as rocks are compressed
Bedding planes.
Surfaces between layers of sediments (bedding planes) are usually deposited in horizontal sheets, but cross-bedding is inclined. Graded beds are horizontal and are usually sorted from coarse at the bottom to fine at the top.
Shale - a sedimentary rock formed from clay or mud by considerable pressure. splits easy into thin laminations along its bedding planes and shrinks when dried out cracking to form pieces that often curl slightly to resemble tiles. when moistened it has an earthy smell Mudstone - a fine textured sedimentary rock similar to shale but is compact and is not, like shale, arranged in bedding planes
Igneous intrusions that are concordant (parallel to bedding planes of country rocks) are known as sills, whereas dykes cut through the bedding.
rocky
Bedding planes are found exclusively in sedimentary rock. Joints are more common in igneous rock, but can be found in sedimentary rock as well. Igneous rock can never have bedding planes, but does have pseudo-bedding planes.
They are called bedding planes
gabbro
Bedding planes.
They indicate a depositional event.
Angles are formed by the intersection of two planes.
Curtains are formed when water containing calcium carbonate drips slowly through the joints and bedding planes of the limestone and comes out through a long crack in the ceiling of the cave . The water evaporates, leaving the calcium carbonate behind .
ONLY a line can be formed by the intersection of two planes...and always.
Limestone is formed in layers called Bedding Planes and the vertical cracks are called Joints. The horizontal cracks are not given a specific name - however I am sure someone will want to contradict this
with glue
A bedding plane is the area of separation between rock strata made by a cyclical or situational deposition of sediment. Bedding planes are originally parallel to the horizon, but the strata inclination can be altered by crust moving events.
Surfaces between layers of sediments (bedding planes) are usually deposited in horizontal sheets, but cross-bedding is inclined. Graded beds are horizontal and are usually sorted from coarse at the bottom to fine at the top.