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prolonged wetting will slake any so
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Thanks David,
A nicely researched response (once again!).
Randy
_________________________________
RF Lauff
Way in the boonies of
Antigonish County, NS.
On 23 May 2014 21:26, David & Alison Webster <dwebster@glinx.com> wrote:
> Hi Randy & All, A picture helps.
> I remembered that I had a fairly large scale soil map of NS
> (MacDougall & Nowland, 1972; 1:450,000) so dug it out. Your library should
> have one if you don't. And a Google Earth image suggests that the slacks
> are predominantly along the southerly third of Pomquet Beach and parallel
> to the southerly shore of the beach.
> The soil to the west of the west esturary (Monk's Head and south), and
> south west of the east esturary, is Queens; mostly unstructured, poorly
> drained soil high in silt & clay. So the bottom muds of both estuaries,
> except perhaps where exposed to wave action on sand, are likely high in
> silt & clay and relatively impermeable.
> That large nose of land between the two estuaries is Tormantine
> (moderately coarse and medium textured well drained soil) as is Pomquet
> Beach and land east of the east estuary. All of the Tormantine area is
> nearly free of watercourses except for those that drain less permeable soil
> to the south. So, as a rough estimate for this Tormentine costal region, at
> least 60% of the annual ppt. is disposed of by deep percolation and that
> flow has to go somewhere and exit at some lower elevation.
> According to Google Earth some of that middle nose is about 85' above
> sea level. [But it also had some of the estuary 8' above sea level while
> much of the slacks area was 0' so precision is poor.]
> Movement of water in soil is directly proportional to head, hydraulic
> conductivity and cross-sectional area available for flow and inversely
> proportional to flow length. If there is a sufficiently deep layer of
> permeable bedrock under that nose and under the channel between the nose
> and Pomquet Beach then much of the refill water could be from the nose to
> the south.
> I also wonder if the bottom of some of the slacks may have a lower
> elevation than water in these estuaries when rivers are at full flow. This
> would be flow driven by relatively small head but over a relatively short
> flow path.
> Yt, Dave Webster, Kentville
>
>
> ----- Original Message -----
> *From:* Randy Lauff <randy.lauff@gmail.com>
> *To:* NatureNS <naturens@chebucto.ns.ca>
> *Sent:* Friday, May 23, 2014 3:14 PM
> *Subject:* Re: [NatureNS] slacks - when do they refill?
>
> 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
>> >
>>
>>
> No virus found in this message.
> Checked by AVG - www.avg.com
> Version: 2014.0.4592 / Virus Database: 3950/7543 - Release Date: 05/22/14
>
>
--001a11394fb4e69ed404fa3fbaab
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<div dir=3D"ltr">Thanks David,<div><br></div><div>A nicely researched respo=
nse (once again!).</div><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 23 May 2014 21:26, David & Alison=
Webster <span dir=3D"ltr"><<a href=3D"mailto:dwebster@glinx.com" target=
=3D"_blank">dwebster@glinx.com</a>></span> wrote:<br><blockquote class=
=3D"gmail_quote" style=3D"margin:0 0 0 .8ex;border-left:1px #ccc solid;padd=
ing-left:1ex">
<u></u>
<div bgcolor=3D"#ffffff">
<div>Hi Randy & All,=C2=A0=C2=A0=C2=A0 =C2=A0=C2=A0=C2=A0 =C2=A0=C2=A0=
=C2=A0=20
=C2=A0=C2=A0=C2=A0 =C2=A0=C2=A0=C2=A0 =C2=A0=C2=A0=C2=A0 A picture helps.</=
div>
<div>=C2=A0=C2=A0=C2=A0 =C2=A0I remembered that I had a fairly large scale =
soil=20
map of NS (MacDougall & Nowland, 1972; 1:450,000) so dug it out. Your=
=20
library should have one if you don't.=C2=A0And a Google Earth=20
image=C2=A0suggests that the slacks are predominantly along the=20
southerly=C2=A0third of Pomquet Beach and parallel to the southerly shore o=
f the=20
beach.</div>
<div>=C2=A0=C2=A0=C2=A0 The soil to the west of the=C2=A0west esturary (Mon=
k's=20
Head and south), and south west of the east esturary,=C2=A0is Queens; mostl=
y=20
