Select the range of data that you want to convert. On the Data tab, in the Data Tools group, click Text to Columns. In Step 1 of the Convert Text to Columns Wizard, click Delimited, and then click Next.In Step 2, select the Space check box, and then clear the other check boxes under Delimiters.The Data preview box shows the first and last names in two separate columns. Click Next.n Step 1 of the Convert Text to Columns Wizard, click Delimited, and then click Next. In Step 2, select the Space check box, and then clear the other check boxes under Delimiters. The Data preview box shows the first and last names in two separate columns. Click Next.
Destruction (recycling) of crust takes place along convergent Divergent Margins boundaries where plates are moving toward each other, and sometimes one plate sinks (is subducted) beneath another. The location where the sinking of a plate occurs is called a subduction zone. A transform boundary is where plates slide past each other with no creation or destruction of lithosphere. Plate Margin Examples There are three general types of plate boundaries: divergent, convergent, and transform. Each general type has multiple âspeciesâ: divergent boundaries can be spreading ocean ridges or continental rift zones; convergent boundaries can occur between two continental plates.
1 First, in most subduction zones, large earthquakes occur at the interface between the two plates, at depths ranging from the earth's surface down to about 600 km. 2  This region, called the Benioff Zone , is used to locate the subducting plate, as shown for the case of Japan on the left-hand side of Figure 2. Second, in most subduction zones, there is an inland volcanic arc running parallel to the trench. 2  But in southern Mexico, the volcanic arc bends away from the trench, at about a 15Â° angle (see Figure 1). 3  Finally, in most subduction zones, giant earthquakes occur every few hundred years or so.