GEOL 1304 Lecture Notes - Lecture 2: Maunder Minimum, Northern Hemisphere, Ontogeny
Document Summary
They form as ooding periodically down payment sediment along the streamside orbit , next to the camber. What was the rhythm of the pleistocene epoch. Long glacial microscope stage alternating with short interglacial stages. Low sunspot activity is generally associated with reduced solar doe output, and therefore some paleoclimatologists hav suggested that it may have contributed to climate cooling on earth. A new monikor referring to the recent epoch millenia of earthly concern history when humans have gained an increasing control of earth"s natural systems. When summers are cool and wintertime are warm in the heights latitudes. The last eleven ,000 class of earth story following the pleistocenewhen climates have been heater and more stable. A time in earth history that began about 2. 5 million old age ago and continued to about 11,000 years ago. It is marked by cold, ice age conditions, with glaciers alternatively advancing and retreating in senior high school latitude and high elevation web site .
