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Truncated upland

Index Truncated upland

A truncated upland, truncated highland or bevelled upland (Rumpfgebirge) is the heavily eroded remains of a fold mountain range, often from an early period in earth history. [1]

56 relations: Appalachian Mountains, Austria, Basement (geology), Bavaria, Bavarian Forest, Black Forest, Bohemian Forest, Bohemian Massif, Caledonian orogeny, Carboniferous, Central Uplands, Copper, Crust (geology), Czech Republic, Devonian, Erosion, Fault block, Ferdinand von Richthofen, Fichtel Mountains, Fold mountains, Harz, History of Earth, Iron ore, Magma, Massif Central, Mesozoic, Mineral oil, Mining, Mountain chain, Mountain range, Natural resource, Newfoundland and Labrador, Ore, Ore Mountains, Orography, Paleozoic, Peneplain, Permian, Plain, Plateau, Rammelsberg, Rhenish Massif, Rhine, Scandinavia, Scotland, Sedimentary rock, Siberia, Silver, Southern United States, Tectonics, ..., Type locality (geology), Ural Mountains, Uranium, Valley, Variscan orogeny, Vosges. Expand index (6 more) »

Appalachian Mountains

The Appalachian Mountains (les Appalaches), often called the Appalachians, are a system of mountains in eastern North America.

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Austria

Austria (Österreich), officially the Republic of Austria (Republik Österreich), is a federal republic and a landlocked country of over 8.8 million people in Central Europe.

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Basement (geology)

In geology, basement and crystalline basement are the rocks below a sedimentary platform or cover, or more generally any rock below sedimentary rocks or sedimentary basins that are metamorphic or igneous in origin.

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Bavaria

Bavaria (Bavarian and Bayern), officially the Free State of Bavaria (Freistaat Bayern), is a landlocked federal state of Germany, occupying its southeastern corner.

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Bavarian Forest

The village of Zell in the Bavarian Forest The Bavarian Forest (German: or Bayerwald) is a wooded, low-mountain region in Bavaria, Germany that is about 100 kilometres long.

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Black Forest

The Black Forest (Schwarzwald) is a large forested mountain range in the state of Baden-Württemberg in southwest Germany.

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Bohemian Forest

The Bohemian Forest, known in Czech as Šumava and in German as Böhmerwald, is a low mountain range in Central Europe.

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Bohemian Massif

The Bohemian Massif (Česká vysočina or Český masiv, Böhmische Masse or Böhmisches Massiv) is in the geology of Central Europe a large massif stretching over central Czech Republic, eastern Germany, southern Poland and northern Austria.

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Caledonian orogeny

The Caledonian orogeny was a mountain building era recorded in the northern parts of Ireland and Britain, the Scandinavian Mountains, Svalbard, eastern Greenland and parts of north-central Europe.

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Carboniferous

The Carboniferous is a geologic period and system that spans 60 million years from the end of the Devonian Period million years ago (Mya), to the beginning of the Permian Period, Mya.

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Central Uplands

The Central UplandsDickinson (1964), p.18 ff.

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Copper

Copper is a chemical element with symbol Cu (from cuprum) and atomic number 29.

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Crust (geology)

In geology, the crust is the outermost solid shell of a rocky planet, dwarf planet, or natural satellite.

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Czech Republic

The Czech Republic (Česká republika), also known by its short-form name Czechia (Česko), is a landlocked country in Central Europe bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the northeast.

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Devonian

The Devonian is a geologic period and system of the Paleozoic, spanning 60 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya.

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Erosion

In earth science, erosion is the action of surface processes (such as water flow or wind) that remove soil, rock, or dissolved material from one location on the Earth's crust, and then transport it to another location (not to be confused with weathering which involves no movement).

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Fault block

Fault blocks are very large blocks of rock, sometimes hundreds of kilometres in extent, created by tectonic and localized stresses in the Earth's crust.

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Ferdinand von Richthofen

Baron Ferdinand Freiherr von Richthofen FRSFor HFRSE BGS (5 May 18336 October 1905), better known in English as was a German traveller, geographer, and scientist.

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Fichtel Mountains

The Fichtel Mountains (Fichtelgebirge, Smrčiny), form a small horseshoe-shaped mountain range in northeastern Bavaria, Germany.

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Fold mountains

Fold mountains are mountains that form mainly by the effects of folding on layers within the upper part of the Earth's crust.

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Harz

The Harz is a Mittelgebirge that has the highest elevations in Northern Germany and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt, and Thuringia.

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History of Earth

The history of Earth concerns the development of planet Earth from its formation to the present day.

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Iron ore

Iron ores are rocks and minerals from which metallic iron can be economically extracted.

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Magma

Magma (from Ancient Greek μάγμα (mágma) meaning "thick unguent") is a mixture of molten or semi-molten rock, volatiles and solids that is found beneath the surface of the Earth, and is expected to exist on other terrestrial planets and some natural satellites.

