Kame and Kettle terrain is correct answer.
A kame is a stratified geomorphologic feature which is created by deposition action of glacier meltwater, an irregularly shaped hill or mound composed of sand, gravel, and till, commonly associated with end moraine. A kame may occur as an isolated hill but in general each kame is one mound in a low-lying terrain of many hammocks, terraces, ridges, and hollows.
Kettles are depressions in the outwash plains, which formed due to the melting of large ice blocks and this is referred to as kame and kettle topography.
Kame and kettle topography is an indicator of a high-discharge supraglacial and englacial drainage system of a glacier in the final stages of melt, and large quantities of glacially derived debris associated with meltwater.
Question 192 (1 point) Salt mining occurs in Windsor, Nova Scotia. The area is marked by...
Question 191 (1 point) The Rocky Mountains in western Canada are the result of what type of plate boundary? A convergent margin Tensional stress / rifting A strike-slip boundary A passive margin Question 192 (1 point) Salt mining occurs in Windsor, Nova Scotia. The area is marked by pitted, hilly terrain, and sinkholes. What kind of landscape is this? Karst
Question 193 (1 point) In 2005, Geologist Bruce Wilkinson said that humans in the modern era are times more active in shaping landscape than natural processes. 1.5 10 100 20 Question 194 (1 point) In Tuktoyaktuk, Northwest Territories, sandbags and concrete blocks are being placed along the shoreline to minimize the effects of shoreline erosion. Why is this not a good long-term solution? A. Permafrost melt will destabilize the barriers