Gianmarco Guglielmi Essays - Michelangelo, Angel,

Gianmarco Guglielmi Local church Italian scholars said Tuesday that they may have discovered an early version of a Michelangelo statue of Christ, discarded by the painstaking artist for a flaw in the marble. RAI state TV showed pictures Tuesday evening of the possible Michelangelo, depicting a sorrowful Christ with the cross. The recognized final version of the statue is at the church of St. Mary over Minerva in Rome. But scholars took note of the look a like at a church at Bassano Romano outside Rome two years ago, Silvia Danesi Squarzina, an art historian at Rome's La Sapienza University, told Italy's ANSA news service. Subsequent research examined early documentation describing a first version of the statue. A 1521 letter has Michelangelo setting aside the early version for a flaw in the marble -- a black line on Christ's face. Well, the Christ of Bassano has a black stain on the face, Danesi Squarzina said. An early sketch for the statue and similar incisions on both statues support the hypothesis that the Bassano piece is a work by Michelangelo, the art historian said. I thought that this show was particularly interesting because it talks about Michelangelo's work, which I find quite intriguing because he was one of the most talented painters I have ever seen. When I heard about this I thought to myself that this is amazing and the segment was beautifully laid out and each segment of the show was put together and kept u watching. Bibliography www vm

Learn About Rock Cycle in the Earths Crust

Learn About Rock Cycle in the Earth's Crust Rocks are composed primarily of minerals and can be an amalgam of different minerals or can be composed of one mineral. Over 3500 minerals have been identified; most of these can be found in the Earths crust. Some of the Earths minerals are exceedingly popular - fewer than 20 minerals compose more than 95% of the Earths crust. There are three different ways rock can be created on Earth and thus there are three main classifications of rock, based on the three processes - igneous, sedimentary, and metamorphic. Igneous Rock Igneous rocks are formed from the molten liquid minerals that lie below the Earths crust. Theyre formed from magma that cools beneath the Earths surface or from lava that cools upon the Earths surface. These two methods of igneous rock formation are known as intrusive and extrusive, respectively. Intrusive igneous formations can be forced to the surface of the Earth where they can exist as masses of rock known as plutons. The largest types of exposed plutons are called batholiths. The Sierra Nevada mountains are a large batholith of igneous granite rock. Slowly cooling igneous rock will usually contain larger mineral crystals than igneous rock that cools more quickly. The magma that forms igneous rock beneath the surface of the earth can take thousands of years to cool. Quickly cooling rock, often extrusive lava that comes from volcanoes or fissures in the Earths surface has small crystals and may be quite smooth, such as the volcanic obsidian rock. All rocks on Earth were originally igneous as thats the only method entirely new rock can be formed. Igneous rocks continue to form today under and above the earths surface as magma and lava cool to form new rock. The word igneous comes from Latin and means fire formed. Most of the rocks of the Earths crust are igneous although sedimentary rocks usually cover them. Basalt is the most common type of igneous rock and it covers the ocean floor and thus, exists over two-thirds of the Earths surface. Sedimentary Rock Sedimentary rocks are formed by the lithification (cementing, compacting, and hardening) of existing rock or the bones, shells, and pieces of formerly living things. Rocks are weathered and eroded into tiny particles which are then transported and deposited along with other pieces of rock called sediments. Sediments are cemented together and compacted and hardened over time by the weight and pressure of up to thousands of feet of additional sediments above them. Eventually, the sediments are lithified and become solid sedimentary rock. These sediments that come together are known as clastic sediments. Sediments usually sort themselves by the size of the particles during the deposition process so sedimentary rocks tend to contain similarly sized sedimentary particles. An alternative to clastic sediments are chemical sediments which are minerals in solution that harden. The most common chemical sedimentary rock is limestone, which is a biochemical product of calcium carbonate created by the parts of dead creatures. Approximately three-quarters of the Earths bedrock on the continents is sedimentary. Metamorphic Rock Metamorphic rock, which comes from the Greek to change form, is formed by applying great pressure and temperature to existing rock converting it into a new distinct type of rock. Igneous rocks, sedimentary rocks, and even other metamorphic rocks and be modified into metamorphic rocks. Metamorphic rocks are usually created when they come under extreme pressure such as under many thousands of feet of bedrock or through being crushed at the junction of tectonic plates. Sedimentary rocks can become metamorphic rocks if the thousands of feet of sediments above them apply enough heat and pressure to further change the structure of the sedimentary rock. Metamorphic rocks are harder than other types of rock so theyre more resistant to weathering and erosion. Rock always converts into the same type of metamorphic rock. For example, the sedimentary rocks limestone and shale become marble and slate, respectively, when metamorphosed. The Rock Cycle We know that all three rock types can be turned into metamorphic rocks but all three types can also be changed through the rock cycle. All rocks can be weathered and eroded into sediments, which can then form sedimentary rock. Rocks can also be completely melted into magma and become reincarnated as igneous rock.