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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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