3 Types of Rocks:
- Igneous Rocks - This type of rock is formed by the cooling and solidifying of molten materials. These types of rock can be found beneath, or at, the Earth's surface as lava. An example of this type of rock is Pumice. Pumice is a light and porous rock formed by explosive volcanic eruptions. Below is a picture of Pumice.
- Metamorphic Rocks - A metamorphic rock is a rock that was once in one form and changed to another due to the exposure to eat, pressure, or some other experience. This process is called metamorphism. Much of the Earth's crust is made up of metamorphic rocks. Marble is a prime example of a metamorphic rock. Marble is composed of recrystallized carbonate materials, mostly dolomite or calcite. Below is a picture o marble.
- Sedimentary Rocks - This type of rock comes from the deposition and solidification of sediment. These rocks are often found in layers and commonly contain fossils. The Earth's crust is estimated to contain about 8% sedimentary rock. The study of this type of rock can provide useful information for civil engineers. An example of this rock would be Sandstone. Sandstone is a Clastic sedimentary rock formed mostly of sand-size minerals and rock grains. Below is a picture of Sandstone.
Types of Soils:
Gelisols, Histosols, Spodosols, Andisols, Oxisols, vertisols, aridisols, Ultisols, Mollisols, Alfisols, Inceptisols, Entisols
Sunday, April 6, 2014
Tuesday, April 1, 2014
Maps Lab
In learning about maps the four we focused on were the choropleth, dot density, proportional symbol map and isopleth.
Choropleth Map:
Areas on a Choropleth map are shaded or patterned in order to differentiate the proportion of statistics the map is based off of. This type of map makes it easy to visualize the different proportions of studies over a geographic area on a big scale and also can bode easy for visualizing a region on a smaller scale. Below is an example of a Choropleth map.
Dot Density Map:
This type of map uses the dot symbol to give a visual example of a feature or phenomenon on a map. The heavier the dots in a given area, the greater the density of that feature. One dot can represent one unit or a single dot can represent many units. Below is an example of a Dot Density Map
Proportional Symbol Map:
These maps are used to represent Geographical data. The data is scaled proportionally and placed next to it's corresponding geographic location. One problem with these maps is that cartographers are not entirely sure viewers can decipher the size difference between values. Below is an example of a Proportional Symbol Map.
Isopleth Map:
This type of map shows data in a third dimension. For this reason most of these maps are used to show things such as elevation. This third dimension is shown by a series of lines called isopleths. Below is an example of an isopleth map.
Choropleth Map:
Areas on a Choropleth map are shaded or patterned in order to differentiate the proportion of statistics the map is based off of. This type of map makes it easy to visualize the different proportions of studies over a geographic area on a big scale and also can bode easy for visualizing a region on a smaller scale. Below is an example of a Choropleth map.
Dot Density Map:
This type of map uses the dot symbol to give a visual example of a feature or phenomenon on a map. The heavier the dots in a given area, the greater the density of that feature. One dot can represent one unit or a single dot can represent many units. Below is an example of a Dot Density Map
Proportional Symbol Map:
These maps are used to represent Geographical data. The data is scaled proportionally and placed next to it's corresponding geographic location. One problem with these maps is that cartographers are not entirely sure viewers can decipher the size difference between values. Below is an example of a Proportional Symbol Map.
Isopleth Map:
This type of map shows data in a third dimension. For this reason most of these maps are used to show things such as elevation. This third dimension is shown by a series of lines called isopleths. Below is an example of an isopleth map.
Barometer Lab
For this lab we used homemade barometer to measure the pressure in the atmosphere. The purpose of the lab was to determine the pressure changes according to the different changes in weather.
In order to make the barometer we cut a balloon's top off and stretched the remainder of the balloon over a glass bowl. Once this procedure was done we cut a straw at the top into a pointed tip in order to read what I was pointing at. Then this pointed straw was taped to the top of the balloon covered glass bowl. Using the graph below, the atmospheric pressure on a given day could be recorded.
Based on the picture above of the homemade barometer on this given day, the atmospheric pressure is .8 ATM.
In order to make the barometer we cut a balloon's top off and stretched the remainder of the balloon over a glass bowl. Once this procedure was done we cut a straw at the top into a pointed tip in order to read what I was pointing at. Then this pointed straw was taped to the top of the balloon covered glass bowl. Using the graph below, the atmospheric pressure on a given day could be recorded.
Based on the picture above of the homemade barometer on this given day, the atmospheric pressure is .8 ATM.
Pressure (ATM) | Ruler Reading (mm) |
0.80 | 5 |
0.85 | 10 |
0.90 | 15 |
0.95 | 20 |
1.00 | 25 |
1.05 | 30 |
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