What options are available to individuals when their nation does not live up to its ideals? how did susan b. anthony confront the differences she experienced between ideals and reality in the united states and work for change?

Many campaigns and associations, staging rally and giving speeches are the options which are left in order to make the country live up to the ideals and Susan B Anthony was a well-known abolitionist who played a pivotal role in the women suffrage movement.

Explanation:

Born in the Quaker family, Elizabeth worked for the enfranchisement rights of women. She also protested against slavery and collected anti-slavery supplications at the time of her early adolescence. She along with her counterpart Elizabeth Cady Stanton worked for the women reforms.

She also was the organizer of a team that worked for abolition of slavery and women suffrage rights. She also published an editorial and journalistic broadsheet which highlighted the importance of women being granted equal rights. She also fought for the equal wages for both the genders in the society.  

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)

answer; presidential election years;