admin on May 4th, 2016


A look at rocks exposed in today’s Appalachian mountains reveals elongated belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor, which provides strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges, some 300 million years ago, marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians near the center. Because North America and Africa were connected, the Appalachians form part of the same mountain chain as the Anti-Atlas in Morocco. To the northeast, the same mountain chain continues into Scotland, from the North America/Europe collision.

During the middle Ordovician Period (about 496-440 million years ago), a change in plate motions set the stage for the first Paleozoic mountain building event (Taconic orogeny) in North America. The once-quiet Appalachian passive margin changed to a very active plate boundary when a neighboring oceanic plate, the Iapetus, collided with and began sinking beneath the North American craton. With the birth of this new subduction zone, the early Appalachians were born. Along the continental margin, volcanoes grew, coincident with the initiation of subduction. Thrust faulting uplifted and warped older sedimentary rock laid down on the passive margin. As mountains rose, erosion began to wear them down. Streams carried rock debris down slope to be deposited in nearby lowlands. The Taconic Orogeny was just the first of a series of mountain building plate collisions that contributed to the formation of the Appalachians, culminating in the collision of North America and Africa (see Appalachian 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 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 the Coal Region of northeastern Pennsylvania. The bituminous coal fields of western Pennsylvania, western Maryland, southeastern Ohio, eastern Kentucky, southwestern Virginia, and West Virginia is the sedimentary form. Some plateaus of the Appalachian Mountains contain metallic minerals such as iron and zinc.

-)Next article : “Appalachians Ecology”


admin on May 3rd, 2016



The floras 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 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 4000 feet (1219 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 the southern Appalachians, as in North Carolina and Tennessee. In the central Appalachians it is usually confined above 3000 feet (914 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, 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), which is confined to the highest parts of the southern Appalachian mountains. 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 is usually confined above 3900 feet (1189 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 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 is, unfortunately, 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) 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 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 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 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 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 Hardwoods” 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.

Dryer and rockier uplands and ridges are occupied by Oak-Chestnut type forests dominated by 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 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 dominantly White and Northern Red Oaks, while 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), 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 is near the surface. Hence no ericaceous shrubs are associated with it.

The Appalachian floras 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 thermal environment in which they are found.

Eastern deciduous forests are subject to a number of serious insect and disease outbreaks. Among the most conspicuous is that of the introduced Gypsy 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 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 a variety of other destructive activities continue, albeit in diminished forms; and thus far only a few ecologically based management practices have taken hold.


Animals that characterize the Appalachian forests include five species of tree squirrels. The most commonly seen is the low to moderate elevation Eastern Gray Squirrel (Sciurus carolinensis). Occupying similar habitat is the slightly larger Fox Squirrel (Sciurus niger) and the much smaller Southern Flying Squirrel (Glaucomys volans). More characteristic of cooler northern and high elevation habitat is the Red Squirrel (Tamiasciurus hudsonicus), whereas the Appalachian Northern Flying Squirrel (Glaucomys sabrinus fuscus), which closely resembles the Southern Flying Squirrel, is confined to northern hardwood and spruce-fir forests.

As familiar as squirrels are the Eastern Cottontail rabbit (Silvilagus floridanus) and the White-tailed Deer (Odocoileus virginianus). The latter in particular has greatly increased in abundance as a result of the extirpation of the Gray Wolf (Canis lupus ) and the Eastern Cougar. This has led to the overgrazing and browsing of many plants of the Appalachian forests, as well as destruction of agricultural crops. Other deer include the Moose (Alces alces ), found only in the north, and the Elk (Cervus canadensis), which, although once extirpated, is now making a comeback, through transplantation, in the southern and central Appalachians. In Quebec, the Chic-Chocs host the only population of Caribou (Rangifer tarandus) south of the St. Lawrence River. An additional species that is common in the north but extends its range southward at high elevations to Virginia and West Virginia is the Varying or Snowshoe Hare (Lepus americanus). However, these central Appalachian populations are scattered and very small.

Another species of great interest is the Beaver (Castor canadensis), which is showing a great resurgence in numbers after its near extirpation for its pelt. This resurgence is bringing about a drastic alteration in habitat through the construction of dams and other structures throughout the mountains.

