Comprehensive Land Use Plan of Pasay City

Petrick Neighborhood Landscaping- When I was in seventh grade, I started a business cutting a couple of my neighbor’s lawns for the summer. Over the past eight years, I have grown my business to service over twenty clients on a weekly basis, providing any and all landscaping needs. Since I am still able to independently service all my clients’ needs, I have never had the time or need for any other summer job. This has been a very beneficial experience for me because I have been able to independently handle all aspects of my business, which has continued to grow every year since the beginning.

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,

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Cenozoic sedimentary rocks predominated to the west and east of the central mountain while plutonic rocks predominated in the peninsular ranges. The irregular contact between these geologic regions reflects the ancient topography of the area. The ancient oceanic crustal plate created an archipelago of a volcanic island. The former's subduction created immense volumes of magma. This resulted to the congealation of plutonic rock in the crust. The local rocks that existed before the tectonic forces uplifted, and erosion capped the deeply buried plutonic rocks that formed a steep and rugged mountains coastline, similar to that present one, which in the west coast of south America.

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.

In the area there are three main large igneous intrusions. Two are the granitic intrusions to the north (Beinn Dearg Bheag/Inner Granite) and south (Beinn an Dubhaich) of the map in Figure 5.1.1, the other is a smaller, patchy intrusion of Micro Diorite which curves across the north-east of the map and appears in blobs in other places within the Agglomerate unit.

First, we must examine the sedimentary formations; when they were formed, how they were formed, and what materials they consist of. About ninety-three to one hundred million years ago, the Western Interior Seaway rolled through the North American continent, eventually reaching the geographical area of today’s Mesa Verde National Park (National Park Service 2005). This sea deposited a thick, hard sandstone base that is called Dakota Sandstone, although this layer is not exposed in the park

The latest rocks in this region were formed in Pleistocene time as imperfectly consolidated gravel of river terraces and alluvial deposits of the

The main function of these maps is identifying the area that is suitable for building an education center on McNabs Island. I divided my analysis maps into three parts which are slope and geology, environment and cultural sites, and microclimate. For the slope and geology map, I combined the slope, bedrock and surficial geology together because I think all of them can majorly determine and describe the topography. Bedrock and surficial geology are the materials that are under the ground. They might form different topography by the geological action including weathering and eroding processes. Also, the slopes can decide whether the land is a plain or a hill. Furthermore, I think slope and geology can risk of the environmental hazards like

One piece of this history is the subsurface Paleozoic rocks. Paleozoic rocks are for the most part hidden in the Park despite being in the Colorado Plateau, which is likely due to both erosion, and it being buried in other various rocks. Next is the deposition of the Moenkopi Formation during the early Triassic time period. When North America was still apart of Pangea, the area that was the Colorado Plateau was located within close range of the Equator. 300-600 feet of sand and mud were accumulated during this time, with marine life being included which tells Geologists that the sea sometimes was in the area. The climate at the time was warm, with varying times of humid and dry spells. There is very few beds of the Moenkopi Formation left in the area once again due to erosion. Third is the deposition of the Shinarump Member of the Chinle Formation. This basal conglomerate was deposited on top of the Moenkopi Formation. It is made up of gravel and sand, which indicates that there was water depositing it. The Shinarump Member also averages between 35-50 feet thick. Next in the geological history is the deposition of Chinle beds later in the Triassic time period. When the sea regressed to the west of the area, a large plain was left behind. As the climate changed, so did the environment. Soon grasslands and marshes began to form in the area. During this time hundreds of feet of shaly material accumulated which formed both the Lower Petrified Forest Member and the Upper Petrified Forest Member. In some parts, these two members are separated by the Sonsela Sandstone Member, composed of the most petrified wood compared to all other rock units featured in the Park. The Owl Rock Member is at the top of the Chinle Formation, and completes it. Near the end of the Triassic time period, tectonic activity was occurring heavily in the Arizona basin. In the western sea at this time a chain of volcanoes erupted,

The Tuscarora formation is in the Silurian age, located in Pennsylvania, mostly composed of quartzite, and is secondarily composed of sandstone. Its thickness is 150-200 feet and is in the lower part of the Silurian age. The Tuscarora formation is in the Clinton group. One member would be Castanea located at the top of the Tuscarora Formation. The depositional environment is, as we know it, a continental shelf of some sort of marine zone because of sediment structures like fossils and cross-bedding. The Tuscarora formation is mainly non-porous and neither

Philippines is an archipelago located in Southeast Asia near the equator. The Philippine archipelago consists of 7,107 islands divided into three major groups of islands which is Luzon, Visayas and Mindanao. As of 2016 the Philippine population is estimated to about 102,624,209 (World Fact Book). The Philippine nationality is termed Filipino and its population is made up of various ethnic groups. The national language is called Tagalog, it also the name of the major ethnic group of the country. According to Philippine Statistic Authority the population of urban area accounts for 45.3% of the country’s total population (Urban-Rural Classification). In contrast, the population in rural area is comprised of 54.7% and considered to be the majority population of the entire country. The Philippine climate is predominantly tropical marine where wet season occurs from November to April and is caused by the northeast monsoon. Similarly, the second set of rainy season, is caused by the southwest monsoon during May to October (World Fact Book). Additionally, the Philippine economy has been relatively resilient to global economic struggles because the country is less exposed to troubled international securities. The lower dependence on exports is what makes the country relatively resilient, relying only domestic products, as well as large remittances from millions of migrant and overseas Filipino workers (World Fact Book). The existing account balance has

 299.735 km²  Capital: Manila  92.337.852 inhabitants  45,2% living below US$2 a day (2006)

The Philippines, is a group of islands in Southeast Asia, sitting in the western Pacific Ocean. It is known as the Republic of the Philippines, and consists of seven thousand, one hundred, and seven islands, that are geographically split into three main divisions, Luzon, Visayas, and Mindanao. The capital is Manila, referred to as the Paris of Asia, and the most populated is Quezon City, which are both part of Metro Manila. The Philippines has a population of close to one hundred,

It has three major island groups which are the Luzon, the largest island and where the capital is located; Visayan, and Mindanao. Eleven islands make up 94 percent of the Philippine landmass, and two of these--Luzon and Mindanao--measure 105,000 and 95,000 square kilometers, respectively. They, together with the cluster of the Visayan Islands that separate them, represent the three principal regions of the archipelago (many scattered islands in a large body of water) that are identified by the three stars on the Philippine flag.