Frederick County, Maryland
Frederick County is located in the northern part of the U. S. state of Maryland. As of the 2010 U. S. Census, the population was 240,336; the county seat is Frederick. Frederick County is included in the Washington-Arlington-Alexandria, DC-VA-MD-WV Metropolitan Statistical Area. Like other outlying sections of the Washington metropolitan area, Frederick County has experienced a rapid population increase in recent years, it borders the northeastern border of Virginia. The county is home to Catoctin Mountain Park and to the U. S. Army's Fort Detrick, it has been the home to several important historical figures like Francis Scott Key, Chris Rose, Zach Taylor, Matt Bennett, Thomas Johnson, Roger B. Taney, Barbara Fritchie; the namesake of Frederick County and its county seat is unknown, but it was either Frederick, Prince of Wales, or Frederick Calvert, 6th Baron Baltimore. Frederick County was created in 1748 by the Province of Maryland from parts of Prince George's County and Baltimore County. In 1776 following Independence, Frederick County was divided into three parts.
The westernmost portion became Washington County, named after George Washington, the southernmost portion became Montgomery County, named after another Revolutionary War general, Richard Montgomery. The northern portion remained Frederick County. In 1837 a part of Frederick County was combined with a part of Baltimore County to form Carroll County, east of current day Frederick County; the county has a number of properties on the National Register of Historic Places. According to the U. S. Census Bureau, the county has a total area of 667 square miles, of which 660 square miles is land and 7.2 square miles is water. It is the largest county in Maryland in terms of land area. Frederick County straddles the boundary between the Piedmont Plateau Region and the Appalachian Mountains; the county's two prominent ridges, Catoctin Mountain and South Mountain, form an extension of the Blue Ridge. The Middletown Valley lies between them. Attractions in the Frederick area include the Clustered Spires, a monument to Francis Scott Key, the National Museum of Civil War Medicine, Monocacy National Battlefield and South Mountain battlefields, the Schifferstadt Architectural Museum.
Adams County, Pennsylvania Carroll County Howard County Franklin County, Pennsylvania Montgomery County Washington County Loudoun County, Virginia Catoctin Mountain Park Chesapeake and Ohio Canal National Historical Park Monocacy National Battlefield Frederick County has experienced a rapid increase in population in recent years, including that of minority groups. The summary statistics for Frederick County from the 2000 U. S. Census are provided to contrast with the more current data from the 2010 Census; the following table includes the total persons and self-designated ethnicity based on 2000 Census. 2000 Census total population: 195,277 Male: 96,079 Female: 99,198 Ethnicity as percent total population: White: 176,965 Black or African American: 13,605 American Indian and Alaskan: 1,083 Asian: 4,066 Native Hawaiian and Other Pacific Islander: 156 Some other ethnicity: 2,434 The total of those self-identifying as Hispanic or Latino origin made up 2.4%, those persons who were white alone made up 88.1%.
As of the 2010 United States Census, there were 233,385 people, 84,800 households, 61,198 families residing in the county. The population density was 353.5 inhabitants per square mile. There were 90,136 housing units at an average density of 136.5 per square mile. The racial makeup of the county was 81.5% white, 8.6% black or African American, 3.8% Asian, 0.3% American Indian, 2.9% from other races, 2.8% from two or more races. The total of those self-identifying as Hispanic or Latino origin made up 7.3%, those persons who were white alone made up 77.8% of the population. In terms of ancestry, 26.3% were German, 17.4% were Irish, 12.1% were English, 7.2% were Italian, 6.3% were American. Of the 84,800 households, 37.6% had children under the age of 18 living with them, 57.8% were married couples living together, 10.0% had a female householder with no husband present, 27.8% were non-families, 22.0% of all households were made up of individuals. The average household size was 2.70 and the average family size was 3.17.
