Gliding joints allow bones to slide along each other such as the wrists and ankles. Also known as a synovial joint, these bones use synovial fluid to glide more smoothly.
The term that refers to bones sliding along each other is "gliding joint." This type of joint allows for limited motion in multiple directions.
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
The joints between the carpal bones in the ankles and wrists are known as Gliding Joints (a type of synovial joint). These joints work by allowing the bones to slide over each other, allowing smooth movements in multiple directions.
Where 2 plates slide past each other in a horizontal motion that boundary is called a Transform Boundary, or a fault.
I believe that you are thinking of tectonic plates.
The term that refers to bones that slide along each other is "gliding joints." These joints, also known as planar joints, allow for limited movement in multiple directions, enabling bones to glide past one another. Examples include the joints between the carpal bones in the wrist and the tarsal bones in the ankle.
The term that refers to bones sliding along each other is "gliding joint." This type of joint allows for limited motion in multiple directions.
gliding
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
an example could be by the spine. Sliding joints occur between the bones in your backbones in your backbone. (These bones are called vertebrae.) In these joints the flat surfaces of two bones slide over each other and cause side-to-side and back-and-forth movement.
When two tectonic plates slide past each other, it is called transform boundary. This movement can create earthquakes along the boundary where the plates are in contact.
This process is called "faulting," where rocks break and slide against each other due to tectonic forces, creating faults in the Earth's crust.
Hinge joints
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in between each bone there is a rough sort of rubbery material called cartilage which prevents bones from rubbing against each other.
its called a transition =]
When two tectonic plates slide past each other horizontally, the boundary between them is called a transform boundary. This type of boundary is characterized by lateral movement along fault lines, such as the San Andreas Fault in California.