60% of Top Lottery Jackpots Have These 4 Numbers in Common

 Powerball, Mega Millions, Super Lotto, Fantasy, you name it...

There are 275,223,510 different combinations that can be drawn...

And yet for the BIGGEST WINS IN U.S. HISTORY...

40% of the time the first number was a variation of 1 (either 1, 10, or 11)...

45% of the time the winning Powerball was 19 (notice how 1 + 9 = 10?)...

50% of the time the winning Powerball was a variation of 7 (see here why 7 is such a common number and how it appears every 2 weeks...)

Want to be even more tripped out?

Check out minute 6:10 of this brief video...

You’ll see how the same four numbers show up in 60% of top lottery jackpots...no exceptions!

See the conclusive proof right here.

 

arole (or fumerole) is a vent in the surface of the Earth or other rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field. The predominant vapor emitted by fumaroles is steam, formed by the circulation of groundwater through heated rock. This is typically accompanied by volcanic gases given off by magma cooling deep below the surface. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide, and sometimes hydrogen chloride, hydrogen fluoride, and other gases. A fumarole that emits significant sulfur compounds is sometimes called a solfatara. Fumarole activity can break down rock around the vent, while simultaneously depositing sulfur and other minerals. Valuable hydrothermal mineral deposits can form beneath fumaroles. However, active fumaroles can be a hazard due to their emission of hot, poisonous gases. Description A fumarole (or fumerole; from French fumerolle, a domed structure with lateral openings, built over a kitchen to permit the escape of smoke) is an opening in a planet's crust which emits steam and gases, but no liquid or solid material. The temperature of the gases leaving the vent ranges from about 100 to 1,000 °C (210 to 1,800 °F). The steam forms when groundwater is superheated by hot rock, then flashes (boils due to depressurization) as it approaches the surface. In addition to steam, gases released by fumaroles include carbon dioxide, sulfur oxides, hydrogen sulfide, hydrogen chloride, and hydrogen fluoride. These have their origin in magma cooling underground. Not all these gases are present in all fumaroles; for example, fumaroles of Kilauea in Hawaii, US, contain almost no hydrogen chloride or hydrogen fluoride. The gases may also include traces of carbonyl sulfide, carbon disulfide, hydrogen, methane, or carbon monoxide. A fumarole that emits sulfurous gases can be referred to as a solfatara (from old Italian solfo, "sulfur"). Acid-sulfate hot springs can be formed by fumaroles when some of the steam condenses at the surface. Rising acidic vapors from belo