The median age was 38.6 years. The median income for a household in the county was $81,686 and the median income for a family was $95,036. Males had a median income of $62,494 versus $46,720 for females; the per capita income for the county was $35,172. About 3.2% of families and 4.8% of the population were below the poverty line, including 5.8% of those under age 18 and 5.6% of those age 65 or over. The United States Census Bureau estimates Frederick County's population at 245,322, marking a 5.1% increase since 2010. The racial makeup was estimated to be the following in 2014: 75% White, 9.7% Black, 4.6% Asian, 0.5% Native American, 0.1% Native Hawaiian or Pacific Islander, 2.8% Two or more races, 8.7% were Hispanic or Latino, of any race. Until 2014, Frederick County was governed by county commissioners, the traditional form of county government in the state of Maryland. Effective December 1, 2014, Frederick County transitioned to a "charter home rule government"; the voters approved this governmental change on November 6, 2012 election with 62,469 voting for the transition and 37,368 voting against.
A county executive is responsible for providing direction, supervision
The Cacapon River, located in the Appalachian Mountains of West Virginia's Eastern Panhandle region, is an 81.0-mile-long river known for its fishing, boating and scenery. As part of the Potomac River watershed, it is an American Heritage River; the Cacapon River Watershed is made up of three major river segments and many smaller stream watersheds. The headwaters of the Cacapon River, known as the Lost River, is 31.1 miles long and receives water from a watershed covering 178 square miles. The largest tributary of the Cacapon is the North River, which drains 206 square miles, an area comparable to that of the Lost River. Overall, the Cacapon River watershed includes the Lost and North River watersheds, those of many smaller streams for a total of 680 square miles; the Cacapon watershed is itself part of the Chesapeake Bay watershed. In recent years the Cacapon River and its watershed have become threatened by development, industrial and agricultural growth. Concern about these issues led to the establishment of the Cacapon Institute in 1985.
The Cacapon River emerges from underground in a gap in Sandy Ridge west of Wardensville. It is the reemergence of the Lost River, which sinks into an underground channel east of McCauley near the entrance to Camp Pinnacle. From its emergence, the Cacapon River creates a horseshoe bend shaped gap through Sandy Ridge and flows east paralleling West Virginia Route 55/West Virginia Route 259 to its north. At Wardensville, the river is joined by Trout Run and curves northeastward where it meanders through an expansive valley plain. Here, it is fed by Slate Rock Run and Moores Run further north. Waites Run, a tributary draining some of the western slopes of Great North Mountain enters the Cacapon River near the bridge on Rt. 55, north of Wardensville. Shortly after its confluence with Sine Run, the Cacapon River continues north into Hampshire County. From the county line, the river is bounded to its east by the George Washington National Forest and to its west by Baker Mountain. Throughout this stretch, the Cacapon River is joined by sections of the old Winchester and Western Railroad grade.
It continues its meandering course northeastward, flowing past the community of Intermont and Hebron Church. At Capon Lake, the river is joined by Capon Springs Run and is the site of the historic Capon Lake Whipple Truss Bridge. West Virginia Route 259 parallels the Cacapon River to its west along the eastern flank of Baker Mountain until the road turns east across the Kenneth Seldon Bridge at Yellow Spring. From Yellow Spring Gap, the river is fed by a run whose source is the "Yellow Spring"; the Cacapon River moves north along the eastern flank of Cacapon Mountain with Cacapon River Road paralleling it to its west. From Yellow Spring, the river flows by Camps Rim White Mountain. After another immense horseshoe bend, the Cacapon River moves past the communities of Hooks Mills and Bubbling Spring and is joined by Old Man Run and Kale Hollow's run; the river's stretch through Bubbling Spring is a popular location for summer river camps which consist of cottages and campers on narrow river lots.
