Eastern Shore of Maryland

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The Eastern Shore of Maryland is a part of the U.S. state of Maryland that lies mostly on the east side of the Chesapeake Bay. Nine counties are normally included in the region. The Eastern Shore is part of the larger Delmarva Peninsula that Maryland shares with Delaware and Virginia.

As of the 2020 census, its population was 456,815, with about 7% of Marylanders living in the region. The region is politically more conservative than the rest of the state, generally returning more votes for Republicans than Democrats in statewide and national elections.

Developed in the colonial and federal period for agriculture, the Eastern Shore has remained a relatively rural region. Salisbury is the most populous community on the Eastern Shore of Maryland. The region's economy is dominated by three industry sectors: fishing along the coasts, especially for shellfish such as the blue crab; farming, especially large-scale chicken farms; and tourism, especially centered on the Atlantic coast and beach resort of Ocean City. Because of its coastal and low-lying geography, the region is vulnerable to extreme weather events, including hurricanes and larger environmental issues like climate change and rising sea levels.

The region contains a few major roads; the main connection to the other parts of Maryland is the Chesapeake Bay Bridge, which carries U.S. Route 50 and U.S. Route 301. U.S. Route 13 connects the southern part of the Eastern Shore to both Delaware and points north and Virginia and points south.

Geography

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File:CrisfieldWaterfront.jpg
Crisfield, a seafood center along Chesapeake Bay
File:KentCountyMD.jpg
A farm in Kent County
File:BlackwaterNWR.jpg
Blackwater National Wildlife Refuge in Dorchester County

The Eastern Shore of Maryland comprises Caroline, Cecil, Dorchester, Kent, Queen Anne's, Somerset, Talbot, Wicomico, and Worcester counties.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> These lie on the eastern side of the Chesapeake Bay and Susquehanna River, which is the western border of Cecil County with Harford County. The region borders the Mason–Dixon line with Delaware to the east and north, the Atlantic Ocean on the east, and Virginia's Eastern Shore on the south. Maryland's and Virginia's Eastern Shores, along with most of Delaware, form the Delmarva Peninsula.

The location of the southern border with Virginia was a cause for significant dispute amongst colonists prior to 1668, when Phillip Calvert of Maryland and Edmund Scarborough of Virginia demarcated the Calvert-Scarborough Line. This line ran northeast from Watkins Point in the Chesapeake through the James L. Horsey Farm and beyond to the Atlantic, but was ultimately never observed due to poor marking. The line in use today was established under the Award of 1877; this line travels east from Watkins Point, then up the middle of the Pocomoke River before heading due east along the Calvert-Scarborough Line at the point where it intersects the river.<ref>Template:Cite book</ref>

Like New Castle County, Delaware, Cecil County is crossed by the Fall Line, a geologic division where the rockier highlands of the Piedmont region meet the Atlantic coastal plain, a flat, sandy area that forms the coast. The coastal plain includes the Delmarva Peninsula and hence the Eastern Shore of Maryland. The geology of Delmarva is an inseparable part of the Eastern Shore, which has few rocky outcrops south of Kent County.

The Chesapeake and Delaware Canal crosses from Back Creek on the Elk River to Port Penn, Delaware. While it was a shallow canal with locks after its construction in 1829, it was deepened in the early 20th century to sea level, and physically separates the Delmarva Peninsula from the rest of the United States. Maryland south of the canal is considered the Eastern Shore by residents. The term Western Shore is used by Eastern Shore residents to describe all the counties of Maryland west of the Chesapeake Bay, but especially those of the Baltimore-Washington metropolitan area and Southern Maryland.

The north–south section of the Mason–Dixon line forms the border between Maryland and Delaware. The border was originally marked every mile by a stone, and every five miles by a "crownstone". The line is not quite due north and south, but is as straight as survey methods of the 1760s could make it. It was surveyed as a compromise solution to a century-long wrangle over colonial territory between the Penn and Calvert families of England. If the Chesapeake Bay/Delaware Bay watershed divide had been taken as the borderline, the state of Delaware would be about half its current size.

