Potomac State Forest is an 11,535-acre state forest in the state of Maryland near Oakland .
107-466: The forest offers a wide range of outdoor recreation opportunities, such as cross-country skiing, camping, fishing, hiking, and hunting. 39°29′31″N 79°27′26″W / 39.49194°N 79.45722°W / 39.49194; -79.45722 This article about a location in Garrett County , Maryland is a stub . You can help Misplaced Pages by expanding it . This article related to
214-410: A Democratic presidential candidate. Compared with neighbouring and closely allied Grant County, West Virginia , Garrett has not shown quite the same levels of Republican support – Lyndon Johnson did get within 109 votes of Barry Goldwater in 1964 – but as with Grant County, the only occasion Garrett County has not been carried by the official Republican nominee occurred in 1912 when a major split in
321-472: A cool climate and lack of any large city, Garrett County has remained a sparsely populated rural area. According to the U.S. Census Bureau , the county has a total area of 656 square miles (1,700 km ), of which 647 square miles (1,680 km ) is land and 8.6 square miles (22 km ) (1.3%) is water. It is the second-largest county in Maryland by land area. Garrett County is located entirely within
428-472: A fragile ecosystem known as the Southern Appalachian spruce–fir forest . Fraser fir rarely occurs below 5,500 ft (1,700 m), and becomes the dominant tree type at 6,200 ft (1,900 m). By contrast, balsam fir is found from near sea level to the tree line in the northern Appalachians, but ranges only as far south as Virginia and West Virginia in the central Appalachians, where it
535-735: A great thickness of sediment accumulated. Eventually, the tectonic forces pulling the two continents apart became so strong that an ocean formed off the eastern coast of the Laurentian margin. This was called the Iapetus Ocean and was the precursor of the modern Atlantic Ocean. The rocks of the Valley and Ridge province formed over millions of years, in the Iapetus. Shells and other hard parts of ancient marine plants and animals accumulated to form limey deposits that later became limestone. This
642-433: A household in the county was $ 32,238, and the median income for a family was $ 37,811. Males had a median income of $ 29,469 versus $ 20,673 for females. The per capita income for the county was $ 16,219. 13.30% of the population and 9.80% of families were below the poverty line. Out of the total people living in poverty, 16.60% are under the age of 18 and 13.90% are 65 or older. Garrett County is home to an Amish community in
749-672: A new ocean opened up, the Rheic Ocean , during the Middle to Late Devonian, and subsequently its closure would result in the formation of the Alleghanian orogeny . As the continental plates moved closer together, fragments of oceanic crust, islands, and other continental masses collided with the eastern margin of ancestral North America. By this time, plants had appeared on land, followed by scorpions, insects, and amphibians. The ocean continued to shrink until, about 270 million years ago,
856-504: A number of deciduous rhododendrons (azaleas), and smaller heaths such as teaberry ( Gaultheria procumbens ) and trailing arbutus ( Epigaea repens ). The evergreen great rhododendron ( Rhododendron maximum ) is characteristic of moist stream valleys. These occurrences are in line with the prevailing acidic character of most oak forest soils. In contrast, the much rarer chinquapin oak ( Quercus muehlenbergii ) demands alkaline soils and generally grows where limestone rock
963-444: A number of serious insect and disease outbreaks. Among the most conspicuous is that of the introduced spongy moth ( Lymantria dispar ), which infests primarily oaks, causing severe defoliation and tree mortality. But it also has the benefit of eliminating weak individuals, and thus improving the genetic stock, as well as creating rich habitat of a type through accumulation of dead wood. Because hardwoods sprout so readily, this moth
1070-496: A protected area in Maryland is a stub . You can help Misplaced Pages by expanding it . Garrett County, Maryland Garrett County ( / ɡ ər ɛ t / ) is the westernmost county of the U.S. state of Maryland completely within the Appalachian Mountains . As of the 2020 census , the population was 28,806, making it the third-least populous county in Maryland. Its county seat is Oakland . The county
1177-544: A variety of oaks ( Quercus spp.), hickories ( Carya spp.) and, in the past, by the American chestnut ( Castanea dentata ). The American chestnut was virtually eliminated as a canopy species by the introduced fungal chestnut blight ( Cryphonectaria parasitica ), but lives on as sapling-sized sprouts that originate from roots, which are not killed by the fungus. In present-day forest canopies, chestnut has been largely replaced by oaks. The oak forests of
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#17327986531791284-483: Is a boreal species that forms a few high elevation outliers as far south as West Virginia. All of these species except white pine tend to occupy sandy, rocky, poor soil sites, which are mostly acidic in character. White pine, a large species valued for its timber, tends to do best in rich, moist soil, either acidic or alkaline in character. Pitch pine is also at home in acidic, boggy soil, and Table Mountain pine may occasionally be found in this habitat as well. Shortleaf pine
1391-619: Is a public community college in McHenry, Maryland. The college had three outreach centers in Accident, Grantsville, and Oakland. Appalachian Mountains The Appalachian Mountains , often called the Appalachians , are a mountain range in eastern to northeastern North America . The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used
1498-870: Is also the highest point in the United States east of the Mississippi River . The range is older than the other major mountain range in North America, the Rocky Mountains of the west. Some of the outcrops in the Appalachians contain rocks formed during the Precambrian era. The geologic processes that led to the formation of the Appalachian Mountains started 1.1 billion years ago. The first mountain range in