This stretch of the Cacapon River is the scene for numerous old plantation houses including the Captain David Pugh House at Hooks Mills, listed on the National Register of Historic Places. North of Kale Hollow, the Cacapon River is joined to its west by Dillons Mountain. To its east, the river is paralleled by Christian Church Road, on, located the 18th century Capon Chapel. After its confluence with Mill Branch, the Cacapon River bends through the small historic town of Capon Bridge, it is met by Dillons Run from its west and traversed by a bridge of the Northwestern Turnpike, from which Capon Bridge takes its name. From Capon Bridge, the Cacapon River is bounded to its east by Bear Garden Mountain, it is joined by Edwards Run and Cold Stream near the community of Cold Stream. The river meanders north around Darbys Nose, flanked to its east by Leith Mountain; the stretch of the Cacapon River between Cold Stream and Forks of Cacapon is mountainous and forested with little development. It meanders through a series of mountain ridges, on one of which, Castle Mountain, sits the Caudy's Castle rock outcrop.
Bloomery Pike passes over the river. North of Bloomery Pike lies the actual "Forks of Cacapon" where the Cacapon and North Rivers converge. From Forks of Cacapon to Largent, the river creates a number of horseshoe bends between Sideling Hill and Little Mountain; this stretch of the Cacapon River is mostly undeveloped and forested with the exception of a gated community, The Crossings, located between the WV 127 bridge and Largent. The Cacapon River meanders into Morgan County at Largent where Cacapon Road passes over it and the river is met by Stony Creek, it continues its meandering course northeast between Sideling Hill and Little Mountain until Fisher's Bridge where it is joined to its east by the western flanks of Cacapon Mountain. Tonoloway Ridge bounds the Cacapon River to its west until it reaches the railroad hamlet of Great Cacapon. After passing under the WV 9 and old Baltimore and Ohio Railroad bridges, the Cacapon River joins the Potomac. Cacapon is a name derived from the Shawnee language meaning "medicine water".
Virginia the Commonwealth of Virginia, is a state in the Southeastern and Mid-Atlantic regions of the United States located between the Atlantic Coast and the Appalachian Mountains. Virginia is nicknamed the "Old Dominion" due to its status as the first English colonial possession established in mainland North America and "Mother of Presidents" because eight U. S. presidents were born there, more than any other state. The geography and climate of the Commonwealth are shaped by the Blue Ridge Mountains and the Chesapeake Bay, which provide habitat for much of its flora and fauna; the capital of the Commonwealth is Richmond. The Commonwealth's estimated population as of 2018 is over 8.5 million. The area's history begins with several indigenous groups, including the Powhatan. In 1607 the London Company established the Colony of Virginia as the first permanent New World English colony. Slave labor and the land acquired from displaced Native American tribes each played a significant role in the colony's early politics and plantation economy.
Virginia was one of the 13 Colonies in the American Revolution. In the American Civil War, Virginia's Secession Convention resolved to join the Confederacy, Virginia's First Wheeling Convention resolved to remain in the Union. Although the Commonwealth was under one-party rule for nearly a century following Reconstruction, both major national parties are competitive in modern Virginia; the Virginia General Assembly is the oldest continuous law-making body in the New World. The state government was ranked most effective by the Pew Center on the States in both 2005 and 2008, it is unique in how it treats cities and counties manages local roads, prohibits its governors from serving consecutive terms. Virginia's economy has many sectors: agriculture in the Shenandoah Valley. S. Department of Defense and Central Intelligence Agency. Virginia has a total area of 42,774.2 square miles, including 3,180.13 square miles of water, making it the 35th-largest state by area. Virginia is bordered by Maryland and Washington, D.
C. to the north and east. Virginia's boundary with Maryland and Washington, D. C. extends to the low-water mark of the south shore of the Potomac River. The southern border is defined as the 36° 30′ parallel north, though surveyor error led to deviations of as much as three arcminutes; the border with Tennessee was not settled until 1893, when their dispute was brought to the U. S. Supreme Court; the Chesapeake Bay separates the contiguous portion of the Commonwealth from the two-county peninsula of Virginia's Eastern Shore. The bay was formed from the drowned river valleys of the James River. Many of Virginia's rivers flow into the Chesapeake Bay, including the Potomac, Rappahannock and James, which create three peninsulas in the bay; the Tidewater is a coastal plain between the fall line. It includes major estuaries of Chesapeake Bay; the Piedmont is a series of sedimentary and igneous rock-based foothills east of the mountains which were formed in the Mesozoic era. The region, known for its heavy clay soil, includes the Southwest Mountains around Charlottesville.
