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All mediums and aggregates are local: Although various norming standards for mediums have been defined (ASTM, US DOT, DIN, ANSI, etc.), those norm/standards are only rough averages: they are specific definitions of terms used in contract specifications sheets, architectural or engineering detail sheets, geotechnical designs, and so forth.
Real life stone, gravel and sand densities (weight / volume) vary widely: The local quarry or supplier which you elect to use should be able to provide the densities (tons / cubic yard) of their unique gravel, which they are quoting to you.
To use the below chart in calculating how many tons your job requires:
(your tonnage) x (yards/ton) = your cubic yards
(your metric tonnage) x (m³/tonne) = your cubic meters
(your cubic yards) x (tons / yard) = your US tons
(your cubic meters) x (tonnes / m³) = your metric tonnes
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Below is a chart (it cannot execute any math, it's just a web page).
{source = www.ecoterr.com/media/xls/CHART-COMPLETE_tools_weights_calculators_convertor.xls; download filesize = 62 KB}
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Generic "Gravel" *
(generic "common gravel")
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Specific Gravity *
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"pounds/foot"
(lb. / ft³) *
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"tons/yard"
(t. / yd³)
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"yards/ton"
(yd³ / t.)
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Please note: That your gravel is NOT "common" - rather it is specific to your local supplier. Local gravels are all slightly different and unique to their source.
Below: Loosely defined "gravel" is based upon median specific gravities of typical minerals found in the USA which makeup your local "gravel."
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Gravel, loose, dry
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1.52
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95
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1.2825
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0.7797271
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Gravel, w/sand, natural
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1.92
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120
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1.6200
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0.6172839
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Gravel, dry 1/4 to 2 inch
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1.68
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105
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1.4175
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0.7054674
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Gravel, wet 1/4 to 2 inch
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2.00
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125
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1.6875
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0.5925926
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Typical Weights of various typical minerals found in the USA: *
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Mineral Type (Material) *
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Specific Gravity *
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"pounds/foot"
(lb. / ft³) *
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"tons/yard"
(t. / yd³)
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"yards/ton"
(yd³ / t.)
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Basalt, broken
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1.96
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122
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1.6470
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0.6071645
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Basalt, solid
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3.01
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188
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2.5380
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0.3940110
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Cement, Portland
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3.15
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94
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1.2690
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0.7880221
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Cement, mortar
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2.16
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135
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1.8225
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0.5486968
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Clay, dry excavated
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1.09
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68
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0.9180
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1.0893246
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Clay, wet excavated
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1.83
|
114
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1.5390
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0.6497726
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Clay, dry lump
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1.07
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67
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0.9045
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1.1055832
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Clay, fire
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1.36
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85
|
1.1475
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0.8714597
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Clay, wet lump
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1.60
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100
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1.3500
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0.7407407
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Clay, compacted
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1.75
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109
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1.4715
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0.6795789
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Earth, loam, dry, excavated
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1.25
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78
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1.0530
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0.9496676
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Earth, moist, excavated
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1.44
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90
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1.2150
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0.8230453
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Earth, wet, excavated
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1.60
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100
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1.3500
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0.7407407
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Earth, dense
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2.00
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125
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1.6875
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0.5925926
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Earth, soft loose mud
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1.73
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108
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1.4580
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0.6858711
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Earth, packed
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1.52
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95
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1.2825
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0.7797271
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Feldspar, solid
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2.56
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160
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2.1600
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0.4629630
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Feldspar, pulverized
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1.23
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77
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1.0395
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0.9620010
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2.69
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168
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2.2680
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0.4409171
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Granite, broken
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1.65
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103
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1.3905
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0.7191658
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Gypsum, solid
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2.79
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174
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2.3490
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0.4257131
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Gypsum, broken
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1.81
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113
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1.5255
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0.6555228
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Gypsum, crushed
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1.60
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100
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1.3500
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0.7407407
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Gypsum, pulverized
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1.12
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70
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0.9450
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1.0582011
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Below "Limestone" varies widely across regions, depending upon local geology.
Calcium Carbonate (aka "Limestone" or CaCO3) in some areas is very soft and light, almost soapstone.
In some areas limestone is heavier + harder than granite (i.e. Bedford, Indiana limestone).
In some areas a very immature form of Limestone deposits is called "Caliche."
The below densities are based upon the average-median; or "a typical limestone which one might expect to find in many areas across the USA."
Definition of "limestone": n. A colorless or white crystalline compound, CaCO3, occurring naturally as chalk, limestone, marble, Caliche, and other forms; "Limestone" is also used in a wide variety of manufactured products including commercial chalk, medicines, and dentifrices.
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2.61
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163
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2.2005
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0.4544422
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Limestone, broken
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1.55
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97
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1.3095
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0.7636502
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Limestone, pulverized
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1.39
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87
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1.1745
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0.8514261
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* Caliche (immature limestone)
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1.44
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90
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1.2150
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0.8230453
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Mica, solid
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2.88
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180
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2.4300
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0.4115226
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Mica, broken
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1.60
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100
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1.3500
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0.7407407
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2.64
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165
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2.2275
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0.4489338
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Quartz, lump
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1.55
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97
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1.3095
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0.7636502
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Quartz sand
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1.20
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75
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1.0125
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0.9876543
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Above: About Quartz, aka "Silica Dioxide" or SiO2...
Silica is the second most common element in the earth, following only oxygen (Silica comprises roughly 35% of the entire earth's mass, by most scientific estimates).
Common Quartz is also the fourth hardest natural mineral in the earth, following only: Diamonds, Sapphires and Topaz.
Because Quartz Sand is nonporous - and because it is an extremely adamant mineral - Quartz will not decay into dust or dissolve and wash away: as will all other typical minerals or sands.
This is why the beaches of the world are almost uniquely Quartz sand: all the other types of sand have long ago decayed into microscopic particles (colloidals) and dissolved away.
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Rip-Rap (generic, non-specific)
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1.60
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100
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1.3500
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0.7407407
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Sand, wet
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1.92
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120
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1.6200
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0.6172840
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Sand, wet, packed
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2.08
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130
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1.7550
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0.5698006
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Sand, dry
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1.60
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100
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1.3500
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0.7407407
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Sand, loose
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1.44
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90
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1.2150
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0.8230453
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Sand, rammed
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1.68
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105
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1.4175
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0.7054674
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Sand, water filled
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1.92
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120
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1.6200
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0.6172840
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Sand w/ Gravel, dry
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1.73
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108
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1.4580
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0.6858711
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Sand w/ Gravel, wet
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2.00
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125
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1.6875
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0.5925926
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Sandstone, solid
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2.32
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145
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1.9575
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0.5108557
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Sandstone, broken
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1.51
|
94
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1.2690
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0.7880221
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2.68
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167
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2.2545
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0.4435573
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Shale, broken
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1.59
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99
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1.3365
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0.7482230
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2.69
|
168
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2.2680
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0.4409171
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Slate, broken
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1.67
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104
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1.4040
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0.7122507
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Slate, pulverized
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1.36
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85
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1.1475
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0.8714597
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* Authority cited for typical mineral weights:
Reade at www.reade.com/Particle_Briefings/spec_gra2.html
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(feet wide) x (feet long) x (inches deep) = cubic yards required
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