The mineral sand deposits occur at the top of a series of sedimentary deposits, within a sequence of relatively recent unconsolidated sands.

They generally originate from the adjacent Yilgarn Block, which has been eroded, transported by rivers and streams and deposited as beach sands along former coastlines.

The deposits now form successive north-south linear deposits well inland from the present coast. Upper level deposits that either outcrop or are covered by minimal amounts of nonmineralised material (overburden), occur in the northern half of the tenement. Mid-level deposits are covered with varying depths of overburden. The basement deposits occur below the mid-level deposits and are typically more weathered and of lower heavy mineral grade.

Mining at Cooljarloo is undertaken using dry mining methods to access the upper to mid ore-bodies and dredge mining.

Dewatering pumps are used to evacuate water from the active mining pit in areas below the water table. This water is generally utilised in the process or stored in water holding dams for later use.

Bulldozers push material into an in-pit hopper to screen the ore and remove oversize.

Processing - Both wet and dry mining techniques utilize wet concentrator plants to produce a high grade of heavy mineral concentrate (typically approximately 90% to 98% heavy mineral content). Screened ore is first deslimed, a process by which slimes are separated from larger particles of minerals, and then washed through a series of spiral separators that use gravity to separate the heavy mineral sands from lighter materials, such as quartz. Residue from the concentration process is pumped back into either the open pits or slimes dams for rehabilitation and water recovery. Water used in the process is recycled into a clean water dam with any additional water requirements made up from pit dewatering or rainfall.

Mineral Separation - The non-magnetic (zircon and rutile) and magnetic (ilmenite) concentrates are passed through a dry separation process, known as the “dry mill” to separate out the minerals. Electrostatic and dry magnetic methods are used to further separate the ilmenite, rutile and zircon. Electrostatic separation relies on the difference in surface conductivity of the materials to be separated. Conductive minerals (such as ilmenite, rutile and leucoxene) behave differently from non-conductive minerals (such as zircon) when subjected to electrical forces. Magnetic separation techniques are dependent on the iron content of a mineral. Magnetic minerals (such as ilmenite) will separate from non-magnetic minerals (such as rutile and leucoxene) when subjected to a magnetic field. A combination of gravity and magnetic separation is used to separate zircon from the non-magnetic portion of the heavy mineral concentrate. The heavy mineral concentrate at KZN Sands and Namakwa Sands is passed through wet high-intensity magnetic separation to produce a non-magnetic fraction and a magnetic fraction.