1.
Oakland, California
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Oakland /ˈoʊklənd/ is the largest city and the county seat of Alameda County, California, United States. The city was incorporated in 1852, Oaklands territory covers what was once a mosaic of California coastal terrace prairie, oak woodland, and north coastal scrub. Its land served as a resource when its hillside oak and redwood timber were logged to build San Francisco. In the late 1860s, Oakland was selected as the terminal of the Transcontinental Railroad. Following the 1906 San Francisco earthquake, many San Francisco citizens moved to Oakland, enlarging the citys population, increasing its housing stock and it continued to grow in the 20th century with its busy port, shipyards, and a thriving automobile manufacturing industry. Oakland is known for its sustainability practices, including a top-ranking for usage of electricity from renewable resources, in addition, due to a steady influx of immigrants during the 20th century, along with thousands of African-American war-industry workers who relocated from the Deep South during the 1940s. Oakland is the most ethnically diverse city in the country. The earliest known inhabitants were the Huchiun Indians, who lived there for thousands of years, the Huchiun belonged to a linguistic grouping later called the Ohlone. In Oakland, they were concentrated around Lake Merritt and Temescal Creek, in 1772, the area that later became Oakland was claimed, with the rest of California, by Spanish settlers for the King of Spain. In the early 19th century, the Spanish crown granted the East Bay area to Luis María Peralta for his Rancho San Antonio, the grant was confirmed by the successor Mexican republic upon its independence from Spain. Upon his death in 1842, Peralta divided his land among his four sons, Most of Oakland fell within the shares given to Antonio Maria and Vicente. The portion of the parcel that is now Oakland was called encinal—Spanish for oak grove—due to the oak forest that covered the area. In 1851, three men—Horace Carpentier, Edson Adams, and Andrew Moon—began developing what is now downtown Oakland, on May 4,1852, the Town of Oakland incorporated. Two years later, on March 25,1854, Oakland re-incorporated as the City of Oakland, with Horace Carpentier elected the first mayor, the city and its environs quickly grew with the railroads, becoming a major rail terminal in the late 1860s and 1870s. In 1868, the Central Pacific constructed the Oakland Long Wharf at Oakland Point, a number of horsecar and cable car lines were constructed in Oakland during the latter half of the 19th century. The first electric streetcar set out from Oakland to Berkeley in 1891, at the time of incorporation, Oakland consisted of the territory that lay south of todays major intersection of San Pablo Avenue, Broadway, and Fourteenth Street. The city gradually annexed farmlands and settlements to the east and the north, Oaklands rise to industrial prominence, and its subsequent need for a seaport, led to the digging of a shipping and tidal channel in 1902. This resulted in the town of Alameda being made an island
2.
National Register of Historic Places
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The National Register of Historic Places is the United States federal governments official list of districts, sites, buildings, structures, and objects deemed worthy of preservation. The passage of the National Historic Preservation Act in 1966 established the National Register, of the more than one million properties on the National Register,80,000 are listed individually. The remainder are contributing resources within historic districts, each year approximately 30,000 properties are added to the National Register as part of districts or by individual listings. For most of its history the National Register has been administered by the National Park Service and its goals are to help property owners and interest groups, such as the National Trust for Historic Preservation, coordinate, identify, and protect historic sites in the United States. While National Register listings are mostly symbolic, their recognition of significance provides some financial incentive to owners of listed properties, protection of the property is not guaranteed. During the nomination process, the property is evaluated in terms of the four criteria for inclusion on the National Register of Historic Places, the application of those criteria has been the subject of criticism by academics of history and preservation, as well as the public and politicians. Occasionally, historic sites outside the proper, but associated with the United States are also listed. Properties can be nominated in a variety of forms, including individual properties, historic districts, the Register categorizes general listings into one of five types of properties, district, site, structure, building, or object. National Register Historic Districts are defined geographical areas consisting of contributing and non-contributing properties, some properties are added automatically to the National Register when they become administered by the National Park Service. These include National Historic Landmarks, National