The angle formed by a horizontal line is 180o.
Angles are formed by the intersection of two planes.
No, horizontal planes run parallel to each other, so they do not intersect, but two vertical planes can intersect. Imagine the pages of a books as several planes. When you stand the book up, they are all vertical, but they all intersect at the book spine.
ONLY a line can be formed by the intersection of two planes...and always.
with glue
They are called bedding planes
as rocks are compressed
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
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.
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.
horizontal bedding is sedimentary rock structure in which layers of rocks lies horizontally.
Igneous intrusions that are concordant (parallel to bedding planes of country rocks) are known as sills, whereas dykes cut through the bedding.
The angle formed by a horizontal line is 180o.
gabbro
Bedding planes.
They indicate a depositional event.
Angles are formed by the intersection of two planes.