Article 6 states that the U.S. Constitution is the highest law in the US
Explanation: On the Western Front, the war was fought by soldiers in trenches. Trenches were long, narrow ditches dug into the ground where soldiers lived. They were very muddy, uncomfortable and the toilets overflowed. These conditions caused some soldiers to develop medical problems such as trench foot.
Soldiers in the First World War did not spend the whole of the time in the trenches. The British Army worked on a 16 day timetable. Each soldier usually spent eight days in the front line and four days in the reserve trench. Another four days were spent in a rest camp that was built a few miles away from the fighting.
Tensions between Japan and the United States grew in the late 1930s as a result of Japan's continued expansion into China and its joining of the Axis.
<h3>Why did Japan and the United States become tense in the late 1930s?</h3>
When the Japanese bombed the USS Panay as it was transporting American citizens out of Nanjing, tensions with Japan grew. Attack by Japan on China led to disagreements between Japan and the US in the late 1930s.
Therefore, we can conclude that the events that led to rising tensions between Japan and the United States in the late 1930s were Japan's continued expansion into China.
Therefore, options B and D are correct.
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If we start to travel from the Mississippi River westwards to the Pacific Coast, than the starting point is a lowland, vast one, as we continue to go towards the west we will encounter high mountains, the Rocky Mountains more specifically, and the elevation will go up to 4,400 meters above sea level, than we will go down, elevation wise, to the high plateaus and will be on elevations between 1,000 and 2,000 meters, and after we go up again to almost 4,400 meters as we cross the Cascade Mountains. After the Cascades we go gradually downwards towards the lowlands, where we will first go a bit bellow sea level, and than little up in the lowlands along the Pacific Coast, and at the end reach a point of zero elevation.
