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.
There are three main types of plate boundary: divergent, convergent and transform. Plates move away from one another at divergent boundaries. This happens at mid-ocean ridges. Plates move towards one another at convergent boundaries; one plate is forced below another in a process called subduction.Earthquakes and composite volcanoes are common at this type of boundary. Convergent boundaries are areas where plates move toward each other and collide. 2  These are also known as compressional or destructive boundaries. 3  Subduction zones occur where an oceanic plate meets a continental plate and is pushed underneath it. 4  Subduction zones are marked by oceanic trenches.