When and how did industrialization spread to the european continent and the united states? what factors in those countries tended to support industry?

Industrialization spread to Europe around the start of the 19th century and to The United States after 1850's. The factors in those countries that supported industry was land, resources, labor and capital.

Explanation:

The industrialization started in Great Britain around 1760s and started to spread to Europe in the first half of the 1800's, firstly to countries such as Belgium, Germany and France. Later in the century it spread to The United States as textile machines. The main factors that played role in supporting the industry in the countries that were affected by the spread of the industrial revolution were land, resources, labor and capital. These countries had the necessary land for the factories and production. They also had the resources to be used in the industrialization process. Since there were no factories, the employment rate's were low which meant there were a lot of people who could work in these factories. These advancements also encouraged immigration which provided extra labor. The government and entrepreneurs were supplying the capital for building the factories and railroads which was one of the most important factors of this process.

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)

the answer would be c. sediment buildup on continental slope

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