduction of compulsory ear tags.The practice of cropping for cosmetic purposes is rare in non-canines, although some selectively bred animals have naturally small ears which can be mistaken for cropping.
The Football League has been associated with a title sponsor since 1983. As this sponsor has changed over the years the league has been known in turn as the Canon League, the Today League, the Barclays League, the Endsleigh League, the Nationwide Football League and the Coca-Cola Football League, until the present sponsor npower was adopted in 2010, contracted until 2013.
continue efforts
Thursday, December 8, 2011
Week News Abstract For SFP Series in 10GTEK: Hunter-gatherer
A hunter-gatherer or forage society is one in which most or all food is obtained from wild plants and animals, in contrast to agricultural societies which rely mainly on domesticated species.
Hunting and gathering was the ancestral subsistence mode of Homo, and all modern humans were hunter-gatherers until around 10,000 years ago. Following the invention of agriculture hunter-gatherers have been displaced by farming or pastoralist groups in most parts of the world. Only a few contemporary societies are classified as hunter-gatherers, and many supplement, sometimes extensively, their foraging activity with farming and/or keeping animals.
The Wal-Mart camel is the fossil of a prehistoric camel (Camelops sp.) found at a Wal-Mart construction site in Mesa, Arizona in 2007. Workers digging a hole for an ornamental citrus tree found the bones of two (juvenile and infant) animals that may have lived as long as 10,000 years ago. Arizona State University Geology Museum curator Brad Archer calls it an important and rare find for the area.Wal-Mart officials and Greenfield Citrus Nursery owner John Babiarz whose crew discovered the remains agreed that the bones will go directly to the Geology Museum at Arizona State University where further research and restoration of the fossils could be done. Camels lived in what is now Arizona until about 8,000 years ago.More camel bones were found in Gilbert, Arizona in May 2008.
continue efforts
Hunting and gathering was the ancestral subsistence mode of Homo, and all modern humans were hunter-gatherers until around 10,000 years ago. Following the invention of agriculture hunter-gatherers have been displaced by farming or pastoralist groups in most parts of the world. Only a few contemporary societies are classified as hunter-gatherers, and many supplement, sometimes extensively, their foraging activity with farming and/or keeping animals.
The Wal-Mart camel is the fossil of a prehistoric camel (Camelops sp.) found at a Wal-Mart construction site in Mesa, Arizona in 2007. Workers digging a hole for an ornamental citrus tree found the bones of two (juvenile and infant) animals that may have lived as long as 10,000 years ago. Arizona State University Geology Museum curator Brad Archer calls it an important and rare find for the area.Wal-Mart officials and Greenfield Citrus Nursery owner John Babiarz whose crew discovered the remains agreed that the bones will go directly to the Geology Museum at Arizona State University where further research and restoration of the fossils could be done. Camels lived in what is now Arizona until about 8,000 years ago.More camel bones were found in Gilbert, Arizona in May 2008.
continue efforts
Tuesday, December 6, 2011
Economic versus biological resources
In economics a resource is defined as a commodity, service, or other asset used to produce goods and services that meet human needs and wants (see economic resource).Economics itself has been defined as the study of how society manages its scarce resources.Economics focuses on resource supply and demand as it influences production of goods and services to meet human needs and wants. Classical economics recognizes three categories of resources: land, labor, and capital.Together with entrepreneurship, land, labor, and capital are viewed as the four factors of production in neoclassical economics. Land includes all natural resources and is viewed as both the site of production and the source of raw materials. Labor or human resources consists of human effort provided in the creation of products, paid in wage. Capital consists of human-made goods or means of production (machinery, buildings, and other infrastructure) used in the production of other goods and services, paid in interest. Entrepreneurs serve as managers, risk-takers, leaders, and visionaries.In biology and ecology a resource is defined as a substance or object required by a living organism for normal growth, maintenance, and reproduction (see biological resource). Resources, such as food, water, or nesting sites, can be consumed by an organism and, as a result, become unavailable to other organisms. For animals key resources include food, water, and territory. For plants key resources include sunshine, nutrients, water, and a place to grow.
There are three fundamental differences between economic versus ecological views: the economic resource definition is human-centered (anthropocentric) and the ecological resource definition is nature-centered (biocentric or ecocentric); the economic view includes desire along with necessity, whereas the biological view is about basic biological needs; and economic systems are based on markets of currency exchanged for goods and services, whereas biological systems are based on natural processes of growth, maintenance, and reproduction.
contunue efforts
There are three fundamental differences between economic versus ecological views: the economic resource definition is human-centered (anthropocentric) and the ecological resource definition is nature-centered (biocentric or ecocentric); the economic view includes desire along with necessity, whereas the biological view is about basic biological needs; and economic systems are based on markets of currency exchanged for goods and services, whereas biological systems are based on natural processes of growth, maintenance, and reproduction.
contunue efforts
Sunday, December 4, 2011
Honeyeater
The honeyeaters are a large and diverse family of small to medium sized birds most common in Australia and New Guinea, but also found in New Zealand, the Pacific islands as far east as Samoa and Tonga, and the islands to the north and west of New Guinea known as Wallacea. Bali, on the other side of the Wallace Line, has a single species.