unstructured, poorly drained soil=C2=A0high in silt & clay.=C2=A0 So th=
e=20
bottom muds of both estuaries, except perhaps where exposed to wave action =
on=20
sand,=C2=A0are likely high in silt & clay and relatively impermeable. <=
/div>
<div>=C2=A0=C2=A0=C2=A0 That large nose of land between the two estuaries i=
s=20
Tormantine (moderately coarse and medium textured well drained soil) as is=
=20
Pomquet Beach and land east of the east=C2=A0estuary. All of the Tormantine=
area=20
is nearly free of watercourses except for those that drain less permeable s=
oil=20
to the south. So, as a rough estimate=C2=A0for this Tormentine=C2=A0costal=
=20
region, at least 60% of the annual ppt. is disposed of by deep percolation =
and=20
that flow has to go somewhere and exit at some lower elevation.</div>
<div>=C2=A0=C2=A0=C2=A0 According to Google Earth some of that middle nose =
is=20
about 85' above sea level. [But it also had some of the estuary 8' =
above sea=20
level while much of the slacks area=C2=A0 was 0' so precision is poor.]=
</div>
<div>=C2=A0=C2=A0=C2=A0 Movement of water in soil is directly proportional=
=20
=C2=A0to=C2=A0head,=C2=A0hydraulic conductivity and cross-sectional=20
area=C2=A0available for=C2=A0flow=C2=A0=C2=A0and inversely proportional=20
to=C2=A0flow length. If there is a sufficiently deep layer of permeable bed=
rock=20
under that nose and under the channel between the nose and Pomquet Beach th=
en=20
much of the refill water could be from the nose to the south. </div>
<div>=C2=A0=C2=A0=C2=A0 I also wonder if the bottom of=C2=A0some of the sla=
cks=20
may have a lower elevation than water in these estuaries when rivers are at=
full=20
flow. This would be flow driven by relatively=C2=A0 small head but over a=
=20
relatively short flow path. </div>
<div>=C2=A0=C2=A0=C2=A0 Yt, Dave Webster, Kentville</div>
<div>=C2=A0=C2=A0=C2=A0 </div>
<blockquote style=3D"BORDER-LEFT:#000000 2px solid;PADDING-LEFT:5px;PADDING=
-RIGHT:0px;MARGIN-LEFT:5px;MARGIN-RIGHT:0px" dir=3D"ltr"><div class=3D"">
<div style=3D"FONT:10pt arial">----- Original Message ----- </div>
<div style=3D"FONT:10pt arial;BACKGROUND:#e4e4e4"><b>From:</b>=20
<a title=3D"randy.lauff@gmail.com" href=3D"mailto:randy.lauff@gmail.com" =
target=3D"_blank">Randy=20
Lauff</a> </div>
<div style=3D"FONT:10pt arial"><b>To:</b> <a title=3D"naturens@chebucto.n=
s.ca" href=3D"mailto:naturens@chebucto.ns.ca" target=3D"_blank">NatureNS</a=
> </div>
</div><div><div class=3D"h5"><div style=3D"FONT:10pt arial"><b>Sent:</b> =
Friday, May 23, 2014 3:14 PM</div>
<div style=3D"FONT:10pt arial"><b>Subject:</b> Re: [NatureNS] slacks - wh=
en do=20
they refill?</div>
<div><br></div>
<div dir=3D"ltr">I have posted a picture of the slack here:=C2=A0<a href=
=3D"http://people.stfx.ca/rlauff/307/PomquetSlack.jpg" target=3D"_blank">ht=
tp://people.stfx.ca/rlauff/307/PomquetSlack.jpg</a>.=20
One person I asked locally thought that the slack filled up again with th=
e=20
autumn rains. That's probably right, but I still can't discount s=
now melt=20
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=
=20
of<br>Antigonish County, NS.</div><br><br>
<div class=3D"gmail_quote">On 21 May 2014 18:08, nancy dowd <span dir=3D"=
ltr"><<a href=3D"mailto:nancypdowd@gmail.com" target=3D"_blank">nancypdo=
wd@gmail.com</a>></span> wrote:<br>
<blockquote style=3D"BORDER-LEFT:#ccc 1px solid;MARGIN:0px 0px 0px 0.8ex;=
PADDING-LEFT:1ex" class=3D"gmail_quote">Maybe it is just evaporation. Water=
accumulates in the=20
leaf-lined slacks in the Spring (rain and melt) and eventually warming =
temps=20
and strong sun evaporate it until it is empty. Over the summer heat and=
sun=20
manage to keep up with the rainfall not allowing it to accumulate for a=
ny=20
length of time (it must be hot down in those slacks). Then once the coo=
ler=20
temps and less intense sun of Fall take over rainwater can accumulate o=
nce=20
again in the slacks until it freezes.<br><br>Just a guess.<br><br>Nancy=
<br>
<div>
<div>On 2014-05-21, at 4:39 PM, David & Alison Webster <<a href=
=3D"mailto:dwebster@glinx.com" target=3D"_blank">dwebster@glinx.com</a>>=
=20
wrote:<br><br>> Hi Randy & All,<br>> =C2=A0 =C2=A0 I had imag=
