Is Race a Natural Kind - Free Essay Example

Introduction Natural kind forms a scientific discipline that is frequently divided to derive the actual meaning. Majorly, the scientific study offers two perceptive, one that entails the naturalness of a kind and the kindhood. The naturalness of a kind tries to establish whether the naturalness of a kind is what makes it natural. On the other hand, the kindhood offers a different understanding in that it entails finding out whether the components that make up a thing is what makes it natural (Porcher 2016, 212). However, in consideration of both studies, the naturalness of an element corresponds to the structure of the natural environment, and not on the human interests and actions. Therefore, it is by logical assumption that science has succeeded in revealing all the natural occurrences whereas the classification and the taxonomies are all by scientific realism. As a result, psychology can easily reverse on the kinds that it holds as natural. Therefore, there is a significant connectedness between the study of natural kinds and realism. The realistic position on natural kinds In this regard, realism refers to the view of the existence of entities in natural kinds. On the other hand, naturalism refers to the presence of natural groupings with distinctions among them. Therefore, naturalism has no ontological commitment while realism is an ontologically committed type of view. Notably, the realistic position maintains on the fact that it is not possible to explain the differences between the natural and the non-natural groupings without considering entities in natural kinds. (Franklin-Hall and Laura 2015, 928) Different theories on natural kinds exist and efficiently compete to offer a well-developed concept. Firstly, the cluster of natural kinds is usually developed according to similar objectives and common properties which form a single group. It is challenging to determine a natural kind in realism as opposed to conventional. Therefore, a suitable way to draw an appropriate distinction is through the similarities and the standard features while the later majorly depends on the human interests. Secondly, natural kinds are believed to have essences. According to (Magnus 2015, 7), essence refers to a membership-determining a given property which is not only necessary but also sufficient enough to belong to a specific group. However, the theories fail to agree on the way essential characteristics in a kind. Whereas, the fundamental properties are responsible for other features associated with the type. For instance, having an atomic number 79 makes something a member of a particular group. However, there are other properties regarding color, mass and density. Phenotypical features are sufficient to pick out a natural kind Evidently, contemporary philosophers in the field of biology held for the longest time that biological species are insufficient to be regarded as natural kinds. However, organic features, for instance, phenotypical features are sufficient enough to pick out a natural kind (Marti ­nez 2015, 99). As a result, incorporation of biological characteristics in natural kind offers an in-depth understanding of natural kinds. Notably, it provides that natural kind involves the cases of spatiotemporally of which are not accidental and resemble each other to form a whole species. Majorly, the controversy regarding the biological aspect and the natural kind occurs due to lack of documentation of any limitation concerning the point in place and time where the natural kind happened. However, instances of any natural kind could occur anywhere and at any time. Therefore, a biological perspective of the natural kind offers a standardized characterization. It defines the natural sort as a collection of objects or individuals with similar properties non-accidentally clustered together. Evidently, biological species are also natural kinds. For any organic classification, there is a plurality of traits, phenotypic or genotypic. The attributes play a critical role individually and collectively (Kidwell and Kimberlee, et al. 2015, 29). As a result, their input in such a species is necessary and sufficient. It universally agreed that phenotypic traits are natural kinds. However, one reason that claims it unreasonable is the dimorphism. Notably, in every species, there are abnormal or aberrant members who phenotypic traits are the actual reflection of confined genotypic variations. Indeed, it is evident that biological species are among the natural kinds. Their instances happen to be scattered in space and in time, therefore a typical example in which a collection of cases join together to develop one common reason. A substitute for what picks out the natural kind The similarity relations majorly determine the spontaneous nature. The connections, however, have been defined differently based on their branch of science. For instance, the subject will establish the similarity based on the field they operate. Notably, biology is expected to identify the similarities between the organisms found in the genealogical information or common genes. Therefore, apart from phenotypical classification, the similarities can be reduced to an allele (1000 Genomes Project Consortium 2015, 70). In this regard, some organisms will be more genetically similar. This would drop out resemblance as a genetic concept to a more specific notion; determine the similarity in