The Peter Russell Rock Garden-Free-Samples -Myassignmenthelp.com

Question: Discuss three of the rock samples from the Peter Russell Rock Garden". Answer: The rocks from the Peter Russell Rock Garden Discussion The Peter Russell Rock Garden is one of the famous gardens of rocks which is situated in Ontario in the campus of Waterloo University. The garden was designed in the year of 1982 as a celebration part of the twenty-fifth anniversary of the Waterloo University. The president J. Gerald Hagey inaugurated the garden in the garden of the university campus. The special feature of the garden is the almost 70 kinds of different rocks are present in that garden which makes the best geographical view of that place. In this garden Frank Slide boulder, anthracite coal, and even Wawa gold ore are some rocks which have another geographical names (Waldron, et al. 2016). Jasper Conglomerate Jasper Conglomerate is a form of Paleoproterozoic quartz and jasper pebble conglomerate which was found in the middle part of the Lorrain Formation of the Cobalt Group and the formed under the Huronian Supergroup. The geologist give some specialized name of this rocks are pebble jasper conglomerate, St. Joseph Island puddingstone, Drummond Island puddingstone, Michigan puddingstone (Yorath Gadd, 2017). These rocks are mainly formed near the area of St. Joseph Island and St. Mary River which is situated in the Bruce Mines of the Northern Ontario. The rock is mainly consists of several materials like the red jasper pebbles which is composed by the sandy gravels and also includes white, semi-transparent and black quartzite. This rock is mainly consists of more pebbles than other mixtures. The rock is looks like a cryptocrystalline bolder size pebble which are shown in the glacial erratic in the Pleistocene glacial tills and drift. It is a thick material which is forming in the Mississippi Delta. The Jasper Conglomerate is mainly getting the formation by the river deltas which drained a landmass towards the north. The Jasper Conglomerate mainly formed almost 2.2 2.5 billion years ago and in the Peter Russell Rock Garden it was the first rock that was found. In the park it can be find under the sand and the Ontario Place (Waldron, et al. 2016), Toronto donate this rock in the park. In the park it was also known Pudding Stone in Peter Russell Rock Garden. This stone used as decorative stone which is consists of good polish. It can be formed in different color like bloodstone, green, and lemon. It is the most common types of rock which are uses as gems and the Imperial Jasper and Madagascar Jasper are the rarest among others. People uses this rocks as a gemstone and fashionable junk jewelers (Bonetto, et al. 2017). Gneiss, Grenville Province Gneiss is a form of rock which is mainly processed by the high grade regional metamorphic or the sedimentary rock. It is basically the composed layers of sheet-like planar structures which is foliated in alternative darker and lighter colored bands. The minerals are recrystallized with heat and pressure which made the transformations of the rock (Duca, Alonso Scavia, 2015). It is mainly form from the shale which is also known as sedimentary rock then it is compiling with the phyllite, schist and slate. Thos rock is sometime known as garnet gneiss" and "biotite gneiss." There are different types of Augen gneiss whixch is the formation of metamorphism of granite, Henderson gneiss which is form in two sequentials, Lewisian gneiss which is mainly found in the Scottish mainland and metamorphosed by several mixtures of marble, quartzite and mica schism and another forms is Archean and Proterozoic gneiss which is used in the Sphinx of Taharqo of the Nile Valley. Gneisses from western Greenland comprise the oldest crustal rocks known. Gneiss is an old German word meaning bright or sparkling. These rocks are mainly found before the 1-2 million years ago. They are actually found in the North Bay or Red Bridge of Ontario. The Gneiss is the metamorphosed rock which became the granite and formed the sedimentary rock. The gneiss becomes pink for the presence of Muscovite which is one of the interesting facts about it (Ietto Bernasconi 2016). The gneiss rocks are mainly uses for the flooring in houses, offices and any place. As a ornamental stone, it is very well known rocks which can be find in any places. For the formation of gravestones it is one the favorite rocks which are uses. These kinds of rocks are quite famous in the Peter Russell Rock Garden which help to increase the geographical value of the park. Amabel Dolostone, Paleozoic Sedimentary Rock The Dolostone or dolomite rock is one kind of sedimentary carbonate rock which is consists of mineral dolomite and CaMg(CO3)2. There are equal amount of magnesium and calcium are also found this rock. The formation of the dolostone is mainly occurring with magnesium which is replaced by the limestone or lime mud which can be related with the lithification. The dolomite sometimes becomes dolomitic limestone which is the conversion of calcite to by dolomitization. The dolomites mainly found in different caves which are actually form with limestone which was also dissolute by the carbonic acid. It is the form of Paleozoic Sedimentary Rock which mainly found in the Arizona or several caves. The limestone and sandstones are kinds of the Paleozoic Sedimentary rock (Agbogun, Al Hussein, 2013). The Amabel Dolostone which is the form of Paleozoic Sedimentary rock is found from the 545- 248 million years ago. It is one the evaluated rocks in the rock family which was change through different states of periods. The Amabel Dolostone is nowsays find in the Wiarton, Ontario, this is the greatest formation of caproack of the Niagra Escarpment. The formation of the rock was processed by the warm, sea salt which is located in the Michigan Basin. The presence of the Magnesium helps to destroy the microscopic fossils which fill with the minerals and in the area of Wiarton it is also known as Vugs which is mainly consists with the zinc sulphide and needed minerals (Liu et al., 2014). The Amabel Dolostone is uses as the building stones, crushed stones, flux stone and the products which are made by the dolomite lime. The collective stones from the Adair Marble Quarries are used in one of the famous building in U.S.A which is Canadian Embassy. This is one of the important rocks which are present in the Peter Russell Rock Garden which are used for the making of the buildings. References Agbogun, H. M. D., Al, T. A., Hussein, E. M. (2013). Three dimensional imaging of porosity and tracer concentration distributions in a dolostone sample during diffusion experiments using X-ray micro-CT. Journal of contaminant hydrology, 145, 44-53. Bonetto, S., Comina, C., Colombero, C., Pierre, F. D., Ferrero, A. M., Giordano, N., ... Vagnon, F. (2016). Study of the Mechanical Properties of a Conglomerate. Procedia Engineering, 158, 248-253. Duca, S., Alonso, E. E., Scavia, C. (2015). A permafrost test on intact gneiss rock. International Journal of Rock Mechanics and Mining Sciences, 77, 142-151. Ietto, F., Bernasconi, M. P. (2016). Evidences of fossil landslides from the Lower Pleistocene on the northwestern margin of the Mesima basin (southern Calabria, Italy). RENDICONTI ONLINE SOCIETA GEOLOGICA ITALIANA, 38, 65-68. Liu, H., Wang, B., Shu, L., Jahn, B. M., Lizuka, Y. (2014). Detrital zircon ages of Proterozoic meta-sedimentary rocks and Paleozoic sedimentary cover of the northern Yili Block: Implications for the tectonics of microcontinents in the Central Asian Orogenic Belt. Precambrian Research, 252, 209-222. Waldron, J. W., Locock, A. J., Pujadas-Botey, A. (2016). Building an Outdoor Classroom for Field Geology: The Geoscience Garden. Journal of Geoscience Education, 64(3), 215-230. Waldron, J. W., Locock, A. J., Pujadas-Botey, A. (2016). Building an Outdoor Classroom for Field Geology: The Geoscience Garden. Journal of Geoscience Education, 64(3), 215-230. Yorath, C., Gadd, B. (2017). Of rocks, mountains and Jasper: a visitor's guide to the geology of Jasper National Park. Dundurn.