Príklady glacier

• A glacier is like a river of ice. 

• Alaska has many mountains and glaciers. 

• As the weather got warmer, the glacier started to melt. 

• Glaciers hold about 69 percent of the Earth’s fresh water. 

• Global warming is causing glaciers to melt. 

• Most glaciers move about 0.3 meters a day but can move as fast as 31 meters in one day! 

• Some glaciers are so small you can walk over them in one or two hours. 

• The Matanuska glacier is one of the most beautiful. 

• The biggest glacier in the world, the Lambert Glacier in Antarctica, is more than 40 kilometers wide and more than 400 kilometers long! 

• Then the slow-moving glaciers are going to change into fast-moving rivers again. 

• There are more than 100,000 glaciers in Alaska. 

• This glacier in Alaska is a river of ice. 

• Ushuaia has lakes, forests, glaciers, beautiful rainbows, and the Andes Mountains. 

• We have to hope that the glaciers don’t melt. 

• When a glacier meets the ocean, parts of it break off. 

• Nearly 50% of the shoreline is dominated by the calving ice fronts of the large outlet glaciers.

• Non-scientists regularly assisted in scientific projects, and provided one or more of the three men usually required for safety whenever scientists travelled over the glaciers.

• It is the biological equivalent of the retreating glaciers and ice shelves, and yet to unravel its complexities can take a lifetime's work.

• Thus, this same three-pulse pattern can be seen from tree rings, glacier advances, and last dates on buildings and monuments in the lowlands.

• Is the basal ice of a temperate glacier at the pressure melting point?

• Thus, the evaluation of possible error sources is still a challenging problem in glacier monitoring.

• This is a location rich in wild life because there is upwelling of nutrient rich water immediately at the glacier front.

• Many potential applications follow from the ability to map the surface of the glacier in such high detail.

• You will rarely see better quality photographs of glaciers in terms of sharpness, contrast and composition.

• Investigations of the form and flow of ice sheets and glaciers using radio-echo sounding.

• Field and his co-workers visited many glaciers and recorded (using photography) for the first time how they had receded.

• Application of image crosscorrelation to the measurement of glacier velocity using satellite image data.

• For a high number of data sets, both topography and glacier flow can be estimated with high accuracy.

• The book mainly covers the physical environment such as surface processes (glaciers, frost action, rivers) and ice- ocean interactions.

• These glaciers are described in a single chapter.