1605-673: Is an extension of this hiking trail into the Canadian portion of the Appalachian range in New Brunswick and Quebec . While exploring inland along the northern coast of Florida in 1528, the members of the Narváez expedition , including Álvar Núñez Cabeza de Vaca , found a Native American village near present-day Tallahassee, Florida whose name they transcribed as Apalchen or Apalachen [a.paˈla.tʃɛn] . The name
1712-603: Is divided by kelly green. Although since the Civil War Maryland has been a Democratic-leaning state, Garrett County, owing to its history of German settlement from north of the Mason–Dixon line , plus strong pre-war Unionism resulting from virtual absence of slaves , has always been strongly Republican. Since it was created in 1872, Garrett is one of forty counties across the nation (chiefly Unionist strongholds in antebellum slave states ) to have never voted for
1819-403: Is found at high elevations in the northern Appalachians, and in bogs as far south as Pennsylvania. The Appalachians are also home to two species of fir, the boreal balsam fir ( Abies balsamea ), and the southern high elevation endemic, Fraser fir ( Abies fraseri ). Fraser fir is endemic to the highest parts of the southern Appalachian Mountains, where along with red spruce it forms
1926-533: Is generally found in warmer habitats and at lower elevations than the other species. All the species listed do best in open or lightly shaded habitats, although white pine also thrives in shady coves, valleys, and on floodplains. The Appalachians are characterized by a wealth of large, beautiful deciduous broadleaf (hardwood) trees. Their occurrences are best summarized and described in E. Lucy Braun 's 1950 classic, Deciduous Forests of Eastern North America (Macmillan, New York). The most diverse and richest forests are
2033-414: Is near the surface. Hence no ericaceous shrubs are associated with it. The Appalachian flora also include a diverse assemblage of bryophytes (mosses and liverworts), as well as fungi . Some species are rare and/or endemic. As with vascular plants , these tend to be closely related to the character of the soils and the thermal environment in which they are found. Eastern deciduous forests are subject to
2140-465: Is not as harmful as the hemlock woolly adelgid . Perhaps more serious is the introduced beech bark disease complex, which includes both a scale insect ( Cryptococcus fagisuga ) and fungal components. During the 19th and early 20th centuries, the Appalachian forests were subject to severe and destructive logging and land clearing, which resulted in the designation of the national forests and parks as well many state-protected areas. However, these and
2247-527: Is now the southern United States, the Ococee Basin was formed. Seawater filled the basin. Rivers from the surrounding countryside carried clay, silt, sand, and gravel to the basin, much as rivers today carry sediment from the midcontinent region to the Gulf of Mexico. The sediment spread out in layers on the basin floor. The basin continued to subside, and over a long period of time, probably millions of years,
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#17327986531792354-491: Is of great scientific interest because it is an ombrotrophic system (fed solely by rainwater) with peat layers up to 9 feet (2.7 m) thick, and is one of the oldest examples of mountain peatland in the Appalachians . On the western edge of the Savage River State Forest along Maryland Route 495 lies Bittinger, Maryland , which is named after Henry Bittinger , who first settled in the area and who
2461-721: Is one followed by the United States Geological Survey and the Geological Survey of Canada to describe the respective countries' physiographic regions. The U.S. uses the term Appalachian Highlands and Canada uses the term Appalachian Uplands ; the Appalachian Mountains are not synonymous with the Appalachian Plateau , which is one of the provinces of the Appalachian Highlands. The Appalachian range runs from
2568-520: Is part of Maryland's 6th congressional district . The extreme south of the county lies within the United States National Radio Quiet Zone . In the early 20th century, the railroad and tourism started to decline. Coal mining and timber production continued at a much slower pace. Today, tourism has made a dramatic rebound in the county with logging and farming making up the greatest part of the economic base. Due to
2675-590: Is part of the Pittsburgh, Pennsylvania television market. KDKA-TV and WTAE-TV in Pittsburgh, Pennsylvania, and WJAC-TV in Johnstown, Pennsylvania serves Oakland, the county seat. Oakland also has an educational television station (by way of PBS member station WGPT, part of state-wide Maryland Public Television ; it is also served by Pittsburgh-based member station WQED ). It has a weekly newspaper,
2782-552: Is possible that the cratons of Kalahari , and Rio Plato , were also part of that early collision since they were present as Rodinia broke up). Mountain-building referred to as the Grenville Orogeny occurred along the boundaries of the cratons. The present Appalachian Mountains have at least two areas which are made from rock formations that were formed during this orogeny - the Blue Ridge Mountains and
2889-645: Is subject to the hemlock woolly adelgid ( Adelges tsugae ), an introduced insect, that is rapidly extirpating it as a forest tree. Less abundant, and restricted to the southern Appalachians, is Carolina hemlock ( Tsuga caroliniana ). Like Canada hemlock, this tree suffers severely from the hemlock woolly adelgid. Several species of pines characteristic of the Appalachians are eastern white pine ( Pinus strobus ), Virginia pine ( Pinus virginiana ), pitch pine ( Pinus rigida ), Table Mountain pine ( Pinus pungens ) and shortleaf pine ( Pinus echinata ). Red pine ( Pinus resinosa )
2996-506: Is the same process by which limestone forms in modern oceans. The weathering of limestone, now exposed at the land surface, produces the lime-rich soils that are so prevalent in the fertile farmland of the Valley and Ridge province. During this continental break-up, around 600 million to 560 million years ago, volcanic activity was present along the tectonic margins. There is evidence of this activity in today's Blue Ridge Mountains. Mount Rogers , Whitetop Mountain , and Pine Mountain are all
