Lisa is a single parent who works full time as a firefighter. today, when her shift at the fire station ends, lisa will prepare dinner for her family, oversee her children’s homework, give her youngest child a bath, clean the kitchen, and do a load of laundry. what term best describes the work that lisa will be doing?

The correct answer is second shift

Explanation: Lisa is working in a second shift how most of the women do. In this case Lisa is a single mom but in many cases in our society women have to work hard for have a job career and a "work" as a mother.

Women for many years had to live for their houses, taking care of the husband and their children. And even now women have to fight to have a life outside of their houses.

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)