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--Apple-Mail-6--320296180 Content-Transfer-Encoding: 7bit Content-Type: text/plain; charset=US-ASCII; delsp=yes; format=flowed As most of you know, Bob Bancroft lives very close to Pomquet Beach Provincial Park, where there is a series of these slacks as you drive to or from the beach access. Jim in Wolfville Begin forwarded message: > From: Robert P Bancroft <wild1@eastlink.ca> > Date: May 25, 2014 10:36:28 AM ADT > To: "Jim (James W.) Wolford" <jimwolford@eastlink.ca> > Subject: Re: slacks - when do they refill? > > JIm, > > Sorry - terribly busy here. Those slacks hold water fresh-enough > for deer to drink. I have a longer story dating back to the 1960's > but not right now. I think Nancy Dowd and Randy have it about right. > > Best, > Bob > ----- Original Message ----- > From: Jim (James W.) Wolford > To: Bob Bancroft > Sent: Friday, May 23, 2014 3:30 PM > Subject: slacks - when do they refill? > > Bob, I think I forwarded one message on this earlier, but I have a > bunch more if you care to see them? Cheers from Jim, and looking > forward to a week from today at the Gaelic College! > > Begin forwarded message: > >> From: Randy Lauff <randy.lauff@gmail.com> >> Date: May 23, 2014 3:14:29 PM ADT >> To: NatureNS <naturens@chebucto.ns.ca> >> Subject: Re: [NatureNS] slacks - when do they refill? >> Reply-To: naturens@chebucto.ns.ca >> >> I have posted a picture of the slack here: http://people.stfx.ca/ >> rlauff/307/PomquetSlack.jpg. One person I asked locally thought >> that the slack filled up again with the autumn rains. That's >> probably right, but I still can't discount snow melt accompanied >> by spring rain. I guess I'll find out this year. >> >> Randy >> >> _________________________________ >> RF Lauff >> Way in the boonies of >> Antigonish County, NS. >> >> >> On 21 May 2014 18:08, nancy dowd <nancypdowd@gmail.com> wrote: >> Maybe it is just evaporation. Water accumulates in the leaf-lined >> slacks in the Spring (rain and melt) and eventually warming temps >> and strong sun evaporate it until it is empty. Over the summer >> heat and sun manage to keep up with the rainfall not allowing it >> to accumulate for any length of time (it must be hot down in those >> slacks). Then once the cooler temps and less intense sun of Fall >> take over rainwater can accumulate once again in the slacks until >> it freezes. >> >> Just a guess. >> >> Nancy >> On 2014-05-21, at 4:39 PM, David & Alison Webster >> <dwebster@glinx.com> wrote: >> >> > Hi Randy & All, >> > I had imagined these dunes to be bare sand. With tree cover >> on the peaks and presumably none on the slacks there is another >> effect that will increase effective ppt in the slacks; sublimation >> on the tree canopy in calm weather and selective snow accumulation >> in treeless areas (roads, glades, etc) in windy weather due to >> less turbulence and less speed over glades.. >> > Yt, DW >> > ----- Original Message ----- >> > From: Randy Lauff >> > To: NatureNS >> > Sent: Wednesday, May 21, 2014 9:57 AM >> > Subject: Re: [NatureNS] slacks - when do they refill? >> > >> > Thanks folks, >> > >> > I haven't been there in winter, despite my being in NS now for >> over 20 years. >> > >> > Here's the landscape picture though. Picture an accordion, >> partly open lying on its back. The bellows represent the dune >> system at Pomquet, there are peaks and troughs (slacks), and >> precious little other elevations going on. At the slack in >> question, the surrounding peaks of the dunes are dominated by >> white pine and oak, with other trees as well. >> > >> > Fred asked, if the dunes are sandy, how are they holding water >> in the first place? Basically, I think there is leaf litter which >> may be accumulating