Your lender cannot, however, charge you a fee to reinstate your credit line once the condition that caused them to freeze or reduce your HELOC no longer exists. For more information see, What You Should Know about Home Equity Lines of Credit (PDF) .our lender cannot, however, charge you a fee to reinstate your credit line once the condition that caused them to freeze or reduce your HELOC no longer exists. For more information see, What You Should Know about Home Equity Lines of Credit (PDF) .
Transform Plate Boundaries are locations where two plates slide past one another. The fracture zone that forms a transform plate boundary is known as a transform fault.Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges.A smaller number connect mid-ocean ridges and subduction zones.he fracture zone that forms a transform plate boundary is known as a transform fault. Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges.
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.