Historic Sites, National Historical Parks, National Military Parks/Battlefields, National Memorials, on October 15,1966, the Historic Preservation Act created the National Register of Historic Places and the corresponding State Historic Preservation Offices. Initially, the National Register consisted of the National Historic Landmarks designated before the Registers creation, approval of the act, which was amended in 1980 and 1992, represented the first time the United States had a broad-based historic preservation policy. To administer the newly created National Register of Historic Places, the National Park Service of the U. S. Department of the Interior, hartzog, Jr. established an administrative division named the Office of Archeology and Historic Preservation. Hartzog charged OAHP with creating the National Register program mandated by the 1966 law, ernest Connally was the Offices first director. Within OAHP new divisions were created to deal with the National Register, the first official Keeper of the Register was William J. Murtagh, an architectural historian. During the Registers earliest years in the late 1960s and early 1970s, organization was lax and SHPOs were small, understaffed, and underfunded. A few years later in 1979, the NPS history programs affiliated with both the U. S. National Parks system and the National Register were categorized formally into two Assistant Directorates. Established were the Assistant Directorate for Archeology and Historic Preservation and the Assistant Directorate for Park Historic Preservation, from 1978 until 1981, the main agency for the National Register was the Heritage Conservation and Recreation Service of the United States Department of the Interior. In February 1983, the two assistant directorates were merged to promote efficiency and recognize the interdependency of their programs, jerry L. Rogers was selected to direct this newly merged associate directorate
3.
Beaux-Arts architecture
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Beaux-Arts architecture expresses the academic neoclassical architectural style taught at the École des Beaux-Arts in Paris. The style of instruction that produced Beaux-Arts architecture continued without interruption until 1968. The Beaux-Arts style heavily influenced the architecture of the United States in the period from 1880 to 1920, in contrast, many European architects of the period 1860–1914 outside France gravitated away from Beaux-Arts and towards their own national academic centers. American architects of the Beaux-Arts generation often returned to Greek models, for the first time, repertories of photographs supplemented meticulous scale drawings and on-site renderings of details. Beaux-Arts training emphasized the production of quick conceptual sketches, highly finished perspective presentation drawings, close attention to the program, site considerations tended toward social and urbane contexts. In the façade shown to the right, Diana grasps the cornice she sits on in an action typical of Beaux-Arts integration of sculpture with architecture. A sense of appropriate idiom at the craftsman level supported the teams of the first truly modern architectural offices. The prestige of the École gave the style Beaux-Arts a second wind in combining the new manner with the traditional training and they were followed by an entire generation. Henry Hobson Richardson absorbed Beaux-Arts lessons in massing and spatial planning and his Beaux-Arts training taught him to transcend slavish copying and recreate in the essential fully digested and idiomatic manner of his models. Richardson evolved a personal style freed of historicism that was influential in early Modernism. The White City of the Worlds Columbian Exposition of 1893 in Chicago was a triumph of the movement, the Beaux-Arts curriculum was subsequently begun at Columbia University, the University of Pennsylvania, and elsewhere. From 1916, the Beaux-Arts Institute of Design in New York City schooled architects, painters, bosworth, Carnegie Mellon University, designed by Henry Hornbostel, and the University of Texas, designed by Paul Philippe Cret. Beaux-Arts architecture also brought a civic face to the railroad, two of the best American examples of the Beaux-Arts tradition stand within a few blocks of each other, Grand Central Terminal and the New York Public Library. Another prominent U. S. example of the style is the largest academic dormitory in the world, in the late 1800s, during the years when Beaux-Arts architecture was at a peak in France, Americans were one of the largest groups of foreigners in Paris. Many of them were architects and students of architecture who brought this back to America. Beaux-Arts was very prominent in public buildings in Canada in the early 20th century, notably all three prairie provinces legislative buildings are in this style. Buenos Aires is a center of Beaux-Arts architecture which continued to be built as late as the 1950s, national Theatre, Melbourne General Post Office building, Forrest Place, Perth Argus Building. Beaux-Arts Architecture in New York, A Photographic Guide United States, sixteenth Street Architecture – profiles of Beaux-Arts architecture in Washington D. C
4.