in the slack to slow the water seepage. >> Further to Anne's email, the slack in question is well back from >> the salt water, I suspect there is no salt to speak of in that >> water. Mosquitoes are there in the billions, peepers are >> deafening, both suggesting fresh water (though I realize a few >> mosquitoes can tolerate brackish water). >> > >> > Randy >> > >> > _________________________________ >> > RF Lauff >> > Way in the boonies of >> > Antigonish County, NS. >> > >> > >> > On 20 May 2014 18:24, David & Alison Webster<dwebster@glinx.com> >> wrote: >> > Hi Randy & All, May 20, 2014 >> > I don't have a clear picture of the topography, either dune >> or inland, but one possible source of water in the slacks is >> drifting of snow into pools. >> > >> > In woods south of Kentville, where I used to walk in winter, >> pools in woodland cradlehollows of swampy sites never froze. With >> 2'-3' of snow on the ground, the air cone was typically about ~1' >> across at snow level and 4" across at water level. Even at -20o C, >> with heavy snowfall, 60 mph winds and drifting snow there would >> be no hint of ice. From the viewpoint of ppt per unit area these >> cones act as black holes; snow blows into them but, soon being >> water, can not escape. These air cones were absent when snow was >> not deep enough to act as a good insulator. With sufficient snow >> cover drifted ~level over the swamp, the soil at the base of >> cradlehollows would warm sufficiently by ground heat from below to >> melt overlying snow and eventually generate one of these air cones. >> > >> > If these pools were sufficiently above the water table then >> they would tend to be transient but, in most soils (given >> sufficient iron and decomposable organic matter), infiltration >> rate at constant head will gradually slow due to formation of a >> local iron pan over decades or centuries. This effect interested >> me because ortstein is sometimes very scattered; patches 3-4' wide >> and 10-15' apart and these pools that collect below air cones >> could account for this. Also prolonged wetting will slake any soil >> aggregates and decrease infiltration rate. >> > >> > Getting back to dunes, in the idealized case of parallel >> linear dunes and linear slacks and in deep snow conditions I >> would expect linear narrow pools at the base of linear narrow >> trenches in the snow; V-shaped deposits of ortstein if dunes are >> stable and not advancing. >> > >> > Have you been there in winter and if so does any of this >> register ? >> > Yt, Dave Webster, Kentville >> > ----- Original Message ----- >> > From: Randy Lauff >> > To: NatureNS >> > Sent: Tuesday, May 20, 2014 4:20 PM >> > Subject: Re: [NatureNS] slacks - when do they refill? >> > >> > Thanks Fred, but in a dune system, wouldn't that mean that the >> slacks would be less than half full with water? These are sand >> dunes...very porous, so I'm suspecting water leaching in from the >> hills of the dunes into the slacks just couldn't fill them. This >> is unlike the condition in vernal pools where there can be ample >> elevation around from which water could leach in to the pool area. >> I'm thinking there has to be a significant rain or snow fall to >> fill them. >> > >> > Randy >> > >> > _________________________________ >> > RF Lauff >> > Way in the boonies of >> > Antigonish County, NS. >> > >> > >> > On 20 May 2014 15:30, Fred Schueler <bckcdb@istar.ca>wrote: >> > On 5/20/2014 2:18 PM, Randy Lauff wrote: >> > >> > Between several of the dunes at Pomquet Beach, Ant. Co., the >> slacks (the >> > troughs between dune crests) fill with water, but by summer are >> dry. I >> > guess I've just never been there at the right time to see when >> they fill >> > again...it can't be just from