Analyze the influence of ideas about gender on the reign of elizabeth i and explain how elizabeth responded to these ideas.

Even though there was an unmarried woman on the throne in Elizabethan England, the roles of women in society were very limited. Here are some examples:

All in all,  women had more freedom in the Elizabethan period than they had had previously.  It was thought men and women could do anything and be anything they wanted to be, that their capacity for knowledge was limitless. Thus, noble women, as well as men, were given an impressive education in the classics, mathematics, and all other academic subjects of the day. Elizabeth being on the throne also encouraged noble men to educate their daughters, as they did not want them to look dim in the presence of their very intelligent and highly educated queen.

Paradojically, the ones who suffered most were women, such as que Queen, who didn't want to marry.

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explanation:

literally the answer is aa. not kidding. aa is a group.

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)