Hi,I’ve got an eye-opening quiz for you.

Can you guess which of these common items in your house could be the “fountain of youth?”

Would you say it’s...

A. A pair of shoelaces...

B. A broom stick...

C. A cucumber...

D. Or a bottle of vinegar...

When you have your answer, click here to see if you guessed correctly.

You’ll be shown a short video presentation revealing the answer, plus you’ll also discover how this mechanism can:
  Here’s the most shocking part though...

… you can start experiencing these benefits in as little as 14 days!

To get all the juicy details about this rare anti-aging secret...



Go here to learn more about this Nobel prize winning discovery.

To your healthier and longer life,




































ng the three major types of rock, fossils are most commonly found in sedimentary rock. Unlike most igneous and metamorphic rocks, sedimentary rocks form at temperatures and pressures that do not destroy fossil remnants. Often these fossils may only be visible under magnification. Dead organisms in nature are usually quickly removed by scavengers, bacteria, rotting and erosion, but under exceptional circumstances, these natural processes are unable to take place, leading to fossilisation. The chance of fossilisation is higher when the sedimentation rate is high (so that a carcass is quickly buried), in anoxic environments (where little bacterial activity occurs) or when the organism had a particularly hard skeleton. Larger, well-preserved fossils are relatively rare. Burrows in a turbidite, made by crustaceans, San Vincente Formation (early Eocene) of the Ainsa Basin, southern foreland of the Pyrenees Fossils can be both the direct remains or imprints of organisms and their skeletons. Most commonly preserved are the harder parts of organisms such as bones, shells, and the woody tissue of plants. Soft tissue has a much smaller chance of being fossilized, and the preservation of soft tissue of animals older than 40 million years is very rare. Imprints of organisms made while they were still alive are called trace fossils, examples of which are burrows, footprints, etc. As a part of a sedimentary rock, fossils undergo the same diagenetic processes as does the host rock. For example, a shell consisting of calcite can dissolve while a cement of silica the