3103-464: Is usually confined above 3,900 ft (1,200 m) asl, except in cold valleys. Curiously, it is associated with oaks in Virginia. The balsam fir of Virginia and West Virginia is thought by some to be a natural hybrid between the more northern variety and Fraser fir. While red spruce is common in both upland and bog habitats, balsam fir, as well as black spruce and tamarack, are more characteristic of
3210-521: The 2010 United States Census , there were 30,097 people, 12,057 households, and 8,437 families residing in the county. The population density was 46.5 inhabitants per square mile (18.0/km ). There were 18,854 housing units at an average density of 29.1 per square mile (11.2/km ). The racial makeup of the county was 97.8% white, 1.0% black or African American, 0.3% Asian, 0.1% American Indian, 0.1% from other races, and 0.7% from two or more races. Those of Hispanic or Latino origin made up 0.7% of
3317-683: The 6th congressional district , which includes part of northwestern metro DC. The district is currently represented by Democrat David Trone . The county is policed by the Garrett County Sheriff's Office and the Maryland State Police . The state parks are policed by the Department of Natural Resources Police . The county established an Office of the Fire Marshal in 2022, working in collaboration with
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3424-628: The Adirondacks . After the Grenville orogeny, the direction of the continental drift reversed, and the single supercontinent Rodinia began to break up. The mountains formed during the Grenvillian era underwent erosion due to weathering, glaciation, and other natural processes, resulting in the leveling of the landscape. The eroded sediments from these mountains contributed to the formation of sedimentary basins and valleys. For example, in what
3531-596: The Coal Region of northeastern Pennsylvania . The bituminous coal fields of western Pennsylvania , western Maryland , southeastern Ohio, eastern Kentucky, southwestern Virginia , and West Virginia contain the sedimentary form of coal. The mountain top removal method of coal mining , in which entire mountain tops are removed, is currently threatening vast areas and ecosystems of the Appalachian Mountain region. The surface coal mining that started in
3638-485: The Covid-19 Pandemic , tourism boomed as many people from Washington, DC , Baltimore , and Pittsburgh wanted to get away from the city. Garrett County Airport (2G4) is a general aviation airport surrounded by the mountains of Western Maryland . The airport enhances the region's tourist industry and provides emergency air service evacuation and landing facilities for general aviation . Garrett County
3745-922: The Garrett County Republican , which was purchased by NCWV Media in 2017. Annual events include the Autumn Glory Festival , the Scottish Highland Festival , and the Garrett County Agricultural Fair . The United States Census Bureau recognizes seven census-designated places (CDPs) in Garrett County. The following communities are classified as populated places or locales by the Geographic Names Information System. Garrett College
3852-608: The General Assembly of Maryland , and even those powers are narrowly construed. Garrett County is administered under a line organizational method, with the County Administrator responsible for the general administration of County Government. The administration of the county is centralized with the County Administrator responsible for overseeing the financial planning, annual budget process, personnel management, and direction and management of operations within
3959-437: The Geological Survey of Canada (GSC). The landforms are referred to as physiographic regions. The regions create precise boundaries from which maps can be drawn. The Appalachian Highlands is the name of one of the eight physiographic regions of the contiguous 48 United States. The Appalachian Uplands is the name of one of seven physiographic regions of Canada. The second level in the physiographic classification schema for
4066-758: The Gulf of Mexico . In the central section, north of the New River, the rivers, rising in or just beyond the Valley Ridges, flow through great gorges to the Great Valley, and then across the Blue Ridge to tidal estuaries penetrating the coastal plain via the Roanoke River, James River , Potomac River , and Susquehanna River . In the northern section the height of land lies on the inland side of
4173-661: The Iapetus Ocean , from the North America/Europe collision (See Caledonian orogeny ). By the end of the Mesozoic Era , the Appalachian Mountains had been eroded to an almost flat plain. It was not until the region was uplifted during the Cenozoic Era that the distinctive topography of the present formed. Uplift rejuvenated the streams, which rapidly responded by cutting downward into the ancient bedrock. Some streams flowed along weak layers that define
4280-613: The Island of Newfoundland in Canada, 2,050 mi (3,300 km) southwestward to Central Alabama in the United States; south of Newfoundland, it crosses the 96-square-mile (248.6 km ) archipelago of Saint Pierre and Miquelon , an overseas collectivity of France , meaning it is technically in three countries. The highest peak of the mountain range is Mount Mitchell in North Carolina at 6,684 feet (2,037 m), which
4387-491: The North American craton . Volcanoes grew along the continental margin coincident with the initiation of subduction . Thrust faulting uplifted and warped older sedimentary rock laid down on the passive margin. As the mountains rose, erosion began to wear them down over time. Streams carried rock debris downslope to be deposited in nearby lowlands. The Taconic orogeny ended after about 60 million years, but built much of