Honeyeaters and the Australian chats make up the family Meliphagidae. In total there are 182 species in 42 genera, roughly half of them native to Australia, many of the remainder occupying New Guinea. With their closest relatives, the Maluridae (Australian fairy-wrens), Pardalotidae (pardalotes), and Acanthizidae (thornbills, Australian warblers, scrubwrens, etc.) they comprise the superfamily Meliphagoidea and originated early in the evolutionary history of the oscine passerine radiation.
Although honeyeaters look and behave very much like other nectar-feeding passerines around the world (such as the sunbirds and flowerpeckers), they are unrelated, and the similarities are the consequence of convergent evolution.
The extent of the evolutionary partnership between honeyeaters and Australasian flowering plants is unknown, but probably substantial. A great many Australian plants are fertilised by honeyeaters, particularly the Proteaceae, Myrtaceae, and Epacridaceae. It is known that the honeyeaters are important in New Zealand as well, and assumed that the same applies in other areas.
continue efforts
Honeyeaters and the Australian chats make up the family Meliphagidae. In total there are 182 species in 42 genera, roughly half of them native to Australia, many of the remainder occupying New Guinea. With their closest relatives, the Maluridae (Australian fairy-wrens), Pardalotidae (pardalotes), and Acanthizidae (thornbills, Australian warblers, scrubwrens, etc.) they comprise the superfamily Meliphagoidea and originated early in the evolutionary history of the oscine passerine radiation.
Although honeyeaters look and behave very much like other nectar-feeding passerines around the world (such as the sunbirds and flowerpeckers), they are unrelated, and the similarities are the consequence of convergent evolution.
The extent of the evolutionary partnership between honeyeaters and Australasian flowering plants is unknown, but probably substantial. A great many Australian plants are fertilised by honeyeaters, particularly the Proteaceae, Myrtaceae, and Epacridaceae. It is known that the honeyeaters are important in New Zealand as well, and assumed that the same applies in other areas.
continue efforts
Thursday, December 1, 2011
Indian Ocean
The Indian Ocean is the third largest of the world's oceanic divisions, covering approximately 20% of the water on the Earth's surface.[1] It is bounded on the north by the Indian Subcontinent and Arabian Peninsula (or, more generally, by southern and western Asia); on the west by eastern Africa; on the east by Indochina, the Sunda Islands, and Australia; and on the south by the Southern Ocean (or, depending on definition, by Antarctica). The ocean is named after the geographic location of India.
As one component of the interconnected global ocean, the Indian Ocean is delineated from the Atlantic Ocean by the 20° east meridian running south from Cape Agulhas, and from the Pacific by the meridian of 146°55' east.The northernmost extent of the Indian Ocean is approximately 30° north in the Persian Gulf. The Indian Ocean has asymmetric ocean circulation[citation needed]. This ocean is nearly 10,000 kilometres (6,200 mi) wide at the southern tips of Africa and Australia; its area is 73,556,000 square kilometres (28,350,000 sq mi),including the Red Sea and the Persian Gulf.
The ocean's volume is estimated to be 292,131,000 cubic kilometres (70,086,000 mi3).[8] Small islands dot the continental rims. Island nations within the ocean are Madagascar, the world's fourth largest island; Reunion Island; Comoros; Seychelles; Maldives; Mauritius; and Sri Lanka. The archipelago of Indonesia borders the ocean on the east.
continue efforts
As one component of the interconnected global ocean, the Indian Ocean is delineated from the Atlantic Ocean by the 20° east meridian running south from Cape Agulhas, and from the Pacific by the meridian of 146°55' east.The northernmost extent of the Indian Ocean is approximately 30° north in the Persian Gulf. The Indian Ocean has asymmetric ocean circulation[citation needed]. This ocean is nearly 10,000 kilometres (6,200 mi) wide at the southern tips of Africa and Australia; its area is 73,556,000 square kilometres (28,350,000 sq mi),including the Red Sea and the Persian Gulf.
The ocean's volume is estimated to be 292,131,000 cubic kilometres (70,086,000 mi3).[8] Small islands dot the continental rims. Island nations within the ocean are Madagascar, the world's fourth largest island; Reunion Island; Comoros; Seychelles; Maldives; Mauritius; and Sri Lanka. The archipelago of Indonesia borders the ocean on the east.
continue efforts
Subscribe to:
Posts (Atom)