molecules and genes. Evidently, any similarity between the constituents conforms to the idea of the natural kind. In this regard, nature kind classification based on the allele or the genetic concepts enables appropriate classification. Additionally, it allows getting rid of the many paradigms in the natural kinds which do not count as physical kinds. For instance, the private allele in Native Americans is a pattern in the population genetics natural kind. However, an individual allele offers uniqueness in one of the populations from the entire selection of communities. Therefore, the presence of the Native American society determines the existence of the private allele. Provide at least one objection to the realist position The realistic stand has been for the longest time suffered a complaint from the anti-realist. The antirealism holds a contradicting view in stipulating that theories are untrue and the majority ought to be disregarded. Evidently, the realistic position provides that oak is a natural kind, while a table is not. Therefore, whenever the question to determine what makes natural and non-natural nature, then no answer. As a result, it has proven challenging to develop responses to so, vital clues regarding the natural kind. Currently, developing the answers to the simple questions is yet to be achieved. According to Ludwig (2017, 35), he has given up on the term natural since so far; there is nothing like natural. According to antirealist, they consider that realists generalize all classes of natural kinds and capture a general philosophical advantage of natural kinds. Additionally, they attract natural types in such a manner that they avoid metaphysics. Notably, some of the most significant theories, for instance, Newtons laws have been proved wrong. Additionally, Darwins natural selection and relativity by Einstein still need some modification and develop some adaptation to make them appropriate (Garci ­a del Muro Navarro 2017, 29). Therefore, antirealists strongly believe that theories are merely tools of which people use after being approved to be wrong. According to antirealists, most of what them think to be the cause of the world based on the minds ability to create precise features or offer characteristics on what they perceive. Why realism about race is better than conventionalism Notably, there nothing in particular that makes a natural kind natural. However, some philosophers have denied this assumption and insisted that a natural kind is relative to a specific inquiry. Therefore, race lacks any biological contradictions between members of other races (Winther 2014, 215). As a result, it may be untrue to conclude that race is not a natural kind. Realism refers to that position attributed to positive ontological status. So when one is a realist about the race, that means the race is real and contains several physical attributes. On the other hand, conventionalist is not constant. Humans are not genetically grounded, however; they usually form due to social practices. Hence, races are adopted based on some broad genetic dissimilarity among some populations. Moreover, the color creates only an outward manifestation. As a result, the realism stand about race is more convincing unlike conventionalism. In conclusion, natural kind forms a scientific discipline that is frequently divided to derive the actual meaning. Majorly, the scientific study offers two perceptive, one that entails the naturalness of a kind and the kindhood. Notably, the realistic position on natural kinds provides that it is not possible to explain the differences between the natural and the non-natural groupings without considering entities in natural kinds. Therefore, a suitable way to draw an appropriate distinction is through the similarities and the standard features. Moreover, phenotypical features are sufficient enough to pick out a natural kind. As a result, incorporation of biological characteristics in natural kind offers an in-depth understanding of natural kinds. Nature kind classification based on the allele or the genetic concepts enables appropriate classification offer a suitable substitute what picks natural kind. Majorly, anti-realist offers the major objection to realist and consider majority of the theories as untrue. However, when one is a realist about the race, that means the race is real and contains several physical attributes. Works Cited 1000 Genomes Project Consortium. A global reference for human genetic variation. Nature 526.7571 (2015): 68-74. Franklin-Hall, Laura R. Natural kinds as categorical bottlenecks. Philosophical Studies 172.4 (2015): 925-948. Garci ­a del Muro Navarro, Juan. The Evolution of Ecosystems through Genetic Algorithms and Neural Networks. (2017).24-41 Kidwell, Kimberlee Kae, et al. Glyphosate-tolerant wheat genotypes. U.S. Patent No. 8,927,834. 6 Jan. 2015.7-24 Ludwig, David. Letting go ofNatural Kind. Towards a Multidimensional Framework of Non-Arbitrary Classification Philosophy of Science. (2017). 34-66 Magnus, P. D. Taxonomy, ontology, and natural kinds. Synthese (2015): 1-13. Martinez, Manolo. Informationally-connected property clusters, and polymorphism. Biology Philosophy 30.1 (2015): 99-117. Porcher, Jose Eduardo. Delusion as a folk psychological kind. Filosofia Unisinos? 17.2 (2016): 212. Winther, Rasmus Grinfeldt. The Genetic Reification of Race?: A Story of Two Mathematical Methods. Critical Philosophy of Race 2.2 (2014): 204-223.

