A bar graph titled Estimated Battle Casualties during the Normandy Invasion in World War Two. The x-axis is labeled Number of Battle Casualties in Thousands from 0 to 350. The y-axis is labeled Countries with France, Canada, United Kingdom, United States, and Germany. The blue bar is Wounded/Missing. The orange bar is Killed. The yellow bar is Dead and missing. Germany had around 40,000 killed, and over 300,000 wounded and missing. The U S had around 40,000 killed and almost 150,000 wounded and missing. The U K had around 20,000 killed and over 50,000 wounded and missing. Which conclusion can be drawn from the graph? Check all that apply.

The number of German casualties and their previous losses likely made it difficult for Germany to recover.
The Normandy invasion was a significant turning point during the war.
Germany experienced the most casualties during the Normandy invasion.
France had the strongest military during WWII.
Canada and France were key players in the war’s outcome.

the answer is A, B, C

Explanation:

france

Explanation:

9 out of 9

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)