What are the 7 glacial landforms?

Glacier Landforms

  • U-Shaped Valleys, Fjords, and Hanging Valleys. Glaciers carve a set of distinctive, steep-walled, flat-bottomed valleys.
  • Cirques.
  • Nunataks, Arêtes, and Horns.
  • Lateral and Medial Moraines.
  • Terminal and Recessional Moraines.
  • Glacial Till and Glacial Flour.
  • Glacial Erratics.
  • Glacial Striations.

How is a col landform formed?

Cols form when two cirque basins on opposite sides of the mountain erode the arête dividing them. ∎ Cols create saddles or passes over the mountain. Horns are a single pyramidal peak formed when the summit is eroded by cirque basins on all sides.

What is a glacial structure?

Structure. A glacier originates at a location called its glacier head and terminates at its glacier foot, snout, or terminus. Glaciers are broken into zones based on surface snowpack and melt conditions. The ablation zone is the region where there is a net loss in glacier mass.

What are the two main types of glaciers?

There are two main types of glaciers: continental glaciers and alpine glaciers. Latitude, topography, and global and regional climate patterns are important controls on the distribution and size of these glaciers.

How do you identify a glacial landform?

Erosional glacial landforms can be identified on OS maps by the positioning of the contour lines on the map. The OS map below shows part of Snowdonia. Each label identifies a particular glacial landform. Study the contour lines and other map features at each label, and note the differences between them.

What is col in geography?

In geomorphology, a col is the lowest point on a mountain ridge between two peaks. It may also be called a gap. Particularly rugged and forbidding cols in the terrain are usually referred to as notches. They are generally unsuitable as mountain passes, but are occasionally crossed by mule tracks or climbers’ routes.

What is col and arête?

A col occurs as a rounded low point near the center of the ridgeline. NPS Photo/Jacob W. Frank. An arête is a thin, jagged crest that separates—or that once separated—two adjacent glaciers. These rugged ridgelines often look like serrated knives or saw blades, with steep sides and a sharp crest.

What are the 3 types of glaciers?

Glaciers are classifiable in three main groups: (1) glaciers that extend in continuous sheets, moving outward in all directions, are called ice sheets if they are the size of Antarctica or Greenland and ice caps if they are smaller; (2) glaciers confined within a path that directs the ice movement are called mountain …

What is glacier in geography?

A glacier is a large, perennial accumulation of crystalline ice, snow, rock, sediment, and often liquid water that originates on land and moves down slope under the influence of its own weight and gravity.

What are 3 main types of glacial erosion?

Glacial erosion involves the removal and transport of bedrock or sediment by three main processes: quarrying (also known as plucking), abrasion, and melt water erosion.

How are glaciers formed?

Glaciers form on land, and they are made up of fallen snow that gets compressed into ice over many centuries. They move slowly downward from the pull of gravity.

What are the types of glacial landforms?

Kettle lake: Depression,formed by a block of ice separated from the main glacier,in which the lake forms

  • Tarn: A lake formed in a cirque by overdeepening
  • Paternoster lake: A series of lakes in a glacial valley,formed when a stream is dammed by successive recessional moraines left by an advancing or retreating glacier
  • What landforms are formed by glaciers?

    Esker

  • Outwash plains
  • Drumlins
  • How do glaciers shape the land?

    ice cube tray–you only need one ice cube per group

  • sand and small pebbles (just a handful or two; I got mine from my sandbox and my driveway)
  • clay –1 stick per student group
  • paper towels (I just used the school ones)
  • rolling pin (having more than one is very helpful)
  • Glacier movement recording page –1 per student
  • Which landform is created by a glacier?

    Terminal moraines are found at the terminus or the furthest (end) point reached by a glacier.

  • Lateral moraines are found deposited along the sides of the glacier.
  • Medial moraines are found at the junction between two glaciers.