Colonization .
Glacial advance and retreat is determined by the balance between the accumulation of snow and the removal of ice by sublimation, melting, and calving (ablation). When the rate of ablation below the snowline equal
Cape Cod is made up of glacial moraines and outwash left from the retreat of the Laurentide Ice Sheet during the last ice age.
Yes - and re-form - but over geological time measured in 1000s or 10s of 1000s of years. (The last glacial retreat of the present Ice Age is reckoned to have started about 12000 years ago.)
Yes and no. A lot of the material that forms the San Juan islands are leftovers from glacial action. Material abundant on the islands that the glaciers brought includes most of the sand and gravel as well as 'erratic' boulders. Earlier features were also shaped and changed by the glaciers, but there are indeed rock formations in the San Juans that predate the Pleistocene (the most recent 20 or so glacial advances) glaciations. An interesting way to think about glacial effects (bringing material and changing the shapes and surface formations of material that was already present) to consider the southward advance and northward retreat of the glaciers.
An increase in weight to the crust due to thickening from plate collisions, build up of sediments, or glacial override will necessitate a corresponding downward movement into the ductile asthenosphere in an attempt to achieve gravitational equilibrium as it applies to the difference in buoyancy between the different Earth layers.. As this weight is removed through erosion or glacial retreat, the crust will gradually rebound to achieve equilibrium.
pioneer species
The first organism in barren landscape is pioneer species.
Pioneer species
The first organism in barren landscape is pioneer species.
The first organism in barren landscape is pioneer species.
The first organism in barren landscape is pioneer species.
The first organism in barren landscape is pioneer species.
Their seed dispersal rate.
A drumlin is a land-form from glacial deposition, which was once eroded. It is formed both by erosion and deposition. A drumlin is formed when moraine deposited by a retreating glacier is subsequently reshaped by the returning glacier the following year or after the glacial interval with caused the glacier to retreat in the first place.
Striations are "scratches" left in bedrock by glaciers. A small particle of rock, generally pebble sized or smaller, becomes entrained in the base of the glacier and dragged along the surface of the bedrock. These can often be seen on hard bedrock surfaces that are resistant to subsequent weathering after the retreat of the glacier. Erratics are large rocks that are found out of place in the landscape, i.e. not near where they were formed. They are removed from their provenance by a glacier and transported away, before being deposited in a different part or the landscape when the glacier melts.
Glacial advance and retreat is determined by the balance between the accumulation of snow and the removal of ice by sublimation, melting, and calving (ablation). When the rate of ablation below the snowline equal
Glaciation refers to climatic episode in which much of the Earth becomes covered with glaciers, reaches a peak in glacial coverage, and then ends with the retreat of glaciers.