Most evidence of ice is for the last glaciation as it obliterated the evidence of previous glaciations.
Most of Britain was covered in ice although it stopped to the north of London. The evidence is found in the large areas of glacial till, (loose sediment with lots of different sizes and types of stones without any sorting into layers), striations on smooth outcrops of rock caused by ice grinding over it and erratics, (boulders from other parts of the country left isolated in areas where they would not normally be found). Also "U" shaped valleys carved by glaciers and ice-dammed lakes now only shown by former shorelines along valleys.
There is no definitive evidence of current life on Mars. However, scientists have found evidence that suggests Mars may have had conditions conducive to supporting microbial life in the past. Ongoing research and exploration continue to search for signs of past or present life on Mars.
Rock evidence refers to the geological clues that help scientists understand Earth's history, such as how different rock layers were formed, what types of organisms lived in the past, and how the Earth's surface has changed over time. By studying rock evidence, scientists can reconstruct past environments and events that have shaped the planet.
There is currently no definitive evidence of past or present life on Mars. However, scientists have found potential signs that suggest the planet may have once been habitable in the past. Further exploration and research are needed to conclusively determine if life ever existed on Mars.
Their has been evidence on more they one planet that ice and water were their with can led to a form of live . One is mars. But no evidence confirming that live was their has bee yet discovered.
Yes, Mars has water in the form of ice. Scientists have also discovered evidence of liquid water on the surface in the past.
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Scientists use a variety of evidence to study early migration, including genetic analysis of modern and ancient populations, archaeological artifacts, isotopic analyses of human remains to trace diet and geographic origin, and studies of ancient pollen and plant remains to reconstruct past environments. By combining these different lines of evidence, scientists can piece together the story of how humans migrated and settled around the world.
Scientists can see th fossils and the living organisms.
Because there is no credible evidence to indicate they have.
true
There is no definitive evidence of current life on Mars. However, scientists have found evidence that suggests Mars may have had conditions conducive to supporting microbial life in the past. Ongoing research and exploration continue to search for signs of past or present life on Mars.
Scientists who study ice ages are called paleoclimatologists. They examine evidence like ice cores, tree rings, and sediment layers to reconstruct past climates and understand the mechanisms behind ice age cycles.
Rock evidence refers to the geological clues that help scientists understand Earth's history, such as how different rock layers were formed, what types of organisms lived in the past, and how the Earth's surface has changed over time. By studying rock evidence, scientists can reconstruct past environments and events that have shaped the planet.
There is currently no evidence to suggest that people lived on Mars in the past. Scientists are still exploring the possibility of past microbial life on Mars, but there is no known evidence of past human civilization on the planet.
There is currently no definitive evidence of past or present life on Mars. However, scientists have found potential signs that suggest the planet may have once been habitable in the past. Further exploration and research are needed to conclusively determine if life ever existed on Mars.
the difference is that Primary evidence is took from that moment and secondary is a piece of evidence found from the past.
Scientists use the magnetic properties of some minerals as evidence of past changes in Earth's magnetic field. These changes can provide insight into the Earth's geological history, including continental drift and past climates.