Every year the Lamont Doherty Earth Observatory holds an open house in which scientists share their studies and really let the public see what and how they do what they do. Scientists at this research center are working together studying different fields of the Geologic sciences ranging from Oceanography, Geochemistry, Seismology, and even Marine Biology share their findings with the public. This year like every other year, they set up deferent exhibits and share the current research, studies and illustrations of the different Geologic processes along with their findings with anybody who is interested. For this assignment, we were asked to describe five of the exhibits from the LDEO open house. The five exhibits that called my attention the most were the Seismology, Geochemistry, Oceanography, Demonstration of Hard and Soft behavior of the surface of our, and the Water Current Exhibit. 1- Seismology in simple terms is the study of earthquakes; it involves observations of natural ground vibrations and artificial vibrations.
In this exhibit, the scientists were explaining how and earthquake forms and how it can be detected even hundreds of miles away via a Seismograph. Someone asked the question what is an earthquake. And the response was well, its a trembling or shaking of the ground causes by a sudden release of energy, energy that is stored in the rocks beneath the surface. I thought that was great so then, I asked how is this energy stored And his explanation was very well illustrated by a simple demonstration.
The Term Paper on What is Earthquake
An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth’s crust and cause the shaking that we feel.( readanddigest.com/what-is-an-earthquake) The April 2015 Nepal ...
There sere two bricks joined together by a rubber band, at the end of the first brick there was a nylon thread which was being pulled slowly. He said imagine these two bricks are two plates floating on the mantle, as one moves slowly, it is pulling the rubber band that is attached to the other brick and tension is building over time then very sudden and quickly the rubber band pulls the bric behind it, and this is how the energy builds up and then it is released quickly. (Drawing of bricks) Then he had a Seismograph, a device that measures seismic waves on a table and he was explaining how to read the intensity of the vibrations. He had first one kid jumping in front of he seismograph, then two, then three, then four and so one and one could see the intensity of the vibrations being recorded by the seismograph. He also talked about the use of seismic stations all over to monitors earthquakes and artificial vibrations like explosions, etc. The Seismology department at LDEO monitors seismic activity in the Northeast region of the US; here is a map of the location of those seismographic stations.
2- Geochemistry is the applications of chemical principles and techniques to geologic studies to help us understand how chemical elements are distributed in the crust mantle and core of the earth. Geologists have many ways of gathering data for this kind of study, one of them is of course by taking samples and analyzing them, but in one of the labs at LDEO I saw something I thought was very interesting. Scientists want to know how a mineral of a given chemical composition behaves under extreme heat and pressure such as those found deep within the earth, but because they can not drill that deep to take samples, they came up with the idea of building a press that could replicate specific pressures and temperatures pretty much like those found deep within the earth. The press is relatively simple; it uses hydraulic power to generate the pressure and a special heater to generate tremendous amounts of heat, as much as 3000 degrees centigrade. This press uses angels that press the sample from eight different directions thus increasing and redirecting the pressure exerted by the hydraulic press. By heating and pressuring the samples, they are able to study the chemical and crystal structure of different samples.
The Essay on Ocean Deep
Snelgrove and Grassle in The Deep Sea: Desert and Rainforest published in Oceanus, volume 38 in 1995 argue that the popular belief that the deep sea is little more than an ocean desert is a pure fallacy. Contrary to such thinking a multitude of benthic organisms dwell on the ocean bottom; despite the frigid temperatures and high pressure, a large heterogeneity of creatures, rivaling in variety and ...
The demonstration he gave was with a brass ball which he put inside the press, put the amv els on top and then pressured it just for a brief moment and the result was a ball with eight flat surfaces. I thought this was so interesting that I had to have the brass ball. 3- Deep Sea Sample Repository. The LDEO has an archive of sediment and rock from the beneath the ocean floor.
