Misplaced Pages

#401598

105-518: Founded in 1836 as a literary society by the editors of Harvardiana , the club was granted a charter by the Alpha Delta Phi fraternity on March 29, 1837 . It remained active until surrendering its charter in 1865. With the graduation of the members of the class of 1868, the club was discontinued until 1878, when graduate members, including Edward Everett Hale (class of 1839) and Phillips Brooks (class of 1855), initiated undergraduates from

210-557: A brick facade added in 1902, the Fly clubhouse is located at Two Holyoke Place, near Harvard Square, along the "Gold Coast" of formerly private residences that now comprise Harvard's Adams House , completed 1932. The Fly sits in front of Harvard's Lowell House (1930), across Mt. Auburn Street from the Harvard Lampoon building (1909). The Fly Club Gate is located along the exterior of Winthrop House . An English Baroque structure,

315-494: A different location on campus - into a house designed by John Russell Pope - but the original chapter house, designed and built by William Henry Miller , still stands. The original chapter house at the University of Illinois Urbana-Champaign was built in 1924 and 1925 for the fraternity. This three-story Tudor Revival style chapter house was designed by architect Ralph W. Varney, an Alpha Delta Phi brother. The building

420-472: 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

525-735: 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

630-672: 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,

735-533: A new society of limited membership based on "the loftiest of intellectual and moral ideals." On October 29, 1832, Eells gathered four other members, two from the Phoenix and two from the Philopeuthian, to a meeting in his room. The other men were Lorenzo Latham , John Curtiss Underwood , Oliver Andrew Morse and Henry Lemuel Storrs. At that meeting, Eells wrote the constitution and he and Latham designed

840-504: 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

945-444: 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

1050-544: 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

1155-601: Is a retronym used now to distinguish the all-male Alpha Delta Phi Fraternity from the gender-inclusive Alpha Delta Phi Society (discussed below). In general parlance, the Fraternity refers to itself simply as the "Alpha Delta Phi"; the Society uses either the "Alpha Delta Phi Society" or "The Society". The Brunonian ( Brown University ) chapter first initiated women into its local membership in November 1973, and this

SECTION 10

#1732772801402

1260-930: Is a North American Greek-letter social college fraternity . Alpha Delta Phi was originally founded as a literary society by Samuel Eells in 1832 at Hamilton College in Clinton, New York . Its more than 50,000 alumni include former presidents and senators of the United States , and justices of the Supreme Court . The mission of the Alpha Delta Phi Fraternity is to provide a comprehensive and positive personal growth experience for all undergraduate and alumni brothers: social, ethical, leadership, scholastic, community service, and literary. When Samuel Eells arrived on campus at Hamilton College , he found two existing literary societies ,

1365-483: 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

1470-716: Is a charter member of the North American Interfraternity Conference (formerly known as the National Interfraternity Conference; NIC). A Brother of Alpha Delta Phi, Hamilton W. Mabie (Williams College, class of 1867), was the first President of the NIC. The Alpha Delta Phi Fraternity is today still a member of the NIC; the Alpha Delta Phi Society, a gender-inclusive offshoot of the Fraternity,

1575-870: 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

1680-673: 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

1785-470: Is an oblong slab with rounded corners, displaying on a shield of black enamel a white Crescent bearing the letters Alpha Delta Phi. Above the Crescent is a green Star with a gold center, and below is the date 1832 in gold. On the back is engraved a Monument with crossed Sword and Spear. In addition, the member's initials and surname, chapter, and year of graduation appear on the back of the badge. The Badge

1890-554: Is at the convention; others are held at various chapter houses in the fall, winter, and spring. The governors elect the president, vice president, secretary, and treasurer. The president, with board approval, may appoint an assistant treasurer and committee chairmen, who may or may not be governors. An undergraduate Assistant Secretary is elected by the undergraduate delegates of the convention. The Board of Governors appoints Regional Directors to coordinate activities of interest to nearby chapters and alumni organizations. The Fraternity

1995-403: 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

2100-533: 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

2205-414: 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

SECTION 20

#1732772801402

2310-465: 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

2415-527: 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,

2520-721: 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

2625-405: Is only to be worn with suit and tie attire. The Badge is properly worn over the heart with the horns of the Crescent pointing over the right shoulder. The Crest, which is the coat of arms, consists of the shield or escutcheon divided vertically into equal parts of green and white. It is bordered in black and studded with pearls. There is a small gold line between the center part of the shield and

2730-552: 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

2835-645: 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 )

2940-506: 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

3045-464: 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

3150-628: 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

3255-596: 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

Fly Club - Misplaced Pages Continue

3360-437: 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

3465-758: 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

3570-661: 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

3675-613: 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

3780-491: 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

3885-660: 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

3990-1552: 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

4095-412: The 1832 Foundation is to solicit financial resources, provide faithful stewardship, and engage in high-quality ethical practices in support of the Alpha Delta Phi Fraternity and leadership development. The foundation aims to leave a legacy that builds leaders of good character and well-balanced men. The Foundation is a self-governing, tax-exempt corporation founded August 1961, under Section 501 (c) (3) of

