Eat this Ice Cream Daily to Lose Weight

Did you know there are 2 ingredients you can combine to make a delicious, “Fat-Burning ICE CREAM”?

…so that the moment you have a sweet tooth … or are low on energy … or you just want to kick-start your metabolism and accelerate fat loss…

…it’s waiting for you in the freezer.

And after you enjoy every mouth-watering bite, you won’t feel guilty, lethargic, or bloated.

…because it’s actually fueling your body with all the right fat-burning nutrients … with HALF the calories!

What are the 2 ingredients?

Water is one … and the other is right here (see quick “how to” video halfway down the page)

Imagine how EASY losing fat can be when you’re indulging in delicious ice cream daily.

..and it’s as simple as mixing just two ingredients together.

I hope you love this fat-burning ice cream as much as I do!

Jimmy

P.S. Need PROOF that you really can Eat This ICE CREAM Daily to Lose FAT?

Check out all these amazing before and after photos and videos of real people like YOU who are enjoying mouth-watering ice cream … every single day. … and losing weight.









ced by the action of certain acid on certain metals. This gas was, in fact, hydrogen, which Cavendish correctly guessed was proportioned to two in one water. Although others, such as Robert Boyle, had prepared hydrogen gas earlier, Cavendish is usually given the credit for recognising its elemental nature. Also, by dissolving alkalis in acids, Cavendish made "fixed air" (carbon dioxide), which he collected, along with other gases, in bottles inverted over water or mercury. He then measured their solubility in water and their specific gravity, and noted their combustibility. Cavendish was awarded the Royal Society's Copley Medal for this paper. Gas chemistry was of increasing importance in the latter half of the 18th century, and became crucial for Frenchman Antoine-Laurent Lavoisier's reform of chemistry, generally known as the chemical revolution. ntified and allowed for sources of error. The balance that he used, made by a craftsman named Harrison, was the first of the precision balances of the 18th century, and as accurate as Lavoisier's (which has been estimated to measure one part in 400,000). Cavendish worked with his instrument makers, generally improving existing instruments rather than inventing wholly new ones. Cavendish, as indicated above, used the language of the old phlogiston theory in chemistry. In 1787, he became one of the earliest outside France to convert to the new antiphlogistic theory of Lavoisier, though he remained sceptical about the nomenclature of the new theory.[citation needed] He also objected to Lavoisier's identification of heat as having a material or elementary basis. Working within the framework of Newtonian me In 1783, Cavendish published a paper on eudiometry (the measurement of the goodness of gases for breathing). He described a new eudiometer of his invention, with which he achieved the best results to date, using what in other hands had been the inexact method of measuring gases by weighing them. He next published a paper on the production of water by burning inflammable air (that is, hydrogen) in "dephlogisticated air" (now known to be oxygen), the latter a constituent of atmospheric air (phlogiston theory). Cavendish concluded that dephlogisticated air was dephlogisticated water and that hydrogen was either pure phlogiston or phlogisticated water. He reported these findings to Joseph Priestley, an English clergyman and scientist, no later than March 1783, but did not publish them until the following year. The Scottish inventor James Watt published a paper on the composition of water in 1783; Cavendish had performed the experiments first, but published second. Controversy about priority ensued. In 1785, Cavendish investigated the composition of common (i.e. atmospheric) air, obtaining impressively accurate results. He conducted experiments in which hydrogen and ordinary air were combined in known ratios and then exploded with a spark of electricity. Furthermore, he also described an experiment in which he was able to remove, in modern terminology, both the oxygen and nitrogen gases from a sample of atmospheric air until only a small bubble of unreacted gas was left in the original sample. Using his observations, Cavendish observed that, when he had determined the amounts of phlogisticated air (nitrogen) and dephlo