Best Term Paper Writing Services - How to Find the Best Paid Online Company

Best Term Paper Writing Services - How to Find the Best Paid Online CompanyMany online sources of information are filled with advertisements and advertisement rates for term paper writing services. There are numerous payment options, including fixed, variable, per-paper or per-page, and you can also opt for private billers and personal correspondents. The advertisement includes much information about the services that are provided, the number of copies, the cost per copy, delivery costs, time period, number of revisions, etc.However, there are certain specific course of action that you should take to look for the best term paper writing services. You should decide on a minimum limit for each customer, for example, you can choose the minimum number of words per customer. This is important because these include facts, legal or other documents and also the details of past and present processes of your company.It is always better to avoid signing up for any service, even if it is for pro fessional term paper writing services, if you are uncertain as to how to choose the one that best suits your company. A well-known article for the Internet about online term paper writing services states that the main purpose of an online quote is to make the process easier. In a more or less informative article on the internet, it was mentioned that these companies are geared towards converting a client into a loyal customer. Therefore, they maintain reasonable charges to enable customers to perform their essential role, which is to make the process of writing a term paper easier.This gives you an opportunity to save some money if you are in a position to pay a good rate. If you find that your company has limited funds to pay a reasonable price, then you can search for the alternative solutions, such as requesting quotations, or searching for a quote from a freelance writer who will make the process of writing more efficient.It is possible that, if you don't want to pay for a new p aper every month, you should look for quotes from freelance writers. Although, you might not get the same quality of paper writing service as that of a professional writer, you can still save some money. If you are willing to write the paper yourself, then you may have to pay for the rate, but this is not likely to be very expensive. There are many freelance writers on the internet, and there are also numerous sites that offer you all the relevant information about terms of service.If you really want to avail of a professional term paper writing service, you can search the World Wide Web for a term paper writing service provider. The requirements of a regular client may vary with the nature of the paper and may even depend on the situation. The description of the job can also vary; so, you need to evaluate this properly before deciding on a certain service provider.Most of the things can be acquired on the internet and can make it easier for you to make the best decision. You may al so get the opportunity to communicate with various companies through various websites and emails. You just need to bear in mind that, these businesses depend on customers to fulfil their requirement, so you should look for a reliable online company. This can be the best time to look for the best term paper writing services and pay at a suitable rate.

Biography of Thomas Gage, British Army General

Thomas Gage (March 10, 1718 or 1719–April 2, 1787) was a British Army general who commanded troops during the beginning of the American Revolution. Prior to this, he served as the colonial governor of Massachusetts Bay. In 1775, he was replaced as the British military commander-in-chief by General William Howe. Fast Facts: Thomas Gage Known For: Gage commanded British Army forces during the early stages of the American Revolution.Born: March 10, 1718 or 1719 in Firle, EnglandParents: Thomas Gage and Benedicta Maria Teresa HallDied: April 2, 1787 in London, EnglandEducation: Westminster SchoolSpouse: Margaret Kemble Gage (m. 1758)Children: Henry Gage, William Gage, Charlotte Gage, Louisa Gage, Marion Gage, Harriet Gage, John Gage, Emily Gage Early Life The second son of the 1st Viscount Gage and Benedicta Maria Teresa Hall, Thomas Gage was born in Firle, England, in 1718 or 1719. At the Westminster School, he became friends with John Burgoyne, Richard Howe, and the future Lord George Germain. Gage developed a fierce attachment to the Anglican Church and a deep distaste for Roman Catholicism. After leaving school, he joined the British Army as an ensign and commenced recruiting duties in Yorkshire. Flanders and Scotland In 1741, Gage purchased a commission as a lieutenant in the 1st Northampton Regiment.  The following year, in May 1742, he transferred to Battereaus Foot Regiment with the rank of captain-lieutenant. In 1743, Gage was promoted to captain and joined the Earl of Albemarles staff as an aide-de-camp in Flanders for service during the War of the Austrian Succession. With Albemarle, Gage saw action during the Duke of Cumberlands defeat at the Battle of Fontenoy. Shortly thereafter, he, along with the bulk of Cumberlands army, returned to Britain to deal with the Jacobite Rising of 1745. Gage served in Scotland during the Culloden campaign. Peacetime After campaigning with Albemarle in the Low Countries from 1747 to 1748, Gage was able to purchase a commission as a major. After moving to Colonel John Lees 55th Regiment of Foot, Gage began a long friendship with future American general Charles Lee. A member of Whites Club in London, he proved popular with his peers and cultivated important political connections. With the 55th, Gage proved himself an able leader and was promoted to lieutenant colonel in 1751. Two years later, he mounted a campaign for Parliament but was defeated in the election of April 1754. After remaining in Britain another year, Gage and his regiment, re-designated the 44th, was sent to North America in to take part in General Edward Braddocks campaign against Fort Duquesne during the French and Indian War. Service in America Braddocks army moved slowly as it sought to cut a road through the wilderness. On July 9, 1755, the British column neared its target from the southeast with Gage leading vanguard. Spotting a mixed force of French and Native Americans, his men initiated the