High-rise building
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A tower block, high-rise, apartment tower, residential tower, apartment block, block of flats, or office tower is a tall building or structure used as a residential and/or office building. In some areas it may be referred to as an MDU, in the United States, such a structure is referred to as an apartment building or office building, while a group of such buildings is called an apartment complex or office complex. High-rise buildings became possible with the invention of the elevator and cheaper, the materials used for the structural system of high-rise buildings are reinforced concrete and steel. Most North American style skyscrapers have a frame, while residential blocks are usually constructed of concrete. There is no difference between a tower block and a skyscraper, although a building with fifty or more stories is generally considered a skyscraper. They also pose challenges to firefighters during emergencies in high-rise structures. Studies are often required to ensure that pedestrian wind comfort and wind danger concerns are addressed, in order to allow less wind exposure, to transmit more daylight to the ground and to appear more slender, many high-rises have a design with setbacks. In contrast with low-rise and single-family houses, apartment blocks accommodate more inhabitants per unit of area of land, various bodies have defined high-rise, Emporis Standards defines a high-rise as A multi-story structure between 35–100 meters tall, or a building of unknown height from 12–39 floors. According to the code of Hyderabad, India, a high-rise building is one with four floors or more. The New Shorter Oxford English Dictionary defines a high-rise as a building having many storeys, most building engineers, inspectors, architects and similar professionals define a high-rise as a building that is at least 75 feet tall. The lower floors were occupied by either shops or wealthy families. Surviving Oxyrhynchus Papyri indicate that seven-story buildings even existed in provincial towns, in Arab Egypt, the initial capital city of Fustat housed many high-rise residential buildings, some seven stories tall that could reportedly accommodate hundreds of people. By the 16th century, Cairo also had high-rise apartment buildings where the two floors were for commercial and storage purposes and the multiple stories above them were rented out to tenants. The skyline of many important medieval cities was dominated by large numbers of high-rising urban towers, the residential Towers of Bologna numbered between 80 and 100 at a time, the largest of which still rise to 97.2 m. In Florence, a law of 1251 decreed that all buildings should be reduced to a height of less than 26 m. Even medium-sized towns such as San Gimignano are known to have featured 72 towers up to 51 m in height, the oldest still standing tulou dates back from the 14th century. Tower blocks were built in the Yemeni city of Shibam in the 16th century. The houses of Shibam are all out of mud bricks, but about five hundred of them are tower houses
5.