winter melt water, since the >> slacks are >> > almost full (and snow melts to about 10% its volume as water). >> Do the >> > autumn rains fill them again, or the spring rains? Or is it a >> > case-by-case scenario, which I'd just have to monitor? >> > >> > * I had the same thought about vernal pools at the CARCNET >> meeting at Quebec City in 1999, during a presentation on Marbled >> Salamanders, which come down into the vernal pools to lay their >> eggs on the dry pondbed in the fall, and stay with them all >> winter. It turns out that the vernal pools fill from the water >> table, as one would think sandy dunes would. And yes, I've been >> monitoring water level in our local Wood Frog ponds, fall and late >> winter, ever since then. >> > >> > fred. >> > ------------------------------------------------------------ >> > Frederick W. Schueler & Aleta Karstad >> > Daily Paintings -http://karstaddailypaintings.blogspot.com/ >> > Vulnerable Watersheds -http://vulnerablewaters.blogspot.ca/ >> > study our books -http://pinicola.ca/books/index.htm >> > RR#2 Bishops Mills, Ontario, Canada K0G 1T0 >> > on the Smiths Falls Limestone Plain 44* 52'N 75* 42'W >> > (613)258-3107 <bckcdb atistar.ca> http://pinicola.ca/ >> > ------------------------------------------------------------ >> > >> > No virus found in this message. >> > Checked by AVG - www.avg.com >> > Version: 2014.0.4577 / Virus Database: 3950/7502 - Release Date: >> 05/15/14 >> > >> > >> > No virus found in this message. >> > Checked by AVG - www.avg.com >> > Version: 2014.0.4577 / Virus Database: 3950/7529 - Release Date: >> 05/20/14 >> > >> >> > > > > __________ Information from ESET NOD32 Antivirus, version of virus > signature database 9841 (20140523) __________ > > The message was checked by ESET NOD32 Antivirus. > > part000.txt - is OK > part001.htm - is OK > > http://www.eset.com --Apple-Mail-6--320296180 Content-Transfer-Encoding: quoted-printable Content-Type: text/html; charset=US-ASCII <html><body style=3D"word-wrap: break-word; -webkit-nbsp-mode: space; = -webkit-line-break: after-white-space; "> As most of you know, Bob Bancroft lives very close to Pomquet Beach = Provincial Park, where there is a series of these slacks as you drive to = or from the beach access. Jim in Wolfville<br><div><br><div>Begin = forwarded message:</div><br = class=3D"Apple-interchange-newline"><blockquote type=3D"cite"><div = style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: 0px; = margin-left: 0px; "><font face=3D"Helvetica" size=3D"3" color=3D"#000000" = style=3D"font: 12.0px Helvetica; color: #000000"><b>From: = </b></font><font face=3D"Helvetica" size=3D"3" style=3D"font: 12.0px = Helvetica">Robert P Bancroft <<a = href=3D"mailto:wild1@eastlink.ca">wild1@eastlink.ca</a>></font></div><d= iv style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: 0px; = margin-left: 0px; "><font face=3D"Helvetica" size=3D"3" color=3D"#000000" = style=3D"font: 12.0px Helvetica; color: #000000"><b>Date: = </b></font><font face=3D"Helvetica" size=3D"3" style=3D"font: 12.0px = Helvetica">May 25, 2014 10:36:28 AM ADT</font></div><div = style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: 0px; = margin-left: 0px; "><font face=3D"Helvetica" size=3D"3" color=3D"#000000" = style=3D"font: 12.0px Helvetica; color: #000000"><b>To: </b></font><font = face=3D"Helvetica" size=3D"3" style=3D"font: 12.0px Helvetica">"Jim = (James W.) Wolford" <<a = href=3D"mailto:jimwolford@eastlink.ca">jimwolford@eastlink.ca</a>></fon= t></div><div style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: = 0px; margin-left: 0px; "><font face=3D"Helvetica" size=3D"3" = color=3D"#000000" style=3D"font: 12.0px Helvetica; color: = #000000"><b>Subject: </b></font><font face=3D"Helvetica" size=3D"3" = style=3D"font: 12.0px Helvetica"><b>Re: slacks - when do they = refill?