The Blue Ridge Mountains are a physiographic province of the Appalachian Mountains with the highest points in the state, the tallest being Mount Rogers at 5,729 feet. The Ridge and Valley region includes the Great Appalachian Valley; the region includes Massanutten Mountain. The Cumberland Plateau and the Cumberland Mountains are in the southwest corner of Virginia, south of the Allegheny Plateau. In this region, rivers flow northwest, into the Ohio River basin; the Virginia Seismic Zone has not had a history of regular earthquake activity. Earthquakes are above 4.5 in magnitude, because Virginia is located away from the edges of the North American Plate. The largest earthquake, at an estimated 5.9 magnitude, was in 1897 near Blacksburg. A 5.8 magnitude earthquake struck central Virginia on August 2011, near Mineral. The earthquake was felt as far away as Toronto and Florida. 35 million years ago, a bolide impacted. The resulting Chesapeake Bay impact crater may explain what earthquakes and subsidence the region does experience.
Coal mining takes place in the three mountainous regions at 45 distinct coal beds near Mesozoic basins. Over 64 million tons of other non-fuel resources, such as slate, sand, or gravel, were mined in Virginia in 2018; the state's carbonate rock is filled with more than 4,000 caves, ten of which are open for tourism, including the popular Luray Caverns and Skyline Caverns. The climate of Virginia is humid subtropical and becomes warmer and more humid farther south and east. Seasonal extremes vary from average lows of 26 °F in January to average highs of 86 °F in July; the Atlantic Ocean has a strong effect on southeastern coastal areas of the state. Influenced by the Gulf Stream, coastal weather is subject to hurricanes, most pronouncedly near the mouth of Chesapeake Bay. In spite of its position adjacent to the Atlantic Ocean the coastal areas have a significant continental influence with quite large temperature differences between summ
Maryland is a state in the Mid-Atlantic region of the United States, bordering Virginia, West Virginia, the District of Columbia to its south and west. The state's largest city is Baltimore, its capital is Annapolis. Among its occasional nicknames are Old Line State, the Free State, the Chesapeake Bay State, it is named after the English queen Henrietta Maria, known in England as Queen Mary. Sixteen of Maryland's twenty-three counties border the tidal waters of the Chesapeake Bay estuary and its many tributaries, which combined total more than 4,000 miles of shoreline. Although one of the smallest states in the U. S. it features a variety of climates and topographical features that have earned it the moniker of America in Miniature. In a similar vein, Maryland's geography and history combines elements of the Mid-Atlantic and South Atlantic regions of the country. One of the original Thirteen Colonies of Great Britain, Maryland was founded by George Calvert, a Catholic convert who sought to provide a religious haven for Catholics persecuted in England.
In 1632, Charles I of England granted Calvert a colonial charter, naming the colony after his wife, Queen Mary. Unlike the Pilgrims and Puritans, who enforced religious conformity in their settlements, Calvert envisioned a colony where people of different religious sects would coexist under the principle of toleration. Accordingly, in 1649 the Maryland General Assembly passed an Act Concerning Religion, which enshrined this principle by penalizing anyone who "reproached" a fellow Marylander based on religious affiliation. Religious strife was common in the early years, Catholics remained a minority, albeit in greater numbers than in any other English colony. Maryland's early settlements and population centers clustered around rivers and other waterways that empty into the Chesapeake Bay, its economy was plantation-based, centered on the cultivation of tobacco. The need for cheap labor led to a rapid expansion of indentured servants, penal labor, African slaves. In 1760, Maryland's current boundaries took form following the settlement of a long-running border dispute with Pennsylvania.