Battle of the Monongahela. The engagement quickly went against the British and in several hours of fighting, Braddock was killed and his army routed. In the course of the battle, the commander of the 44th, Colonel Peter Halkett, was killed and Gage was slightly wounded. Following the battle, Captain Robert Orme accused Gage of poor field tactics. While the accusations were dismissed, it prevented Gage from receiving permanent command of the 44th. In the course of the campaign, he became acquainted with George Washington and the two men stayed in contact for several years after the battle. After a role in a failed expedition along the Mohawk River intended to resupply Fort Oswego, Gage was sent to Halifax, Nova Scotia, to take part in an abortive attempt against the French fortress of Louisbourg. There, he received permission to raise a regiment of light infantry for service in North America. New York Frontier Promoted to colonel in December 1757, Gage spent the winter in New Jersey recruiting for his new unit. On July 7, 1758, Gage led his new command against Fort Ticonderoga as part of Major General James Abercrombies failed attempt to capture the fortress. Slightly wounded in the attack, Gage, with some assistance from his brother Lord Gage, was able to secure promotion to brigadier general. In New York City, Gage met with Jeffery Amherst, the new British commander-in-chief in America. While in the city, he married Margaret Kemble on December 8, 1758. The following month, Gage was appointed to command Albany and its surrounding posts. Montreal Amherst gave Gage command of British forces on Lake Ontario with orders to capture Fort La Galette and Montreal. Concerned that expected reinforcements from Fort Duquesne had not arrived, Gage suggested reinforcing Niagara and Oswego instead while Amherst and Major General James Wolfe moved into Canada. This lack of aggression was noted by Amherst and when the attack on Montreal was launched, Gage was placed in command of the rear guard. Following the citys capture in 1760, Gage was installed as military governor. Though he disliked Catholics and Native Americans, he proved an able administrator. Commander-in-Chief In 1761, Gage was promoted to major general and two years later returned to New York as acting commander-in-chief. The appointment was made official on November 16, 1764. As the new commander-in-chief in America, Gage inherited a Native American uprising known as Pontiacs Rebellion. Though he sent out expeditions to deal with the Native Americans, he also pursued diplomatic solutions to the conflict as well. After two years of sporadic fighting, a peace treaty was signed in July 1766. At the same time, however, tensions were rising in the colonies due to a variety of taxes imposed by London. Revolution Approaches In response to the outcry raised against the 1765 Stamp Act, Gage began recalling troops from the frontier and concentrating them in coastal cities, particularly New York. To accommodate his men, Parliament passed the Quartering Act (1765), which allowed troops to be housed in private residences. With the passage of the 1767 Townshend Acts, the focus of resistance shifted north to Boston, and Gage responded by sending troops to that city. On March 5, 1770, the situation came to a head with the Boston Massacre. After being taunted, British troops fired into a crowd, killing five civilians.  Gages understanding of the underlying issues evolved during this time.  Initially thinking the unrest to be the work of a small number of elites, he later came to believe that the problem was the result of democracy in colonial governments. In 1772, Gage requested a leave of absence and returned to England the following year. He missed the Boston Tea Party (December 16, 1773) and the outcry in response to the Intolerable Acts. Having proven himself an able administrator, Gage was appointed to replace Thomas Hutchinson as governor of Massachusetts on April 2, 1774. Gage was initially well received, as Bostonians were happy to be rid of Hutchinson. His popularity quickly began to decline, though, as he moved to implement the Intolerable Acts. With tensions increasing, Gage began a series of raids in September to seize colonial munitions. While an early raid on Somerville, Massachusetts, was successful, it touched off the Powder Alarm, which saw thousands of colonial militiamen mobilize and move toward Boston.  Though later dispersed, the event had an impact on Gage. Concerned about not escalating the situation, Gage did not attempt to quash groups such as the Sons of Liberty and was criticized by his own men for being too lenient as a result. In April 1775, Gage ordered 700 men to march to Concord to capture colonial powder and guns. On the way, active fighting began at Lexington and was continued at Concord. Though British troops were able to clear each town, they sustained heavy casualties during their march back to Boston. Following the fighting at Lexington and Concord, Gage found himself besieged in Boston by a growing colonial army. Concerned that his wife, a colonial by birth, was aiding the enemy, Gage sent her away to England. Reinforced in May by 4,500 men under Major General William Howe, Gage began planning a breakout. This was thwarted in June when colonial forces fortified Breeds Hill north of the city. In the resulting Battle of Bunker Hill, Gages men were able to capture the heights but sustained over 1,000 casualties in the process. That October, Gage was recalled to England and Howe was given temporary command of the British forces in America. Death In England, Gage reported to Lord George Germain, now the Secretary of State of the American Colonies, that a large army would be necessary to defeat the Americans and that foreign troops would need to be hired. In April 1776, a command was permanently given to Howe and Gage was placed on the inactive list. He remained in semi-retirement until April 1781, when Amherst called upon him to raise troops to resist a possible French invasion. Promoted to general on November 20, 1782, Gage saw little active service and died at the Isle of Portland on April 2, 1787. Legacy Gage was survived by his wife and five children. His son Henry went on to become a British Army officer and member of Parliament, while his son William became a commander in the British Navy. The Canadian village of Gagetown was named after him.