History

File:1Queen Anne's Co. courthouse.jpg
Queen Anne's County courthouse

Early history

William Claiborne was granted land that was then part of the Colony of Virginia in 1629. He named it "Kent County". In 1631, he sailed north up the Chesapeake Bay from its south and west side to the area known today as Kent Island. There he made a fortified settlement that is considered to be the first English settlement within the Province of Maryland. Talbot County was formed in 1662. Cecil County was formed in 1674, by proclamation of the Governor, from eastern portions of Baltimore County and the northern portion of Kent County. Wicomico County was formed in 1867, as the 9th and last county, created from Somerset and Worcester counties.

Formation of counties

19th century

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File:Chesapeake Bay Maritime Museum.JPG
Chesapeake Bay Maritime Museum in St. Michaels

Ocean City was founded on July 4, 1875,<ref>Ocean City History Template:Webarchive. ococean.com. Retrieved July 1, 2008.</ref> when the Atlantic Hotel opened on Assateague Island. At the time, Assateague Island was continuous from the Delaware state line to well south of Ocean City: the Ocean City Inlet was not formed until a hurricane in August 1933 cut across the south end of the town. The inlet was cut not by waves sweeping inland, but by 4 or 5 days' worth of freshwater runoff from the coastal creeks running seaward. By 1935, government money had built jetties to make the inlet permanent, dividing Fenwick Island (north) from Assateague Island (south). Early transportation to the island was by train.

Until the 1820s, travel and commerce between the Eastern Shore and Baltimore were less important than the connections between it and Philadelphia. Water travel by sailboat and steamer linked the Eastern Shore to Baltimore more tightly beginning about 1813, when the first steamboat traveled the Bay. By the 1880s, railroad lines linked the Eastern Shore to Philadelphia and later, Norfolk, Virginia, by way of a railroad line straight south from Wilmington to Dover, Delmar, Salisbury, and Cape Charles. Maryland's Eastern Shore was served by branch lines running generally southwest from the main route. See List of railroad lines in the Delmarva Peninsula. The Eastern Shore's many branchlines were built after the Civil War by local companies; by the late nineteenth century, all were controlled by the Pennsylvania Railroad (which also bought control of the steamboat and ferry routes), then Conrail and Norfolk Southern. Today the remaining active railroad tracks on the Eastern Shore are operated by short-line railroads Delmarva Central Railroad and the Maryland and Delaware Railroad.

Commercial east–west ties between Delaware towns and Maryland towns were culturally significant in Colonial and Early American periods despite the border line, which largely cut through woods and swamps. Trade with Philadelphia was conducted by overland routes to Delaware towns such as Odessa (then called Cantwell's Bridge) and Smyrna, then called Duck Creek. Agricultural products and milled grain were taken up the Delaware River by "shallop men" in small vessels called shallops. These cultural connections continue to this day.

20th and 21st centuries

An east–west rail route ran from a ferry terminal at Claiborne, west of St. Michaels, to Ocean City, via the Baltimore and Eastern Shore Railroad and the Wicomico and Pocomoke Railroad. Travelers could also take a ferry to Love Point on Kent Island, board a Queen Anne's Railroad train, and travel east to Lewes and Rehoboth Beach, Delaware.

Automobile transportation across the Chesapeake Bay was by ferryboat until 1952, when the first Chesapeake Bay Bridge was opened for traffic.

In the late 1950s and early 1960s, developers began selling lots on Assateague Island, south of the inlet. However, a storm on March 6, 1962 destroyed houses, shacks, and roads.<ref>Assateague Island Administrative History Template:Webarchive The Becoming of the Seashore</ref> The state and federal governments intervened before reconstruction by creating the Assateague Island National Seashore and Assateague State Park to preserve this area rather than have it be developed.