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4494-468: The census of 2000, there were 29,846 people, 11,476 households, and 8,354 families residing in the county. The population density was 18/km (46/sq mi). There were 16,761 housing units at an average density of 10/km (26/sq mi). The racial makeup of the county was 98.83% White , 0.43% Black or African American , 0.07% Native American , 0.19% Asian , 0.02% Pacific Islander , 0.09% from other races , and 0.37% from two or more races. 0.44% of
4601-660: The eastern seaboard of the United States and the Midwest region of the country. The Eastern Continental Divide follows the Appalachian Mountains from Pennsylvania to Georgia. The Appalachians, particularly the Central and Southern regions, is one of the most biodiverse places in North America. The north–south orientation of the long ridges and valleys contributes to the high number of plant and animal species. Species were able to migrate through these from either direction during alternating periods of warming and cooling, settling in
4708-1552: The mixed-mesophytic or medium-moisture types, which are largely confined to rich, moist montane soils of the southern and central Appalachians, particularly in the Cumberland and Allegheny Mountains, but also thrive in the southern Appalachian coves. Characteristic canopy species are white basswood ( Tilia heterophylla ), yellow buckeye ( Aesculus octandra ), sugar maple ( Acer saccharum ), American beech ( Fagus grandifolia ), tuliptree ( Liriodendron tulipifera ), white ash ( Fraxinus americana ) and yellow birch ( Betula alleganiensis ). Other common trees are red maple ( Acer rubrum ), shagbark and bitternut hickories ( Carya ovata and C. cordiformis ) and black or sweet birch ( Betula lenta ). Small understory trees and shrubs include paw paw ( Asimina tribola ), flowering dogwood ( Cornus florida ), hophornbeam ( Ostrya virginiana ), witch-hazel ( Hamamelis virginiana ) and spicebush ( Lindera benzoin ). There are also hundreds of perennial and annual herbs, among them such herbal and medicinal plants as American ginseng ( Panax quinquefolius ), goldenseal ( Hydrastis canadensis ), bloodroot ( Sanguinaria canadensis ) and black cohosh ( Cimicifuga racemosa ). The foregoing trees, shrubs, and herbs are also more widely distributed in less rich mesic forests that generally occupy coves, stream valleys and flood plains throughout
4815-596: The 1940s has significantly impacted the central Appalachian Mountains in Kentucky , Tennessee , Virginia and West Virginia. Early mining methods were unregulated and mined land reclamation research, including acid base reaction , was led by the West Virginia University in the 1960s and 1970s. West Virginia developed rigorous mine reclamation standards for state coal mines in the late 1960s. Regulations were introduced by most federal states to protect
4922-564: The Appalachian Basin. Some plateaus of the Appalachian Mountains contain metallic minerals such as iron and zinc . There are many geological issues concerning the rivers and streams of the Appalachians. In spite of the existence of the Great Appalachian Valley, many of the main rivers are transverse to the mountain system axis. The drainage divide of the Appalachians follows a tortuous course that crosses
5029-627: The Appalachian Mountains by the late 1960s. Social and political activism brought about the Surface Mining Control and Reclamation Act of 1977 . The 1859 discovery of commercial quantities of petroleum in the Appalachian Mountains of western Pennsylvania started the modern United States petroleum industry . Recent discoveries of commercial natural gas deposits in the Marcellus Shale formation and Utica Shale formations have once again focused oil industry attention on
5136-552: The Blue Ridge again reaches 2,000 ft (600 m) and higher. In the Virginia Blue Ridge, the following are some of the highest peaks north of the Roanoke River : Stony Man 4,031 ft (1,229 m), Hawksbill Mountain 4,066 ft (1,239 m), Apple Orchard Mountain 4,225 ft (1,288 m) and Peaks of Otter 4,001 and 3,875 ft (1,220 and 1,181 m). South of the Roanoke River, along
5243-738: The Blue Ridge, are Virginia's highest peaks including Whitetop Mountain 5,520 ft (1,680 m) and Mount Rogers 5,729 ft (1,746 m), the highest point in the Commonwealth. Chief summits in the southern section of the Blue Ridge are located along two main crests, the Western or Unaka Front along the Tennessee - North Carolina border and the Eastern Front in North Carolina, or one of several "cross ridges" between
5350-579: The Garrett County Board of Education. The municipal parks of Garrett County provide sport facilities, hiking, bike and walk paths, playgrounds, picnic areas, boat ramps, and fishing. The Ruth Enlow Library was founded in 1915 as the Oakland Free Public Library. Since then, an additional four branches have been added to the library system in Accident, Friendsville, Grantsville, and Kitzmiller. The present director of
5457-931: The Great Balsams. The Western Blue Ridge Front is subdivided into the Unaka Range , the Bald Mountains , the Great Smoky Mountains , and the Unicoi Mountains , and its major peaks include Roan Mountain 6,285 ft (1,916 m) in the Unakas, Big Bald 5,516 ft (1,681 m) and Max Patch 4,616 ft (1,407 m) in the Bald Mountains, Kuwohi 6,643 ft (2,025 m), Mount Le Conte 6,593 feet (2,010 m), and Mount Guyot 6,621 ft (2,018 m) in
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#17327986531795564-749: The Great Smokies, and Big Frog Mountain 4,224 ft (1,287 m) near the Tennessee- Georgia -North Carolina border. Prominent summits in the cross ridges include Waterrock Knob (6,292 ft (1,918 m)) in the Plott Balsams . Across northern Georgia, numerous peaks exceed 4,000 ft (1,200 m), including Brasstown Bald , the state's highest, at 4,784-and-4,696 ft (1,458-and-1,431 m) Rabun Bald . In north-central Alabama , Mount Cheaha rises prominently to 1,445 feet (440 m) over its surroundings, as part of
5671-441: The Maryland State Office established in 1894. Garrett County produces natural gas , the only county in the state to do so. Much of the economic activity in the area centers around tourism. In the winter, the Wisp ski resort in Oakland and New Germany State Park's cross-country skiing trail are frequent destinations, and Deep Creek Lake sees much activity in the summer. The state parks in the county are frequented year-round. During
