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The climate later became more arid, the lake's size diminished, and as the brine's Ca content was reduced the sodium concentration increased. This caused ulexite to be deposited in massive beds over the colemanite. As the lake further evaporated, the Ca content became very low in the central zone (most of it precipitated in the margins where the runoff water entered the lake), the concentration of boron increased, and borax crystallized. The lake periodically reflooded, with the stratified strong brine and the runoff water's mud layers protecting the borax from dissolving.

B507(OH)4] 32. Probertite NaCaB509" 5H20 Ulexite NaCaB509" 8H20 C. Medium to high calcium, dilute solutions \ / H 0 \ (-)/ 0 /B\ O O I/ B (-)B / ~O / \ I O /H / O H 3 0o:z~ + 2T, chains [B 3 04 (OH) 3 ]2- 1. Colemanite (higher temperature) Ca2B6011" 5H20 2. Inyoite (colder)" Ca2 B6011" 13H2O; structure as D2 E. Medium calcium, magnesium, dilute solutions 1. Hydroboracite (structure as C1) D. Medium to high magnesium, dilute solutions H H\ /H \ 0 \(-)/ B /\ /0 0 \ H 0 0 \ (-)/ 0 0/ \(-)/ B / \ 0 O\ / H H 0/ / O H 2: T, isolated [B20 (OH)6]21.

S. playas at present. 2 Playa Near-Surface Crystal Cluster Deposits The formation of large clusters of borax crystals in the mud at a moderate depth has also been fairly common in modern carbonate-borax or Ca-depleted ulexite playas. Such deposits have been commercially worked at Borax Lake Specific Origin Theories 33 and Searles Lake, California, as well as Rhodes Marsh, Nevada, and have been observed in a number of playas in Argentina (Acazoque, Cauchari, Centenario, Lagunita, Lina Lari, Rincon, and Turi Lari).

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