4200-596: 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

4305-564: 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

Fly Club - Misplaced Pages Continue

4410-627: 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

4515-552: 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

4620-738: 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

4725-533: The Board of Governors and the Chapters. Between the business and leadership training sessions, Conventions are characterized by considerable socializing. Brothers from all over the continent get acquainted, swap stories and songs, and raise a glass in the spirit of brotherhood. Whether as a voting delegate or as an observer, all brothers are encouraged to attend a Convention at some time. The convention also elects

4830-469: The Board of Governors. There are eleven Alumni Governors, elected for three-year terms, and a Student Governor elected annually. The terms of the Alumni Governors are staggered to provide continuity. There are other restrictions on who may be elected to ensure that no region or chapter may dominate the Board. The Board of Governors generally holds four regular meetings each year. One of these

4935-623: The Fraternity. The convention is composed of one delegate elected from each undergraduate chapter and alumni organization, each delegate being entitled to one vote. Each August, the convention is hosted at a different location and presided over by an Honorary Chairman, both of which are chosen by the Board of Governors. The convention hears annual reports from the Governors, approves the International's budget, decides constitutional questions, and has appellate jurisdiction over decisions of

5040-931: 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

5145-749: 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

5250-477: The Internal Revenue Code. It accepts deductible donations from Alpha Delts and others and makes grants and loans to chapters, individuals, and institutions of higher learning. The grants are intended to promote intellectual interest or achievement with qualified educational and literary programs. The Foundation has its own Board of Directors and functions independently of but in communication with

5355-411: The Phoenix and the Philopeuthian, the latter of which he reluctantly joined. Eells quickly became disenchanted with both societies' unscrupulous recruiting tactics and dispassionately small sizes and considered creating his own society which would disavow what he described as jealous and angry competition between the two. Eells proposed to select members from both the Phoenix and the Philopeuthian and found

SECTION 50

#1732772801402

5460-609: 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

5565-429: The Society's license to use the name "Alpha Delta Phi Society." It also removed most of the limitations on where either organization could have chapters. The Society as a national organization is gender-inclusive, and the Society continues to espouse "home rule" for its chapters, allowing them to determine their own membership rules. As of today, every Society chapter has been a gender-inclusive organization since at least

5670-705: The Society's use of the name "Alpha Delta Phi". On August 12, 2017, at the Fraternity's 185th Annual Convention held in Minneapolis, Minnesota, the Fraternity and the Society entered into a new agreement that replaced the Fraternity-Society Agreement of 1992. The new agreement maintained the original rights of the two independent and legally separate organizations to license and share the Greek letters alpha, delta, and phi, and other intellectual property. The new agreement removed all restrictions on

5775-433: 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

5880-433: 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

5985-414: 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

6090-403: The border which has no particular significance except as a line of partition. On the shield in honor point are three Greek letters, horizontally aligned, alpha, delta, and phi in gold. Above the shield is an esquires helmet in profile facing left with the visor closed. Behind the shield is a Sword and Spear, both pointing upwards and both crossed saltirewise. Flanking the shield and issuing from

6195-414: The class of 1879, to whom the old Harvard chapter charter of ΑΔΦ was restored. In 1906, the fraternity's charter was once again surrendered, and in 1910, the organization officially adopted the name "Fly Club," its unofficial title since 1885. More recently, in 1996, the Fly Club merged with the DU Club, another final club, and the combined entity retained the name Fly Club. Some sources maintain that

6300-410: The club's name was derived by combining the "PH" from "Al ph a," the "l" from "De l ta," and the "i" from "Ph i ," to get "Phli," pronounced "Fly". The club motto, suggested by Prof. Morris H. Morgan (class of 1881) and adopted Feb. 1902, reads DURATURIS HAUD DURIS VINCULIS, an ablative absolute construction translated as "Bonds should be lasting, not chafing or hard." Constructed in 1896, with

6405-457: 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

SECTION 60

#1732772801402

6510-416: 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

6615-455: The date of the Society's founding (for chapters that predate the foundation) or since the creation of the chapter (for newer chapters). 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

6720-412: 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

6825-399: 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

6930-529: 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 ),

7035-440: 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 / ;

7140-425: 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

7245-458: The fraternity (the Brunonian, Columbia , Middletown ( Wesleyan University ), Stanford and Bowdoin chapters) and to allow those chapters wishing to be gender-inclusive to create their organization, which resulted in the legal formation of two separate organizations, the all-male Alpha Delta Phi Fraternity and the Alpha Delta Phi Society, the latter of which granted each of its chapters "home rule" permission to determine its gender make-up. Under