An Eastern Shore Baseball League operated during three periods between 1922 and 1949.<ref>MLB Top 100 Teams Template:Webarchive. MLB.com. Retrieved July 1, 2008.</ref> It was a Class D minor league with teams in all three states of Delmarva.

Demographics

Although the Eastern Shore comprises a large part of Maryland's land area, it had a population of 456,815 as of the 2020 Census, representing about 7.4% of Maryland's total population.<ref name="pop2020" /><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The most populous city in the region is Salisbury, and the most populous county is Cecil.<ref name="MDregions">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref name="pop2020" />

Elections

The Eastern Shore is considerably more conservative than the more densely populated and urban Western Shore. Since the late 20th century, when conservative whites shifted to the Republican Party, the region has strongly supported Republican candidates for governor. The three Republican nominees for governor from 1994 to 2018Ellen Sauerbrey, Bob Ehrlich, and Larry Hogan– swept all nine counties. This streak ended in 2022 when Democrat Wes Moore won Kent and Talbot counties, though Republican Dan Cox still won the Eastern Shore overall.

At the presidential level, the Eastern Shore also leans Republican. But Kent and Somerset counties have flipped back and forth in supporting Democratic and Republican presidential candidates. The last Democrat to win Dorchester County was Bill Clinton from Arkansas in 1996. Cecil County has not gone Democratic since Jimmy Carter from Georgia won the county in 1976. Queen Anne's, Caroline, Wicomico, and Worcester counties have voted Republican at every election subsequent to Lyndon Johnson's landslide. Up until 2020, this was true for Talbot County as well, but it was won by Joe Biden.<ref>Sullivan, Robert David; ‘How the Red and Blue Map Evolved Over the Past Century’ Template:Webarchive; America Magazine, in The National Catholic Review; June 29, 2016</ref>

The Eastern Shore has long been a part of Maryland's 1st Congressional district.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}Template:Dead link</ref> Democrat Roy Dyson represented the 1st district from 1981 until 1990, when he was defeated by Republican Wayne Gilchrest. Gilchrest held the seat until 2008, when State Senator Andy Harris defeated him in the Republican primary. Harris narrowly lost the subsequent general election to Democrat Frank Kratovil, Queen Anne's County state's attorney. In 2010, Harris again ran for the district and handily defeated Kratovil after a single term in office. Harris has held the seat without serious difficulty since.

In the Maryland General Assembly, the Eastern Shore encompasses a portion of district 35B and all of districts 35A, 36, 37A and 37B, 38A, 38B and 38C. All seats are held by Republicans except for a state delegate seat in district 37A.

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Gubernatorial election results
Year Republican Democratic Other Total
2022<ref>{{#invoke:citation/CS1|citation CitationClass=web

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55.33% 91,425 41.24% 68,137 3.43% 5,661 165,223
2018<ref>{{#invoke:citation/CS1|citation CitationClass=web

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75.80% 131,649 23.02% 39,986 1.16% 1,279 173,657
2014<ref>{{#invoke:citation/CS1|citation CitationClass=web

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71.45% 100,608 26.93% 37,919 1.62% 2,277 140,804
2010<ref>{{#invoke:citation/CS1|citation CitationClass=web

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59.35% 92,231 38.19% 59,343 2.46% 3,827 155,401
2006<ref>{{#invoke:citation/CS1|citation CitationClass=web

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62.05% 90,319 36.92% 53,748 1.03% 1,502 145,569
2002<ref>{{#invoke:citation/CS1|citation CitationClass=web

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68.07% 90,000 31.19% 41,241 0.73% 970 132,211
1998<ref>{{#invoke:citation/CS1|citation CitationClass=web

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59.02% 66,434 40.94% 46,079 0.04% 50 112,563
1994<ref>{{#invoke:citation/CS1|citation CitationClass=web

