The Shale Is A Rock

    C.quartz chert.   Correct  D.shale.   Answer Key: D   Feedback: The correct answer is D. shale.     Question 18 of 33 3.03/ 3.0303 Points Specimen #16 is composed of Correct  A.silica.     B.calcium carbonate.

In site one there was a high proportion of very unspherical rocks. According to this the hypothesis is right, in site two there is a lot more smother rocks medium sized and in site 3 there are very small pebbles which are very smooth and spherical. The pebbles get smoother and rounder while it goes downstream. Due to us only taking about 10 rocks our result may have been not right as there were some pebbles which were largely over sized. Most of the other load is dissolved by solution such as limestone and chalk

Approximately 17 meters thick, Unit A defines the lowest third of the Juniata Formation. Fragments of marine fossils, including bryozoans, brachiopods, and gastropods, are commonly found in the bottom-most portion of this unit of structureless mudstone and quartz arenite. Quartz grains in the sandstone beds of Unit A are typically immature and fine-grained, though the sandstone packages tend to coarsen upwards. Though typically structureless, intermittent bedding of the sandstone and shale packages is observed in this unit, and some areas display

With our observation of the Shawangunk formation, we see a sedimentary rock formation containing a range of grain size. Such sizes range from pebbles (3cm-5cm), fine-grain sand, and medium-grain sand. There is some grading towards the bottom left of the outcrop known as a reverse grading with some small cross beds present (Figure 2). The grading occurs towards a slight part of the outcrop where we see the grading beginning as fine grain sediments and working up to coarser grain. With moderate sorting we see variations of degree of sorting per bed. As the degree of sorting varies as does the sphericity. The sediment bedding is well seen ranging in sizes of +/--20 cm to 40 cm. This outcrop has thick beds as one can see the basic units with cracks in between each (Figure 3). With mostly tabular beds consisting of sub-angular, and sub-rounded sediments, this outcrop also consists of some ventricular beds (Figure 4). When looking at figure 4, we have a small space of a ventricular bed present. This is because the bed comes in, pinches thicker bedding,

The site is of major geoconservation significance because of being the only place on earth where rocks from the earth’s mantle - 6 km

Next, we can see that the rock displays a subtle porphyritic texture with plagioclase comprising the phenocrysts. The overall texture of the surrounding groundmass is granoblastic equigranular. Under thin section we also see a weakly defined foliation evidenced in the preferential alignment of actinolite grains and to a lesser extent chlorite grains. Undulose extinction is also observed in quartz indicating the rock was subject to deformation. The normalized quartz, alkali-feldspar, and plagioclase (QAP) values of this rock indicate that it is classified as a grano-diorite according to the IUGS QAPF classification system which is consistent with the hand sample interpretation.

11. Perform the Mohs hardness test on all of the samples in your set; determine which is the hardest and softest.

Determine the relative age each of the geologic structures shown in the geologic cross section below (Figure 9.17) from youngest to oldest; then answer the questions below. As before, a wiggly line running across the geologic cross section indicates an unconformity and a fault is indicated with a bold straight line.

CHM130 Lab 6 Exploring Density Name A. Data Tables Place your completed Data Tables here Part IIIa (3 points) Volume of water in graduated cylinder (mL)10 mlMass of rubber stopper (g)11.15Volume of water and rubber stopper (mL)16.5 Part IIIb (6 points) Volume of water in graduated cylinder (mL)20Mass of iron nail (g)3.66Volume of water and iron nail (mL)20.5 Part IV (20 points) Type of Aluminum FoilMass (g)Length (cm)Width (cm)Volume (cm3)Thickness (cm)Regular.63g15 cm 10.02 cm.21 cm3.0014 cm Heavy Duty.97g15 cm10.01 cm .36 cm3.0024 cm B. Follow Up Questions Show all work for questions involving calculations. Part I Use the concepts/vocabulary of density to explain why the liquids formed layers in Part I of the procedure. (8 pts)

Lyons sandstone can be divided into two distinct types which are the red and grey facies. The red facies are the red- colored sandstone which contains no hydrocarbons and the gray facies are the white to black- colored sandstone which contain hydrocarbon in its matrix (Levandowski,

In Measuring and Understanding Density, several experiments were performed to find density of regularly shaped objects, irregularly shaped objects, liquids and gasses. An additional experiment was done to find the specific gravity of a sampling of liquids. The purpose of the experiment was to provide a better understanding of density and to be able to extrapolate unknowns based upon these calculations. The experiments yielded data in keeping with Kinetic-molecular theory in regards to the density of water versus its temperature. Key measurements and formulae were also used to determine densities of metal and plastic objects as well as irregularly shaped rocks. It is possible to find the density of an object (be it liquid, gas or

In terms of the placement, the rock was positioned to be right smack in the middle of this community-balanced on a couple of woods. It’s strange to see how it is placed because since it is balanced on unalligned chunks of wood, I

Secondly, the photo taken of site E shows that it is most likely sedimentary rock. Since there is no pressure or heat in the sedimentary

The MOHS scale of hardness is an essential part of this experiment. This method was invented by a German mineralogist, Frederich Mohs (1773-1839) in 1812. The purpose of the Mohs scale is to identify the hardness of materials and minerals using items that can be found in a classroom. The MOHS scale is done using a scale to measure the hardness of a material by the resistance to scratching. The process is to apply slight pressure to the object being tested (an egg in this case) using an item like a nail or coin, and pull the item along the surface of the object. If there is a scratch, then that is the hardness of the object. However, if there is only some residue from the object being scratched, then that is not considered the hardness. To check if there is a scratch or residue, gently wipe off the area. If the mark remains, then it is a scratch, not just residue. These are easy to get confused. Make sure to perform the test again in a different area to check the results to make sure they are accurate. There are different items used to test this

Before we get started, I guess we should actually distinguish, ‘What IS the Burgess Shale?’ Well, it is said to be a “shrouded legend” deep in the Canadian Rockies discovered in the early 1900s by Charles D. Walcott, notorious Smithsonian Secretary (Adler 2013). According to Haug, Caron, and Haug in their research article ‘Demecology in the Cambrian: Synchronized Molting in Arthropods from the Burgess Shale’ the Burgess is “arguably the best-known Konservat-Lagerstätte”. While the Burgess Shale is primarily known for the intricate preservation of soft-bodied creatures dating from the early Cambrian Period (Haug, Caron, Haug 2013); furthermore, what seems to make this specific site so special is the fact that not only the soft parts of