Other common forest animals are the Black Bear (Ursus americanus), Striped Skunk (Mephitis mephitis), Raccoon (Procyon lotor), Woodchuck (Marmota monax), Bobcat (Felis rufus), Gray Fox (Urocyon cinereoargenteus) and in recent years, the Coyote (Canis latrans), another species favored by the advent of Europeans and the extirpation of the Gray Wolf.

Characteristic birds of the forest are Wild Turkey (Meleagris gallopavo), Ruffed Grouse (Bonasa umbellus), Mourning Dove (Zenaida macroura), Common Raven (Corvus corax), Wood Duck (Aix sponsa), Great Horned Owl (Bubo virginianus), Barred Owl (Strix varia), Screech Owl (Megascops asio), Red-tailed Hawk (Buteo jamaicensis), Red-shouldered Hawk (Buteo lineatus), and Northern Goshawk (Accipiter gentilis), as well as a great variety of “songbirds” (Passeriformes), like the warblers in particular.

Of great importance are the many species of salamanders, and in particular the lungless species (Family Plethodontidae) that live in great abundance concealed by leaves and debris, on the forest floor. Most frequently seen, however, is the Eastern or Red-spotted Newt (Notophthalmus viridescens), whose terrestrial eft form is often encountered on the open, dry forest floor. It has been estimated that salamanders represent the largest class of animal biomass in the Appalachian forests. Frogs and toads are of lesser diversity and abundance, but the Wood Frog (Rana sylvatica) is, like the eft, commonly encountered on the dry forest floor, while a number of species of small frogs, such as Spring Peepers (Pseudacris crucifer), enliven the forest with their calls. Salamanders and other amphibians contribute greatly to nutrient cycling through their consumption of small life forms on the forest floor and in aquatic habitats.

Although reptiles are less abundant and diverse than amphibians, a number of snakes are conspicuous members of the fauna. One of the largest is the non-poisonous Black Rat Snake (Elaphe obsoleta obsoleta), while the Common Garter Snake (Thamnophis sirtalis) is among the smallest but most abundant. The American Copperhead (Agkistrodon contortrix) and the Timber Rattler (Crotalus horridus) are poisonous pit vipers. There are few lizards, but the Broad-headed Skink (Eumeces laticeps), at up to 13 inches (33 cm) in length, and an excellent climber and swimmer, is one of the largest and most spectacular in appearance and action. The most common turtle is the Eastern Box Turtle (Terrapene carolina carolina), which is found in both upland and lowland forests in the central and southern Appalachians. Prominent among aquatic species is the large Common Snapping Turtle (Chelydra serpentina), which occurs throughout the Appalachians.

Appalachian streams are notable for their highly diverse freshwater fish life. Among the most abundant and diverse are those of the minnow family (Family Cyprinidae), while species of the colorful Darters (Percina spp.) are also abundant.

A characteristic fish of shaded, cool Appalachian forest streams is the Wild Brook or Speckled Trout (Salvelinus fontinalis), which is much sought after for its sporting qualities. However in past years such trout waters have been much degraded by increasing temperatures because of timber cutting, global warming and by pollution from various sources.


admin on May 3rd, 2016
admin on May 2nd, 2016

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admin on May 2nd, 2016

Oke, Sudah sekian lama blog ini berisikan dengan artikel-artikel berbahasa Inggris, namum mulai hari ini dan juga belum tahu sampai kapan :) blog ini akan berisikan dengan artkel berbahasa indonesia. dengan begitu Warga Indonesia tercinta dapat menikmati bahasan yang di Share di blog ini…

Sebelumnya kami mohon maaf karena beberapa waktu yang lalu kami mengatakan bahwa untuk posting-an berbahasa Inggris hanya untuk 10 hari setelahnya, eh malah kebablasan deh… :P

jadi mohon maaf yah… mulai sekarang blog ini akan saya isi dengan berbagai informasi mengenai kegiatan outdoor dan artikel-artikel lainnya yang berkaitan dalam bahasa indonesia, bagaimana?? setuju?? :)