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62.60% 65,585 37.40% 39,187 0.00% 3 104,775
1990<ref>{{#invoke:citation/CS1|citation CitationClass=web

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59.43% 52,288 40.57% 35,692 0.00% 0 87,980

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Year Democratic Republican Others
align="center" Template:Party shading/Republican|2020 align="center" Template:Party shading/Democratic|41.0% 94,716 align="center" Template:Party shading/Republican|56.6% 130,622 align="center" Template:Party shading/None|2.4% 5,588
align="center" Template:Party shading/Republican|2016 align="center" Template:Party shading/Democratic|36.3% 77,104 align="center" Template:Party shading/Republican|58.4% 123,991 align="center" Template:Party shading/None|5.3% 11,329
align="center" Template:Party shading/Republican|2012 align="center" Template:Party shading/Democratic|42.0% 86,879 align="center" Template:Party shading/Republican|56.0% 115,669 align="center" Template:Party shading/None|2.0% 4,062
align="center" Template:Party shading/Republican|2008 align="center" Template:Party shading/Democratic|42.9% 87,700 align="center" Template:Party shading/Republican|55.5% 113,518 align="center" Template:Party shading/None|1.6% 3,285
align="center" Template:Party shading/Republican|2004 align="center" Template:Party shading/Democratic|38.8% 71,435 align="center" Template:Party shading/Republican|60.1% 110,661 align="center" Template:Party shading/None|1.1% 1,942
align="center" Template:Party shading/Republican|2000 align="center" Template:Party shading/Democratic|43.0% 64,336 align="center" Template:Party shading/Republican|53.7% 80,329 align="center" Template:Party shading/None|3.2% 4,787
align="center" Template:Party shading/Republican|1996 align="center" Template:Party shading/Democratic|42.8% 54,537 align="center" Template:Party shading/Republican|46.7% 59,522 align="center" Template:Party shading/None|10.6% 13,510
align="center" Template:Party shading/Republican|1992 align="center" Template:Party shading/Democratic|36.5% 50,121 align="center" Template:Party shading/Republican|44.1% 60,518 align="center" Template:Party shading/None|19.4% 26,713
align="center" Template:Party shading/Republican|1988 align="center" Template:Party shading/Democratic|36.3% 41,797 align="center" Template:Party shading/Republican|63.3% 72,886 align="center" Template:Party shading/None|0.5% 551
align="center" Template:Party shading/Republican|1984 align="center" Template:Party shading/Democratic|32.5% 34,934 align="center" Template:Party shading/Republican|67.1% 72,235 align="center" Template:Party shading/None|0.4% 454
align="center" Template:Party shading/Republican|1980 align="center" Template:Party shading/Democratic|42.9% 43,447 align="center" Template:Party shading/Republican|51.3% 52,000 align="center" Template:Party shading/None|5.8% 5,919
align="center" Template:Party shading/Republican|1976 align="center" Template:Party shading/Democratic|48.6% 43,838 align="center" Template:Party shading/Republican|51.4% 46,301 align="center" Template:Party shading/None|–
align="center" Template:Party shading/Republican|1972 align="center" Template:Party shading/Democratic|27.5% 23,215 align="center" Template:Party shading/Republican|71.2% 60,020 align="center" Template:Party shading/None|1.3% 1,088
align="center" Template:Party shading/Republican|1968 align="center" Template:Party shading/Democratic|30.0% 25,506 align="center" Template:Party shading/Republican|46.6% 39,578 align="center" Template:Party shading/None|23.3% 19,808
align="center" Template:Party shading/Democratic|1964 align="center" Template:Party shading/Democratic|57.0% 45,899 align="center" Template:Party shading/Republican|43.0% 34,585 align="center" Template:Party shading/None|–
align="center" Template:Party shading/Republican|1960 align="center" Template:Party shading/Democratic|47.1% 38,722 align="center" Template:Party shading/Republican|52.9% 43,534 align="center" Template:Party shading/None|–

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Economy

Tourism

File:Ocean City MD beach looking north from pier.jpeg
Ocean City, Maryland's beach, looking north from the pier

Ocean City's skyline, containing tall hotels and condominiums, stands out within Delmarva. At the southern end of the town, a recreational boardwalk spans over thirty blocks, containing carnival rides and games, restaurants, bars, arcades, and clothing boutiques.