</b></font></div><div style=3D"margin-top: 0px; margin-right: = 0px; margin-bottom: 0px; margin-left: 0px; min-height: 14px; = "><br></div> <span class=3D"Apple-style-span" style=3D"border-collapse: = separate; color: rgb(0, 0, 0); font-family: Helvetica; font-style: = normal; font-variant: normal; font-weight: normal; letter-spacing: = normal; line-height: normal; orphans: 2; text-align: auto; text-indent: = 0px; text-transform: none; white-space: normal; widows: 2; word-spacing: = 0px; -webkit-border-horizontal-spacing: 0px; = -webkit-border-vertical-spacing: 0px; = -webkit-text-decorations-in-effect: none; -webkit-text-size-adjust: = auto; -webkit-text-stroke-width: 0px; font-size: medium; "><div><font = size=3D"2" face=3D"Arial">JIm,</font></div><div><font size=3D"2" = face=3D"Arial"></font> </div><div><font size=3D"2" = face=3D"Arial">Sorry - terribly busy here. Those slacks hold = water fresh-enough for deer to drink. I have a longer = story dating back to the 1960's but not right now. I = think Nancy Dowd and Randy have it about = right.</font></div><div><font size=3D"2" = face=3D"Arial"></font> </div><div><font size=3D"2" = face=3D"Arial">Best,</font> </div><div><font size=3D"2" = face=3D"Arial">Bob</font></div><blockquote style=3D"border-left-color: = rgb(0, 0, 0); border-left-width: 2px; border-left-style: solid; = padding-left: 5px; padding-right: 0px; margin-left: 5px; margin-right: = 0px; "><div style=3D"font: normal normal normal 10pt/normal arial; = ">----- Original Message -----</div><div style=3D"font: normal normal = normal 10pt/normal arial; background-image: initial; = background-attachment: initial; background-origin: initial; = background-clip: initial; background-color: rgb(228, 228, 228); = background-position: initial initial; background-repeat: initial = initial; "><b>From:</b><span = class=3D"Apple-converted-space"> </span><a = title=3D"jimwolford@eastlink.ca" = href=3D"mailto:jimwolford@eastlink.ca">Jim (James W.) = Wolford</a></div><div style=3D"font: normal normal normal 10pt/normal = arial; "><b>To:</b><span class=3D"Apple-converted-space"> </span><a = title=3D"wild1@eastlink.ca" href=3D"mailto:wild1@eastlink.ca">Bob = Bancroft</a></div><div style=3D"font: normal normal normal 10pt/normal = arial; "><b>Sent:</b><span = class=3D"Apple-converted-space"> </span>Friday, May 23, 2014 3:30 = PM</div><div style=3D"font: normal normal normal 10pt/normal arial; = "><b>Subject:</b><span class=3D"Apple-converted-space"> </span>slacks= - when do they refill?</div><div><br></div>Bob, I think I forwarded one = message on this earlier, but I have a bunch more if you care to see = them? Cheers from Jim, and looking forward to a week from today at = the Gaelic College!<br><div><br><div>Begin forwarded message:</div><br = class=3D"Apple-interchange-newline"><blockquote type=3D"cite"><div = style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: 0px; = margin-left: 0px; "><font color=3D"#000000" size=3D"3" face=3D"Helvetica" = style=3D"font: normal normal normal 12px/normal Helvetica; color: rgb(0, = 0, 0); "><b>From:<span = class=3D"Apple-converted-space"> </span></b></font><font size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; ">Randy Lauff <<a = href=3D"mailto:randy.lauff@gmail.com">randy.lauff@gmail.com</a>></font>= </div><div style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: = 0px; margin-left: 0px; "><font color=3D"#000000" size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; color: rgb(0, 0, 0); "><b>Date:<span = class=3D"Apple-converted-space"> </span></b></font><font size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; ">May 23, 2014 3:14:29 PM ADT</font></div><div = style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: 0px; = margin-left: 0px; "><font color=3D"#000000" size=3D"3" face=3D"Helvetica" = style=3D"font: normal normal normal 12px/normal Helvetica; color: rgb(0, = 0, 0); "><b>To:<span = class=3D"Apple-converted-space"> </span></b></font><font size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; ">NatureNS <<a = href=3D"mailto:naturens@chebucto.ns.ca">naturens@chebucto.ns.ca</a>></f= ont></div><div style=3D"margin-top: 0px; margin-right: 0px; = margin-bottom: 0px; margin-left: 0px; "><font color=3D"#000000" size=3D"3"= face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; color: rgb(0, 0, 0); "><b>Subject:<span = class=3D"Apple-converted-space"> </span></b></font><font size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; "><b>Re: [NatureNS] slacks - when do they = refill?</b></font></div><div style=3D"margin-top: 0px; margin-right: = 0px; margin-bottom: 0px; margin-left: 0px; "><font color=3D"#000000" = size=3D"3" face=3D"Helvetica" style=3D"font: normal normal normal = 12px/normal Helvetica; color: rgb(0, 0, 0); "><b>Reply-To:<span = class=3D"Apple-converted-space"> </span></b></font><font size=3D"3" = face=3D"Helvetica" style=3D"font: normal normal normal 12px/normal = Helvetica; "><a = href=3D"mailto:naturens@chebucto.ns.ca">naturens@chebucto.ns.ca</a></font>= </div><div style=3D"margin-top: 0px; margin-right: 0px; margin-bottom: = 0px; margin-left: 0px; min-height: 14px; "><br></div><div dir=3D"ltr">I = have posted a picture of the slack here: <a = href=3D"http://people.stfx.ca/rlauff/307/PomquetSlack.jpg">http://people.s= tfx.ca/rlauff/307/PomquetSlack.jpg</a>. One person I asked locally = thought that the slack filled up again with the autumn rains. That's = probably right, but I still can't discount snow melt accompanied by = spring rain. I guess I'll find out this = year.<div><br></div><div>Randy</div></div><div class=3D"gmail_extra"><br = clear=3D"all"><div>_________________________________<br>RF Lauff<br>Way = in the boonies of<br>Antigonish County, NS.</div><br><br><div = class=3D"gmail_quote">On 21 May 2014 18:08, nancy dowd<span = class=3D"Apple-converted-space"> </span><span dir=3D"ltr"><<a = href=3D"mailto:nancypdowd@gmail.com" = target=3D"_blank">nancypdowd@gmail.com</a>></span><span = class=3D"Apple-converted-space"> </span>wrote:<br><blockquote = class=3D"gmail_quote" style=3D"border-left-color: rgb(204, 204, 204); = border-left-width: 1px; border-left-style: solid; margin-top: 0px; = margin-right: 0px; margin-bottom: 0px; margin-left: 0.8ex; padding-left: = 1ex; ">Maybe it is just evaporation. Water accumulates in the leaf-lined = slacks in the Spring (rain and melt) and eventually warming temps and = strong sun evaporate it until it is empty. Over the summer heat and sun = manage to keep up with the rainfall not allowing it to accumulate for = any length of time (it must be hot down in those slacks). Then once the = cooler temps and less intense sun of Fall take over rainwater can = accumulate once again in the slacks until it freezes.<br><br>Just a = guess.<br><br>Nancy<br><div><div class=3D"h5">On 2014-05-21, at 4:39 PM, = David & Alison Webster <<a = href=3D"mailto:dwebster@glinx.com">dwebster@glinx.com</a>> = wrote:<br><br>> Hi Randy & All,<br>> I had = imagined these dunes to be bare sand. With tree cover on the peaks and = presumably none on the slacks there is another effect that will increase = effective ppt in the slacks; sublimation on the tree canopy in calm = weather and selective snow accumulation in treeless areas (roads, = glades, etc) in windy weather due to less turbulence and less speed over = glades..<br>> Yt, DW<br>> ----- Original Message -----<br>> = From: Randy Lauff<br>> To: NatureNS<br>> Sent: Wednesday, May 21, = 2014 9:57 AM<br>> Subject: Re: [NatureNS] slacks - when do they = refill?