A rigid brittle rock is called a "fault rock". This type of rock typically forms along fault lines due to the intense pressure and tectonic forces acting on it, leading to its rigid and brittle nature.
Igneous rock is typically rigid and strong due to the interlocking nature of its mineral crystals. However, its brittleness can vary depending on factors such as mineral composition, texture, and cooling rate during formation. In general, igneous rock can fracture along existing planes but can also deform plastically under high pressure and temperature conditions.
The zone of rigid, brittle rock that makes up the outermost layer of Earth is called the lithosphere. It includes the crust and the uppermost part of the mantle, and is divided into tectonic plates that move and interact with each other. Beneath the lithosphere lies the asthenosphere, which is a more ductile and deformable region of the upper mantle.
Earth's crust and brittle upper mantle is called the lithosphere.
A window is not typically rigid but can be brittle if it is made of glass. Glass is a brittle material that can shatter easily upon impact. Other window materials, such as plastic or acrylic, may be more flexible and less likely to break.
Igneous rocks are the major type of rock most likely to experience brittle deformation. Due to their rigid and solid structure, they can fracture when subjected to stress, particularly at lower temperatures and pressures. This contrasts with sedimentary and metamorphic rocks, which may exhibit more ductile behavior under similar conditions.
WHAT IS RIGID BRITTLE ROCK CALLED? WHAT IS RIGID BRITTLE ROCK CALLED? we have no clue
WHAT IS RIGID BRITTLE ROCK CALLED? WHAT IS RIGID BRITTLE ROCK CALLED? we have no clue
Rigid, brittle rock.
Igneous rock is typically rigid and strong due to the interlocking nature of its mineral crystals. However, its brittleness can vary depending on factors such as mineral composition, texture, and cooling rate during formation. In general, igneous rock can fracture along existing planes but can also deform plastically under high pressure and temperature conditions.
The zone of rigid, brittle rock that makes up the outermost layer of Earth is called the lithosphere. It includes the crust and the uppermost part of the mantle, and is divided into tectonic plates that move and interact with each other. Beneath the lithosphere lies the asthenosphere, which is a more ductile and deformable region of the upper mantle.
Earth's crust and brittle upper mantle is called the lithosphere.
A window is not typically rigid but can be brittle if it is made of glass. Glass is a brittle material that can shatter easily upon impact. Other window materials, such as plastic or acrylic, may be more flexible and less likely to break.
Lithosphere
inflexible, unyielding, rigid, brittle
The rigid layer of rock in the Earth's crust is called the lithosphere. It is made up of the crust and the outermost part of the mantle, and it is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
The lithosphere has a rigid texture, made up of the Earth's crust and the upper portion of the mantle. It is composed of solid rock that can vary in thickness and density across different regions of the Earth.
No one will force you to, but it would be wise to include the lithosphere, which is the brittle hard rock of which the tectonic plates are composed of. Crust + rigid uppermost mantle = lithosphere.