Tourists visit St. Michaels on a neck surrounded by water; the colonial former port of Oxford; Chestertown; and isolated Smith Island in the Chesapeake Bay. North of Crisfield is Janes Island State Park, with camping and kayaking trails through marshlands. Cambridge continues to be a popular destination for tourism because of the Blackwater National Wildlife Refuge, the Hyatt Chesapeake Bay Resort, Spa & Marina, and the Harriet Tubman National Park.

Fishing

Template:Further At the southern end of the Chesapeake coast of Maryland, the town of Crisfield is home to a fishing, crabbing, and seafood processing industry.

Agriculture

Template:Further In the 21st century, the main economic activities on the Eastern Shore are vegetable and grain farming, seafood, large-scale chicken breeding (Perdue Farms was founded in Salisbury and is still headquartered there today), and tourism. Tobacco was the chief commodity crop during colonial times. The agricultural economy switched to mixed products, including grain, in the second half of the 18th century.<ref>Template:Citation</ref>Template:Unreliable source?

Energy

Template:Further Energy in the Eastern shore is provided by five oil and natural gas plants.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Pipeline

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Environment

Template:Further As part of the broader Chesapeake Bay watershed, the Eastern Shore confronts common environmental issues of the watershed, such as nutrient runoff from agriculture, but it is also vulnerable to climate change.

Because of its low-lying geography and sandy soil, the region is particularly vulnerable to sea level rise and salt water intrusion.<ref name="EPA">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Moreover, because of the coastal geography, infrastructure is already being damaged both due to sea level rise, and storm surge from tropical storms and hurricanes.<ref name="EPA" />

The Eastern Shore's economy depends on the larger fisheries and farming, both of which are sensitive to climate change.<ref name="EPA" />

Transportation

File:Chesapeake Bay Bridge MD1.jpg
Chesapeake Bay Bridge, which connects the Eastern Shore with the Washington, D.C. and Baltimore metropolitan area and the rest of Maryland

Various waterways provide a medium for commerce and boaters: the Atlantic Ocean, Chesapeake Bay, the Susquehanna River, and the Chesapeake and Delaware Canal.

There are three major routes to the Eastern Shore:

The two major highways on the Eastern Shore are U.S. Route 13 and U.S. Route 50, which meet in Salisbury.

Airports

Salisbury-Ocean City Wicomico Regional Airport, in Salisbury,<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> is the only commercial airport on the Delmarva Peninsula.

Airports for private aircraft include:

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Secession

The Eastern Shore has made several attempts to separate from Maryland. Proposals were debated in Maryland's General Assembly in 1833–1835, 1852, and 1998. There were earlier proposals visualizing a state encompassing the Delmarva Peninsula. The 1998 proposal by state Senators Richard F. Colburn and J. Lowell Stoltzfus did not specify a status for Eastern Shore's nine counties following secession, but suggested the new state's name could be "Delmarva".<ref>Template:Cite news</ref>

Sports

File:Shorebirdsgame.jpg
Arthur W. Perdue Stadium, home of the Delmarva Shorebirds Minor League baseball team

The Delmarva Shorebirds are a minor league baseball team who play Class A baseball in the Carolina League at Arthur W. Perdue Stadium in Salisbury, affiliated with the Baltimore Orioles.

Notable people

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  • Maggie Rogers, singer. From Easton, Talbot County.
  • Paul Sarbanes, former US Senator. Born in Salisbury, Wicomico County.<ref>{{#invoke:citation/CS1|citation

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Towns and cities

County seats:

See also

References

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