@article {595,
	title = {Rapid viscoelastic uplift in southeast Alaska caused by post-Little Ice Age glacial retreat},
	journal = {Earth and Planetary Science Letters},
	volume = {237},
	year = {2005},
	note = {968ijTimes Cited:109Cited References Count:44},
	month = {Sep 15},
	pages = {548-560},
	abstract = {Our observations show that extreme uplift in southeast Alaska began about 1770 AD, with relative sea level (RSL) change to 5.7 m and current uplift rates to 32 mm/yr. This region experienced widespread glacial melting following the Little Ice Age (LIA), with the collapse of the Glacier Bay Icefield alone equivalent to 8 mm of global sea level rise. Geodynamic modelling links the uplift to post-LIA isostatic rebound, with the extreme uplift signal and a priori knowledge of ice load changes requiring the presence of a low viscosity asthenosphere (3.7 X 10(18) Pa s). These crustal deformations are triggered by climate change through glacier wastage. (c) 2005 Elsevier B.V. All rights reserved.},
	issn = {0012-821x},
	doi = {10.1016/j.epsl.2005.06.032},
	author = {Larsen, C. F. and Motyka, R. J. and Freymueller, J. T. and Echelmeyer, K. A. and Ivins, E. R.}
}
@article {2074,
	title = {Post little ice age uplift at Juneau, Alaska reconstructed from dendrochronology and geomorphology},
	journal = {Quaternary Research},
	volume = {59},
	year = {2003},
	note = {id: 698},
	month = {2003},
	pages = {300-309},
	author = {Motyka, R. J.}
}
