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Rock Weight Calculator and Density Chart
A rock weight estimate is a mass calculation: mass equals volume multiplied by mass density. Strictly, weight is a force, but everyday searches use rock weight to mean mass, so GeoMiner reports kilograms, pounds, and metric tonnes. The SI density unit is kilograms per cubic metre; one gram per cubic centimetre equals 1,000 kilograms per cubic metre and approximately 62.428 pounds per cubic foot. The density chart uses five transparent, illustrative calculator presets: sandstone 2.30 grams per cubic centimetre, or 2,300 kilograms per cubic metre and 143.6 pounds per cubic foot; limestone 2.55, or 2,550 and 159.2; quartzite 2.65, or 2,650 and 165.4; granite 2.67, or 2,670 and 166.7; and basalt 2.90, or 2,900 and 181.0. These are single-point orientation values, not universal ranges, measured values, or design inputs. Choose a volume method first. A rectangular approximation multiplies length, width, and height. A sphere uses four-thirds pi times radius cubed, with radius equal to half the measured diameter. A cylinder uses pi times radius squared times length and is useful for regular drill core or cylindrical specimens. A measured volume can be entered directly in cubic centimetres, litres, cubic metres, cubic inches, or cubic feet. Keep units consistent and multiply by quantity only after calculating one object's volume. Geometry is often the largest uncertainty: an enclosing box includes empty corners, a sphere ignores irregular faces, and a cylinder ignores taper, broken ends, and voids. Water displacement can better represent a small irregular specimen only when the material is known to be stable and water-compatible. Trapped air and water entering connected pores still bias the result. Never immerse soluble, friable, porous, swelling, reactive, contaminated, valuable, mounted, fragile, or unknown material. Density is not one fixed number per rock name. Mineral proportions, pores, fractures, weathering, alteration, moisture, saturation, temperature, and measurement method all affect bulk density. Published granite, sandstone, limestone, basalt, and quartzite values are illustrative starting references, not certificates for an unknown rock. Specific gravity, particle density, dry bulk density, saturated bulk density, and in-place bulk density are related but not interchangeable. Record the property, moisture condition, specimen representativeness, and meth