The Earths Crust Everything You Need to Know

The Earths crust is an extremely thin layer of rock that makes up the outermost solid shell of our planet. In relative terms, its thickness is like that of the skin of an apple. It amounts to less than half of 1 percent of the planets total mass but plays a vital role in most of Earths natural cycles.   The crust can be thicker than 80 kilometers in some spots and less than one kilometer thick in others. Underneath it lies  the mantle, a layer of silicate rock approximately 2700 kilometers thick. The mantle accounts for the bulk of the Earth. The crust is composed of many different types of rocks that fall into three main categories: igneous, metamorphic and sedimentary. However, most of those rocks originated as either granite or basalt. The mantle beneath is made of peridotite. Bridgmanite, the most common mineral on Earth, is found in the deep mantle.   How We Know the Earth Has a Crust We didnt know the Earth had a crust until the early 1900s. Up until then, all we knew was that our planet wobbles in relation to the sky as if it had a large, dense core  -- at least, astronomical observations told us so. Then along came seismology, which brought us a new type of evidence from below: seismic velocity. Records of seismic waves allow seismologists to locate and measure the size of events like these, and to map the Earths internal structure. jamesbenet/Getty Images   Seismic velocity measures the speed at which earthquake waves propagate through the different materials (i.e. rocks) below the surface. With a few important exceptions, seismic velocity within the Earth tends to increase with depth.   In 1909, a paper by the seismologist Andrija Mohorovicic established a sudden change in seismic velocity -- a discontinuity of some sort -- about 50 kilometers deep in the Earth. Seismic waves bounce off it (reflect) and bend (refract) as they go through it, the same way that light behaves at the discontinuity between water and air. That discontinuity named the Mohorovicic discontinuity or Moho is the accepted boundary between the crust and mantle. Crusts and Plates The crust and tectonic plates  are not the same. Plates are thicker than the crust and consist of the crust plus the shallow mantle just beneath it. This stiff and brittle two-layered combination is called the ​lithosphere (stony layer in scientific Latin). The lithospheric plates lie on a layer of softer, more plastic mantle rock called the asthenosphere (weak layer). The asthenosphere allows the plates to move slowly over it like a raft in thick mud.   We know that the Earths outer layer is made of two grand categories of rocks: basaltic and granitic. Basaltic rocks underlie the seafloors and granitic rocks make up the continents. We know that the seismic velocities of these rock types, as measured in the lab, match those seen in the crust down as far as the Moho. Therefore were confident that the Moho marks a real change in rock chemistry. The Moho isnt a perfect boundary because some crustal rocks and mantle rocks can masquerade as the other. However, everyone who talks about the crust, whether in seismological or petrological terms, fortunately, means the same thing. In general, then, there are two kinds of crust: oceanic crust (basaltic) and continental crust (granitic). Oceanic Crust An illustration of oceanic crust. Dorling Kindersley/Getty Images   Oceanic crust covers about 60 percent of the Earths surface. Oceanic crust is thin and young -- no more than about 20 km thick and no older than about 180 million years. Everything older has been pulled underneath the continents by subduction. Oceanic crust is born at the mid-ocean ridges, where plates are pulled apart. As that happens, the pressure upon the underlying mantle is released and the peridotite there responds by starting to melt. The fraction that melts becomes basaltic lava, which rises and erupts while the remaining peridotite becomes depleted. The mid-ocean ridges migrate over the Earth like Roombas, extracting this basaltic component from the peridotite of the mantle as they go. This works like a chemical refining process. Basaltic rocks contain more silicon and aluminum than the peridotite left behind, which has more iron and magnesium. Basaltic rocks are also less dense. In terms of minerals, basalt has more feldspar and amphibole, less olivine and pyroxene, than peridotite. In geologists shorthand, oceanic crust is mafic while oceanic mantle is ultramafic. Oceanic crust, being so thin, is a very small fraction of the Earth -- about 0.1 percent -- but its life cycle serves to separate the contents of the upper mantle into a heavy residue and a lighter set of basaltic rocks. It also extracts the so-called incompatible elements, which dont fit into mantle minerals and move into the liquid melt. These, in turn, move into the continental crust as plate tectonics proceeds. Meanwhile, the oceanic crust reacts with seawater and carries some of it down into the mantle. Continental Crust Continental crust is thick and old -- on average about 50 km thick and about 2 billion years old -- and it covers about 40 percent of the planet. Whereas almost all of the oceanic crust is underwater, most of the continental crust is exposed to the air. The continents slowly grow over geologic