7350-425: The fraternity had 33 active chapters and 2 colonies. Its regional alumni organization, the Midwest Association of Alpha Delta Phi, is more than 125 years old. Alpha Delta Phi chapter at Hamilton College is the third oldest continuously operating chapter in the North American Fraternity System and the second oldest Alpha chapter. At Yale University , it was mostly brothers of Alpha Delta Phi who were invited to join

7455-417: The fraternity's emblem and symbols. Later in the year, other members were added. Alpha Delta Phi was the first fraternity to establish a chapter west of the Appalachian Mountains when it formed a chapter at Miami University in 1832. This chapter preceded the formation of three national fraternities at Miami University known as the Miami Triad in the years that followed. The Alpha Delta Phi Fraternity

7560-592: The gate was built in 1914 by a grant from members of the Fly Club. The Fly's symbol, a "leopard rampant gardant" (known as the "Kitty"), is centered within the ironwork above the entry. Inscribed below is a dedication: "For Friendships Made in College the Fly Club in Gratitude has Built this Gate." Alpha Delta Phi Alpha Delta Phi ( ΑΔΦ ; commonly known as Alpha Delt , AD , ADPhi , A-Delt , or ADP )

7665-485: 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

7770-469: 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

7875-540: 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

7980-788: 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 ,

8085-787: 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

8190-550: 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

8295-432: 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

8400-554: The national organization and formed an independent one, Alpha Delta. The University of Michigan 's Peninsular chapter was founded on August 5, 1846, and is the oldest continuous Greek-letter fraternity on the campus. Authorized on June 12, 1846, by the President of the Alpha Delta Phi, William Henry Goodrich (Yale 1843), seven members were the first of the chapter to be initiated as brothers. In 1847, however, faculty at

8505-467: 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

8610-424: 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

8715-460: 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

8820-506: 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

8925-488: 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

9030-532: 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

9135-505: The scroll is the date 1832. The Brothers-in-Arms statue is a unique memorial to the 2,300 men of the fraternity, of Canada and the United States, who served in World War I, and especially for the 93 Brothers who made the supreme sacrifice. The pledge pin is a shield divided vertically with the left half-colored green and the right half-colored white. Rules regarding the wearing of the pledge pin are established by each chapter. In 2024,

9240-513: The scroll on either side are two gold sprays of laurel leaved in gold. Beneath the escutcheon is a motto ribbon bearing the Latin phrase "Manus Multae Cor Unum", meaning "many hands, one heart". The whole escutcheon is radiant, meaning rays emanate from the top between the Spearpoint and Sword and base. There is a nimbus of very fine stars around the outer perimeter of the lower nimbus. Beneath

9345-498: 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

9450-416: 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,

9555-413: 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

9660-511: 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

9765-544: 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

9870-573: 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

9975-532: The terms of this agreement, the Fraternity and the Society would be completely separate and independent legal entities, with separate governing bodies. The two organizations were not part of the same entity and did not share membership, except for male members of the Society who joined before 1992. Both groups would be licensees who share the Greek letters and intellectual property such as history and songs. The agreement put limitations on both organizations as to where they could have chapters, and there were limitations on

10080-440: 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

10185-628: 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

10290-591: The university began barring class admission and expelling students who were members of secret societies. The conflict ended in 1852 when the chapter gained full recognition from the university, though its membership was reduced to three. " In 1877, the Cornell University chapter's alumni group built its first house for the undergraduates, which has been described as the "first house in America built solely for fraternity use." The chapter has since moved to

10395-444: The university's top-ranked senior society Skull and Bones . Students at Harvard formed a chapter of Alpha Delta Phi but disaffiliated to form the independent final club, the A.D. Alpha Delta Phi's Dartmouth College chapter was the inspiration for National Lampoon's Animal House . The movie was co-written by Chris Miller and Doug Kenney. The chapter was affiliated with Alpha Delta Phi from 1846 until 1969, when it broke away from

10500-551: Was added to the National Register of Historic Places on May 21, 1990. The house was demolished in 2018. The University of Michigan chapter house, known as Stone House, was the first fraternity house built on the campus. It was erected in 1883 and continued to house the brothers of the Alpha Delta Phi until the current house was constructed on the same site in 1910. The fraternity has 1,521 active members and 53,344 total initiated members as of 2024. The mission of

10605-661: 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,

10710-591: 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

10815-550: Was followed by a proposal at the 1974 national convention to either allow individual chapters to admit women or to do so fraternity-wide. This debate was often contentious, with most chapters opposed, and some members lobbying for full admission of women, but a larger number wanting to ban women altogether or grant them some form of associate membership. In 1992, at the Fraternity's 160th Annual Convention held in Brainerd, Minnesota , an agreement allowed five chapters to withdraw from

10920-560: Was not able to maintain membership in the NIC as a result of its decision to admit non-male-identifying members. Alpha Delta Phi is both a social fraternity and a literary society. As part of this focus, the Alpha Delta Phi Foundation (formerly the Samuel Eells Literary and Educational Foundation) makes educational grants and sponsors annual literary competitions, which award cash prizes. The Badge

11025-518: 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

#401598