John Lewis’s Speech Guiding Questions NOTE: SNCC stands for the "Student Nonviolent Coordinating Committee, a civil rights organization" that played a critical role in the Freedom Rides of 1961 and the voter registration efforts of the 1960s. 1. Who wrote this document? Where was it delivered? Who was the audience? (You might need to look up the March on Washington to answer this question). 2. When was the speech delivered? Is this before or after Kennedy’s speech? 3. According to Lewis, what was the problem with Civil Rights Act? Explain.

1. Who wrote this document?

Many members of SNCC helped write the document

Where was it delivered?

It was delivered in Lincoln memorial in Washington DC.

Who was the audience?

The audience was an estimated 250,000 civil rights marchers gathered around the Lincoln memorial in Washington.

2. When was the speech delivered?

The speech was delivered on August 28, 1963.

Is this before or after Kennedy’s speech? It was after Kennedy's speech on civil rights in June 11, 1963.

3. According to Lewis, what was the problem with Civil Rights Act?

The civil rights Act was Partial

Explanation

The Civil Rights Act did not protect the black men as well as young children and old women from police brutality, arrest on trumped up charges and right to engage in peaceful protest.

The voting section of the act did not make provision for thousands of black people who want to vote.

The act also did not provide for better wages and working conditions for blacks

your answer should be c, it seems to be the only one that makes sense. mark me branliest : )

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)