Azomite International

A Natural Source of Minerals and Trace Elements

AZOMITE® And Other Volcanic Deposits

AZOMITE® is a unique volcanic deposit with over 67 trace elements. Below are a few comparisons of different volcanic ash deposits around the world. You can clearly see that AZOMITE® has a higher concentration and broader range of trace mineral elements.

Essential Trace Elements in AZOMITE® vs Two Volcanic Bentonites in Uruguay*

Trace Element

AZOMITE®

Bentonites

Copper (Cu)

13.5 ppm

4.3 ppm

Molybdenum (Mo)

12.6 ppm

0.05 ppm

Chromium (Cr)

7.8 ppm

1.28 ppm

Cobalt (Co)

22.3 ppm

4.3 ppm

Boron (B)

29 ppm

0 ppm

Iodine (I)

3.2 ppm

0 ppm

Selenium (Se)

0.79 ppm

0 ppm

Lanthanum (La)

257 ppm

47.2 ppm

Cerium (Ce)

360 ppm

94.4 ppm

Praseodymium (Pr)

27 ppm

13.1 ppm

Nickel (Ni)

2.6 ppm

0 ppm

Rubidium (Rb)

325 ppm

6.2 ppm

Tungsten

31 ppm

0.69 ppm

Sulphur

210 ppm

0 ppm

*Annals of the Brazilian Academy of Sciences;
2006 78(3) 525-541; “Chemical Signature of Two
Permian Volcanic Ash Deposits within a bentonite bed from Melo, Uruguay”

Properties of Five Volcanic Ash Deposits from Four Countries** vs. AZOMITE®

Mineral Element

AZOMITE®

Volcanic Ash

Boron (B)

29 ppm

0.25 ppm

Cobalt (Co)

22.3 ppm

0.03 ppm

Copper (Cu)

13.5 ppm

0.66 ppm

Iron (Fe)

10,370 ppm

2.51 ppm

Manganese (Mn)

200 ppm

5.93 ppm

Vanadium (V)

9.3 ppm

0.09 ppm

Zinc (Zn)

64.3

1.96 ppm

**US Geological Survey: Volcanic Ash: Effects & Mitigation Strategies

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