*
    Peter Knight's Photos of Landscapes and
                   Glaciers
              (Keele University)
Niche glaciers

The smallest scale of
glaciation: Niche glaciers
and ice aprons in the Grand
Tetons, Wyoming, USA.
Small glaciers such as these
are often the most sensitive
to local climate change.
The summit ice cap of the volcano,
                Cotopaxi, Ecuador




The ice cap extends further on one side of the mountain. The side
of the mountain facing the moisture-bearing winds has higher
snowfall and hence more extensive glaciation. The deep channels
carved by meltwater and by volcanic mudflows (lahars) caused by
melting of snow and ice during eruptions.
VALLEY GLACIER




RUTH GLACIER, MOUNT MC KINLEY
Regal and Nizina Glaciers, Alaska
ICE SHEET



A




                     B
    West Greenland
August 67N

            Greenland



April 67N

Greenland
Snout or
                  Ice Front




Russell Glacier
  Ice Front
*




CREVASSE
             ICE CAVE

 SUPRAGLACIAL STREAM
Subglacial
            stream




Ice cliff
1954    Franz Josef Glacier, located in New Zealand      1958




1960    retreated dramatically in the twentieth century    1964
*
              Clean ice sliding on bedrock




Ice scoured
topography
MOUNT MC KINLEY


               A

               B        C




Athabasca
 Glacier
Striations




Erratics
1       2
                    1




        3
                4
1
                        1
Lateral and terminal
                moraines, Bylot
                Island, Canada




End moraine,
Bylot Island,
  Canada
Moraines of
            different ages   *




Ice Front
PUSH MORAINE
Proglacial
  zone




             Ice-dammed
                 lake
OUTWASH
                   PLAINS




BRAIDED CHANNEL
RAISED BEACH, W. SCOTLAND

Glacial landforms

  • 1.
    * Peter Knight's Photos of Landscapes and Glaciers (Keele University)
  • 2.
    Niche glaciers The smallestscale of glaciation: Niche glaciers and ice aprons in the Grand Tetons, Wyoming, USA. Small glaciers such as these are often the most sensitive to local climate change.
  • 3.
    The summit icecap of the volcano, Cotopaxi, Ecuador The ice cap extends further on one side of the mountain. The side of the mountain facing the moisture-bearing winds has higher snowfall and hence more extensive glaciation. The deep channels carved by meltwater and by volcanic mudflows (lahars) caused by melting of snow and ice during eruptions.
  • 4.
  • 5.
    Regal and NizinaGlaciers, Alaska
  • 6.
    ICE SHEET A B West Greenland
  • 7.
    August 67N Greenland April 67N Greenland
  • 8.
    Snout or Ice Front Russell Glacier Ice Front
  • 9.
    * CREVASSE ICE CAVE SUPRAGLACIAL STREAM
  • 10.
    Subglacial stream Ice cliff
  • 11.
    1954 Franz Josef Glacier, located in New Zealand 1958 1960 retreated dramatically in the twentieth century 1964
  • 12.
    * Clean ice sliding on bedrock Ice scoured topography
  • 13.
    MOUNT MC KINLEY A B C Athabasca Glacier
  • 14.
  • 15.
    1 2 1 3 4 1 1
  • 16.
    Lateral and terminal moraines, Bylot Island, Canada End moraine, Bylot Island, Canada
  • 17.
    Moraines of different ages * Ice Front
  • 18.
  • 19.
    Proglacial zone Ice-dammed lake
  • 20.
    OUTWASH PLAINS BRAIDED CHANNEL
  • 21.