time as oceanic crust and seafloor sediments are pulled beneath them by subduction. The descending basalts have the water and incompatible elements squeezed out of them, and this material rises to trigger more melting in the so-called subduction factory. The continental crust is made of granitic rocks, which have even more silicon and aluminum than the basaltic oceanic crust. They also have more oxygen thanks to the atmosphere. Granitic rocks are even less dense than basalt. In terms of minerals, granite has even more feldspar and less amphibole than basalt and almost no pyroxene or olivine. It also has abundant quartz. In geologists shorthand, continental crust is felsic. Continental crust makes up less than 0.4 percent of the Earth, but it represents the product of a double refining process, first at mid-ocean ridges and second at subduction zones. The total amount of continental crust is slowly growing. The incompatible elements that end up in the continents are important because they include the major radioactive elements uranium, thorium, and potassium. These create heat, which makes the continental crust act like an electric blanket on top of the mantle. The heat also softens thick places in the crust, like the Tibetan Plateau, and makes them spread sideways. Continental crust is too buoyant to return to the mantle. Thats why it is, on average, so old. When continents collide, the crust can thicken to almost 100 km, but that is temporary because it soon spreads out again. The relatively thin skin of limestones and other sedimentary rocks tend to stay on the continents, or in the ocean, rather than return to the mantle. Even the sand and clay that is washed off into the sea returns to the continents on the conveyor belt of the oceanic crust. Continents are truly permanent, self-sustaining features of the Earths surface. What the Crust Means The crust is a thin but important zone where dry, hot rock from the deep Earth reacts with the water and oxygen of the surface, making new kinds of minerals and rocks. Its also where plate-tectonic activity mixes and scrambles these new rocks and injects them with chemically active fluids. Finally, the crust is the home of life, which exerts strong effects on rock chemistry and has its own systems of mineral recycling. All of the interesting and valuable variety in geology, from metal ores to thick beds of clay and stone, finds its home in the crust and nowhere else. It should be noted that the Earth isnt the only planetary body with a crust. Venus, Mercury, Mars and the Earths Moon have one as well.   Edited by Brooks Mitchell

American Revolution - New York, Philadelphia, Saratoga

Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South The War Shifts to New York Having captured Boston in March 1776, General George Washington began shifting his army south to block an anticipated British move against New York City. Arriving, he divided his army between Long Island and Manhattan and awaited British General William Howes next move. In early June, the first British transports began appearing in lower New York Harbor and Howe established camps on Staten Island. Over the next several weeks Howes army grew to over 32,000 men. His brother, Vice Admiral Richard Howe commanded the Royal Navys forces in the area and stood by to provide naval support. The Second Continental Congress Independence While the British amassed strength near New York, the Second Continental Congress continued to meet in Philadelphia. Convening in May 1775, the group contained representatives from all thirteen American colonies. In final effort to reach an understanding with King George III, the Congress drafted the Olive Branch Petition on July 5, 1775, which asked the British government to address their grievances in order to avoid further bloodshed. Arriving in England, the petition was discarded by the king who was angered by the language used in confiscated letters written by American radicals such as John Adams. The failure of the Olive Branch Petition gave strength to those elements in Congress that wished to press for full independence. As the war continued, Congress began to assume the role of a national government and worked to make treaties, supply the army, and build a navy. Since it lacked the ability to tax, Congress was forced to rely on the governments of the individual colonies to provide the needed money and goods. In early 1776, the pro-independence faction began to assert more influence and pressured colonial governments to authorize reluctant delegations to vote for independence. After extended debate, Congress passed a resolution for independence on July 2, 1776. This was followed by the approval of the Declaration of Independence two days later. The Fall of New York In New York, Washington, who lacked naval forces, remained concerned that Howe could outflank him by sea anywhere in the New York area. Despite this, he felt compelled to defend the city due to its political importance. On August 22, Howe moved around 15,000 men across to Gravesend Bay on Long Island. Coming ashore, they probed the American defenses along the Heights of Guan. Finding an opening at Jamaica Pass, the British moved through the heights on the night of August 26/27 and struck American forces the next day. Caught by surprise, American