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                            BEAR RIVER ZEOLITE
                             Preston Idaho Clinoptilolite Zeolite


                             
                            (406) 827-3523

                            tfl3543@blackfoot.net
                            Monday - Friday: 8:00 a.m. - 4:30 p.m. MST

                             

                            BRZ?GEOLOGY

                            The deposit is a very thick sedimentary deposit of zeolitized volcanic ash of Tertiary age known as the Salt Lake Formation. The sedimentary interval in which the clinoptilolite zeolite occurs is more than 1000 feet thick in the area. Thick intervals of the zeolite are separated by thin limestone beds deposited in the freshwater lake where the volcanic ash accumulated. The deposit includes an 800 foot mountain. Zeolite can be sampled over a vertical extent of 800 feet and on more than 700 acres. The current pit covers more than 3 acres. Within the pit, the clinoptilolite zeolite is remarkably homogeneous. 

                            Despite the apparent huge size of the deposit, the Company claims no reserves.


                            Aerial view of BRZ?span style="font-size: 10pt; "> pit near Preston, Idaho 

                            BRZ? TOPOGRAPHY SHOWING LIMESTONE BEDS IN ZEOLITE


                             

                             

                            BRZ? CROSS SECTIONS-LIMESTONE BEDS IN ZEOLITE

                                 

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                            Bear River Zeolite Co.
                            Mine and Plant
                            4005 East Glendale Road
                            Preston, Idaho 83263

                               Copyright?019 Bear River Zeolite Co.

                                 

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