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  2. Geology of the Appalachians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Appalachians

    Land added to Laurentia during the Grenville orogeny. The first mountain-building tectonic plate collision that initiated the construction of what are today the Appalachian Mountains occurred during the Mesoproterozoic era at least one billion years ago when the pre-North-American craton called Laurentia collided with other continental segments, notably Amazonia.

  3. Alleghanian orogeny - Wikipedia

    en.wikipedia.org/wiki/Alleghanian_orogeny

    The Alleghanian orogeny, a result of three separate continental collisions. USGS. The immense region involved in the continental collision, the vast temporal length of the orogeny, and the thickness of the pile of sediments and igneous rocks known to have been involved are evidence that at the peak of the mountain-building process, the Appalachians likely once reached elevations similar to ...

  4. List of subranges of the Appalachian Mountains - Wikipedia

    en.wikipedia.org/wiki/List_of_subranges_of_the...

    The following is a list of subranges within the Appalachian Mountains, a mountain range stretching ~2,050 miles from Newfoundland and Labrador, Canada to Alabama, US. The Appalachians, at their initial formation, were a part of the larger Central Pangean Mountains along with the Scottish Highlands , the Ouachita Mountains , and the Anti-Atlas ...

  5. Appalachian Mountains - Wikipedia

    en.wikipedia.org/wiki/Appalachian_Mountains

    The Appalachian Mountains, [b] 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.

  6. Allegheny Plateau - Wikipedia

    en.wikipedia.org/wiki/Allegheny_Plateau

    Major fault at the dividing line between the Allegheny Plateau and the Appalachian Mountains in Williamsport, Pennsylvania The Allegheny Plateau ( / ˌ æ l ɪ ˈ ɡ eɪ n i / AL -ig- AY -nee ) is a large dissected plateau area of the Appalachian Mountains in western and central New York , northern and western Pennsylvania , northern and ...

  7. Geology of the United States - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_United_States

    These two plates converge at 3–4 centimeters per year at present. This is only about half the rate of convergence of 7 million years ago. [4] The small Juan de Fuca plate and two platelets, the Explorer plate and Gorda plate are the meager remnants of the much larger Farallon oceanic plate. The Explorer plate broke away from the Juan de Fuca ...

  8. Marcellus Formation - Wikipedia

    en.wikipedia.org/wiki/Marcellus_Formation

    The black shales also contain iron ore that was used in the early economic development of the region, and uranium and pyrite which are environmental hazards. At the base of the Marcellus, in the pyrite - carbonate bed between the carbonaceous black shale and a green calcareous shale bed, [ 19 ] pyrite, carbonate, and groundwater reacted to form ...

  9. Cumberland Plateau - Wikipedia

    en.wikipedia.org/wiki/Cumberland_Plateau

    The Cumberland Plateau is a deeply dissected plateau, with topographic relief commonly of about 400 feet (120 metres), and frequent sandstone outcroppings and bluffs.. At Kentucky's Pottsville Escarpment, which is the transition from the Cumberland Plateau to the Bluegrass in the north and the Pennyrile in the south, there are many spectacular cliffs, gorges, rockhouses, natural bridges, and ...

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