Mississippi River
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The Mississippi River is the chief river of the largest drainage system on the North American continent. Flowing entirely in the United States, it rises in northern Minnesota, with its many tributaries, the Mississippis watershed drains all or parts of 31 U. S. states and 2 Canadian provinces between the Rocky and Appalachian Mountains. The Mississippi ranks as the fourth longest and fifteenth largest river in the world by discharge, the river either borders or passes through the states of Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and Louisiana. Native Americans long lived along the Mississippi River and its tributaries, most were hunter-gatherers, but some, such as the Mound Builders, formed prolific agricultural societies. The arrival of Europeans in the 16th century changed the way of life as first explorers, then settlers. The river served first as a barrier, forming borders for New Spain, New France, and the early United States, and then as a vital transportation artery and communications link. Formed from thick layers of the silt deposits, the Mississippi embayment is one of the most fertile agricultural regions of the country. In recent years, the river has shown a shift towards the Atchafalaya River channel in the Delta. The word itself comes from Messipi, the French rendering of the Anishinaabe name for the river, see below in the History section for additional information. In addition to historical traditions shown by names, there are at least two measures of a rivers identity, one being the largest branch, and the other being the longest branch. Using the largest-branch criterion, the Ohio would be the branch of the Lower Mississippi. Using the longest-branch criterion, the Middle Mississippi-Missouri-Jefferson-Beaverhead-Red Rock-Hellroaring Creek River would be the main branch and its length of at least 3,745 mi is exceeded only by the Nile, the Amazon, and perhaps the Yangtze River among the longest rivers in the world. The source of this waterway is at Browers Spring,8,800 feet above sea level in southwestern Montana and this is exemplified by the Gateway Arch in St. Louis and the phrase Trans-Mississippi as used in the name of the Trans-Mississippi Exposition. It is common to qualify a regionally superlative landmark in relation to it, the New Madrid Seismic Zone along the river is also noteworthy. These various basic geographical aspects of the river in turn underlie its human history and present uses of the waterway, the Upper Mississippi runs from its headwaters to its confluence with the Missouri River at St. Louis, Missouri. The source of the Upper Mississippi branch is traditionally accepted as Lake Itasca,1,475 feet above sea level in Itasca State Park in Clearwater County, however, the lake is in turn fed by a number of smaller streams. From its origin at Lake Itasca to St. Louis, Missouri, fourteen of these dams are located above Minneapolis in the headwaters region and serve multiple purposes, including power generation and recreation. The remaining 29 dams, beginning in downtown Minneapolis, all locks and were constructed to improve commercial navigation of the upper river
6.
New York City
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The City of New York, often called New York City or simply New York, is the most populous city in the United States. With an estimated 2015 population of 8,550,405 distributed over an area of about 302.6 square miles. Located at the tip of the state of New York. Home to the headquarters of the United Nations, New York is an important center for international diplomacy and has described as the cultural and financial capital of the world. Situated on one of the worlds largest natural harbors, New York City consists of five boroughs, the five boroughs – Brooklyn, Queens, Manhattan, The Bronx, and Staten Island – were consolidated into a single city in 1898. In 2013, the MSA produced a gross metropolitan product of nearly US$1.39 trillion, in 2012, the CSA generated a GMP of over US$1.55 trillion. NYCs MSA and CSA GDP are higher than all but 11 and 12 countries, New York City traces its origin to its 1624 founding in Lower Manhattan as a trading post by colonists of the Dutch Republic and was named New Amsterdam in 1626. The city and its surroundings came under English control in 1664 and were renamed New York after King Charles II of England granted the lands to his brother, New York served as the capital of the United States from 1785 until 1790. It has been the countrys largest city since 1790, the Statue of Liberty greeted millions of immigrants as they came to the Americas by ship in the late 19th and early 20th centuries and is a symbol of the United States and its democracy. In the 21st century, New York has emerged as a node of creativity and entrepreneurship, social tolerance. Several sources have ranked New York the most photographed city in the world, the names of many of the citys bridges, tapered skyscrapers, and parks are known around the world. Manhattans real estate market is among the most expensive in the world, Manhattans Chinatown incorporates the highest concentration of Chinese people in the Western Hemisphere, with multiple signature Chinatowns developing across the city. Providing continuous 24/7 service, the New York City Subway is one of the most extensive metro systems worldwide, with 472 stations in operation. Over 120 colleges and universities are located in New York City, including Columbia University, New York University, and Rockefeller University, during the Wisconsinan glaciation, the New York City region was situated at the edge of a large ice sheet over 1,000 feet in depth. The ice sheet scraped away large amounts of soil, leaving the bedrock that serves as the foundation for much of New York City today. Later on, movement of the ice sheet would contribute to the separation of what are now Long Island and Staten Island. The first documented visit by a European was in 1524 by Giovanni da Verrazzano, a Florentine explorer in the service of the French crown and he claimed the area for France and named it Nouvelle Angoulême. Heavy ice kept him from further exploration, and he returned to Spain in August and he proceeded to sail up what the Dutch would name the North River, named first by Hudson as the Mauritius after Maurice, Prince of Orange
7.