5778-486: The Oakland area that consists of a church district of about 70 homes. The Amish community dates back to 1850 and became associated with the New Order Amish , with electricity permitted inside of homes. The county is governed by an elected three-member Board of County Commissioners , whose members serve four-year terms and must live in the district they represent. The Board is the traditional form of county government in Maryland. It may exercise only those powers conferred by
5885-483: The Pinnacle 3,007 feet (917 m) and Pidgeon Roost 3,400 ft (1,000 m). In West Virginia, more than 150 peaks rise above 4,000 ft (1,200 m), including Spruce Knob 4,863 ft (1,482 m), the highest point in the Allegheny Mountains . A number of other points in the state rise above 4,800 ft (1,500 m). Cheat Mountain ( Snowshoe Mountain ) at Thorny Flat 4,848 ft (1,478 m) and Bald Knob 4,842 ft (1,476 m) are among
5992-402: The Potomac, drains about a third of the county. The Casselman River , a tributary of the Youghiogheny, flows north from the county's central section into Pennsylvania. The Youghiogheny itself drains the westernmost area of the county and flows north into Pennsylvania, where it empties into the Monongahela River at McKeesport , just south of Pittsburgh . The Glades' 601 acres (2.43 km )
6099-471: The Republican Party allowed "Bull Moose Party" nominee and former President Theodore Roosevelt to claim the county. Since 1996, no Democratic presidential nominee has won even 30% of the county's vote, and not since 2010 has Garrett County voted Democratic in any statewide election. Garrett County has been the most conservative county in Maryland in the 21st century. Owing to its strong Republican lean, Garrett County sometimes votes against ballot measures that
6206-433: The USGS is "province", the same word as Canada uses to divide its political subdivisions, meaning that the terminology used by the two countries do not match below the region level. The lowest level of classification is "section". The Appalachian Uplands are one of the seven physiographic divisions in Canada . Canada's GSC does not use the same classification system as the USGS below the division level. The agency does break
6313-433: The United States and Canada, and partly because the range was formed over numerous geologic time periods, one of which is sometimes termed the Appalachian orogeny , writing communities struggle to agree on an encyclopedic definition of the mountain range. However, each of the governments has an agency that informs the public about the major landforms that make up the countries, the United States Geological Survey (USGS) and
6420-414: The border of the coastal plain through the central and southern Atlantic states; and on the northwest, the Allegheny and Cumberland plateaus declining toward the Great Lakes and the interior plains. A remarkable feature of the belt is the longitudinal chain of broad valleys, including the Great Appalachian Valley , which in the southerly sections divides the mountain system into two unequal portions, but in
6527-457: The continent that are now exposed. The first mountain-building tectonic plate collision that initiated the construction of what are today the Appalachians occurred at least a billion years ago when the pre-North American craton called Laurentia collided with at least one other craton - Amazonia . All the other cratons of the earth also collided at about this time to form the supercontinent Rodinia and were surrounded by one single ocean. (It
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#17327986531796634-416: The continents that were ancestral to North America and Africa collided during the formation of the supercontinent Pangea . Because North America and Africa were once geographically connected, the Appalachians formed part of the same mountain chain as the Little Atlas in Morocco . This mountain range, known as the Central Pangean Mountains , extended into Scotland , before the Mesozoic Era opening of
6741-410: The county's mountains. The colors are peacock blue for the sky and water. The blue and white background is divided by kelly green. The official flag for Garrett County is elliptical. The flag illustrates a large snowflake to depict winter; water to represent sailing; and oaks and conifer to represent the county's mountains. The colors are peacock blue for the sky and water. The blue and white background
6848-437: The county, drained by the Youghiogheny River , is the only part of Maryland within the Mississippi River drainage basin . All other parts of the county are in the Chesapeake Bay basin. The National Register of Historic Places listings in Garrett County, Maryland has 20 National Register of Historic Places properties and districts, including Casselman Bridge, National Road a National Historic Landmark . Garrett County
6955-412: The deciduous needle-leaf conifer, the tamarack , or eastern larch ( Larix laricina ). The dominant northern and high elevation conifer is the red spruce ( Picea rubens ), which grows from near sea level to above 4,000 ft (1,200 m) above sea level (asl) in northern New England and southeastern Canada. It also grows southward along the Appalachian crest to the highest elevations of
7062-399: The divisions of the Appalachian Uplands into 13 subsections that are in four different political provinces of Canada. While the Appalachian Highlands and Appalachian Uplands are generally continuous across the U.S./Canadian border, the St. Lawrence Valley area is handled differently in the physiographic classification schemas. The part of the St. Lawrence Valley in the United States is one of
7169-529: The driest sites are dominated by chestnut oak, or sometimes by scarlet or northern red oaks. In the northern Appalachians the oaks, except for white and northern red, drop out, while the latter extends farthest north. The oak forests generally lack the diverse small tree, shrub and herb layers of mesic forests. Shrubs are generally ericaceous , and include the evergreen mountain laurel ( Kalmia latifolia ), various species of blueberries ( Vaccinium spp.), black huckleberry ( Gaylussacia baccata ),
