A mound, ridge, or other distint accumulation of unsorted, unstratified glacial drift, deposited chiefly by direct action of glacier ice The geomorphic name for a landform composed mainly of till that has been deposited by either a living or extinct glacier
Deposits of rocks, boulders, gravel and sand (called glacial drift) left behind by glaciers as they melted Terminal moraines are at the end of a glacier
a mass of earth or pieces of rock moved along by a glacier and left in a line at the bottom of it. Accumulation of rock debris (till) carried or deposited by a glacier. The material may range in size from blocks or boulders to sand and clay, is unstratified when dropped by the glacier, and shows no sorting or bedding. Several kinds of moraines are recognized, depending on how they are deposited by the glacier; these include lateral moraines along the margins of the glacier and terminal moraines at its leading edge
The rocks and soil carried and deposited by a glacier An "end moraine," either a ridge or low hill running perpendicular to the direction of ice movement, forms at the end of a glacier when the ice is melting
An accumulation of unsorted unstratified glacial drift mainly till, deposited by glacial ice Drift deposited in the flanks of a valley glacier form a lateral moraine Glacial deposits which have accumulated at the front of a glacier form a terminal moraine Deposits of drift which have been dragged along beneath the ice form ground moraine
A ridge formed by the unsorted gravel, sand and boulders carried along by the glacier and deposited at the outer edge, or front, of the glacier Some are only 10' high while others rise 250' to 300' Moraines define the basic route of the Trail, so they can be found in many places
When a glacier moves forward, its weight and movement causes dirt, rocks and debris to be literally bulldozed along in front of it Then as the glacier recedes, it leaves behind piles known as moraines Lateral moraines flank the sides of glaciers while a terminal moraine marks the farthest glacial advance
landforms composed of unsorted materials deposited by glaciers They can cover broad geographic areas of millions of acres Topography can vary from nearly level "till" plains to rough end moraine landscapes composed of steep dry ridges interspersed with deep kettle holes These glacial "kettles" are frequent locations for lakes and wetlands