<br>><br>> Thanks folks,<br>><br>> I haven't been = there in winter, despite my being in NS now for over 20 = years.<br>><br>> Here's the landscape picture though. Picture an = accordion, partly open lying on its back. The bellows represent the dune = system at Pomquet, there are peaks and troughs (slacks), and precious = little other elevations going on. At the slack in question, the = surrounding peaks of the dunes are dominated by white pine and oak, with = other trees as well.<br>><br>> Fred asked, if the dunes are sandy, = how are they holding water in the first place? Basically, I think there = is leaf litter which may be accumulating in the slack to slow the water = seepage. Further to Anne's email, the slack in question is well back = from the salt water, I suspect there is no salt to speak of in that = water. Mosquitoes are there in the billions, peepers are deafening, both = suggesting fresh water (though I realize a few mosquitoes can tolerate = brackish water).<br>><br>> Randy<br>><br>> = _________________________________<br>> RF Lauff<br>> Way in the = boonies of<br>> Antigonish County, NS.<br>><br>><br>> On 20 = May 2014 18:24, David & Alison Webster<<a = href=3D"mailto:dwebster@glinx.com">dwebster@glinx.com</a>> = wrote:<br>> Hi Randy & All, = May 20, = 2014<br>> I don't have a clear picture of the = topography, either dune or inland, but one possible source of water in = the slacks is drifting of snow into pools.<br>><br>> = In woods south of Kentville, where I used to walk in winter, pools in = woodland cradlehollows of swampy sites never froze. With 2'-3' of snow = on the ground, the air cone was typically about ~1' across at snow level = and 4" across at water level. Even at -20o C, with heavy snowfall, 60 = mph winds and drifting snow there would be no hint of ice. =46rom = the viewpoint of ppt per unit area these cones act as black holes; snow = blows into them but, soon being water, can not escape. These air cones = were absent when snow was not deep enough to act as a good insulator. = With sufficient snow cover drifted ~level over the swamp, the soil at = the base of cradlehollows would warm sufficiently by ground heat from = below to melt overlying snow and eventually generate one of these air = cones.<br>><br>> If these pools were sufficiently = above the water table then they would tend to be transient but, in most = soils (given sufficient iron and decomposable organic matter), = infiltration rate at constant head will gradually slow due to formation = of a local iron pan over decades or centuries. This effect interested me = because ortstein is sometimes very scattered; patches 3-4' wide and = 10-15' apart and these pools that collect below air cones could account = for this. Also prolonged wetting will slake any soil aggregates and = decrease infiltration rate.<br>><br>> Getting back = to dunes, in the idealized case of parallel linear dunes and linear = slacks and in deep snow conditions I would expect linear narrow = pools at the base of linear narrow trenches in the snow; V-shaped = deposits of ortstein if dunes are stable and not = advancing.<br>><br>> Have you been there in winter = and if so does any of this register ?<br>> Yt, Dave Webster, = Kentville<br>> ----- Original Message -----<br>> From: Randy = Lauff<br>> To: NatureNS<br>> Sent: Tuesday, May 20, 2014 4:20 = PM<br>> Subject: Re: [NatureNS] slacks - when do they = refill?<br>><br>> Thanks Fred, but in a dune system, wouldn't that = mean that the slacks would be less than half full with water? These are = sand dunes...very porous, so I'm suspecting water leaching in from the = hills of the dunes into the slacks just couldn't fill them. This is = unlike the condition in vernal pools where there can be ample elevation = around from which water could leach in to the pool area. I'm thinking = there has to be a significant rain or snow fall to fill = them.