7276-440: The early 19th century, Washington Irving proposed renaming the United States either Appalachia or Alleghania. In U.S. dialects in the southern regions of the Appalachians, the word is pronounced / ˌ æ p ə ˈ l æ tʃ ɪ n z / , with the third syllable sounding like "latch". In northern parts of the mountain range, it is pronounced / ˌ æ p ə ˈ l eɪ tʃ ɪ n z / or / ˌ æ p ə ˈ l eɪ ʃ ɪ n z / ;
7383-425: The folds and faults created many millions of years earlier. Other streams downcut so rapidly that they cut right across the resistant folded rocks of the mountain core, carving canyons across rock layers and geologic structures. The Appalachian Mountains contain major deposits of anthracite coal as well as bituminous coal . In the folded mountains the coal is in metamorphosed form as anthracite , represented by
7490-434: The highland zone of the Appalachian Mountains known variously as the Allegheny Mountains , the Allegheny Plateau , and the Appalachian Plateau . The county's highest elevations are located along four flat-topped ridges and range to a height of 3,360 feet (1,020 m) at Hoye-Crest along Backbone Mountain , the highest point in the state of Maryland. As is typical in the Allegheny region, broad flats generally lie below
7597-431: The land mass that is now New England and southwestward to Pennsylvania. The Taconic Orogeny was the second of four mountain building plate collisions that contributed to the formation of the Appalachians, culminating in the collision of North America and Africa (see Alleghanian orogeny ). The third mountain-building event was the Acadian orogeny which occurred between 375 and 359 million years ago. The Acadian orogeny
7704-491: The last great ice sheet over North America. A series of low mounds can be seen in the fields on the west side of Maryland Route 495 that are "loess" (wind-blown) material. Apparently, these are the only ones still visible in the northern part of Garrett County. The mounds were formed when a glacier lake existed in the Casselman valley, and the ice around the edges of the frozen lake melted. Wind blew fine grains of earth into
7811-469: The latter. However, balsam fir also does well in soils with a pH as high as 6. Eastern or Canada hemlock ( Tsuga canadensis ) is another important evergreen needle-leaf conifer that grows along the Appalachian chain from north to south but is confined to lower elevations than red spruce and the firs. It generally occupies richer and less acidic soils than the spruce and firs and is characteristic of deep, shaded and moist mountain valleys and coves . It
7918-631: The library is Thomas Vose. The Garrett County Historical Society and Museums include a Historical Museum, a Transportation Museum, the Grantsville Museum and the Leo Beachley Photographic Archives. Note: the US Census treats Hispanic/Latino as an ethnic category. This table excludes Latinos from the racial categories and assigns them to a separate category. Hispanics/Latinos can be of any race. As of
8025-540: The microclimates that best suited them. The flora of the Appalachians are diverse and vary primarily in response to geology, latitude, elevation and moisture availability. Geobotanically, they constitute a floristic province of the North American Atlantic Region . The Appalachians consist primarily of deciduous broad-leaf trees and evergreen needle-leaf conifers, but also contain the evergreen broad-leaf American holly ( Ilex opaca ), and
8132-788: The more notable peaks in West Virginia. The Blue Ridge Mountains , rising in southern Pennsylvania and there known as South Mountain , attain elevations of about 2,000 ft (600 m) in Pennsylvania. South Mountain achieves its highest point just below the Mason-Dixon line in Maryland at Quirauk Mountain 2,145 ft (654 m) and then diminishes in height southward to the Potomac River . Once in Virginia ,
8239-787: The mountainous belt just north of the New River in Virginia. South of the New River, rivers head into the Blue Ridge, cross the higher Unakas, receive important tributaries from the Great Valley, and traversing the Cumberland Plateau in spreading gorges ( water gaps ), escape by way of the Cumberland River and the Tennessee River rivers to the Ohio River and the Mississippi River, and thence to
8346-550: The mountainous belt, and thus the main lines of drainage run from north to south, exemplified by the Hudson River . However, the valley through which the Hudson River flows was cut by the gigantic glaciers of the ice ages —the same glaciers that deposited their terminal moraines in southern New York and formed the east–west Long Island . The Appalachian region is generally considered the geographical divide between
8453-432: The name of the tribe to the mountains themselves. The first cartographic appearance of Apalchen is on Diego Gutiérrez 's map of 1562; the first use for the mountain range is the map of Jacques le Moyne de Morgues in 1565. The name was not commonly used for the whole mountain range until the late 19th century. A competing and often more popular name was the "Allegheny Mountains", "Alleghenies", and even "Alleghania". In
8560-467: The northernmost lies west of all the ranges possessing typical Appalachian features, and separates them from the Adirondack group. The mountain system has no axis of dominating altitudes, but in every portion, the summits rise to rather uniform heights, and, especially in the central section, the various ridges and intermontane valleys have the same trend as the system itself. None of the summits reaches
8667-424: The oceans, but there were no plants or animals on land. Then, during the middle Ordovician Period about 500 to 470 million years ago, the motion of the crustal plates changed, and the continents began to move back toward each other. The once-quiet Appalachian passive margin changed to a very active plate boundary when a neighboring Iapetus oceanic plate containing a volcanic arc collided with and began sinking beneath
