Is The Sky Falling Or Are Chemtrails A Paranoid Delusion?
Thursday, March 27th, 2008
A jet leaves a contrail across the sky.Chances are, that you have seen an airplane high in the sky leaving a contrail. Contrails most commonly form as water vapor from jet exhaust pushes the water content of the surrounding air past the point of saturation leading to the formation of water droplets or ice crystals that hang in the sky forming an artificial cloud. These contrails usually dissipate very quickly. However on occasion the contrails left behind a jet do not dissipate. Instead they hang in the sky overhead, slowly spreading, sometimes taking hours to fully disappear. Some people believe that these long lasting contrails are something much more vile than a normal trail of condensed water vapor. They theorize that instead of water vapor these contrails are made up of some sort of aerosolized chemical, purposefully sprayed out of specially designed jets.
Why you ask, would someone want to spray large areas covertly? Well, if you subscribe to the conspiracy theories, 
1966 photo of Project Stormfury personnel.the reasons are many ranging from the reasonably plausible to the incredible. On the easier to believe side of the scale, we have weather control - potentially to try and reverse the effects of global warming. Weather modification is something that does happen on a regular basis round the world when clouds are “seeded” to produce rain, though the effectiveness of this technique has never been proven and is hotly debated. It is also a topic that has been extensively researched by the US government which ran Project Stormfury from the early 60’s to the early 80’s in an attempt to discover a means of weakening hurricanes. The project was canceled after it failed to produce any viable results. Though over ten years past since the last official experimental flight and the projects cancelation in 1983, which may lead some to believe that Project Stormfury did uncover something in those intervening years before its cancelation.
