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.
pioneer species
pioneer species
Their seed dispersal rate.
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.
A glacial lake is a lake with origins in a melted glacier. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
It hasn't ended. We're in a warm phase. After the last glacial phase ended some 10-12000 years BP: Retreat of ice cover to higher latitudes and altitudes. Rise in sea-level - forming among other things the English Channel in what had been a river valley. Temperate climate zones moving Polewards.
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.
Colonization .
pioneer species
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.
The gradual melting of glaciers during the last Ice Age, which ended around 11,700 years ago, played a significant role in flattening the interior lowlands by depositing sediments and reshaping the landscape through processes like erosion and glacial retreat.
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