8774-476: The organization. On December 15, 1977, the seal of Garrett County went into effect by virtue of Resolution #7. The seal is elliptical, with the name "Garrett County" inscribed above the upper fourth of the ellipse, and "Maryland 1872" inscribed below the lower fourth of the ellipse. The date "1872" depicts the year of the formation of Garrett County. The seal illustrates a large snowflake to depict winter; water to represent sailing; and oaks and conifer to represent
8881-483: The population were Hispanic or Latino of any race. 36.1% were of German , 22.9% identified as American , 9.6% English and 8.8% Irish ancestry. There were 11,476 households, out of which 32.60% had children under the age of 18 living with them, 60.70% were married couples living together, 8.40% had a female householder with no husband present, and 27.20% were non-families. 23.50% of all households were made up of individuals, and 10.60% had someone living alone who
8988-436: The population. In terms of ancestry, 35.4% were German , 13.6% identified as American , 11.3% were Irish , and 11.3% were English . Of the 12,057 households, 30.0% had children under the age of 18 living with them, 56.4% were married couples living together, 9.3% had a female householder with no husband present, 30.0% were non-families, and 25.5% of all households were made up of individuals. The average household size
9095-460: The region of perpetual snow. In Pennsylvania , there are over sixty summits that rise over 2,500 ft (800 m); the summits of Mount Davis and Blue Knob rise over 3,000 ft (900 m). In Maryland, Eagle Rock and Dans Mountain are conspicuous points reaching 3,162 and 2,882 ft (964 and 878 m) respectively. On the same side of the Great Valley, south of the Potomac, are
9202-506: The region was created when the continents of Laurentia and Amazonia collided, creating a supercontinent called Rodinia . The collision of these continents caused the rocks to be folded and faulted, creating the first mountains in the region. Many of the rocks and minerals that were formed during that event can currently be seen at the surface of the present Appalachian range. Around 480 million years ago, geologic processes began that led to three distinct orogenic eras that created much of
9309-420: The rest of the state approves by large margins. In 2022, Garrett County was the only county in the state to vote against legalizing recreational cannabis via 2022 Maryland Question 4 . In 2024, Garrett County was the only county in the state to vote against enshrining a right to abortion in the state constitution via 2024 Maryland Question 1 . Garrett County is represented in the U.S. House of Representatives by
9416-488: The result of volcanic activity that occurred around this time. Evidence of subsurface activity, dikes and sills intruding into the overlying rock, is present in the Blue Ridge as well. For instance, mafic rocks have been found along the Fries Fault in the central Blue Ridge area of Montgomery County, VA. The Iapetus continued to expand and during that time bacteria, algae, and many species of invertebrates flourished in
9523-527: The ridge crests at elevations of approximately 500 feet (150 m). River valleys are generally narrow and deep, with ravines typically 1,000 to 1,800 feet (550 m) below surrounding peaks. The county contains over 76,000 acres (310 km ) of parks, lakes, and publicly accessible forestland. It is drained by two river systems, the Potomac and the Youghiogheny . The Savage River , a tributary of
9630-532: The ridges are not high, the terrain is extremely rugged. In Ohio and New York, some of the plateau has been glaciated , which has rounded off the sharp ridges and filled the valleys to some extent. The glaciated regions are usually referred to as hill country rather than mountains. The Appalachian belt includes the plateaus sloping southward to the Atlantic Ocean in New England , and southeastward to
9737-498: The second-level classifications, part of the Appalachian Highlands. In Canada, the area is part of the first-level classification, the St. Lawrence Lowlands . This includes the area around the city of Montreal, Anticosti Island , and the northwest coastline of Newfoundland. The dissected plateau area, while not actually made up of geological mountains, is popularly called "mountains", especially in eastern Kentucky and West Virginia, and while
9844-416: The southern Appalachians, as in North Carolina and Tennessee . In the central Appalachians it is usually confined above 3,000 ft (900 m) asl, except for a few cold valleys in which it reaches lower elevations. In the southern Appalachians, it is restricted to higher elevations. Another species is the black spruce ( Picea mariana ), which extends farthest north of any conifer in North America,
9951-413: The southern and central Appalachians consist largely of black , northern red , white , chestnut and scarlet oaks ( Quercus velutina, Q. rubra, Q. alba, Q. prinus and Q. coccinea ) and hickories, such as the pignut ( Carya glabra ) in particular. The richest forests, which grade into mesic types, usually in coves and on gentle slopes, have predominantly white and northern red oaks, while
10058-511: The southern and central Appalachians at low and intermediate elevations. In the northern Appalachians and at higher elevations of the central and southern Appalachians these diverse mesic forests give way to less diverse northern hardwood forests with canopies dominated only by American beech, sugar maple, American basswood ( Tilia americana ) and yellow birch and with far fewer species of shrubs and herbs. Drier and rockier uplands and ridges are occupied by oak–chestnut forests dominated by
10165-544: The southernmost spur of the Blue Ridge Mountains. Sources written prior to the recognition of the concept of physiographic regions divided the Appalachian Mountains into three major sections: Plate tectonics over the period dating back at least 1 billion years led to geological creation of the land that is now the Appalachian Mountain range. The continental movement led to collisions that built mountains and they later pulled apart creating oceans over parts of
