Sea levels rose over 300 feet
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.
A land bridge connected Siberia and Alaska.
Geologists believe that during the last ice age, large continental ice sheets expanded and covered much of North America, Europe, and Asia. This period was marked by cycles of advance and retreat of these ice sheets, shaping the landscape through processes like erosion and deposition. The last ice age ended around 11,700 years ago as the Earth's climate began to warm, causing the ice sheets to melt and sea levels to rise.
A land bridge connected Siberia and Alaska
Geologists believe that during the last ice age, global temperatures dropped, causing glaciers to advance and covering much of the planet with ice. This period of extensive glaciation significantly altered landscapes, ocean levels, and climate patterns. The ice age ended about 11,700 years ago as temperatures began to rise, leading to the retreat of glaciers and the beginning of the current interglacial period.
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.
A land bridge connected Siberia and Alaska.
Geologists believe that during the last ice age, large continental ice sheets expanded and covered much of North America, Europe, and Asia. This period was marked by cycles of advance and retreat of these ice sheets, shaping the landscape through processes like erosion and deposition. The last ice age ended around 11,700 years ago as the Earth's climate began to warm, causing the ice sheets to melt and sea levels to rise.
A land bridge connected Siberia and Alaska
Geologists believe that during the last ice age, global temperatures dropped, causing glaciers to advance and covering much of the planet with ice. This period of extensive glaciation significantly altered landscapes, ocean levels, and climate patterns. The ice age ended about 11,700 years ago as temperatures began to rise, leading to the retreat of glaciers and the beginning of the current interglacial period.
A land bridge connected Siberia and Alaska.
Many geologists consider what you call the "last ice age" to be the last glacial of the present Ice Age, with the ice retreat starting only about 10-12ka. There was no mass extinction. A good many species did migrate or disappear altogther as the ice retreated, but in no way was it a mass extinction.
The last ice age is commonly placed in the Quaternary Period, specifically within the Pleistocene Epoch. This period is characterized by multiple glaciations and the presence of large ice sheets in the Northern Hemisphere.
Geologists estimate that the Earth is approximately 4.54 billion years old based on radiometric dating of rocks and meteorites. This age is determined by analyzing the decay of radioactive elements in these materials.
they tell the absoute age of rcoks which they occur
Geologists use a method called radiometric dating to determine the age of fossils. This technique measures the decay of radioactive isotopes in the fossil to calculate its age. By analyzing the ratio of parent isotopes to daughter isotopes present, geologists can estimate the age of the fossil.
Geologists can measure the abundance of certain radioactive isotopes, such as carbon-14 or uranium-lead, in a specimen to calculate its age. By comparing the ratio of parent isotopes to daughter isotopes in a sample, geologists can determine the age of rocks, fossils, or other geological specimens. This process is known as radiometric dating.