<br>><br>> Randy<br>><br>> = _________________________________<br>> RF Lauff<br>> Way in the = boonies of<br>> Antigonish County, NS.<br>><br>><br>> On 20 = May 2014 15:30, Fred Schueler <<a = href=3D"mailto:bckcdb@istar.ca">bckcdb@istar.ca</a>>wrote:<br>> On = 5/20/2014 2:18 PM, Randy Lauff wrote:<br>><br>> Between several of = the dunes at Pomquet Beach, Ant. Co., the slacks (the<br>> troughs = between dune crests) fill with water, but by summer are dry. I<br>> = guess I've just never been there at the right time to see when they = fill<br>> again...it can't be just from winter melt water, since the = slacks are<br>> almost full (and snow melts to about 10% its volume = as water). Do the<br>> autumn rains fill them again, or the spring = rains? Or is it a<br>> case-by-case scenario, which I'd just have to = monitor?<br>><br>> * I had the same thought about vernal pools at = the CARCNET meeting at Quebec City in 1999, during a presentation on = Marbled Salamanders, which come down into the vernal pools to lay their = eggs on the dry pondbed in the fall, and stay with them all winter. It = turns out that the vernal pools fill from the water table, as one would = think sandy dunes would. And yes, I've been monitoring water level in = our local Wood Frog ponds, fall and late winter, ever since = then.<br>><br>> fred.<br>> = ------------------------------------------------------------<br>> = Frederick W. Schueler & Aleta = Karstad<br>> Daily Paintings -<a = href=3D"http://karstaddailypaintings.blogspot.com/" = target=3D"_blank">http://karstaddailypaintings.blogspot.com/</a><br>> = Vulnerable Watersheds -<a href=3D"http://vulnerablewaters.blogspot.ca/" = target=3D"_blank">http://vulnerablewaters.blogspot.ca/</a><br></div></div>= > study our books -<a = href=3D"http://pinicola.ca/books/index.htm" = target=3D"_blank">http://pinicola.ca/books/index.htm</a><br><div>> = RR#2 Bishops Mills, Ontario, Canada = K0G 1T0<br>> on the Smiths Falls Limestone Plain 44* 52'N 75* = 42'W<br></div>> <a href=3D"tel:%28613%29258-3107" = value=3D"+16132583107">(613)258-3107</a><span = class=3D"Apple-converted-space"> </span><bckcdb<span = class=3D"Apple-converted-space"> </span><a href=3D"http://atistar.ca"= target=3D"_blank">atistar.ca</a>><span = class=3D"Apple-converted-space"> </span><a = href=3D"http://pinicola.ca/" = target=3D"_blank">http://pinicola.ca/</a><br><div class=3D"HOEnZb"><div = class=3D"h5">> = ------------------------------------------------------------<br>><br>&g= t; No virus found in this message.<br>> Checked by AVG -<span = class=3D"Apple-converted-space"> </span><a = href=3D"http://www.avg.com" target=3D"_blank">www.avg.com</a><br>> = Version: 2014.0.4577 / Virus Database: 3950/7502 - Release Date: = 05/15/14<br>><br>><br>> No virus found in this message.<br>> = Checked by AVG -<span class=3D"Apple-converted-space"> </span><a = href=3D"http://www.avg.com" target=3D"_blank">www.avg.com</a><br>> = Version: 2014.0.4577 / Virus Database: 3950/7529 - Release Date: = 05/20/14<br>><br><br></div></div></blockquote></div><br></div></blockqu= ote></div><br><br><br>__________ Information from ESET NOD32 Antivirus, = version of virus signature database 9841 (20140523) = __________<br><br>The message was checked by ESET NOD32 = Antivirus.<br><br>part000.txt - is OK<br>part001.htm - is OK<br><br><a = href=3D"http://www.eset.com">http://www.eset.com</a><br></blockquote></spa= n></blockquote></div><br></body></html>= --Apple-Mail-6--320296180--
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