Summary of the geology of Gunung Jerai Gunung Jerai is a mountainous region located in central Kedah, between the borders of Kuala Muda and Yan district. The highest point of Gunung Jerai is recorded to be 1217 meters and Gunung Jerai covers a total area of 86.4 square kilometers (Lee et al., 2004). According to Bradford (1972), the existence of Gunung Jerai can be related to the Jerai Formation and the Patani Formation. The Jerai Formation, named after Gunung Jerai itself, is of Cambrian age with a thickness of 1425 meters. Jones (1970) has divided the Jerai Formation into two members which are the lower member and the upper member. The lower member is near 900 meters thick and it consists of quartz-mica, schist and phyllite. Also present is the occasional amphibole and garnet-bearing schist. On the other hand, the upper member is 525 meters thick with made up of quartz arenite with an infrequent presence of feldspar grit (Lee et al., 2004). The Jerai Formation is believed to have a shallow marine shelf depositional environment. …show more content…
The Patani Formation is of Silurian age and the boundaries of this formation actually overlie the Jerai Formation. The thickness of Patani Formation is 1524 meters. Bradford (1972) has divided the Patani Formation into three facies which are argillaceous, arenaceous and calcareous. The lithology of Patani Formation consists of argillaceous sequence of shale and mudstone, commonly ferruginous and subject to lateritization and in places phyllitic or pyritiferous. A less extensive arenaceous facies of sandstones or orthoquartzite can also be found with the presence of limestone on Bidan Island. The Patani Formation is believed to have a deep gulf or geosynclinal basin depositional
Pierre shale is a formation of marine origin from the Cretaceous period that resulted from the Western Interior Seaway. The formation stretches from New Mexico to North Dakota, is up to 700 feet thick and rests on top of the Niobrara formation. The Niobrara Formation is a geological formation that appeared around 87-82 Mya during the Cretaceous, also a result of the Western Interior Seaway. It is composed of two layers: a chalk and limestone layer. The chalk was formed due to calcium carbonate left behind by decomposed shells of microscopic algae that populated the Seaway.
While on station after transporting Deadrick Allen, this officer (Ofc. J. Jaques #64) was told by Det Sgt. Sibley #42 to place Allen into cell #3. While in the process of searching Allen 's person before placing him into the cell I located a small ziplock style baggy filled with a green and brown plantlike substance in his front right small front pocket. After removing the baggy Allen began being uncooperative.
My name is Walaha Gee and I am one of the residents that live near your business. I understand that your business involves music and audio but the volume is just entirely too loud. It has been going on for about two weeks now. I’ve been having a hard time sleeping and this has been affecting my productivity at work.
The Teton Range consists of a core of igneous and metamorphic Precambrian rocks overlain in most of the range by westward dipping sedimentary Paleozoic rocks. The Grand Teton Range consists of rocks ranging from the Precambrian, Paleozoic, Mesozoic, and Cenozoic time periods. The erosion-resistant Precambrian rocks comprise the highest peaks of the Teton Range and are part of the Wyoming Craton. The oldest units (>2680 Ma), observed in the north, south, and the eastern part of the central Tetons, are Archean layered gneisses, including biotite gneiss, plagioclase gneiss, amphibole gneiss, and some amphibolite (Reed and
The sites stratigraphy was studied again in the 80s and it was
Behavior Progress: Since Jamesha’s last court review, Jamesha has continued to participate in the program with minimal difficulty. Jamesha did not acquire any sanctions or room restrictions this period. However, Jamesha did express some difficulties with peers in regards to her concerns with their behavior and disposition. The treatment team emphasized to Jamesha focus on her goals and objectives and to allow staff to redirect and focus on the behavior of her fellow Post D residents. This period staff did report that there were fewer periods where Jamesha seemed to present a lingering, negative mood when re-directed, although this is an area Jamesha will need to continue to demonstrate improvement.