Maryland was an active participant in the events leading up to the American Revolution, by 1776 its delegates signed the Declaration of Independence. Many of its citizens subsequently played key military roles in the war. In 1790, the state ceded land for the establishment of the U. S. capital of Washington, D. C. Although a slave state, Maryland remained in the Union during the U. S. Civil War, its strategic location giving it a significant role in the conflict. After the war, Maryland took part in the Industrial Revolution, driven by its seaports, railroad networks, mass immigration from Europe. Since the Second World War, the state's population has grown to six million residents, it is among the most densely populated states in the nation; as of 2015, Maryland had the highest median household income of any state, owing in large part to its close proximity to Washington, D. C. and a diversified economy spanning manufacturing, higher education, biotechnology. Maryland has been ranked as one of the best governed states in the country.
The state's central role in American history is reflected by its hosting of some of the highest numbers of historic landmarks per capita. Maryland is comparable in overall area with Belgium, it is the 42nd largest and 9th smallest state and is closest in size to the state of Hawaii, the next smaller state. The next larger state, its neighbor West Virginia, is twice the size of Maryland. Maryland possesses a variety of topography within its borders, contributing to its nickname America in Miniature, it ranges from sandy dunes dotted with seagrass in the east, to low marshlands teeming with wildlife and large bald cypress near the Chesapeake Bay, to rolling hills of oak forests in the Piedmont Region, pine groves in the Maryland mountains to the west. Maryland is bounded on its north by Pennsylvania, on its west by West Virginia, on its east by Delaware and the Atlantic Ocean, on its south, across the Potomac River, by West Virginia and Virginia; the mid-portion of this border is interrupted by District of Columbia, which sits on land, part of Montgomery and Prince George's counties and including the town of Georgetown, Maryland.
This land was ceded to the United States Federal Government in 1790 to form the District of Columbia.. The Chesapeake Bay nearly bisects the state and the counties east of the bay are known collectively as the Eastern Shore. Most of the state's waterways are part of the Chesapeake Bay watershed, with the exceptions of a tiny portion of extreme western Garrett County, the eastern half of Worcester County, a small portion of the state's northeast corner. So prominent is the Chesapeake in Maryland's geography and economic life that there has been periodic agitation to change the state's official nickname to the "Bay State", a nickname, used by Massachusetts for decades; the highest point in Maryland, with an elevation of 3,360 feet, is Hoye Crest on Backbone Mountain, in the southwest corner of Garrett County, near the bo
The Potomac River is located within the Mid-Atlantic region of the United States and flows from the Potomac Highlands into the Chesapeake Bay. The river is 405 miles long, with a drainage area of about 14,700 square miles. In terms of area, this makes the Potomac River the fourth largest river along the Atlantic coast of the United States and the 21st largest in the United States. Over 5 million people live within the Potomac watershed; the river forms part of the borders between Maryland and Washington, D. C. on the left descending bank and West Virginia and Virginia on the river's right descending bank. The majority of the lower Potomac River is part of Maryland. Exceptions include a small tidal portion within the District of Columbia, the border with Virginia being delineated from "point to point". Except for a small portion of its headwaters in West Virginia, the North Branch Potomac River is considered part of Maryland to the low water mark on the opposite bank; the South Branch Potomac River lies within the state of West Virginia except for its headwaters, which lie in Virginia.
The Potomac River runs 405 miles from Fairfax Stone Historical Monument State Park in West Virginia on the Allegheny Plateau to Point Lookout and drains 14,679 square miles. The length of the river from the junction of its North and South Branches to Point Lookout is 302 miles; the average daily flow during the water years 1931-2018 was 11,498 cubic feet /s. The highest average daily flow recorded on the Potomac at Little Falls, was in March 1936 when it reached 426,000 cubic feet /s; the lowest average daily flow recorded at the same location was 601.0 cubic feet /s in September 1966 The highest crest of the Potomac registered at Little Falls was 28.10 ft, on March 19, 1936. The river has two sources; the source of the North Branch is at the Fairfax Stone located at the junction of Grant and Preston counties in West Virginia. The source of the South Branch is located near Hightown in northern Highland Virginia; the river's two branches converge just east of Green Spring in Hampshire County, West Virginia, to form the Potomac.
