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One product. Four convenient sizes.

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4 lb Jar $40.96

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12 lb Pail $103.74

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22.5 lb Pail $168.34

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40 lb Pail $255.15

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Shared label directions

Daily use for one horse

Average 1,100 lb horse

2 scoops — 2 oz daily

Horse under 700 lb

1 scoop — 1 oz daily

1 scoop = 1 oz

Use the current product label.

Container size	Price	Price / lb	1,100 lb horse 2 oz / day	Under 700 lb 1 oz / day	Quick add
4 lb Jar	$40.96	$10.24	Approx. 32 days	Approx. 64 days	Add to Cart
12 lb Pail	$103.74	$8.65	Approx. 96 days	Approx. 192 days	Add to Cart
22.5 lb Pail	$168.34	$7.48	Approx. 180 days	Approx. 360 days	Add to Cart
40 lb Pail	$255.15	$6.38	Approx. 320 days	Approx. 640 days	Add to Cart

Duration estimates assume 16 ounces per pound and consistent daily use. Always follow the current product label.

Learn
Learn

Montmorillonite Fulvic acid Mineral profile

Montmorillonite

The Natural Mineral Matrix

Montmorillonite is a naturally occurring layered clay mineral. Two silica-rich sheets surround an alumina-rich sheet, with water and exchangeable mineral ions between neighboring layers.

Its layered structure and electrical charge give it the ability to exchange certain ions with its surroundings. Animal Trace Minerals describes this naturally occurring material as the mineral matrix of its product.

Layered
structure

Surface
charge

Active
surfaces

Exchangeable
ions

Layered clay structure

Tetrahedral sheets

Octahedral sheet

Interlayer space

In the 2:1 clay layer, two tetrahedral sheets surround one octahedral sheet. Interlayer spaces lie between successive layers.

Fulvic Acid

Naturally Associated Compounds

Fulvic acids belong to a diverse family of naturally occurring organic compounds formed as plant and microbial material breaks down.

They can associate with mineral ions to form complexes, making them part of the chemistry of natural mineral and organic materials. Historical Animal Trace Minerals information describes humic and fulvic compounds associated with this mineral source.

Organic functional groups Organic groups provide sites where mineral interactions can occur.

Mineral associations Binding depends on the mineral, the organic material, and surrounding conditions.

Part of the natural matrix The organic material is discussed alongside the clay and its naturally occurring elements.

Fulvic substances · conceptual organic network

Illustrative organic groups—not a single molecular formula or a product-specific laboratory structure.

Naturally occurring organic compounds and minerals are part of the same source material.

Broad Trace
Mineral Profile

A 76-element natural mineral profile

The Montmorillonite Technical Report and Dr. Carlos Cortelezzi’s original equine study describe a natural mineral profile containing 76 elements. Selected elements from that profile are shown below.

Ca Calcium

Mg Magnesium

Zn Zinc

Cu Copper

Mn Manganese

K Potassium

Natural mineral composition can vary. Follow the current product label for declared composition and feeding directions.

Naturally occurring mineral matrix

Selected elements shown for orientation; the network is illustrative rather than a quantitative analysis.

Mineral science references

These references explain the clay structure and organic chemistry illustrated above.

Clay structure: USGS · Smectite group . Exchange chemistry: USGS · Ion exchange .

Organic substances: International Humic Substances Society .

Patent & Supporting Research

Our documentation includes U.S. Patent No. 6,764,692 B1, issued to Carlos Cortelezzi in 2004, the Montmorillonite Technical Report, and his 1997 equine field study. The patent describes the mineral composition, preparation method, and equine applications. The field study records qualitative observations involving hoof condition, mobility, and feeding.

Read the original documents for their methods, findings, and context. Reported observations are not a guarantee of individual results; current product labeling and veterinary guidance remain important.

U.S. Patent 6,764,692 (PDF) Montmorillonite Technical Report (PDF) Original Laminitis Study · 1997 (PDF)
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