000			01704cam a2200301 4500
008			240105t2013 xxk 000 0 eng u
041			_aeng
110	2		_aRoyal Institution of Chartered Surveyors _94900
245	0	0	_aSurveying and Dating Post-Glacial Lake Shorelines in New Zealand _h[electronic resource]
260			_aLondon, _bRICS, _c2013
300			_a27p.
490		0	_aRICS Research
520			_aNatural fluctuations in Earth’s climate, between cold ‘glacial’ and warm ‘interglacial’ periods, produce a wide range of changes to the Earth’s surface. One of these changes is related to glacial isostatic adjustment (GIA), which is a phenomenon whereby the loading and unloading of the Earth’s crust and mantle due to the growth and retreat of large ice sheets induces regional deformation. The towns of Queenstown, Glenorchy, Frankton, and Kingston are located on the shores of Lake Wakatipu. They are popular tourist destinations and have significant flood and earthquake hazards. This study was focused on identifying evidence of post-glacial rebound and a history of lake level changes that may influence ongoing hazards in the region.
522			_aScotland
650	2	4	_aGLACIERS
650	2	4	_aCLIMATE CHANGE
650	2	4	_aSHORELINES
651		4	_aNew Zealand
662			_aNew Zealand
690			_aRICS _96277
700	1		_aCook, Simon
700	1		_aMcColl, Sam
700	1		_aStahl, Timothy
700	1		_aEriksson, Clare
700	1		_aJohal, Amanprit
856	4	8	_uhttp://www.propertyresearchtrust.org/uploads/1/3/4/8/134819607/post-glacial_lake_shorelines.pdf _zAvailable from the Property Research Trust
942			_n0 _2ddc
999			_c121766 _d121766