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BSLTBig Sur Land Trust
BSLTBasalt (lithological term)
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References in periodicals archive ?
Addition of macroparticles of basalt into FeCrSiB-alloy based HVOF sprayed coating has resulted in the reduction of wear resistance under most of the conditions where dynamic loading takes place.
The high initial permeability subsequently decreased due to secondary mineral deposition, leading to the formation of individual closed systems (Keith and Staples, 1985) Although there is zoning sequence and textural evidence of open-system hydrothermal activity for the formation of the Skye basalt zeolites in amygdales and veins, restricted domains may have developed as pore space became filled by precipitates of mixed-layer nontronite-celadonite, calcite, cryptocrystalline silica and zeolites.
This proves that the basalt fiber reinforced structural glulam effectively.
Modern basalt busts of (left to right) Churchill, Shakespeare and John F Kennedy.
The basalt flows and sedimentary strata on Grand Manan are generally within a few degrees of horizontal, but with limited areas of wide gentle folds and a few normal faults.
In this study were used natural basalt rocks, of volcanic origin, crystalline, compact, composed of a mixture of silicates, from Luncani, Timis county, Romania.
While the deep water in that area contained only between 8,000 and 90,000 microorganisms per cubic centimeter, the seafloor basalt held, in its pore spaces, between 3 million and 1 billion microbes per gram.
The survey conducted at Giv'at Kipod revealed several accumulations of knapped basalt, some of which include thousands of pieces of debitage (Shimelmitz et al.
31 73 145 167 111 119 121 Rock type Basalt Basalt Basalt Basalt Basalt Basalt Basalt Plagioclase phenocrysts 26.
Chemistry can also help us to study trade and cultural exchange using rock artifacts such as this 5,000-year-old ancient Egyptian basalt vessel.
By determining fundamental surface charge characteristics of these variable charge soils, it was possible to show that the additional base cations released from the basalt dust were present as exchangeable cations, and that the amounts released were controlled by the number of negatively charged sites available, i.