I think it's called Tanakh. Sorry if I'm wrong!
Who led the Solidarity movement in Poland was Lech Walesa, an outspoken electrician. He gave voice to the workers demands for the legislation of independent labour unions
I don't know what you're referring to, and don't think it was much different than defending against a number of well-armed, trained, and disciplined troops. If anything, the German Army in WWII was a really tough bunch.
<span>Two things may show some differences, however, at least in the war in the Pacific. Japanese were far more willing to fight to the last man, rather than surrender, whereas most German units would stick the white flag up when it was clear that they had lost the engagement, and had no retreat. In "island hopping", the US also took on extremely fortified Japanese positions that were not destroyed with even massive bombing and naval fire</span>
<span><span><span>The crust: low density silicate rock, 5-70 km thick. There are two distinct types of crust.<span><span>Continental crust is variable in thickness and composition. Thickness ranges from 5-70 km. The composition ranges from mafic to felsic.</span><span>Oceanic crust is uniform in thickness and composition. It is 5-6 km thick and is mafic in composition.</span><span>The differences in thickness and density between continental and oceanic are responsible for the existence of ocean basins due to isostatic balance as the crust floats on the more dense mantle.</span></span></span><span>The mantle: high density, ultramafic silicate rock which can flow when subjected to long duration stresses. The mantle is over 2900 km thick and makes up over 80% of the volume of the Earth. The mantle is not molten!</span></span><span>The core: iron and nickel, liquid outer region with a solid center. The core is just over half the diameter of the Earth.</span></span>
Dormant. a volcano that is active but not erupting and will erupt again