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Massif Central

The Massif Central (Massís Central) is a highland region in the middle of southern France, consisting of mountains and plateaus.

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Mesozoic

The Mesozoic Era is an interval of geological time from about.

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Mineral oil

Mineral oil is any of various colorless, odorless, light mixtures of higher alkanes from a mineral source, particularly a distillate of petroleum.

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Mining

Mining is the extraction of valuable minerals or other geological materials from the earth, usually from an orebody, lode, vein, seam, reef or placer deposit.

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Mountain chain

A mountain chain is a row of high mountain summits, a linear sequence of interconnected or related mountains, or a contiguous ridge of mountains within a larger mountain range.

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Mountain range

A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground.

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Natural resource

Natural resources are resources that exist without actions of humankind.

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Newfoundland and Labrador

Newfoundland and Labrador (Terre-Neuve-et-Labrador; Akamassiss; Newfoundland Irish: Talamh an Éisc agus Labradar) is the most easterly province of Canada.

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Ore

An ore is an occurrence of rock or sediment that contains sufficient minerals with economically important elements, typically metals, that can be economically extracted from the deposit.

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Ore Mountains

The Ore Mountains or Ore Mountain Range (Erzgebirge; Krušné hory; both literally "ore mountains") in Central Europe have formed a natural border between Saxony and Bohemia for around 800 years, from the 12th to the 20th centuries.

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Orography

Orography (from the Greek όρος, hill, γραφία, to write) is the study of the topographic relief of mountains, and can more broadly include hills, and any part of a region's elevated terrain.

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Paleozoic

The Paleozoic (or Palaeozoic) Era (from the Greek palaios (παλαιός), "old" and zoe (ζωή), "life", meaning "ancient life") is the earliest of three geologic eras of the Phanerozoic Eon.

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Peneplain

In geomorphology and geology a peneplain is a low-relief plain formed by protracted erosion.

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Permian

The Permian is a geologic period and system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic period 251.902 Mya.

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Plain

In geography, a plain is a flat, sweeping landmass that generally does not change much in elevation.

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Plateau

In geology and physical geography a plateau (or; plural plateaus or plateaux),is also called a high plain or a tableland, it is an area of a highland, usually consisting of relatively flat terrain that is raised significantly above the surrounding area, often with one or more sides with steep slopes.

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Rammelsberg

The Rammelsberg is a mountain, high, on the northern edge of the Harz range, south of the historic town of Goslar in the North German state of Lower Saxony.

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Rhenish Massif

The Rhenish Massif, Rhine Massif or Rhenish Uplands (Rheinisches Schiefergebirge: 'Rhenish Slate Mountains') is a geologic massif in western Germany, eastern Belgium, Luxembourg and northeastern France.

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Rhine

--> The Rhine (Rhenus, Rein, Rhein, le Rhin,, Italiano: Reno, Rijn) is a European river that begins in the Swiss canton of Graubünden in the southeastern Swiss Alps, forms part of the Swiss-Liechtenstein, Swiss-Austrian, Swiss-German and then the Franco-German border, then flows through the German Rhineland and the Netherlands and eventually empties into the North Sea.

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Scandinavia

Scandinavia is a region in Northern Europe, with strong historical, cultural and linguistic ties.

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Scotland

Scotland (Alba) is a country that is part of the United Kingdom and covers the northern third of the island of Great Britain.

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Sedimentary rock

Sedimentary rocks are types of rock that are formed by the deposition and subsequent cementation of that material at the Earth's surface and within bodies of water.

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Siberia

Siberia (a) is an extensive geographical region, and by the broadest definition is also known as North Asia.

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Silver

Silver is a chemical element with symbol Ag (from the Latin argentum, derived from the Proto-Indo-European ''h₂erǵ'': "shiny" or "white") and atomic number 47.

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Southern United States

The Southern United States, also known as the American South, Dixie, Dixieland, or simply the South, is a region of the United States of America.

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Tectonics

Tectonics is the process that controls the structure and properties of the Earth's crust and its evolution through time.

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Type locality (geology)

Type locality, also called type area, type site, or type section, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified.

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Ural Mountains

The Ural Mountains (p), or simply the Urals, are a mountain range that runs approximately from north to south through western Russia, from the coast of the Arctic Ocean to the Ural River and northwestern Kazakhstan.

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Uranium

Uranium is a chemical element with symbol U and atomic number 92.

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Valley

A valley is a low area between hills or mountains often with a river running through it.

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Variscan orogeny

The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.

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Vosges

The Vosges (or; Vogesen), also called the Vosges Mountains, are a range of low mountains in eastern France, near its border with Germany.

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Redirects here:

Bevelled upland, Truncated highland, Truncated uplands, Uplifted peneplain.

References

[1] https://en.wikipedia.org/wiki/Truncated_upland

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