As it flows from its headwaters down to the Chesapeake Bay, the Potomac traverses five geological provinces: the Appalachian Plateau, the Ridge and Valley, the Blue Ridge, the Piedmont Plateau, the Atlantic coastal plain. Once the Potomac drops from the Piedmont to the Coastal Plain at the Atlantic Seaboard fall line at Little Falls, tides further influence the river as it passes through Washington, D. C. and beyond. Salinity in the Potomac River Estuary increases thereafter with distance downstream; the estuary widens, reaching 11 statute miles wide at its mouth, between Point Lookout and Smith Point, before flowing into the Chesapeake Bay. "Potomac" is a European spelling of Patawomeck, the Algonquian name of a Native American village on its southern bank. Native Americans had different names for different parts of the river, calling the river above Great Falls Cohongarooton, meaning "honking geese" and "Patawomke" below the Falls, meaning "river of swans"; the spelling of the name has taken many forms over the years from "Patawomeck" to "Patomake", "Patowmack", numerous other variations in the 18th century and now "Potomac".
The river's name was decided upon as "Potomac" by the Board on Geographic Names in 1931. The river itself is at least 3.5 million years old extending back ten to twenty million years before present when the Atlantic Ocean lowered and exposed coastal sediments along the fall line. This included the area at Great Falls, which eroded into its present form during recent glaciation periods; the Potomac River brings together a variety of cultures throughout the watershed from the coal miners of upstream West Virginia to the urban residents of the nation's capital and, along the lower Potomac, the watermen of Virginia's Northern Neck. Being situated in an area rich in American history and American heritage has led to the Potomac being nicknamed "the Nation's River." George Washington, the first President of the United States, was born in, spent most of his life within, the Potomac basin. All of Washington, D. C. the nation's capital city lies within the watershed. The 1859 siege of Harper's Ferry at the river's confluence with the Shenandoah was a precursor to numerous epic battles of the American Civil War in and around the Potomac and its tributaries, such as the 1861 Battle of Ball's Bluff and the 1862 Battle of Shepherdstown.
General Robert E. Lee crossed the river, thereby invading the North and threatening Washington, D. C. twice in campaigns climaxing in the battles of Antietam and Gettysburg. Confederate General Jubal Early crossed the river in July 1864 on his attempted raid on the nation's capital; the river not only divided the Union from the Confederacy, but gave name to the Union's largest army, the Army of the Potomac. The Patowmack Canal was intended by George Washington to connect the Tidewater region near Georgetown with Cumberland, Maryland. Started in 1785 on the Virginia side of the river, it was not completed until 1802. Financial troubles led to the closure of the canal in 1830; the Chesapeake and Ohio Canal operated along the banks of the Potomac in Maryland from 1831 to 1924 and connected Cumberland to Washington, D. C; this allowed freight to be transported around the rapids known as the
West Virginia is a state located in the Appalachian region in the Southern United States, considered to be a part of the Middle Atlantic States. It is bordered by Pennsylvania to the north, Maryland to the east and northeast, Virginia to the southeast, Kentucky to the southwest, Ohio to the northwest. West Virginia is the 41st largest state by area, is ranked 38th in population; the capital and largest city is Charleston. West Virginia became a state following the Wheeling Conventions of 1861, after the American Civil War had begun. Delegates from some Unionist counties of northwestern Virginia decided to break away from Virginia, although they included many secessionist counties in the new state. West Virginia was admitted to the Union on June 20, 1863, was a key border state during the war. West Virginia was the only state to form by separating from a Confederate state, the first to separate from any state since Maine separated from Massachusetts, was one of two states admitted to the Union during the American Civil War.
