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Maryland

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Maryland

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Maryland

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USAClimateChange.com is presenting an opportunity for investors to lead the way for the State of Maryland and other states in this Climate Change industry boom.

Maryland

The Old Line State

Maryland is a state in the Mid-Atlantic and Southern regions of the United States, bordering Virginia, West Virginia, and the District of Columbia to its south and west; Pennsylvania to its north; and Delaware and the Atlantic Ocean to its east.

Baltimore is the largest city in the state, and the capital is Annapolis. Among its occasional nicknames are Old Line State, the Free State, and the Chesapeake Bay State. It is named after the English Queen Henrietta Maria, known in England as Queen Mary, who was the wife of King Charles.

Before its coastline was explored by Europeans in the 16th century, Maryland was inhabited by several groups of Native Americans – mostly by the Algonquin, and, to a lesser degree, by the Iroquois and Siouan. As one of the original Thirteen Colonies of England, Maryland was founded by George Calvert, 1st Baron Baltimore, a Catholic convert who sought to provide a religious haven for Catholics persecuted in England.

In 1632, Charles I of England granted Lord Baltimore a colonial charter, naming the colony after his wife, Queen Mary (Henrietta Maria of France). Unlike the Pilgrims and Puritans, who rejected Catholicism in their settlements,

Lord Baltimore 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.

Nevertheless, religious strife was common in the early years, and 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 heavily plantation-based and centered mostly on the cultivation of tobacco.

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, and by 1776, its delegates signed the Declaration of Independence. Many of its citizens subsequently played key political and military roles in the war. In 1790, the state ceded land for the establishment of the U.S. capital of Washington, D.C.

Maryland remained in the Union during the American Civil War, its strategic location giving it a significant role in the conflict. After the Civil War, Maryland took part in the Industrial Revolution, driven by its seaports, railroad networks, and mass immigration from Europe.

Since the 1940s, the state’s population has grown rapidly, to approximately six million residents, and it is among the most densely populated U.S. states. As of 2015, Maryland had the highest median household income of any state, owing in large part to its proximity to Washington, D.C. and a highly diversified economy spanning manufacturing, services, higher education, healthcare, and biotechnology. The state’s central role in U.S. history is reflected by its hosting of some of the highest numbers of historic landmarks per capita.

Sixteen of Maryland’s twenty-three counties, as well as the city of Baltimore, 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, culture, and history combine elements of the Mid-Atlantic, Northeastern, and Southern regions of the country.

 

 

CLIMATE

Maryland has a wide array of climates, due to local variances in elevation, proximity to water, and protection from colder weather due to downslope winds.

The eastern half of Maryland—which includes the cities of Ocean City, Salisbury, Annapolis, and the southern and eastern suburbs of Washington, D.C. and Baltimore—lies on the Atlantic Coastal Plain, with flat topography and sandy or muddy soil.

This region has a humid subtropical climate with hot, humid summers and a short, mild to cool winter; it falls under USDA Hardiness zone.

The Piedmont region—which includes northern and western greater Baltimore, Westminster, Gaithersburg, Frederick, and Hagerstown—has average seasonal snowfall totals generally exceeding 20 inches (51 cm) and, as part of USDA Hardiness zones, temperatures below 10 °F (−12 °C) are less rare. From the Cumberland Valley on westward, the climate begins to transition to a humid continental climate.

In western Maryland, the higher elevations of Allegany and Garrett counties—including the cities of Cumberland, Frostburg, and Oakland—display more characteristics of the humid continental zone, due in part to elevation. They fall under USDA Hardiness zones 6b and below.

Precipitation in the state is characteristic of the East Coast. Annual rainfall ranges from 35 to 45 inches (890 to 1,140 mm) with more in higher elevations. Nearly every part of Maryland receives 3.5–4.5 inches (89–114 mm) per month of rain. Average annual snowfall varies from 9 inches (23 cm) in the coastal areas to over 100 inches (250 cm) in the western mountains of the state.

Because of its location near the Atlantic Coast, Maryland is somewhat vulnerable to tropical cyclones, although the Delmarva Peninsula and the outer banks of North Carolina provide a large buffer, such that strikes from major hurricanes (category 3 or above) occur infrequently. More often, Maryland gets the remnants of a tropical system that has already come ashore and released most of its energy. Maryland averages around 30–40 days of thunderstorms a year, and averages around six tornado strikes annually.

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