The Ice freezes the landscapes so it can break easily. The landscape can break easily since it becomes ice.
Not quite, if you define the landscape as the rocks that form it. Freezing water within cracks in the rock will split it eventually, but the primary effect is glaciation. Glaciers scour out huge U-section valleys and deposit the spoil as moraines or various kinds, erratics, sheets of till, outwash plains and on the sea-bed, huge sediment fans and drop-stones. They also leave assorted traces of their passing such as striations and plucking.
The moraines can also create natural dams ponding water to create lakes that may eventually drain as the river incises the moraine but still leaves evidence of its existence as old shore-lines.
Ice-dammed lakes at altitude can overflow through cols, cutting distinct notches in the ridge.
In slightly less icy conditions, snow can create nivation hollows in the flanks of Chalk hills: the chalk is slowly dissolved by meltwater under remnant snow-patches usually on the North-facing (in Northern hemisphere) flanks.
The changes of sea-levels consequent on glacial and interstadial periods leave tell-tales such as drowned river valleys and raised beaches.
Following ice-retreat, isostatic rebound of an area of continental crust that had been depressed by the sheer weight of a deep ice-cover can locally activate faults, creating irregular profiles in rock surfaces and ridges, with accompanying earthquakes. Those in Norway continued into historical times but the rebound there has more or less ended.
As a handle on the weight of an ice-cover on the landscape, that over Scandinavia in the last glaciation reached 3km thick, but if we take a mean cover of only 2km, and the density of ice as 0.9 Tonne/m3, that gives a mass of
0.9 x 2 x 103 x 103 x 103 Tonnes per square kilometre,
= 1.8 x 109 T/km2
The area of the Scandinavian Peninsula + that of Denmark is about 820 000 sq.km. so an ice-sheet of mean thickness 2km over that lot will weigh:
1.8 x 8.2 x 109 x 105 Tonnes
= 1.48 x 1015 tonnes.
Or if you prefer, getting on for fifteen million million Tonnes of ice.
No wonder that part of the European Plate was depressed significantly.
When the ice age ended, the land once covered with ice was covered with newly exposed land and water from melting ice sheets. This led to the formation of new landscapes and ecosystems as vegetation began to grow in the previously glaciated areas.
After the last ice age, known as the Pleistocene Epoch, geologists believe that the Earth warmed, causing the ice to melt and the glaciers to retreat. This led to rising sea levels and the formation of many of the landscapes and features we see today. Additionally, it triggered the end of the ice age and the beginning of the current epoch, the Holocene.
The Ice Age had significant impacts on Earth's geography and climate, including the formation of glaciers, ice sheets, and the reshaping of landscapes. It also led to lower sea levels as water was locked up in ice, influencing ocean currents and affecting global climates. Additionally, the Ice Age had a profound effect on the distribution and evolution of plant and animal species.
Geologists and glaciologists study the Ice Age to understand past climate patterns, changes in Earth's surface, and the effects of ice sheets on landscapes. This research helps scientists predict future climate changes and understand how glaciers and ice sheets impact global sea levels.
The ice age had a profound impact on the planet, causing significant changes in climate, landscapes, and ecosystems. It led to the expansion of ice sheets, glaciers, and polar ice caps, lowering global sea levels and creating new land bridges. Many species adapted to the changing conditions, while others went extinct. The ice age also influenced human evolution and migration patterns.
because everything would freeze and turn to ice
When the ice age ended, the land once covered with ice was covered with newly exposed land and water from melting ice sheets. This led to the formation of new landscapes and ecosystems as vegetation began to grow in the previously glaciated areas.
it would get colder
By and large it pushed them further south.
it's too clod for people to live
After the last ice age, known as the Pleistocene Epoch, geologists believe that the Earth warmed, causing the ice to melt and the glaciers to retreat. This led to rising sea levels and the formation of many of the landscapes and features we see today. Additionally, it triggered the end of the ice age and the beginning of the current epoch, the Holocene.
The ice age affected living things because it caused living things to extinct.Also it made it hard for living things to survive.
The Ice Age had significant impacts on Earth's geography and climate, including the formation of glaciers, ice sheets, and the reshaping of landscapes. It also led to lower sea levels as water was locked up in ice, influencing ocean currents and affecting global climates. Additionally, the Ice Age had a profound effect on the distribution and evolution of plant and animal species.
Geologists and glaciologists study the Ice Age to understand past climate patterns, changes in Earth's surface, and the effects of ice sheets on landscapes. This research helps scientists predict future climate changes and understand how glaciers and ice sheets impact global sea levels.
Yes
The Ice Age Trail was established in 1958 by Ray Zillmer, a conservationist and writer from Wisconsin. It was created to showcase the unique landscapes created by the last glacier in Wisconsin, known as the Wisconsin glaciation.
The ice age had a profound impact on the planet, causing significant changes in climate, landscapes, and ecosystems. It led to the expansion of ice sheets, glaciers, and polar ice caps, lowering global sea levels and creating new land bridges. Many species adapted to the changing conditions, while others went extinct. The ice age also influenced human evolution and migration patterns.