What factor does not contribute to the strength and stability of a synovial joint? synovial fluid the shape of the articular surfaces the arrangement of ligaments muscle tone

Explanation:

Synovial joints are joints that can move in many directions. Hips, shoulders, elbow, knees, wrists and ankles have synovial joints, they are filled with synovial fluid, it is a lubricants for the joints so that they can move easily but it doesn't strengthens or stabilises the joint. There are six types of this joints pivot , hinge, plane, saddle, ball and socket and condyloid.

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)

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