Granite
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Granite is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Granites can be white, pink, or gray in color. The word granite comes from the Latin granum, a grain, in reference to the structure of such a holocrystalline rock. By definition, granite is a rock with at least 20% quartz. The term granitic means granite-like and is applied to granite and a group of igneous rocks with similar textures and slight variations in composition. Occasionally some individual crystals are larger than the groundmass, in case the texture is known as porphyritic. A granitic rock with a texture is known as a granite porphyry. Granitoid is a general, descriptive field term for lighter-colored, coarse-grained igneous rocks, petrographic examination is required for identification of specific types of granitoids. The extrusive igneous rock equivalent of granite is rhyolite, Granite is nearly always massive, hard and tough, and therefore it has gained widespread use throughout human history, and more recently as a construction stone. The average density of granite is between 2.65 and 2.75 g/cm3, its compressive strength usually lies above 200 MPa, and its viscosity near STP is 3–6 •1019 Pa·s. The melting temperature of dry granite at ambient pressure is 1215–1260 °C, it is reduced in the presence of water. Granite has poor primary permeability, but strong secondary permeability, true granite according to modern petrologic convention contains both plagioclase and alkali feldspars. When a granitoid is devoid or nearly devoid of plagioclase, the rock is referred to as alkali feldspar granite, when a granitoid contains less than 10% orthoclase, it is called tonalite, pyroxene and amphibole are common in tonalite. A granite containing both muscovite and biotite micas is called a binary or two-mica granite, two-mica granites are typically high in potassium and low in plagioclase, and are usually S-type granites or A-type granites. A worldwide average of the composition of granite, by weight percent, based on 2485 analyses. Much of it was intruded during the Precambrian age, it is the most abundant basement rock that underlies the relatively thin veneer of the continents. Outcrops of granite tend to form tors and rounded massifs, granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite often occurs as small, less than 100 km² stock masses
8.
Terracotta
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Terracotta, terra cotta or terra-cotta, a type of earthenware, is a clay-based unglazed or glazed ceramic, where the fired body is porous. The term is used to refer to the natural, brownish orange color, of most terracotta. This article covers the senses of terracotta as a medium in sculpture, as in the Terracotta Army and Greek terracotta figurines, asian and European sculpture in porcelain is not covered. Glazed architectural terracotta and its version as exterior surfaces for buildings were used in Asia for some centuries before becoming popular in the West in the 19th century. In archaeology and art history, terracotta is used to describe objects such as figurines not made on a potters wheel. An appropriate refined clay is formed to the desired shape, after drying it is placed in a kiln or atop combustible material in a pit, and then fired. The typical firing temperature is around 1,000 °C, though it may be as low as 600 °C in historic and archaeological examples. In some contexts, such as Roman figurines, white-colored terracotta is known as pipeclay, as such clays were later preferred for tobacco pipes, fired terracotta is not watertight, but surface-burnishing the body before firing can decrease its porousness and a layer of glaze can make it watertight. It is suitable for use below ground to carry pressurized water, for garden pots or building decoration in many environments, most other uses, such as for tableware, sanitary piping, or building decoration in freezing environments, require the material to be glazed. Terracotta, if uncracked, will ring if lightly struck, painted terracotta is typically first covered with a thin coat of gesso, then painted. It has been widely used but the paint is only suitable for indoor positions and is much less durable than fired colors in or under a ceramic glaze. Terracotta sculpture was rarely left in its raw fired state in the West until the 18th century. Terracotta/earthenware was the known type of ceramic produced by Western and pre-Columbian people until the 14th century. Terracotta has been used throughout history for sculpture and pottery as well as for bricks, in ancient times, the first clay sculptures were dried in the sun after being formed. They were later placed in the ashes of open hearths to harden, however, only after firing to high temperature would it be classed as a ceramic material. Terracotta female figurines were uncovered by archaeologists in excavations of Mohenjo-daro, along with phallus-shaped stones, these suggest some sort of fertility cult and a belief in a mother goddess. The Burney Relief is a terracotta plaque from Ancient Mesopotamia of about 1950 BC. In Mesoamerica, the majority of Olmec figurines were in terracotta
9.