troops under Major General Israel Putnam were defeated in the resulting Battle of Long Island. Falling back to a fortified position on Brooklyn Heights, they were reinforced and joined by Washington. Though aware that Howe could cut him off from Manhattan, Washington was initially reluctant to abandon Long Island. Approaching Brooklyn Heights, Howe turned cautious and ordered his men to begin siege operations. Realizing the dangerous nature of his situation, Washington left the position on the night of August 29/30 and succeeded in moving his men back to Manhattan. On September 15, Howe landed on Lower Manhattan with 12,000 men and at Kips Bay with 4,000. This forced Washington to abandon the city and assume a position to the north at Harlem Heights. The next day his men won their first victory of the campaign in the Battle of Harlem Heights. With Washington in a strong fortified postion, Howe elected to move by water with part of his command to Throgs Neck and then on to Pells Point. With Howe operating to the east, Washington was forced to abandon his position on northern Manhattan for fear of being cut off. Leaving strong garrisons at Fort Washington on Manhattan and Fort Lee in New Jersey, Washington withdrew to a strong defensive position at White Plains. On October 28, Howe assaulted part of Washingtons line at the Battle of White Plains. Driving the Americans off of a key hill, Howe was able to compel Washington to retreat again. Rather than pursue the fleeing Americans, Howe turned south to consolidate his hold on the New York City area. Assaulting Fort Washington, he captured the fortification and its 2,800-man garrison on November 16. While Washington was criticized for attempting to hold the post, he did so on Congress orders. Major General Nathanael Greene, commanding at Fort Lee, was able to escape with his men before being attacked by Major General Lord Charles Cornwallis. The Battles of Trenton Princeton Having taken Fort Lee, Cornwallis was ordered to pursue Washingtons army across New Jersey. As they retreated, Washington faced a crisis as his battered army began to disintegrate through desertions and expiring enlistments. Crossing the Delaware River into Pennsylvania in early December, he made camp and attempted to reinvigorate his shrinking army. Reduced to around 2,400 men, the Continental Army was poorly supplied and ill-equipped for winter with many of the men still in summer uniforms or lacking shoes. As in the past, Howe displayed a lack of killer instinct and ordered his men into winter quarters on December 14, with many strung out in a series of outposts from New York to Trenton. Believing an audacious act was needed to restore the publics confidence, Washington planned a surprise attack on the Hessian garrison at Trenton for December 26. Crossing the ice-filled Delaware on Christmas night, his men struck the following morning and succeeded in defeating and capturing the garrison. Evading Cornwallis who had been sent to catch him, Washingtons army won a second victory at Princeton on January 3, but lost Brigadier General Hugh Mercer who was mortally wounded. Having achieved two unlikely victories, Washington moved his army to Morristown, NJ and entered winter quarters. Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South Burgoynes Plan In the spring of 1777, Major General John Burgoyne proposed a plan for defeating the Americans. Believing that New England was the seat of the rebellion, he proposed cutting the region off from the other colonies by moving down the Lake Champlain-Hudson River corridor while a second force, led by Colonel Barry St. Leger, advanced east from Lake Ontario and down the Mohawk River. Meeting at Albany, Burgoyne and St. Leger would press down the Hudson, while Howes army advanced north. Though approved by Colonial Secretary Lord George Germain, Howes role in the plan was never clearly defined and issues of his seniority precluded Burgoyne from issuing him orders. The Philadelphia Campaign Operating on his own, Howe prepared his own campaign for capturing the American capital at Philadelphia. Leaving a small force under Major General Henry Clinton at New York, he embarked 13,000 men on transports and sailed south. Entering the Chesapeake, the fleet traveled north and the army landed at Head of Elk, MD on August 25, 1777. In position with 8,000 Continentals and 3,000 militia to defend the capital, Washington dispatched units to track and harass Howes army. Aware that he would have to face Howe, Washington prepared to make a stand along the banks of the Brandywine River. Forming his men in a strong position near Chadds Ford, Washington awaited the British. In surveying the American position on September 11, Howe elected to use the same strategy he employed at Long Island. Using Lieutenant General Wilhelm von Knyphausens Hessians, Howe fixed the American center in place along the creek with a diversionary attack, while marching the bulk of this army around Washingtons right flank. Attacking, Howe was able to drive the Americans from the field and captured the bulk of their artillery. Ten days later, Brigadier General Anthony Waynes men were beaten at the Paoli Massacre. With Washington defeated, Congress fled Philadelphia and reconvened at York, PA. Outmaneuvering Washington, Howe entered