The war between Britain and France was virtually over. King Edward VII visited France in 1903 and won the hearts of the French people by speaking great French and acting graciously everywhere he went. He even gave a famous actress gallant compliments in her native tongue (this kind of thing goes a long way in France). The Anglo-French Entente was ratified in less than a year. The hatred of Edward by Kaiser Wilhelm was another cause (who was his uncle). In truth, the English had already proposed an equivalent entente to Germany in 1899 and 1901, but the Germans had rejected it because they thought it was a ruse. At a dinner with 300 guests in Berlin, the Kaiser made a public statement "He is the devil! You simply cannot comprehend what a Satan he is!" He was irate that he couldn't intimidate or win Edward over, envious of his fame, and worried about what he thought were English designs to "encircle" Germany. But it was for the Belgians, not the French, that Britain allied with France in World War I. Britain had committed to defend Belgium in return for its Continent-wide neutrality. The British intervened to defend them when Germany invaded Belgium without cause (Belgium had done nothing to deserve it) and started massacring civilians.
He gave a speech praising men who refused to serve in the military.
<span>B)Lyndon Baines Johnson was sworn in as the President of the United States. </span>
The correct answer is - True.
The transform plate boundaries are the boundaries where the tectonic plates are not moving away, or moving towards one another, but instead they are sliding past each other.
At this type of boundaries, a fracture zone is forming, which causes the formation of a transform faults. Most of the transform faults can be found in the ocean basins and they are connecting the offsets of the mid-ocean ridges.
As the plates slide past one another, the boundary between them exist no more as their movement has set them apart from each other. The transform boundary than can continue as a new transform boundary, as a divergent plate boundary, or as subduction zone.