This material is used for studies in oceanography, and marine geology. Most of the core samples are from the Atlantic Ocean, and during the open house, scientists took the time to show us how they collect the samples and how they store them. The only ways to get core samples from the ocean floor is by going on a ship and physically drill the ocean floor and collect the samples. Deep-sea cores are long cylinders of sediment taken from beneath the ocean floor, they contain microscopic fossils of marine animals, volcanic glass, sands originally from land (terrigenous sediments), cosmic material, and other unusual materials only found in a marine environment which are very sensitive to temperature changes and chemical changes in the environment and are therefore used as environmental indicators for research; Volcanic glass is an important time marker and records geological events. Sands can indicate oceanic currents, etc. The deep-sea samples hold a permanent record of magnetic history letting us know about the magnetic orientation of the poles as we studied in class.
At the Repository scientists showed us how they drill and I was able to see and touch the actual drill bits that they use to drill the Ocean floor. In addition, we were taken to four cold rooms were they store the core samples, they were very big and very cold, the reason the samples are kept in a cold environment is to prevent dryness and decay from bacteria. Here is a map with all the locations were cores have been taken for research, notice the high concentration of locations found in the Atlantic Ocean. (Map of locations) 4- Hard and Soft Surface. The fourth exhibit that called my attention was the demonstration of the sometimes hard and sometimes plastic soft surface of our planet. As we studied in class, the surface of the earth is hard and plates move through it over time, this is the basic principle of the Plate Tectonics Theory.
The Essay on The major ocean surface current patterns
An ocean surface current is a constantly directed and continuous movement or flow of ocean water. Major ocean surface current patterns are powered by the wind. However, these patterns are also largely influenced by other factors such as the Corolis effect, which is the deflection of the water to the direction of the wind, the differences in heating across the globe, and the structure of the ...
In order for movement of the plates to occur there has to be an underlying plastic soft layer (asthenosphere) that allows the plates to move through it over time. In this exhibit the scientist took a very simple approach to illustrate this. He took a bathtub, two hundred pounds of cornstarch and mixed them together to form this plastic hard and yet soft solution that resembles the surface of our planet. I never thought this solution was so hard, it feels just like plastic and if you try to break it, it breaks and it feels brittle. I hit it, touched it and I asked the person if one could stand on it and he said of course, its so hard that it can hold your weight, but if you apply force slowly and gradually, just like the stress affects the rocks you can sink and move through it. This is a great experiment to try and he even gave out sheets with the recipe on how to make this solution at home.
This was a lot of fun especially for the kids. 5- Water Currents. The fifth exhibit that I was interested in was the water convection model. Moreover, how it illustrates ocean currents. This was a very simple model, it consisted of a fish tank, a light bulb as a source of heat, a block of ice as a source of cold, and some kind of die to show the water moving. The tank was about half way full, the light bulb was at one side of the tank pointing down at the water, the ice was at the opposite side floating in the water, and the die was in the middle of the tank in the bottom.
I could really see the ink moving to the hot spot and then rising again as it became less dense and then sinking again as it cooled and became more dense. This I think was a very realistic and vivid illustration of what really happens the oceans of our planet. As we saw in class, ocean currents are responsible for many geological structures and erosion and this model can help us how some currents form and how they affect the ocean floor in terms of the transportation of sediments, etc. (Drawing of tank) In conclusion, this was a very positive experience that gave a broader understanding of geology and helped me with the terms and ideas that we discuss in class. This really helps to visualize some of the concepts like earthquakes, the surface of the earth, and the ocean currents. Thank you for giving me the opportunity to better understand the planet I live in..
The Essay on Waves Wind Generated Waves That Travel In Water Wave Speed Ocean
Savage Seas The Wave Machine The wave machine is a simulator that will allow you to create an ocean wave and determine its height. Most ocean waves are formed when the wind blows across the water's surface. The wave height is determined by three factors: wind speed, fetch, and duration. Wind Speed In 1805, Sir Francis Beaufort, observing the effects of wind speed upon the sea, devised the Beaufort ...
