Potash Arizona, Inc. is advancing plans to initially develop, build, and operate a selective solution mine before developing a conventional potash mine and state-of-the-art production facility. This decision is driven by several strategic and competitive advantages, including the shallowness of the deposit, established infrastructure, and proximity to year-round markets.
We are committed to conducting our operations in a manner that protects the environment and safeguards our employees and the public from unacceptable risks. Through integrated business planning, clear goals, and responsible decision-making, we aim to support sustainable development—conserving resources, maximizing the value of what we extract, and enhancing environmental, social, and economic outcomes.
The Holbrook Salt Basin, located in eastern Arizona, lies within the Permian-aged Supai Salt Formation. This formation is divided into five distinct cycles, with Cycle 5, the uppermost layer, hosting significant potash mineralization.
Mineralized zones are typically found at depths ranging from 800 to 2,000 feet (243 to 609 meters) below the surface. Potash, primarily in the form of sylvite, is usually concentrated in the upper parts of these evaporite sequences.
This depth profile is comparable to the Carlsbad potash mine in New Mexico and is considered relatively shallow compared to many other potash basins worldwide—offering potential advantages in development and operating costs.
In comparison to other deposits around the world, the Holbrook Basin has several competitive advantages:
Potash in the Holbrook Basin lies in two primary seams within the Supai Formation, the KR-1 and KR-2 seams. The KR-1 seam lies above the KR-2 seam and is unevenly distributed throughout the basin. The KR-2 seam is the primary target for delineation and development. In 2012, North Rim produced an NI 43-101 compliant technical report which estimated the Holbrook Project Resource in accordance with CIM standards and using a 40%-ft (grade x thickness) cutoff estimated the following:
Selective solution mining is an efficient, environmentally conscious method for extracting potash. It works by circulating heated brine, which is water saturated with common salt (sodium chloride) but undersaturated with potash (potassium chloride), through high‑grade ore zones. The heat, which requires a dedicated energy source, enhances the dissolution of valuable potassium chloride while leaving sodium chloride in place. As the process involves salts, it is carefully engineered to manage corrosion, scaling, and brine chemistry. This targeted approach minimizes waste, reduces surface tailings, conserves water, and can be paired with low‑energy crystallization methods, making it a sustainable and cost‑effective choice for modern potash production.
The Vertical Cavern Method of selective solution mining is shown in the four images below:
Image source: Qiu, B. & Hardy, M., An Overview of Solution-Mining Methodologies for Potash Mining, SMRI Spring Technical Conference 2023 (used with permission).
Selective solution mining of potash offers significant economic and environmental advantages compared to traditional underground mining methods.
Economic Advantages:
Environmental Advantages:
In summary, selective solution mining offers a cleaner, more sustainable approach to potash extraction, aligning with modern environmental goals while delivering compelling economic benefits through lower initial investment and operational efficiencies.
Copyright © 2025 Potash Arizona, Inc. - All Rights Reserved.
We use cookies to analyze website traffic and optimize your website experience. By accepting our use of cookies, your data will be aggregated with all other user data.