ined=20
these dunes to be bare sand. With tree cover on the peaks and presumabl=
y=20
none on the slacks there is another effect that will increase effective=
ppt=20
in the slacks; sublimation on the tree canopy in calm weather and selec=
tive=20
snow accumulation in treeless areas (roads, glades, etc) in windy weath=
er=20
due to less turbulence and less speed over glades..<br>> Yt, DW<br>&=
gt;=20
----- Original Message -----<br>> From: Randy Lauff<br>> To:=20
NatureNS<br>> Sent: Wednesday, May 21, 2014 9:57 AM<br>> Subject:=
Re:=20
[NatureNS] slacks - when do they refill?<br>><br>> Thanks=20
folks,<br>><br>> I haven't been there in winter, despite my b=
eing in=20
NS now for over 20 years.<br>><br>> Here's the landscape pict=
ure=20
though. Picture an accordion, partly open lying on its back. The bellow=
s=20
represent the dune system at Pomquet, there are peaks and troughs (slac=
ks),=20
and precious little other elevations going on. At the slack in question=
, the=20
surrounding peaks of the dunes are dominated by white pine and oak, wit=
h=20
other trees as well.<br>><br>> Fred asked, if the dunes are sandy=
, how=20
are they holding water in the first place? Basically, I think there is =
leaf=20
litter which may be accumulating in the slack to slow the water seepage=
.=20
Further to Anne's email, the slack in question is well back from th=
e salt=20
water, I suspect there is no salt to speak of in that water. Mosquitoes=
are=20
there in the billions, peepers are deafening, both suggesting fresh wat=
er=20
(though I realize a few mosquitoes can tolerate brackish=20
water).<br>><br>> Randy<br>><br>>=20
_________________________________<br>> RF Lauff<br>> Way in the=
=20
boonies of<br>> Antigonish County, NS.<br>><br>><br>> On 20=
May=20
2014 18:24, David & Alison Webster<<a href=3D"mailto:dwebster@gl=
inx.com" target=3D"_blank">dwebster@glinx.com</a>> wrote:<br>>=20
Hi Randy & All, =C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0 =
=C2=A0=20
=C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0May 20, 2014<br>> =C2=A0 =
=C2=A0=20
I don't have a clear picture of the topography, either dune or inla=
nd, but=20
one possible source of water in the slacks is drifting of snow into=20
pools.<br>><br>> =C2=A0 =C2=A0 In woods south of Kentville, where=
I=20
used to walk in winter, pools in woodland cradlehollows of swampy sites=
=20
never froze. With 2'-3' of snow on the ground, the air cone was=
typically=20
about ~1' across at snow level and 4" across at water level. E=
ven at -20o C,=20
with heavy snowfall, 60 mph winds and drifting snow =C2=A0there would b=
e no=20
hint of ice. From the viewpoint of ppt per unit area these cones act as=
=20
black holes; snow blows into them but, soon being water, can not escape=
.=20
These air cones were absent when snow was not deep enough to act as a g=
ood=20
insulator. With sufficient snow cover drifted ~level over the swamp, th=
e=20
soil at the base of cradlehollows would warm sufficiently by ground hea=
t=20
from below to melt overlying snow and eventually generate one of these =
air=20
cones.<br>><br>> =C2=A0 =C2=A0 If these pools were sufficiently a=
bove=20
the water table then they would tend to be transient but, in most soils=
=20
(given sufficient iron and decomposable organic matter), infiltration r=
ate=20
at constant head will gradually slow due to formation of a local iron p=
an=20
over decades or centuries. This effect interested me because ortstein i=
s=20
sometimes very scattered; patches 3-4' wide and 10-15' apart an=
d these pools=20
that collect below air cones could account for this. Also prolonged wet=
ting=20
will slake any soil aggregates and decrease infiltration=20
rate.<br>><br>> =C2=A0 =C2=A0 Getting back to dunes, in the ideal=
ized=20
case of parallel linear dunes and linear slacks and =C2=A0in deep snow=
=20
conditions I would expect linear narrow pools at the base of linear nar=
row=20
trenches in the snow; V-shaped deposits of ortstein if dunes are stable=
and=20
not advancing.<br>><br>> =C2=A0 =C2=A0 Have you been there in win=
ter=20
and if so does any of this register ?<br>> Yt, Dave Webster,=20
