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Index of Subjects This is a multi-part message in MIME format. ------=_NextPart_000_0025_01CB1D13.6C8F35E0 Content-Type: text/plain; charset="iso-8859-1" Content-Transfer-Encoding: quoted-printable Dusan, going from memory of the years I lived there:- Glacial outwash deposits are common throughout the valley and provide = some extensive areas of coarse soils. They are believed to be the source = of the wind-blown sands and loess found in the Kingston -Greenwood area. = According to locals the steep sand hill that you must climb on the = Highway 101 from Aylesford to Kingston is the largest stabilized sand = dune in the Province. If you go to the Natural History of Nova Scotia = website and look at Theme Region 610, you will see some of this. Hope this helps, John Belbin - Hantsport ----- Original Message -----=20 From: Dusan Soudek=20 To: NatureNS=20 Sent: Tuesday, July 06, 2010 8:39 AM Subject: [NatureNS] Annapolis Valley "sandhills?" Last week I had a chance to canoe the upper Annapolis River, from = Aylesford to Kingston. Again, I was impressed by the depth and extent of = the sandy deposits through which the river meanders in much of this = stretch. Almost the entire "sandhills" area is covered by a thin veneer = of soil and by vegetation. The sand is visible only where its cover has = been disturbed on roads or in sandpits. It is best viewed from the = river, where in places there are 20 - 30 foot vertical sandy banks.=20 What exactly created this massive sand deposit? The continental = glacier? A post-glacial lake? The ocean? Do these 'sandhills' have a = formal name? Any good references on them?=20 Dusan Soudek -------------------------------------------------------------------------= ----- No virus found in this incoming message. Checked by AVG - www.avg.com=20 Version: 9.0.830 / Virus Database: 271.1.1/2984 - Release Date: = 07/05/10 15:36:00 ------=_NextPart_000_0025_01CB1D13.6C8F35E0 Content-Type: text/html; charset="iso-8859-1" Content-Transfer-Encoding: quoted-printable <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN"> <HTML><HEAD> <META content=3D"text/html; charset=3Diso-8859-1" = http-equiv=3DContent-Type> <META name=3DGENERATOR content=3D"MSHTML 8.00.6001.18928"> <STYLE></STYLE> </HEAD> <BODY bgColor=3D#ffffff> <DIV><FONT size=3D2 face=3DArial>Dusan,</FONT></DIV> <DIV><FONT size=3D2 face=3DArial>going from memory of the years I lived=20 there:-</FONT></DIV> <DIV><FONT size=3D2 face=3DArial>Glacial outwash deposits are common = throughout the=20 valley and provide some extensive areas of coarse soils. They are = believed to be=20 the source of the wind-blown sands and loess found in the Kingston = -Greenwood=20 area. According to locals the steep sand hill that you must climb on the = Highway=20 101 from Aylesford to Kingston is the largest stabilized sand dune in = the=20 Province. If you go to the Natural History of Nova Scotia website and = look at=20 Theme Region 610, you will see some of this.</FONT></DIV> <DIV><FONT size=3D2 face=3DArial>Hope this helps,</FONT></DIV> <DIV><FONT size=3D2 face=3DArial>John Belbin - Hantsport</FONT></DIV> <BLOCKQUOTE=20 style=3D"BORDER-LEFT: #000000 2px solid; PADDING-LEFT: 5px; = PADDING-RIGHT: 0px; MARGIN-LEFT: 5px; MARGIN-RIGHT: 0px"> <DIV style=3D"FONT: 10pt arial">----- Original Message ----- </DIV> <DIV=20 style=3D"FONT: 10pt arial; BACKGROUND: #e4e4e4; font-color: = black"><B>From:</B>=20 <A title=3Dsoudekd@ns.sympatico.ca = href=3D"mailto:soudekd@ns.sympatico.ca">Dusan=20 Soudek</A> </DIV> <DIV style=3D"FONT: 10pt arial"><B>To:</B> <A = title=3Dnaturens@chebucto.ns.ca=20 href=3D"mailto:naturens@chebucto.ns.ca">NatureNS</A> </DIV> <DIV style=3D"FONT: 10pt arial"><B>Sent:</B> Tuesday, July 06, 2010 = 8:39=20 AM</DIV> <DIV style=3D"FONT: 10pt arial"><B>Subject:</B> [NatureNS] Annapolis = Valley=20 "sandhills?"</DIV> <DIV><BR></DIV> <DIV><FONT size=3D4> Last week I had a chance to = canoe the=20 upper Annapolis River, from Aylesford to Kingston. Again, I was = impressed by=20 the depth and extent of the sandy deposits through which the river = meanders in=20 much of this stretch. Almost the entire "sandhills" area is covered by = a thin=20 veneer of soil and by vegetation. The sand is visible only where its = cover has=20 been disturbed on roads or in sandpits. It is best viewed from the = river,=20 where in places there are 20 - 30 foot vertical sandy=20 banks. </FONT></DIV> <DIV><FONT size=3D4> What exactly created this = massive sand=20 deposit? The continental glacier? A post-glacial lake? The ocean? Do = these=20 'sandhills' have a formal name? Any good references on them? = </FONT></DIV> <DIV><FONT size=3D4> Dusan Soudek</FONT></DIV> <P> <HR> <P></P><BR>No virus found in this incoming message.<BR>Checked by AVG = -=20 www.avg.com <BR>Version: 9.0.830 / Virus Database: 271.1.1/2984 - = Release=20 Date: 07/05/10 15:36:00<BR></BLOCKQUOTE></BODY></HTML> ------=_NextPart_000_0025_01CB1D13.6C8F35E0--
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