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  2. Peneplain - Wikipedia

    en.wikipedia.org/wiki/Peneplain

    In geomorphology and geology, a peneplain is a low-relief plain formed by protracted erosion. This is the definition in the broadest of terms, albeit with frequency the usage of peneplain is meant to imply the representation of a near-final (or penultimate) stage of fluvial erosion during times of extended tectonic stability. [ 1 ]

  3. List of inselbergs - Wikipedia

    en.wikipedia.org/wiki/List_of_inselbergs

    Argentina. Various ignimbrite inselbergs in Sierra de Lihuel Calel, La Pampa Province [3]; Brazil. Pedra Agulha in Pancas, Espírito Santo; Canada. Gaff Topsails in Newfoundland [citation needed]

  4. Inselberg - Wikipedia

    en.wikipedia.org/wiki/Inselberg

    Pietra di Bismantova in the Apennines, Italy. An inselberg or monadnock (/ m ə ˈ n æ d n ɒ k / mə-NAD-nok) is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain.

  5. Perris Block - Wikipedia

    en.wikipedia.org/wiki/Perris_Block

    The Perris Plain, an uplifted peneplain, is drained primarily in the San Jacinto Basin, the San Jacinto River watershed flowing into Lake Elsinore, that is dotted by monadnocks and by several other ranges of mountains and hills.

  6. Mount Monadnock - Wikipedia

    en.wikipedia.org/wiki/Mount_Monadnock

    Mount Monadnock, or Grand Monadnock, is a mountain in the town of Jaffrey, New Hampshire. [3] It is the most prominent mountain peak in southern New Hampshire and is the highest point in Cheshire County.

  7. Laurentian Upland - Wikipedia

    en.wikipedia.org/wiki/Laurentian_Upland

    A peneplain with the occasional moderately high monadnocks left behind during the peneplanation of the rest of the surface. The erosion of the region must have been far advanced in prehistoric times, even practically completed, because the even peneplain surface is overlapped by fossiliferous marine strata from an early geological date ...

  8. Cycle of erosion - Wikipedia

    en.wikipedia.org/wiki/Cycle_of_erosion

    That landscape of low relief is called a peneplain and may contain residual heights standing out from the general level. The peneplain can be uplifted, which starts a second erosion cycle. [5] Davis acknowledged that a full cycle was a special case and that initial uplift was not necessarily rapid or followed by a prolonged period of quiescence.

  9. Geography of West Bengal - Wikipedia

    en.wikipedia.org/wiki/Geography_of_West_Bengal

    Because of long and continuous erosion, the whole region has been transformed into an undulating peneplain. This area is interspersed by small monadnocks locally known as tila. Some of the important hills in the area include Ajodhya Hills (677 m), Panchet (643 m), and Baghmundi in Purulia, and Biharinath (452 m) and Susunia (442 m) in Bankura ...