On the second floor, you may search the bookshelves next to the stairs to obtain The History of the Kinshra, a book chronicling the foundation of the Kinshra and the kingdom of Asgarnia. Next, speak to Lieutenant Graves in the hallway, who will inform you that the witch has escaped and the operation has been sabotaged.
The North American plate also serves to illustrate this difference. The west coast is the active margin, and is the location of earthquakes, volcanoes, and mountains. The Eastern Seaboard is a passive margin, as is the Gulf Coast. These are the low-relief areas of our continent, and are the locations of such exciting places as New Jersey, the Barrier Islands, the swamps of Florida, and the Mississippi delta.
Constructive or Divergent Margins. At these types of plate margins two plates are moving apart (DIVERGE) from each other in opposite directions. Convection currents moving in opposite directions (caused by the intense heat of the Earth's interior) in the mantle move two plates apart.rocesses: seismicity and vulcanicity. Associated landforms: young fold mountains, rift valleys, ocean ridges, deep sea trenches and island arcs. . Volcanoes and earthquakes mainly occur along plate boundaries where magma can escape from the earth s mantle or where stresses build up between 2 plates rubbing together.