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KAMES

9

Aantal letters

5

Is palindroom

Nee

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AM
AME
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KA
KAM
ME
MES

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106
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AES
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AKE
AKS
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Voorbeelden van het gebruik van KAMES in een zin

  • Henry Home, Lord Kames (1696–27 December 1782) was a Scottish writer, philosopher and judge who played a major role in Scotland's Agricultural Revolution.
  • The town contains many kames, eskers, drumlins, kettles, rivers, and streams created by the glacier.
  • Kames are often associated with kettles, and this is referred to as kame and kettle or knob and kettle topography.
  • Under Cullen's patronage, Walker further distinguished himself as a chemist and a mineralogist and this led him to function as a scientific advisor for Lord Bute, Lord Hopetoun, Lord Cathcart, and Judge Advocate Lord Kames.
  • Henry Home, Lord Kames was conspicuously absent from such socialising; while Kames and Monboddo served on the high court at the same time and had numerous interactions, they were staunch intellectual rivals.
  • The poet's ardour in his love-songs led, at least in one case, to a feeling of resentment on the part of a lady, who consulted his close friend Henry Home, Lord Kames in her dilemma, and, acting on his advice to profess a return of affection, quickly startled Hamilton into an attitude of distant reserve.
  • Later, when the glaciers retreated leaving behind their freight of crushed rock and sand, depositional landforms were created, such as moraines, eskers, drumlins, and kames.
  • However, his design was not initially considered suitable for construction, and was reviewed by a committee, including the law judges Lord Kames (1696–1782), Lord Elliock (1712–1793) and Lord Hailes (1726–1792) and architects John Adam and William Mylne (1734–1790), and Sir James Clerk, 3rd Baronet (1709–1783).
  • Drift is often subdivided into (unsorted and) unstratified drift (glacial till) that forms moraines and stratified drift (glaciolacustrine and fluvioglacial sediments) that accumulates as stratified and sorted sediments in the form of outwash plains, eskers, kames, varves, and so forth.
  • The Papakating valley's topography and surficial geology is defined by stratified and unstratified drift as well as till and gravel deposits left behind by the retreating glaciers during the Wisconsin glaciation (the last ice age) and feature several kames and kame terraces.



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