The Most Comfortable Waist Holster on the Market..

 

 

Why Do You Need This Holster?

This Holster Will Keep Your Weapon Concealed

Your weapon will be concealed easily underneath your shirt. Many other holsters make the weapon protrude from your body so much that the weapon can get caught on seat belts or chairs. Not this one.

Now you can carry your weapon comfortably anytime, anywhere without raising the suspicion of friends, coworkers or family members.

>>>You'll probably forget you're wearing it.
 

This Concealed Holster Might Be The Last One You Ever Need

Concealed carriers need at least one good waist holster in their arsenal. Unfortunately most of them make you sweat, or slip as you move around.

Even worse, they are uncomfortable for sitting for long periods of time.

You AND your friends won't notice you're wearing this holster...

 











 

Pumice is composed of highly microvesicular glass pyroclastic with very thin, translucent bubble walls of extrusive igneous rock. It is commonly, but not exclusively of silicic or felsic to intermediate in composition (e.g., rhyolitic, dacitic, andesite, pantellerite, phonolite, trachyte), but basaltic and other compositions are known. Pumice is commonly pale in color, ranging from white, cream, blue or grey, to green-brown or black. It forms when volcanic gases exsolving from viscous magma form bubbles that remain within the viscous magma as it cools to glass. Pumice is a common product of explosive eruptions (plinian and ignimbrite-forming) and commonly forms zones in upper parts of silicic lavas. Pumice has an average porosity of 90%[citation needed], and initially floats on water.  

Scoria differs from pumice in being denser. With larger vesicles and thicker vesicle walls, it sinks rapidly. The difference is the result of the lower viscosity of the magma that forms scoria. When larger amounts of gas are present, the result is a finer-grained variety of pumice known as pumicite. Pumice is considered a glass because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in water. After the explosion of Krakatoa, rafts of pumice drifted through the Indian Ocean for up to 20 years, with tree trunks floating among them. In fact, pumice rafts disperse and support several marine species. In 1979, 1984 and 2006, underwater volcanic eruptions near Tonga created large pumice rafts, some as large as 30 kilometers (19 mi)[citation needed] that floated hundreds of kilometres to Fiji. There are two main forms of vesicles. Most pumice contains tubular microvesicles that can impart a silky or fibrous fabric. The elongation of the microvesicles occurs due to ductile elongation in the volcanic conduit or, in the case of pumiceous lavas, during flow. The other form of vesicles are subspherical to spherical and result from high vapor pressure during eruption.