There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock (
clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined as grains 2–62
μm in diameter, or 4 to 8 on the
Krumbein phi (φ) scale. An alternate definition is that siltstone is any sedimentary rock containing 50% or more of silt-sized particles. Siltstones can be distinguished from claystone in the
field by chewing a small sample; claystone feels smooth while siltstone feels gritty. Siltstones differ significantly from
sandstones due to their smaller pores and a higher propensity for containing a significant
clay fraction. Although often mistaken for a
shale, siltstone lacks the laminations and
fissility along horizontal lines which are typical of shale. Siltstones may contain
concretions. Unless the siltstone is fairly shaly,
stratification is likely to be obscure and it tends to
weather at oblique angles unrelated to bedding. == Origin ==