Geology & Civil Engineering Essay

GEOLOGY & CIVIL ENGINEERING
As living creatures, the importance of understanding the earth we live in is paramount for our survival and development. Geology is the “scientific study of the origin, history and structure of the earth”. It involves understanding earth’s processes, materials and its effects on all forms of life. From earth elements such as rocks and mountains to natural phenomenon such as volcanoes and earthquakes, the field of geology encompasses a wide range of concepts fundamental to many professions and to civilization in general. Scientific disciplines such as civil engineering and environmental sciences, for instance, rely on a deeper understanding and appreciation for earth’s landforms and processes. Generally, any environmentally-related field requires a background on geological studies. Since civil engineers are ideally responsible for the built environment, an understanding of the ground upon which various infrastructures and facilities are built is of great importance. The works of a civil engineer includes structures that facilitate transport, water supply, shelter and living dwellings, hydropower, flood control and environmental protection, sewage and waste disposal, urban development and more. These structures include the highways, bridges and railways we traverse on a daily basis, dams and reservoirs that service a community with water, different energy systems and much more. We can clearly see the contributions made to civilization through civil engineering works. These contributions cannot however be possible without our natural environment – the earth. Consequently, the understanding of this natural building material is indispensable for the construction of safe and reliable infrastructures. One of the tallest standing skyscrapers in the world, Burj Khalifa, stands 838m tall in the country of Dubai (Fig.1). Imagine if this structure was unknowingly built on top of a fault line and crumbled under the impact of an earthquake. The persons inside and in the near vicinity of the building would suffer tremendously. In addition to safety, the cost (both economic and social) of such a catastrophic event could be crimpling. Consider the 1928 failure of the St. Francis Dam in California which led to a flood resulting in the death of up to 600. Two of the reasons for failure were due to the instability of landslide material upon which the dam was built and the position material upon which the dam was built and the position of the dam with respect to the underground fault.

Many failures have occurred worldwide due to the inconsistency and unknown behaviour of the ground conditions above which such structures are constructed. Thus the understanding of how the ground will behave with respect to infrastructures is fundamental to civil engineering. In addition to safety issues and costs, the scope of geology is also important for civil engineering when it comes to knowledge of construction materials. For example, cement, one of the most widely used construction materials, is comprised of inert granular materials such as sand, gravel, or crushed stone known as aggregates. Clays, limestone, laterite and other building stones are other construction materials of the earth whose occurrence, composition, durability and other properties of concern to the construction industry are studied in geology. Other features of geology important to civil engineering include: The knowledge of natural elements and phenomena such as water, wind, ice and earthquake The knowledge of erosion, transportation and deposition with solving river control, coastal and harbour work, and soil conservation problems The knowledge of groundwater present in subsurface rocks important for water supply irrigation, excavation etc. Foundation problems, as mentioned before, of dams, bridges, and buildings due to the geology of the site In tunnelling, constructing roads, canals, and docks and in determining the stability of cuts and slopes, the knowledge about the nature and structure of rocks is very necessary. The knowledge of geological features such as faults, joints, folding and solution channels can assist greatly with the stability of civil engineering structures The study of soil material is important generally

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Geology is integrated in foundation engineering, construction materials engineering, infrastructure engineering, disaster mitigation, land-use engineering, water resources engineering and environmental engineering. Generally, civil engineers depend on geology to attain information about how the earth and its processes will affect their designs and how the earth as a material can be used for the improvements of structures.

GEOLOGICAL FEATURES:
Certain regions across the world have interesting and unique geological features. Some of the world’s most amazing geological wonders shown in Fig.2
include The Wave on the border of Arizona and Utah, the Antelope Canyon in Arizona, the Great Blue Hole of Belize, The Blue Lake Cave in Brazil, The Crystal Cave of the Giants in Mexico, the Eye of the Sahara in Mauritania, Giants Causeway in Ireland, Hell Gate in Turkmenistan and many more.

Fig.2 Geological Feature of the World
The islands of the Lesser Antilles form another region of geological interest – a volcanic island arc. Volcanic arcs refer to a chain of volcanoes arranged in an arc shape, as the name implies. They are formed as a result of the subduction of an oceanic tectonic plate under another tectonic plate, usually parallel to an oceanic trench. Volcanic island arcs consist of islands characterized by offshore volcanoes. They are formed by the ongoing process of subduction where two areas of oceanic crusts collide. The difference between a volcanic arc and volcanic island arc is shown in Fig.3.

Volcanic Island arc formed by
oceanic-oceanic subduction
Volcanic arc formed by
oceanic-continental subduction
Fig.3 Plate Movements of a Volcanic Island Arc (left) and Volcanic Arc (right)

THE LESSER ANTILLES ISLAND ARC
The Lesser Antilles island arc is comprised of a chain of about 15 major and many minor volcanic islands. It stretches about 530 miles between Puerto Rico and Venezuela, separating the Atlantic Ocean and the Caribbean Sea. The arc is bordered to the north and west by the Puerto Rican Trench, reaching a depth of up to 9200m. Its formation is a result of the subduction of the oceanic crust of the North American Plate under the Caribbean Plate in the Lesser Antilles subduction zone. The Caribbean plate slides about 2cm/yr eastward relative to the North American Plate. Along its northern boundary, the motion of the Caribbean plate is primarily strike-slip (a geological fault in which an adjacent surface moves horizontally), with a small component of shortening. The eastern boundary of the Caribbean plate, however, overrides the North American plate creating the Lesser Antilles
islands.