Marble
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Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. Geologists use the marble to refer to metamorphosed limestone, however. Marble is commonly used for sculpture and as a building material and this stem is also the basis for the English word marmoreal, meaning marble-like. In Hungarian it is called márvány, Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite rock. Metamorphism causes variable recrystallization of the carbonate mineral grains. The resulting marble rock is composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the carbonate rock have typically been modified or destroyed. Pure white marble is the result of metamorphism of a very pure limestone or dolomite protolith, green coloration is often due to serpentine resulting from originally magnesium-rich limestone or dolostone with silica impurities. These various impurities have been mobilized and recrystallized by the intense pressure, examples of historically notable marble varieties and locations, White marble has been prized for its use in sculptures since classical times. This preference has to do with its softness, which made it easier to carve, relative isotropy and homogeneity, construction marble is a stone which is composed of calcite, dolomite or serpentine which is capable of taking a polish. More generally in construction, specifically the dimension stone trade, the marble is used for any crystalline calcitic rock useful as building stone. For example, Tennessee marble is really a dense granular fossiliferous gray to pink to maroon Ordovician limestone that geologists call the Holston Formation. Ashgabat, the city of Turkmenistan, was recorded in the 2013 Guinness Book of Records as having the worlds highest concentration of white marble buildings. According to the United States Geological Survey, U. S. domestic marble production in 2006 was 46,400 tons valued at about $18.1 million, compared to 72,300 tons valued at $18.9 million in 2005. Crushed marble production in 2006 was 11.8 million tons valued at $116 million, of which 6.5 million tons was finely ground calcium carbonate and the rest was construction aggregate. For comparison,2005 crushed marble production was 7.76 million tons valued at $58.7 million, of which 4.8 million tons was finely ground calcium carbonate, U. S. dimension marble demand is about 1.3 million tons. The DSAN World Demand for Marble Index has shown a growth of 12% annually for the 2000–2006 period, the largest dimension marble application is tile. In 1998, marble production was dominated by 4 countries that accounted for almost half of production of marble
10.
1989 Loma Prieta earthquake
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The 1989 Loma Prieta earthquake occurred in Northern California on October 17 at 5,04 p. m. local time. With a moment magnitude of 6.9 and a maximum Mercalli intensity of IX, no surface faulting occurred, though a large number of other ground failures and landslides were present, especially in the Summit area of the Santa Cruz Mountains. Due to the coverage of the 1989 World Series, it became the first major earthquake in the United States that was broadcast live on national television. Andrew Lawson, a geologist from the University of California, Berkeley, had named the fault after the San Andreas Lake and later led an investigation into that event. The San Andreas Fault ruptured for a length of 290 mi during the 1906 shock, several long term forecasts for a large shock along the San Andreas Fault in that area had been made public prior to 1989 but the earthquake that transpired was not what had been anticipated. The 1989 Loma Prieta event originated on an undiscovered oblique-slip reverse fault that is located adjacent to the San Andreas Fault, since many forecasts had been presented for the region near Loma Prieta, seismologists were not taken by surprise by the October 1989 event. Two moderate shocks, referred to as the Lake Elsman earthquakes by the USGS, occurred in the Santa Cruz Mountains region in June 1988, each events aftershock sequence and effect on stress drop was closely examined, and their study indicated that the shocks affected the mainshocks rupture process. The June 27,1988, shock occurred with an intensity of VI. Its effects included broken windows in Los Gatos, and other damage in Holy City. Farther away from the Santa Cruz Mountains, pieces of concrete fell from a structure at the Sunnyvale Town Center. More moderate damage resulted from the August 8,1989, shock