Part 1
What a period! Miocene period occurred in (25-5Mya) during the Cenozoic era, termed as the age of mammals (Balasubramanian, 2014). The Miocene period falls under the tertiary era, which is a further subdivision of the Cenozoic era. This period has so many events with the Southern Hemisphere, having extensive glaciation while the Northern Hemisphere is characterized by the occurrence of mountain orogeny (Balasubramanian, 2014). Additionally, basalt flows and widespread volcanism is visible. The Miocene climate is a moderate icehouse in which grasslands are spreading as the forests contract thus, packing accordingly is necessary. The first apes appear during this period, diversification of mastodons and horses (Balasubramanian, 2014).
More so, bird families and modern mammals become recognizable during this period. Nevertheless, great and notable development on the elephant and horses' families occur while grazing mammals, apes, and whale dominate the period. However, whiffs of gases that are toxic, lava flows, ash blanket, and acidic clouds of the vaporized seawater are some of the dangers associated with the widespread volcanism of the period hence protective gears are necessary (Balasubramanian, 2014). The Miocene period is worth visiting because of its diversified flora and fauna, the landscape shaping from the erosion of rocks, soil, and sediment transportation and their deposits from glaciers in the Southern Hemisphere. Nonetheless, visiting the Miocene period is interesting, as it would help with understanding the global climatic changes, the formation of the various natural resources such as gases and mountain building.
Delegate your assignment to our experts and they will do the rest.
Part 2
What a beautiful view and learning experience! The Carboniferous period marking the end of the Paleozoic Era was worth a visit hence a huge honor to have gotten a chance to visit. The opportunity was short, but from your prowess in research and outlining of the various features to observe during the trip each minute of the visit period was well utilized. The evolution of plants to form complex versions were visible from the large trees that were primitive, with the tetrapod breaking their boundaries and moving onto the land as part of abundant life in water and land (Balasubramanian, 2014).
What a view with the two supercontinents moving towards each other and Pangea appearing for the first time with other beautiful views of the limestones, coal deposits, and grit stones (Balasubramanian, 2014). I dislike insects, but the visit displayed the various types such as spiders, dragonflies, scorpions in such an appealing manner they captured my attention fully. The warm climate was breathtaking with the warning on swampy lands that facilitated the packing that made the visit even more comfortable and appealing. The whole trip to the carboniferous period was impeccable.
Reference
Balasubramanian, A. (2014). The Geological Time Scale. The University of Mysore. https://www.researchgate.net/publication/309464865_
