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ERRATICS

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Voorbeelden van het gebruik van ERRATICS in een zin

  • In places covered by ice sheets during ice ages, such as Scandinavia, northern North America, and Siberia, glacial erratics are common.
  • The park contains the tallest mountain on the Atlantic Coast of the United States (Cadillac Mountain), exposed granite domes, glacial erratics, U-shaped valleys, and cobble beaches.
  • Wetlands, glacial erratics, concentric bands of ridges, and large flat areas characterize the land surrounding Fonda.
  • The Punchbowl on Turkey Run's Trail 3 is an example of a pothole that was scoured out by glacial erratics caught in swirling backwash.
  • Glacial striation and the presence of chalk and flint erratics that originated from the bed of the North Sea demonstrate the influence of ice action on the geomorphology of the islands.
  • In 2018 a book devoted specifically to the problem of bluestone provenance and transport concluded that the Stonehenge bluestones are essentially an ill-sorted assemblage of glacial erratics.
  • Large boulders composed of 415-million-year-old Devonian granite, called glacial erratics, were lifted by the ice and carried for long distances before being deposited upon the landscape as the ice receded, leaving rugged barrens.
  • When the glacier receded about 11,000 years ago, it left behind moraines which impeded the flow of rivers to the sea and filled the gouged-out glacial valley; the large blocks of rock it dropped, known as glacial erratics, can still be found in the surrounding bush.
  • He was the first to describe a trilobite fossil found on the South Shetland Islands in the Antarctic, a pycnogonid, and the presence of glacial erratics.
  • Whitbarrow, like most of the Lake District, shows many signs of the last ice age, including glacial erratics (boulders left behind when the ice retreated), and the limestone pavement itself, formed when ice left bare limestone exposed to the elements which eroded it and left us with the grikes and clints we see today.
  • Prior research described Suilven and many other mountains in Northwest Scotland as nunataks, but cosmogenic isotope dating of mountaintop erratics has since disproved this hypothesis.
  • Such evidence includes glacial erratics, glacial scouring, glacial striations, deranged drainage, highland swamps, and roches moutonnées, so called "sheepback mountains" because they often resemble the shape of a sheep in profile.
  • They have dark, weathered charnockite bedrock that is littered with light-coloured quartz-rich, granitic gneiss glacial erratics.
  • Glacial erratics such as flint and rhomb porphyry, thought to originate from the Skagerrak and Oslo areas respectively, and deformed glacial tills found on the coast of Jæren provide the main onshore evidence for the Norwegian Channel Ice Stream.
  • The landscape was shaped by the last glaciation, which left glacial barrens, erratics, drumlins, eskers, moraines, hummocks, outwash plains and kettle lakes.
  • Typically, rocking stones are residual corestones formed initially by spheroidal weathering and have later been exposed by erosion or glacial erratics left by retreating glaciers.
  • The tuya formed by effusion of flatlying flows within erratics on its summit and lack of erosional features attributable to glacial suggest that The Table was also formed during the early Holocene.
  • Evidence for glaciation on the Waterville Plateau includes polished and striated bedrock, glacial erratics, drumlinoid topography, eskers, moraines, meltwater channels, and glacial till.
  • In addition, the atypically linear string of glacial erratics that comprise the Foothills Erratics Train was created by the parallel, non-turbulent flowage of two very large ice masses—the Cordilleran Ice Sheet to the west, and the Laurentide Ice Sheet to the east—that occurred at the boundary between them.
  • Temporary lakes such as Lake Lewis in Washington as well as Lake Condon and Lake Allison in Oregon and the evidence for these temporary lakes as seen in the ice rafted erratics and in the deposits of the Touchet Formation.


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