In this economic system, people completely control supply and demand, and the factors of production. Options: Traditional, Command, Market, or Mixed

Market

Explanation:

Here are a brief difference between the four systems.

Market : People/the Private sector control the supply/demand along with factors of production

Command : Government control the supply/demand along with factors of production

Mixed : Both the Government and the people control the supply/demand along with factors of production

Traditional : Traditions control the supply/demand along with factors of production

Under the Full market economy, people have the full freedom to determine the outcome in the market. The resources such as land, materials, and   skills will be privately owned and the government has no influence within the market.

One advantage of this system is that the winners of the competition in the market will accumulate high amount of wealth in relatively fast period. But on the downside, lack government involvement often turns the competition dirty and those who hurt other individuals in the process wouldn't receive any repercussions.

this is a pretty broad question and can be a pretty lengthy answer. since 1900, women have gained a lot more rights and have become active in the workforce. with women being in the workforce, men play a larger role in family life. many family tasks are shared between men and women, whereas, women used to be the sole family caretakers.

that should get you started at least.

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)