when chimneys were toppled in Cupertino, Los Gatos, other damage included cracked walls and foundations and broken underground pipes. At the office of the Los Gatos City Manager, a window that was cracked had also broken in the earlier shock. Also in Los Gatos, one man died when he exited a building through a window, the Loma Prieta earthquake was named for Loma Prieta Peak in the Santa Cruz Mountains, which lies just to the east of the mainshock epicenter. At sites with rocky terrain, the duration was shorter and the shaking was much less intense, the strong motion records also allowed for the causative fault to be determined – the rupture was related to the San Andreas Fault System. While a Mercalli Intensity of VIII covered a large swath of territory relatively close to the further to the north. At more than 44 miles distant, the San Francisco Bay Area recorded peak horizontal accelerations that were as high as 0. 26g, in a general way, the location of aftershocks of the event delineated the extent of the faulting, which extended about 24 miles in length. Because the rupture took place bilaterally, the duration of strong shaking was about half of what it would have been had it ruptured in one direction only, the duration of a typical M6.9 shock with a comparable rupture length would have been about twice as long. Gregory Beroza, a seismologist with Stanford University, made several distinctions regarding the 1906 and 1989 events, near Loma Prieta, the 1906 rupture was more shallow, had more strike-slip, and occurred on a fault that was near vertical
11.
Port of Oakland
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The Port of Oakland is a major container ship facility located in Oakland, California, in the San Francisco Bay. It was the first major port on the Pacific Coast of the United States to build terminals for container ships and it is now the fifth busiest container port in the United States, behind Long Beach, Los Angeles, Newark, and Savannah. Originally, the estuary,500 feet wide, had a depth of two feet at low tide. 22 years later, in 1874, the dredged shipping channel was deepened to make Oakland a deep water port. In the late 19th century, the Southern Pacific was granted rights to the port. This act, protested by the SP and later held up in court, the courts ruled that all landfill since the date of the agreement did not belong to the SP. This ruling ended SP control and made the modern Port of Oakland possible, on May 6,1915, the Admiral Dewey became the first vessel to dock at the foot of Clay street. Captain J. Daniels, master of the vessel, was greeted by Commissioner of Public Works Harry S. Anderson, keith, the two men who had so much to do with the upbuilding of the citys waterfront, were the first aboard the boat. Captain do you realize that you are the commander of the first big vessel that has ever tied up to what will eventually be the busiest wharf on the Pacific Coast, Anderson asked that official as he shook Captain J. Daniels hand. I certainly do realize that, Mr. Anderson, returned Captain Daniels, and I assure you that I appreciate the honor. Ive been many years on the sea, but I have never docked a ship at a better wharf than this. -Source Oakland Tribune May 7,1915. However, the port was not officially named the Port of Oakland until 1927, in 1962, the Port of Oakland began to admit container ships. Container traffic greatly increased the amount of loaded and unloaded in the Port. By the late 1960s, the Port of Oakland was the second largest port in the world in container tonnage, during an expansion of the Port in the late 1960s, fill material was added to what remained of the old Southern Pacific mole. The fill came largely from the concurrent excavation of the Berkeley Hills Tunnel during the construction of the BART system. The BART trunk line also crosses over part of the port, one of the main limitations to growth was the inability to transfer containers to rail lines, all cranes historically operating between ocean vessels and trucks. The Port retained VZM, Korve Engineering and Earth Metrics to perform engineering and that brought the cumulative investment of port expansion to over 1.4 billion dollars since 1962, half of which was comprised by the intermodal facility. Also, the Port is now reaping the benefits of investment in post-panamax cranes, dredging, and the transfer of military property, deepening of the port from 42 feet to 50 feet to accommodate larger ships has been completed
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