While a portion of its residents held slaves, most of the residents were yeomen farmers, the delegates provided for gradual abolition of slavery in the new state Constitution. The Census Bureau and the Association of American Geographers classify West Virginia as part of the Southern United States; however the Bureau of Labor Statistics classifies West Virginia as a part of the Mid-Atlantic. The northern panhandle extends adjacent to Pennsylvania and Ohio, with the West Virginia cities of Wheeling and Weirton just across the border from the Pittsburgh metropolitan area, while Bluefield is less than 70 miles from North Carolina. Huntington in the southwest is close to the states of Ohio and Kentucky, while Martinsburg and Harpers Ferry in the Eastern Panhandle region are considered part of the Washington metropolitan area, in between the states of Maryland and Virginia; the unique position of West Virginia means that it is included in several geographical regions, including the Mid-Atlantic, the Upland South, the Southeastern United States.
It is the only state, within the area served by the Appalachian Regional Commission. The state is noted for its mountains and rolling hills, its significant logging and coal mining industries, its political and labor history, it is known for a wide range of outdoor recreational opportunities, including skiing, whitewater rafting, hiking, mountain biking, rock climbing, hunting. Many ancient man-made earthen mounds from various prehistoric mound builder cultures survive in the areas of present-day Moundsville, South Charleston, Romney; the artifacts uncovered in these give evidence of village societies. They had a tribal trade system culture. In the 1670s during the Beaver Wars, the powerful Iroquois, five allied nations based in present-day New York and Pennsylvania, drove out other American Indian tribes from the region in order to reserve the upper Ohio Valley as a hunting ground. Siouan language tribes, such as the Moneton, had been recorded in the area. A century the area now identified as West Virginia was contested territory among Anglo-Americans as well, with the colonies of Pennsylvania and Virginia claiming territorial rights under their colonial charters to this area before the American Revolutionary War.
Some speculative land companies, such as the Vandalia Company, the Ohio Company and Indiana Company, tried to legitimize their claims to land in parts of West Virginia and present day Kentucky, but failed. This rivalry resulted in some settlers petitioning the Continental Congress to create a new territory called Westsylvania. With the federal settlement of the Pennsylvania and Virginia border dispute, creating Kentucky County, Kentuckians "were satisfied, the inhabitants of a large part of West Virginia were grateful."The Crown considered the area of West Virginia to be part of the British Virginia Colony from 1607 to 1776. The United States considered this area to be the western part of the state of Virginia from 1776 to 1863, before the formation of West Virginia, its residents were discontented for years with their position in Virginia, as the government was dominated by the planter elite of the Tidewater and Piedmont areas. The legislature had electoral malapportionment, based on the counting of slaves toward regional populations, the western white residents were underrepresented in the state legislature.
More subsistence and yeoman farmers lived in the west and they were less supportive of slavery, although many counties were divided on their support. The residents of this area became more divided after the planter elite of eastern Virginia voted to secede from the Union during the Civil War. Residents of the western and northern counties set up a separate government under Francis Pierpont in 1861, which they called the Restored Government. Most voted to separate from Virginia, the new state was admitted to the Union in 1863. In 1864 a state constitutional convention drafted a constitution, ratified by the legislature without putting it to popular vote. West Virginia abolished slavery by a gradual process and temporarily disenfranchised men who had held Confederate office or fought for the Confederacy. West Virginia's history has been profoundly affected by its mountainous terrain and vast river valleys, rich natural resources; these were all factors driving its economy and the lifestyles of its residents, who tended to live in many small isolated communities in the mountain valleys.
A 2010 analysis of
Pennsylvania the Commonwealth of Pennsylvania, is a state located in the northeastern and Mid-Atlantic regions of the United States. The Appalachian Mountains run through its middle; the Commonwealth is bordered by Delaware to the southeast, Maryland to the south, West Virginia to the southwest, Ohio to the west, Lake Erie and the Canadian province of Ontario to the northwest, New York to the north, New Jersey to the east. Pennsylvania is the 33rd-largest state by area, the 6th-most populous state according to the most recent official U. S. Census count in 2010, it is the 9th-most densely populated of the 50 states. Pennsylvania's two most populous cities are Philadelphia, Pittsburgh; the state capital and its 10th largest city is Harrisburg. Pennsylvania has 140 miles of waterfront along the Delaware Estuary; the state is one of the 13 original founding states of the United States. Part of Pennsylvania, together with the present State of Delaware, had earlier been organized as the Colony of New Sweden.