Fig. 4 Caribbean and North American Plates

Fig.4 The Subduction of Caribbean and North American Plates
THE SUBDUCTION PROCESS
The process of subduction occurs whenever two sections of the Earth’s crust collide, forcing one section back into the Earth. Subduction zone volcanism occurs when one plate containing the oceanic lithosphere is forced under the adjacent plate due to the action of convection currents. The submerged oceanic lithosphere plate is then reabsorbed into the earth’s mantle. Where the descending plate bends downward at the surface, a large linear depression known as an oceanic trench is formed- in this case, the Puerto Rican Trench. These trenches are the deepest topographic features on the earth’s surface, reaching up to 11 km below sea level (Mariana Trench). The crustal portion of the subducting slab contains a vast amount of surface water, and water contained in hydrated minerals within the seafloor basalt. Now as the subducting slab descends deeper and deeper into the earth, it encounters increasingly greater temperatures and pressures which cause the slab to release water into the mantle wedge overlaying the descending plate.

The water then lowers the melting temperature of the mantle, causing it to melt. Magma, varying from basalt to andesite, is produced and rises upwards to form a linear belt of volcanoes parallel to the oceanic trench.

ISLANDS OF THE LESSER ANTILLES
The Lesser Antilles include:
Leeward Islands:
Virgin Islands
St. Thomas
St. John
St. Croix
Water Island
Tortola
Virgin Gorda
Anegada
Jost Van Dyke
Anguilla
Saint Martin/Sint Maarten
Saint-Barthélemy
Saba
Sint Eustatius
Fig.5 The Lesser Antilles
Saint Kitts
Nevis (St. Kitts and Nevis)
Barbuda (Antigua and Barbuda)
Antigua (Antigua and Barbuda)
Redonda (Antigua and Barbuda)
Montserrat
Guadeloupe
La Désirade
Marie-Galante
les Saintes archipelago
Dominica
Windward Islands:
Martinique
Saint Lucia
Saint Vincent
Grenadines
Barbados
Grenada
Tobago
Trinidad (Sometimes considered part of the Windward Islands.) Leeward Antilles – islands north of the Venezuelan coast (from west to east): Aruba
Curaçao
Bonaire
Los Roques Archipelago
La Orchila
La Tortuga
La Blanquilla
Margarita Island
Coche
Cubagua
Other islands

The Lesser Antilles consists of about seventeen active volcanoes. Active strato-volcanoes can be found in the submarine Kick ‘em Jenny, north of Grenada; at Soufriere at the northern end of St Vincent; at the well-known Mt Pelee at the northern end of Martinique; at Soufriere on the island of BasseTerre, Guadeloupe; and at Montserrat. Strato-volcanoes mean that there are numerous layers of lava flows and fragmented debris. There is also the geothermal area at Soufriere, St. Lucia. Other islands, while not active in historic times cannot be considered extinct, including the islands of Saba at extreme north-western end of the active arc, St. Eustatius (or “Statia”); St Kitts, dominated by the Mt Misery centre, Nevis which has a single cone and crater also has some geothermal activity; and Dominica. Grenada alone which has reached the usually late stage of producing alkaline orogenic basalts is probably completely extinct. Kick ‘em Jenny is an active underwater (submarine) volcano on the floor of the Caribbean Sea. It is located about 8km north of Grenada. It is the most frequently active volcano in the region. Between 1939 (first eruption) and 2001 (most recent eruption), at least 12 eruptions were noted. With each submarine eruption, deposits of volcanic material then accumulate around the summit. This demonstrates how the volcanic islands of the Lesser Antilles were formed and began from submarine eruptions.

Soufriere volcano forms the northern end of the island of St. Vincent. This stratovolcano reaches about 1178 m high with its peak (to the left) being the NW rim of a large crater created by a massive volcanic landslide. Since 1718, multiple powerful explosive eruptions have occurred.

Mt Pelee is one of the deadliest volcanoes in the world. It is famous for its 1902 eruption that led to the death of about 30,000 people. It is located at the northern end of the island and French overseas department of Martinique. The volcano has an elevation of 1,397 m.

Due to volcanic and tectonic activity, other geological phenomenon such as tsunamis and earthquakes are common occurrences of this region. Strong earthquakes often accompany the rise of magma to the surface. The subduction process and resulting volcanic eruptions leading to the formation of the islands of the Lesser Antilles are processes still ongoing today. Although most of the volcanoes are dormant, the major ones explained above are quite a cause for concern and could explode unexpectedly.

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