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Lebanon Rock Type TripLebanon consists mostly of Sedimentary rocks by nature. There are some igneous stones, but mostly Basalt, and a little Metamorphic located in Hamra, although they are imported and not located in Lebanon by nature. Lebanon actually consists of sixty percent limestone, ten percent sandstone, twenty-five percent shale, and five percent Basalt. When the class went on a field trip last week we saw many rocks, such as Basalt, Limestone, Sandstone, and etc. On our trip we made three main stops, I will be explaining by location the variations of rocks that we saw, and the description of the rocks. On our first stop on the field trip we stopped of at Quaternary Alluvium (Dog River). While in Quaternary Alluvium we discovered that the site we were exploring had been a river that had all dried up. In this river we saw a lot of gravel, mixed with different stones. In the gravel the rock sizes varied from silt, all the way up to boulders. In the river we saw a lot of gray limestone. The limestone varied from pebbles, up to boulders. I discovered that the rocks were limestones, because the rocks fit the description of sedimentary rocks. The outside was a smooth surface, and once we broke it there was a layered surface in straight patterns. When we also tested the rock for calcite, by putting acid the rock fizzed, which was a sign that the rock consisted of calcite, which is another property of limestone. From those facts, I deduced that the stone was a limestone. We also discovered that some of the rocks that were found in the dog river were sandstones from the Sedimentary class. I discovered this because of the characteristics of the rock, was sandy silt all combined together in a bunch with no certain pattern with the color of tan. These characteristics fit into place of the rock, sandstone. I tested to see if there was any calcite in this stone, and discovered that the stone did consist of calcite.
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One rock that I thought might not be found was basalt. Basalt was found in this river, and I discovered that this stone was basalt, because this stone had no layers, and no bands, it was all bunched together, and seemed to be very fine grained. When we broke this igneous rock open, we discovered that there were a lot of holes in it, as well as pyroxene. The Basalt fizzed when it was mixed with basalt, which meant that it also consisted of calcite. This stone was very dark and according to the information of basalt rocks the stone consisted of low silica and high iron.While we were outside we discovered that shale might have been found in this river, although due to the rivers flow, the shale may have been broken and has disintegrated. Shale is classified as a sedimentary stone, because it has very thin layers, and is a tanish color that consists of calcite according to our testing.The rock is known as conglomerate, which consists of all of the rocks I have just described. The conglomerate is located on top of a cliff, which in my opinion occurred due to erosion of the mountain above it, and then the formation of the conglomerate where they were last set. This stone I saw was combined together by shale, it was of all different colors, and had no stable layer, nor a stable shape. It is similar to gravel, although with some bigger stones, and all of them connected together, to form one outcrop.While on our way to our second location we looked at some stones from the bus, the stones seemed to be from the Sedimentary category, because it was layered and had the characteristics of a limestone. The stone is known as Karsts, this stone is called Karsts because it is a form of limestone, with a vertically layered pattern around it.The shale was brownish black in color. Shale's characteristic is very sensitive, the average human can break shale with his hand. A shale stone is layered with very thin layers. It is a fine-grained stone, which is classified as sedimentary. Shale located on a mountain once eroded travels and lays on the bottom of the mountain, until some natural mineral such as water comes and makes it disintegrate. The Shale has calcite in it.The Basalt in Mayrouba Mountains contains pyroxene, which is a small fine-grained black mineral. The Basalt on the outside covering has a lot of rust on it, due to water and Iron Oxygen mixed together. The Basalt also contains large veins, of calcite. The Basalt once we broke inside was very dark black, and consisted of some small minerals, which are known as Zeolite, and have no color, but are see through. This Basalt is from the rock class, Igneous, because it has no bands and no layers, and is a dark color. The Final rock that we saw before we returned to the school was a stone that contained a mixture of Limestone on the top, and Sandstone on the bottom. The mixture of these two stones into each other where the top is all limestone, the middle is a mix of limestone and sandstone, and the bottom is only sandstone is known as a cradational mixture. This sandstone had very little calcite in it, although it did consist of a little bit of calcite. The rock consisted of veins, and the veins in the rock also had calcite in it. The limestone was gray on the top, tanish on the bottom, and a mixture of tanish gray in the mid part.
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