{"thcode":62,"term":{"code":"GC-128","name":"Recessional Moraine","parent":"GC-122","scope":"Geoform Type: An end or lateral moraine, built during a temporary?but significant?halt in the final retreat of a glacier. May also refer to a moraine built during a minor re-advance of the ice front during a period of general recession."},"uf":[],"bt":[{"code":"GC-122","name":"Moraine","parent":"GC-011","scope":"Geoform: A mound, ridge, or other distinct accumulation of unsorted, unstratified, glacial drift (predominantly till) that is deposited chiefly by direct action of glacier ice."},{"code":"GC-011","name":"Geologic","parent":"GC-C052","scope":"Geoform Origin: Geologic geoforms are formed by the abiotic processes of uplift, erosion, volcanism, deposition, fluid seepage, and material movement. ..."},{"code":"GC-C052","name":"Geoform (levels 1 and 2 subcomponents)","parent":"GC-C005","scope":null},{"code":"GC-C005","name":"Geoform","parent":"root","scope":null},{"code":"root","name":"CMECS","parent":null,"scope":"Coastal and Marine Ecological Classification Standard: Category terms encompassing waters from the head of tide or inland incursion of ocean salinity to the splash zone of the coasts to the deepest portions of the oceans and the deep waters of the Great Lakes."}],"nt":[],"rt":[]}