After the passage of the North American Free Trade Agreement, which made it less expensive to import goods from Mexico, workers in some industries found their factories being relocated to Mexico to take advantage of lower labor costs. These workers experienced what type of unemployment?

The correct answer is Structural

Structural unemployment is that generated by the introduction of new technologies or systems and processes aimed at reducing costs. These new elements affect the sectors of the economy of a country (industry, commerce and services), causing dismissal, generally, in great quantity.

The globalization of the economy, which gained strength since the 1970s, played a major role in increasing structural unemployment worldwide. Economic globalization has increased competitiveness at the international level, mainly through foreign trade, making companies look for ways to reduce production, marketing and transportation costs. Among these forms, we can mention the main causes of structural unemployment: adoption of new technologies and reduced cost administrative and productive systems (both with a decrease in labor).

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explanation:

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)