Kentville<br>> ----- Original Message -----<br>> From: Randy=20
Lauff<br>> To: NatureNS<br>> Sent: Tuesday, May 20, 2014 4:20=20
PM<br>> Subject: Re: [NatureNS] slacks - when do they=20
refill?<br>><br>> Thanks Fred, but in a dune system, wouldn't=
that=20
mean that the slacks would be less than half full with water? These are=
sand=20
dunes...very porous, so I'm suspecting water leaching in from the h=
ills of=20
the dunes into the slacks just couldn't fill them. This is unlike t=
he=20
condition in vernal pools where there can be ample elevation around fro=
m=20
which water could leach in to the pool area. I'm thinking there has=
to be a=20
significant rain or snow fall to fill them.<br>><br>>=20
Randy<br>><br>> _________________________________<br>> RF=20
Lauff<br>> Way in the boonies of<br>> Antigonish County,=20
NS.<br>><br>><br>> On 20 May 2014 15:30, Fred Schueler <<a =
href=3D"mailto:bckcdb@istar.ca" target=3D"_blank">bckcdb@istar.ca</a>>wr=
ote:<br>> On=20
5/20/2014 2:18 PM, Randy Lauff wrote:<br>><br>> Between several o=
f the=20
dunes at Pomquet Beach, Ant. Co., the slacks (the<br>> troughs betwe=
en=20
dune crests) fill with water, but by summer are dry. I<br>> guess I&=
#39;ve=20
just never been there at the right time to see when they fill<br>>=
=20
again...it can't be just from winter melt water, since the slacks=
=20
are<br>> almost full (and snow melts to about 10% its volume as wate=
r).=20
Do the<br>> autumn rains fill them again, or the spring rains? Or is=
it=20
a<br>> case-by-case scenario, which I'd just have to=20
monitor?<br>><br>> * I had the same thought about vernal pools at=
the=20
CARCNET meeting at Quebec City in 1999, during a presentation on Marble=
d=20
Salamanders, which come down into the vernal pools to lay their eggs on=
the=20
dry pondbed in the fall, and stay with them all winter. It turns out th=
at=20
the vernal pools fill from the water table, as one would think sandy du=
nes=20
would. And yes, I've been monitoring water level in our local Wood =
Frog=20
ponds, fall and late winter, ever since then.<br>><br>> fred.<br>=
>=20
------------------------------------------------------------<br>> =
=C2=A0=20
=C2=A0 =C2=A0 =C2=A0 =C2=A0Frederick W. Schueler & Aleta Karstad<br=
>>=20
Daily Paintings -<a href=3D"http://karstaddailypaintings.blogspot.com/"=
target=3D"_blank">http://karstaddailypaintings.blogspot.com/</a><br>>=
=20
Vulnerable Watersheds -<a href=3D"http://vulnerablewaters.blogspot.ca/"=
target=3D"_blank">http://vulnerablewaters.blogspot.ca/</a><br></div></div>=
>=20
=C2=A0 =C2=A0study our books -<a href=3D"http://pinicola.ca/books/index=
.htm" target=3D"_blank">http://pinicola.ca/books/index.htm</a><br>
<div>> =C2=A0 =C2=A0 =C2=A0 =C2=A0 =C2=A0RR#2 Bishops Mills, Ontario=
,=20
Canada K0G 1T0<br>> =C2=A0 on the Smiths Falls Limestone Plain 44* 5=
2'N=20
75* 42'W<br></div>> =C2=A0 =C2=A0<a href=3D"tel:%28613%29258-310=
7" value=3D"+16132583107" target=3D"_blank">(613)258-3107</a> <bckcdb <a=
href=3D"http://atistar.ca" target=3D"_blank">atistar.ca</a>> <a href=3D=
"http://pinicola.ca/" target=3D"_blank">http://pinicola.ca/</a><br>
<div>
<div>>=20
------------------------------------------------------------<br>><br=
>>=20
No virus found in this message.<br>> Checked by AVG - <a href=3D"htt=
p://www.avg.com" target=3D"_blank">www.avg.com</a><br>> Version:=20
2014.0.4577 / Virus Database: 3950/7502 - Release Date:=20
05/15/14<br>><br>><br>> No virus found in this message.<br>>=
;=20
Checked by AVG - <a href=3D"http://www.avg.com" target=3D"_blank">www.a=
vg.com</a><br>> Version: 2014.0.4577 / Virus Database:=20
3950/7529 - Release Date:=20
05/20/14<br>><br><br></div></div></blockquote></div><br></div><a></a>
</div></div><p align=3D"left" color=3D"#000000"></p><div><div class=3D"h5=
">No virus found in this=20
message.<br>Checked by AVG - <a href=3D"http://www.avg.com" target=3D"_bl=
ank">www.avg.com</a><br></div></div>Version: 2014.0.4592 / Virus=20
Database: 3950/7543 - Release Date: 05/22/14<p></p></blockquote></div>
</blockquote></div><br></div>
--001a11394fb4e69ed404fa3fbaab--
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