the city on September 26. Eager to redeem the defeat at Brandywine and re-take the city, Washington began planning a counterattack against British forces located at Germantown. Devising a complicated assault plan, Washingtons columns became delayed and confused in the thick morning fog on October 4. In the resulting Battle of Germantown, American forces achieved early success and were on the verge of a great victory before confusion in the ranks and strong British counterattacks turned the tide. Among those who had performed badly at Germantown was Major General Adam Stephen who had been drunk during the fighting. Not hesitating, Washington sacked him in favor of the promising young Frenchmen, the Marquis de Lafayette, who had recently joined the army. With the campaign season winding down, Washington moved the army to Valley Forge for winter quarters. Enduring a hard winter, the American army underwent extensive training under the watchful eye of Baron Friedrich Wilhelm von Steuben. Another foreign volunteer, von Steuben had served as a staff officer in the Prussian army and imparted his knowledge to the Continental forces. The Tide Turns at Saratoga While Howe was planning his campaign against Philadelphia, Burgoyne moved forward with the other elements of his plan. Pressing down Lake Champlain, he easily captured Fort Ticonderoga on July 6, 1777. As a result, Congress replaced the American commander in the area, Major General Philip Schuyler, with Major General Horatio Gates. Pushing south, Burgoyne won minor victories at Hubbardton and Fort Ann and elected to move overland towards the American position at Fort Edward. Moving through the forest, Burgoynes progress was slowed as the Americans felled tree across the roads and worked to obstruct the British advance. To the west, St. Leger laid siege to Fort Stanwix on August 3, and defeated an American relief column at the Battle of Oriskany three days later. Still commanding the American army, Schuyler dispatched Major General Benedict Arnold to break the siege. As Arnold approached, St. Legers Native American allies fled after hearing exaggerated accounts regarding the size of Arnolds force. Left on his own, St. Leger had no choice but to retreat west. As Burgoyne neared Fort Edward, the American army fell back to Stillwater. Though he had won several minor victories, the campaign had cost Burgoyne heavily as his supply lines lengthened and men were detached for garrison duty. In early August, Burgoyne detached part of his Hessian contingent to search for supplies in nearby Vermont. This force was engaged and decisively defeated at the Battle of Bennington on August 16. Three days later Burgoyne made camp near Saratoga to rest his men and await news from St. Leger and Howe. Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South Two miles to the south, Schuylers men began fortifying a series of heights on the west bank of the Hudson. As this work progressed, Gates arrived and took command on August 19. Five days later, Arnold returned from Fort Stanwix and the two began a series of clashes over strategy. While Gates was content to remain on the defensive, Arnold advocated striking at the British. Despite this, Gates gave Arnold command of the left wing of the army, while Major General Benjamin Lincoln led the right. On September 19, Burgoyne moved to attack the American position. Aware that the British were on the move, Arnold secured permission for a reconnaissance in force to determine Burgoynes intentions. In the resulting Battle of Freemans Farm, Arnold decisively defeated the British attack columns, but was relieved after a fight with Gates. Having suffered over 600 casualties at Freemans Farm, Burgoynes position continued to worsen. Sending to Lieutenant General Sir Henry Clinton at New York for aid, he soon learned that none was forthcoming. Short on men and supplies, Burgoyne resolved to renew the battle on October 4. Moving out three days later, the British attacked American positions at the Battle of Bemis Heights. Encountering heavy resistance, the advance soon bogged down. Pacing at headquarters, Arnold finally departed against Gates wishes and rode to the sound of the guns. Aiding on several parts of the battlefield, he led a successful counterattack on the British fortifications before being wounded in the leg. Now outnumbered 3-to-1, Burgoyne attempted to retreat north towards Fort Ticonderoga on the night of October 8. Blocked by Gates and with his supplies dwindling, Burgoyne elected to open negotiations with the Americans. Though he initially demanded an unconditional surrender, Gates agreed to a treaty of convention whereby Burgoynes men would be taken to Boston as prisoners and permitted to return to England on the condition that they not fight in North America again. On October 17, Burgoyne surrendered his remaining 5,791 men. Congress, unhappy with the terms offered by Gates, overruled the agreement and Burgoynes men were placed in prisoner camps around the colonies for the remainder of the war. The victory at Saratoga proved key in securing a treaty of alliance with France. Previous: Opening Campaigns | American Revolution 101 | Next: The War Moves South

Lack Of External Funding And Personnel - 995 Words

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