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.
1 A single plate may be part oceanic and part continental. 2  In that case, the boundary between ocean crust and continental crust is not a plate boundary. 3  The mobile part of the mantle under the lithosphere is called the asthenosphere. An oceanic trench forms offshore, and a chain of volcanic mountains forms just inland of the coast. 2  This type of boundary between oceanic crust and continental crust is called an active continental margin since it is a plate boundary. 3  At other convergent boundaries, oceanic plate meets other oceanic plate.