If a shaping program is not moving forward and there are not questions about the effectiveness of reinforcers, what is likely to be the issue?

What is likely to be the issue is that too much was expected too soon

Explanation:

Shaping is a method for adding practices to an individual's collection. It is utilized when the objective conduct does not yet exist. In Shaping, what is strengthened is some of the objective conduct. In the event that conducts never happens, we state that it isn't in the individual's collection.

There are rules for Shaping. They are, define the target behavior, reinforce successive approximations of the target behavior and monitor results. By reinforcing the nearest approximation of a particular behavior, the main behavior is shaped up.

Therefore, if a shaping program is not moving forward and there are not questions about the effectiveness of reinforces, it means that pressure was put into it, thereby making the progress slow.

hope this .

r3t40

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)