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ARETES

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Aantal letters

6

Is palindroom

Nee

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ARE
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Voorbeelden van het gebruik van ARETES in een zin

  • These cliffs are mostly made of schist, with some being granite, and vary from long smooth slabs to wildly overhung roofs and aretes.
  • The rocks that form Snowdon were produced by volcanoes in the Ordovician period, and the massif has been extensively sculpted by glaciation, forming the pyramidal peak of Snowdon and the arêtes of Crib Goch and Y Lliwedd.
  • To the west the ground drops gently at first but then more steeply down to Thirlmere, while on the eastern side three deep glacial coves, each backed by high cliffs, are separated by two spectacular sharp ridges or arêtes.
  • Carrauntoohil is composed mainly of sandstone, whose glaciation produced distinctive features on the mountain such as the Eagle's Nest corrie and some deep gullies and sharp arêtes in its east and northeastern faces that are popular with rock and winter climbers.
  • Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col.
  • As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined.
  • The rocks that form Snowdon were produced by volcanoes in the Ordovician period, and the massif has been extensively sculpted by glaciation, forming the pyramidal peak of Snowdon and the arêtes of Crib Goch and Y Lliwedd.
  • This region shows a great deal of evidence of glacial activity with flow features, crevasse-like fractures, drumlins, eskers, tarns, arêtes, cirques, horns, U-shaped valleys, and terraces.
  • The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys.
  • In the primary sources Arrian mentions that the Macedonian officer Aretes commanded the prodromoi, in the same context Curtius says that Aretes commanded the sarissophoroi.
  • The Weminuche Wilderness was glaciated during the Pleistocene and the current landscape is dominated by glacial landforms including horns, arêtes, cirques, tarns, moraines, and U-shaped valleys.
  • Its landscape exhibits mature, steep, alpine relief, including horns, arêtes, cirques, and glacially carved valleys.
  • The mountains were subject to significant glaciation with corries and U-shaped valleys, however the range does not have the sharp rocky arêtes and ridges of the MacGillycuddy Reeks range.
  • This region shows a great deal of evidence of glacial activity with flow features, crevasse-like fractures, drumlins, eskers, tarns, aretes, cirques, horns, U-shaped valleys, and terraces.



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