It was the second state to ratify the United States Constitution, on December 12, 1787. Independence Hall, where the United States Declaration of Independence and United States Constitution were drafted, is located in the state's largest city of Philadelphia. During the American Civil War, the Battle of Gettysburg was fought in the south central region of the state. Valley Forge near Philadelphia was General Washington's headquarters during the bitter winter of 1777–78. Pennsylvania is 170 miles north to south and 283 miles east to west. Of a total 46,055 square miles, 44,817 square miles are land, 490 square miles are inland waters, 749 square miles are waters in Lake Erie, it is the 33rd-largest state in the United States. Pennsylvania has 51 miles of coastline along Lake Erie and 57 miles of shoreline along the Delaware Estuary. Of the original Thirteen Colonies, Pennsylvania is the only state that does not border the Atlantic Ocean; the boundaries of the state are the Mason–Dixon line to the south, the Twelve-Mile Circle on the Pennsylvania-Delaware border, the Delaware River to the east, 80° 31' W to the west and the 42° N to the north, with the exception of a short segment on the western end, where a triangle extends north to Lake Erie.
Cities include Philadelphia, Reading and Lancaster in the southeast, Pittsburgh in the southwest, the tri-cities of Allentown and Easton in the central east. The northeast includes the former anthracite coal mining cities of Scranton, Wilkes-Barre and Hazleton. Erie is located in the northwest. State College serves the central region while Williamsport serves the commonwealth's north-central region as does Chambersburg the south-central region, with York and the state capital Harrisburg on the Susquehanna River in the east-central region of the Commonwealth and Altoona and Johnstown in the west-central region; the state has five geographical regions, namely the Allegheny Plateau and Valley, Atlantic Coastal Plain and the Erie Plain. New York Ontario Maryland Delaware West Virginia New Jersey Ohio Pennsylvania's diverse topography produces a variety of climates, though the entire state experiences cold winters and humid summers. Straddling two major zones, the majority of the state, with the exception of the southeastern corner, has a humid continental climate.
The southern portion of the state has a humid subtropical climate. The largest city, has some characteristics of the humid subtropical climate that covers much of Delaware and Maryland to the south. Summers are hot and humid. Moving toward the mountainous interior of the state, the winter climate becomes colder, the number of cloudy days increases, snowfall amounts are greater. Western areas of the state locations near Lake Erie, can receive over 100 inches of snowfall annually, the entire state receives plentiful precipitation throughout the year; the state may be subject to severe weather from spring through summer into fall. Tornadoes occur annually in the state, sometimes in large numbers, such as 30 recorded tornadoes in 2011; as of 1600, the tribes living in Pennsylvania were the Algonquian Lenape, the Iroquoian Susquehannock & Petun and the Siouan Monongahela Culture, who may have been the same as a little known tribe called the Calicua, or Cali. Other tribes who entered the region during the colonial era were the Trockwae, Saponi, Nanticoke, Conoy Piscataway, Iroquois Confederacy—possibly among others.
Other tribes, like the Erie, may have once held some land in Pennsylvania, but no longer did so by the year 1600. Both the Dutch and the English claimed both sides of the Delaware River as part of their colonial lands in America; the Dutch were the first to take possession. By June 3, 1631, the Dutch had begun settling the Delmarva Peninsula by establishing the Zwaanendael Colony on the site of present-day Lewes, Delaware. In 1638, Sweden established the New Sweden Colony, in the region of Fort Christina, on the site of present-day Wilmington, Delaware. New Sweden claimed and, for the most part, controlled the lower Delaware River region (parts of present-day Delaware, New Jersey, Pe