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KAMES
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- 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.
- Hiroshi Kojima, "Demographic Analysis of Muslims in Japan," The 13th KAMES and 5th AFMA International Symposium, Pusan, 2004.
- Using leftover fill from the Marquette Interchange reconstruction project, the new park also includes landforms shaped to resemble typical glacial features from the area's geologic past, such as kames, drumlins, and eskers.
- At the surface, the entire region is "Moraine terrain", with the glacial landforms of moraines, drumlins, eskers, kames, outwash plains and till plains, all relics from recent glaciation.
- Sims Corner Eskers and Kames National Natural Landmark of Douglas County, Washington and nearby McNeil Canyon Haystack Rocks and Boulder Park natural landmarks contain excellent examples of Pleistocene glacial landforms.
- An Instrument of Sasine dated at Edinburgh 28 August 1671, by Sir Alexander Home of Renton, knight, eldest lawful son to the late Sir John Home of Renton, knight, with the consent of his brother Patrick Home, Sir John's second son, granting to George Home of Kames, the lands of Northfield, with East and Wester Lochs, and the lands of Fewalls in the barony of Coldingham, Berwickshire.
- Mendon Ponds contains a number of unique glacially created land structures, including a kettle hole known as the "Devil's Bathtub", eskers, a floating sphagnum moss peat bog, and kames.
- Fluvio-glacial landforms and erosional surfaces include: outwash plains, kames, kame terraces, kettle holes, eskers, varves, and proglacial lakes.
- The climate warmed rapidly at the end of the last ice age, following which huge quantities of water were released, washing silts, sands, gravels and rocks across the landscape, leading to the formation of many discernible glacial features across the Muir of Dinnet, including kettle hole lochs, kames and eskers.
- Formed in the Late Wisconsinan period, it consists of a till plain and drumlins from the Port Bruce Stadial, and kettles, eskers and kames from the Port Huron Stadial.
- Evidence of ice stagnation is present in the form of outflow channels, eskers, kames, kettles and morainal ridges on the northern side of the MEVC adjacent to Buckley Lake.
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