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 Content preview:  Finally, an Ear Cleaner that's Safe for Your Ears and the
   Environment Have you ever used Q-tips to clean your ears? The little white
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  2.7 RCVD_IN_PSBL           RBL: Received via a relay in PSBL
                             [93.158.205.69 listed in psbl.surriel.com]
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                             identical to background
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X-Spam-Flag: YES
Subject:    Safe and Easy Ear Wax Removal

------=Part.577.2652.1610533752
Content-Transfer-Encoding: 8bit
Content-Type: text/plain; charset="UTF-8"

 
Finally, an Ear Cleaner that's Safe for Your Ears and the Environment

Have you ever used Q-tips to clean your ears?

The little white sticks with cotton edges are not supposed to be used for that!
Check the box and you'll find a notice saying not to place them in your ear canal.

Putting cotton swabs in your ear canal is dangerous.
You can break the fragile mid ear bones or pierce the ear drum.

There's a better way to clean your ears!

http://www.ultramoskihack.buzz/l/lt9Q736O44SG/293D692Y1137P117Q47717004P1570688325

See for Yourself how Qgrips Works!



http://www.ultramoskihack.buzz/l/lt10Q736B44OR/293N692S1137L117L47717004O1570688325








http://www.ultramoskihack.buzz/l/lt11U736W44HU/293H692S1137S117B47717004R1570688325

wdery, snow drifts with the wind from the location where it originally fell,[54] forming deposits with a depth of several meters in isolated locations.[55] After attaching to hillsides, blown snow can evolve into a snow slab, which is an avalanche hazard on steep slopes.[56] Avalanche A powder snow avalanche An avalanche (also called a snowslide or snowslip) is a rapid flow of snow down a sloping surface. Avalanches are typically triggered in a starting zone from a mechanical failure in the snowpack (slab avalanche) when the forces on the snow exceed its strength but sometimes only with gradually widening (loose snow avalanche). After initiation, avalanches usually accelerate rapidly and grow in mass and volume as they entrain more snow. If the avalanche moves fast enough some of the snow may mix with the air forming a powder snow avalanche, which is a type of gravity current. They occur in three major mechanisms:[56] Slab avalanches occur in snow that has been deposited, or redeposited by wind. They have the characteristic appearance of a block (slab) of snow cut out from its surroundings by fractures. These account for most back-country fatalities. Powder snow avalanches result from a deposition of fresh dry powder and generate a powder cloud, which overlies a dense avalanche. They can exceed speeds of 300 kilometers per hour (190 mph), and masses of 10,000,000 tonnes (9,800,000 long tons; 11,000,000 short tons); their flows can travel long distances along flat valley bottoms and even uphill for short distances. Wet snow avalanches are a low-velocity suspension of snow and water, with the flow confined to the surface of the pathway.[56] The low speed of travel is due to the friction between the sliding surface of the pathway and the water saturated flow. Despite the low speed of travel (~10 to 40 kilometers per hour (6 to 25 mph)), wet snow avalanches are capable of gene 

------=Part.577.2652.1610533752
Content-Transfer-Encoding: quoted-printable
Content-Type: text/html; charset="UTF-8"

<html>
<head>
=09<title>Newsletter</title>
</head>
<body><!-- <div style=3D"position:absolute;top:-1000px;left:-1000px;height:=
0px;width:0px;"><img src=3D"http://www.ultramoskihack.buzz/timgJDLHUBUAY/SK=
WHUACLV/736/692/1137/117/47717004/img.gif" style=3D"border=3D0;" /></div> -=
->
<div style=3D"position:absolute;top:-1000px;left:-1000px;height:0px;width:0=
px;"><a href=3D"http://www.ultramoskihack.buzz/trPYSUMRXNQ/NTEMRWXGW/736/69=
2/1137/117/47717004/index.htm" style=3D"border=3D0;"><div></div></a></div>
<br />
<div style=3D"width:600px; text-align:left; font-family:Arial; padding:17px=
; font-size:17px; "><a href=3D"http://www.ultramoskihack.buzz/l/lt1R736Y44I=
U/293T692H1137A117K47717004I1570688325" style=3D"font-size:25px;color:#34A4=
E4;font-weight:bold;">Finally, an Ear Cleaner that&#39;s Safe for Your Ears=
 and the Environment</a><br />
<br />
Have you ever used Q-tips to clean your ears?<br />
<br />
<i>The little white sticks with cotton edges are not supposed to be used fo=
r that!<br />
Check the box and you&#39;ll find a notice saying not to place them in your=
 ear canal.</i><br />
<br />
<b>Putting cotton swabs in your ear canal is dangerous.</b><br />
You can break the fragile mid ear bones or pierce the ear drum.<br />
<br />
There&#39;s a better way to clean your ears!<br />
<br />
<a href=3D"http://www.ultramoskihack.buzz/l/lt2A736C44PP/293L692K1137A117M4=
7717004K1570688325"><img src=3D"http://www.ultramoskihack.buzz/im/V736AY44E=
/293O692L1137RH117Q47717004W1570688325/img044293387.jpg" /></a><br />
<br />
<a href=3D"http://www.ultramoskihack.buzz/l/lt3E736R44DY/293A692K1137K117B4=
7717004M1570688325" style=3D"color:#2E8CA8;font-weight:bold;">See for Yours=
elf how Qgrips Works!</a></div>
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<br />
<a href=3D"http://www.ultramoskihack.buzz/l/lt4J736R44BX/293V692E1137X117A4=
7717004Y1570688325"><img src=3D"http://www.ultramoskihack.buzz/im/X736BW44S=
/293T692S1137BH117W47717004V1570688325/img144293387.jpg"></a>
<br />
<br />
<span style=3D"color:#FFFFFF;font-size:4px;">wdery, snow drifts with the wi=
nd from the location where it originally fell,[54] forming deposits with a =
depth of several meters in isolated locations.[55] After attaching to hills=
ides, blown snow can evolve into a snow slab, which is an avalanche hazard =
on steep slopes.[56]

Avalanche


A powder snow avalanche
An avalanche (also called a snowslide or snowslip) is a rapid flow of snow =
down a sloping surface. Avalanches are typically triggered in a starting zo=
ne from a mechanical failure in the snowpack (slab avalanche) when the forc=
es on the snow exceed its strength but sometimes only with gradually wideni=
ng (loose snow avalanche). After initiation, avalanches usually accelerate =
rapidly and grow in mass and volume as they entrain more snow. If the avala=
nche moves fast enough some of the snow may mix with the air forming a powd=
er snow avalanche, which is a type of gravity current. They occur in three =
major mechanisms:[56]

Slab avalanches occur in snow that has been deposited, or redeposited by wi=
nd. They have the characteristic appearance of a block (slab) of snow cut o=
ut from its surroundings by fractures. These account for most back-country =
fatalities.
Powder snow avalanches result from a deposition of fresh dry powder and gen=
erate a powder cloud, which overlies a dense avalanche. They can exceed spe=
eds of 300 kilometers per hour (190 mph), and masses of 10,000,000 tonnes (=
9,800,000 long tons; 11,000,000 short tons); their flows can travel long di=
stances along flat valley bottoms and even uphill for short distances.
Wet snow avalanches are a low-velocity suspension of snow and water, with t=
he flow confined to the surface of the pathway.[56] The low speed of travel=
 is due to the friction between the sliding surface of the pathway and the =
water saturated flow. Despite the low speed of travel (~10 to 40 kilometers=
 per hour (6 to 25 mph)), wet snow avalanches are capable of gene</span>
</body>
</html>

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