Holocene

Massachusetts ROCKS
Massachusetts ROCKS
Massachusetts ROCKS! APES F Geology 120,000 years ago ice began to form at a rapid pace in northern Canada(Grette, www.biomass.umass.edu). This sheet quickly (on a geologic scale) swept down the eastern seaboard and engulfed the northeast down to present day Long Island, New York in a sheet of solid ice. This icesheet later in history became known as the Laurentide icesheet, named after the region in Canada in which it made its descent(Oldale, http://pubs.usgs.gov). Little did anything know b
Twenty thousand years ago during the time of the last ice age period m
Twenty thousand years ago during the time of the last ice age period m
Twenty thousand years ago during the time of the last ice age period, many colossal mammals roamed North America. They survived during the times when much of the earth was covered by immense large bodies of ice that buried forests, fields, and mountains, but rapidly became extinct after the ice began to retreat and melt. Since then the human race has introduced many different theories to explain the extinction of these large mammals. One theory stands above all and explains the truth of this my
Industry and the effects of climate in Italy
Industry and the effects of climate in Italy
Industry and the effects of climate in Italy Industry The structure of industrial production and the service industries is characterized by the prevalence of smarkforce, 30% beingll and medium-sized companies (94% and 5.6% according to 100 workers) thoug981 data), employing, however, only 70% of the workforce, 30% being monopolized by large c ompanies (more than 100 workers) though these comprise only 0.4% of the total. This means that companies are widely dispersed over the whole country, obvio
The Environmental Hierarchy
The Environmental Hierarchy
The Environmental Hierarchy Logan Horrocks A00372572 December 2nd 2015 Sand dunes are dynamic systems of accumulated aeolian sediment. These systems exist in cyclical periods of stability and instability (Hugenholtz and Wolfe, 2005). Active sand dunes are open systems, they migrate and experience a net loss or gain of sediment. Under the proper circumstances, an active sand dune will eventually transition into a state of stability. During this period, the dune becomes a closed system, remaining