10272-573: The surface structure seen in today's Appalachians. During this period, mountains once reached elevations similar to those of the Alps and the Rockies before natural erosion occurred over the last 240 million years leading to what is present today. The Appalachian Mountains are a barrier to east–west travel, as they form a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. This barrier
10379-440: The third syllable is like "lay", and the fourth "chins" or "shins". There is often great debate between the residents of the regions regarding the correct pronunciation. Elsewhere, a commonly accepted pronunciation for the adjective Appalachian is / ˌ æ p ə ˈ l æ tʃ i ə n / , with the last two syllables "-ian" pronounced as in the word "Romanian". Perhaps partly because the range runs through large portions of both
10486-628: The two main crests. Major subranges of the Eastern Front include the Black Mountains , Great Craggy Mountains , and Great Balsam Mountains , and its chief summits include Grandfather Mountain 5,964 ft (1,818 m) near the Tennessee-North Carolina border, Mount Mitchell 6,684 ft (2,037 m) in the Blacks, and Black Balsam Knob 6,214 ft (1,894 m) and Cold Mountain 6,030 ft (1,840 m) in
10593-1399: The water around the edges where it sank to the bottom, and the mounds were the result of the deposit of this wind-blown material. See these articles for information on the forests, rivers, and caves of Garrett County: Garrett County contains over 76,000 acres (310 km ) of parks, lakes, and publicly accessible forestland. Popular activities in the county include camping, hiking, backpacking, rock climbing, alpine and cross-country skiing, snowmobiling, hunting, ice fishing, fly fishing, whitewater canoeing, kayaking, rafting, boating, swimming, sailing, horseback riding, and water skiing. There are seven state parks in Garrett County. All offer picnic and fishing areas; all but Casselman River State Park have hiking paths. Mountain bike paths, swimming areas, and boat launches and rentals are available at Deep Creek, Herrington Manor, and New Germany state parks. Rental cabins are available at Herrington Manor and New Germany state parks. Big Run, Deep Creek, Herrington Manor, and New Germany state parks all offer canoeing, while campsites may be found at Big Run, Deep Creek, New Germany, and Swallow Falls state parks. Garrett County owns four park sites and fifteen recreation facilities. The parks are maintained in cooperation with local associations and civic groups. The recreation areas are attached to public schools and colleges and maintained by
10700-468: Was 2.45 and the average family size was 2.92. The median age was 42.7 years. The median income for a household in the county was $ 45,760 and the median income for a family was $ 56,545. Males had a median income of $ 40,035 versus $ 27,325 for females. The per capita income for the county was $ 23,888. About 8.9% of families and 12.5% of the population were below the poverty line , including 19.2% of those under age 18 and 12.1% of those aged 65 or over. As of
10807-458: Was 65 years of age or older. The average household size was 2.55 and the average family size was 3.00. In the county, the population was spread out, with 25.10% under the age of 18, 7.80% from 18 to 24, 27.60% from 25 to 44, 24.60% from 45 to 64, and 14.90% who were 65 years of age or older. The median age was 38 years. For every 100 females, there were 97.20 males. For every 100 females age 18 and over, there were 93.80 males. The median income for
10914-661: Was caused by a series of collisions of pieces of crust from the Avalonia Terrane, sections broken off from continent of Gondwana , with the North American Plate. The collision initiating this orogeny resulted in the closing of the southern Iapetus Ocean and the formation of a high mountain belt. After the Acadian collision took place, Gondwana began to retreat from Laurentia with the newly accreted Avalonian terranes left behind. As Gondwana moved away,
11021-735: Was defined by the Bauer Report, submitted to Governor Lloyd Lowndes, Jr. on November 9, 1898. The Potomac River and State of West Virginia lie to the south and west. Garrett County lies in the Allegheny Mountains , which here form the western flank of the Appalachian Mountain Range . Hoye-Crest , a summit along Backbone Mountain , is the highest point in Maryland at an elevation of 3,360 feet (1,020 m). The Eastern Continental Divide runs along portions of Backbone Mountain . The western part of
11128-591: Was extremely important in shaping the expansion of the United States in the colonial era. The range is the home of a very popular recreational feature, the Appalachian Trail . This is a 2,175-mile (3,500 km) hiking trail that runs all the way from Mount Katahdin in Maine to Springer Mountain in Georgia , passing over or past a large part of the Appalachian range. The International Appalachian Trail
11235-590: Was joined by other German settlers moving in and taking up the fertile farmland. On the eastern edge of Bittinger is one of the largest glades area of Garrett County. Geographically, this is an area that seems to have been affected by the last great ice sheet of North America. Two miles southeast of Bittinger, there is a large deposit of peat moss . In the Casselman River valley, 1-mile (1.6 km) south of Grantsville, Maryland and beside Maryland Route 495 , one can see remains of geological evidence about
11342-624: Was named for John Work Garrett (1820–1884), president of the Baltimore and Ohio Railroad . Created from Allegany County in 1872, it was the last county to be formed in the state. The county is part of the Western Maryland region of the state. Garrett County is bordered by four West Virginia counties and to the north the Maryland–Pennsylvania boundary known as the Mason–Dixon line . The eastern border with Allegany County
11449-518: Was soon altered by the Spanish to Apalachee and used as a name for the tribe and region spreading well inland to the north. Pánfilo de Narváez 's expedition first entered Apalachee territory on June 15, 1528, and applied the name. Now spelled "Appalachian", it is the fourth-oldest surviving European place-name in the US. After the 1540 expedition of Hernando de Soto , Spanish cartographers began to apply
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