On the other hand, the Mint Canyon Formation along Aqua Dulce Road consists of sedimentary rock that is mostly sandstone and conglomerate. On this stop we learned about the sediments that formed the rock and their deposition from a river 12 million year ago. Our two last stops covered material on faults and rocks. The Vasquez Rocks were said to be form from the San Andrea Fault, and the Vista Point of the San Andreas Fault also covered material on the
It was conducted in order learn how to better manage the barriers in response to growing development in coastal areas. In response to previous research, it was hypothesized that some barrier islands originally formed offshore and were relocated to their present locations through wash over. The study was conducted by examining stratigraphic sections for nine barrier island transects as well as stratigraphic data from previous studies. Over 200 vibracores were examined for the study total.
The reporting party (RP) stated the resident 83 year old Iraj Ajir was found in his closet by his daughter Katra Ajir. According to the daughter he was covered in urine. The resident was also observed to have bruising to his arm and a burn on his leg. CCIB LPA McGaskey left message family representative Katra Ajir at (310) 498-2884 regarding which arm and leg was injured. According to the RP the resident 's room was covered in feces and urine.
The lower parts have been submerged and desiccated, shown by the layers of travertine, strand formations, and beaches (9). Scientists can infer that the basin was once filled with seawater due to the discovery of fossilized marine shells, corals, and oysters in the rock (9). The fossils are now above tide-level showing a change in elevation of the region (9). Dr. Stephen Bowers, who studies the region, writes, "The water of the old Tertiary Sea, which once prevailed here, must have been extremely favorable to the propagation and growth of mollusks, especially oysters”. There is also evidence of volcanic activity around the area in the form of craters stemming from Pinacate, an extinct volcano (9).
In this stage, the type of lava changes and eruptions become more explosive. The new lava flows increase the slope and eruption rate gradually decrease over a period of 250,000 years. As the volcano becomes dormant, the erosional stage takes place. The mountain loses elevation and subsides into the oceanic crust. Erosion also causes deep valleys and coral reefs to form.
R/s on 03/27/16, Ms. Dupuis was brought into the ER unresponsive and covered in feces and urine. R/s on 04/08/16, Ms. Dupuis was locked in the home and covered in feces and urine. R/s home health agency reported that Ms. Dupuis is found soiled in feces and urine. ALLEGATIONS: R/s Lynn Dupuis recently had a stroke and is not able to take care of herself.
The poorly sorted nature of the conglomerates, considered with the inclusion of wood fragments in the older conglomerate members and the graded sandstones and mudstones throughout the formation suggest deposition occurred through successions of debris flows. Presence of volcanics in the lithic fragments further indicate volcanic activity in the process of sedimentation as well—as debris flows associated with lahars are the likely source of the slope failures. Deposition environment was moderate to deep marine, as mudstone deposits require low energy depositional environment, but the style of sedimentation indicate deposition was not on a continental shelf. This is further supported by inclusion of the large overturned clast from an older member within the formation. Cross-bedding, graded bedding, and scouring surfaces provide 3 lines of evidence establishing the northern contact of the formation as the original upward oriented surface.
Environmental Setting The area of the Leakey Site is within 3.1 miles of the Cherokee Upland District and Hightower-Jasper Ridges District of the Piedmont Province, winding around the east side of Cartersville from the northeastern to the southwest along the Cartersville Fault. This is a major physiographic boundary between the sedimentary formations of the Southern Valley and Ridge Section and the igneous and metamorphic formations of the Southern Piedmont Section,
An assessment of the cultural value of the site and its significance in Burra Charter terms. • Aesthetic Value: The Landscape of Mount William quarry is surrounded by ranges such as Macedon Range, Dandenong Ranges and Great Diving Range, and standing on the top of the Mount William quarry will able to see the range and the valley. It also home to restricted pocket of original vegetation in modern day along the edge of ridge. • Historic Value: Mount William Stone Axe Quarry is one of the most importance, largest and intensively worked quarries in Australia, with more than 260 mining pits and many mounds of waste rock and flaking floor scatters across the site surrounding the work station. • Scientific Value: Diabase (greenstone) is suitable to aboriginal lifestyle with tool is a raw material which is product of an age of volcanic activity, tough, fine-grained basalt and shock-resistance so it won’t shattered when impact.