75 Sentences With "became more concentrated"

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Two-thirds of them became more concentrated between 1997 and 2012.
Of America's roughly 900 sectors, two-thirds became more concentrated between 1997 and 2012.
APPLE INC'S SUPPLY CHAIN BECAME MORE CONCENTRATED IN CHINA BETWEEN 2015 AND 2019 - DATA
Two-thirds of them became more concentrated between 353 and 2012 (see charts 2 and 3).
A study by The Economist found that between 1997 and 2012, two-thirds of industries became more concentrated.
An analysis in The Economist in 214 showed that two-thirds of American industries became more concentrated in the 22000s.
The domestic air travel market in Brazil became more concentrated in the quarter after Avianca Brasil ceased operations in late May following a bankruptcy filing.
We show that firms in industries that became more concentrated have enjoyed significantly higher profitability and profit margins, greater gains from mergers, and significantly higher stock returns.
Sicker people would likely stay in the community-rated market, but that market's costs would increase as it became more concentrated with people who have high medical costs.
As cities and towns industrialized, as wealth became more concentrated, and as the rich got richer, the middle class began sinking to the level of the working class.
Budget rival Lion Air, which does not publish financial results, also cut capacity as the market became more concentrated, with Garuda taking operational control of the third-largest player, Sriwijaya Air.
As law professor Tim Wu writes in The Curse of Bigness: Antitrust in the New Gilded Age: In the United States, between 1997 and 2012, 75 percent of American industries became more concentrated.
In support of this argument, we show that over the last two decades, firms in industries that became more concentrated possess, not only a larger number of patents, but also the most valuable ones.
The weakening of antitrust enforcement, and the failure of regulation to keep up with changes in our economy and the innovations in creating and leveraging market power, meant that markets became more concentrated and less competitive.
The historically ethnically diverse areas of North and South Omaha became more concentrated by economics, race, and class. These workers suffered dramatic job losses during the industrial restructuring that increased rapidly in the 1960s, and poverty became more widespread.
On July 11, a low pressure formed southwest of Central America. The next day, the system began to organize. After a decrease in convection, the system became more concentrated. After additional development, the NHC upgraded the disturbance into Tropical Depression Six-E on July 14.
After four days, the system regenerated and under diffluent flow aloft, deep convection became more concentrated; it is estimated that a tropical depression formed at 0000 UTC on October 16, about west-southwest of Manzanillo, Mexico. Initially, due to disorganization, determining the forward movement of depression was difficult, although a few hours later it was estimated that the system was tracking to the north-northwest. With favorable conditions aloft, the deep convection became more concentrated, and 12 hours after first developing, the depression intensified into Tropical Storm Madeline about southwest of Cabo Corrientes. During the afternoon, convective cloud tops warmed slightly although the storm continued to intensify.
A number of these technical schools originally taught poor children trades such as carpentry and building skills for which they could progress to gain apprenticeships and employment. As the National School system and vocational schools developed in the Irish Republic, the Irish Christian Brothers became more concentrated on secondary education.
Lovato's later poems were easily distinguishable from his earlier poems because of their differences not just in style but also in content and theme. Lovato's later poems became more concentrated on the subjects such as politics and morality.Witt, 2000, p. 103. Stylistically Lovato's later poems were more medieval in character.
Lorena eventually became the dominate system, and absorbed the remnants of Kiko on August 29. Moving slowly out to sea, Lorena reached minimal hurricane strength on the September 1 as the convection became more concentrated. Lorena was a hurricane for less than a day. It weakened quickly to a depression on September 3.
The origins of Rachel can be traced back to a tropical wave that moved off the west coast Africa in mid-September 1990. It moved westward into the Caribbean Sea without significant development. Poorly organized, the wave entered the Eastern Pacific on overnight September 22\. The thunderstorm activity became more concentrated two days later.
On June 22, showers increased associated with a tropical wave several hundred miles away from land. Three days later, deep convection became more concentrated, and the system became a tropical depression. It intensified into Tropical Storm Carlos as banding features increased and the outflow became better defined. As it moved west, convection diminished as Carlos moved into cooler water.
Despite the presence of vertical wind shear, convection became more concentrated. The circulation became better-defined, indicating that Tropical Depression Eleven developed at 1800 UTC on August 28, while located about southwest of the western Azores. The depression initially moved westward before turning northwestward on August 29 in response to a weakness in the subtropical ridge. Minimal intensification was predicted, due to dry air and wind shear.
On July 9, showers and thunderstorms associated with an area of disturbed weather located about south of the southern tip of Baja California became more concentrated around a developing low level centre. In the early hours of July 10, the system was designated as Tropical Depression Four-E, and the NHC commenced advisories. Around 2:00 p.m. PDT, the system strengthened into Tropical Storm Carlos.
The first major hurricane of the season originated from a broad area of low pressure on July 8 near the Gulf of Tehuantepec. The thunderstorms gradually became more concentrated and a tropical depression formed on July 12. It strengthened into a tropical storm twelve hours later, and then began to rapidly intensify as convection increased further near the center. It became a hurricane on July 13.
A tropical wave crossed the west coast of Africa between August 15 and August 16. Later that day and early on August 17, the system began developing more convection, while located just west of Sierra Leone. As a result, the National Hurricane Center (NHC) began monitoring the system in the Tropical Weather Outlooks (TWOs). Thereafter, further organization briefly halted, though by early on August 18, associated convection became more concentrated.
The number of farms also decreased and their ownership became more concentrated; for example, between 1967 and 2002, one million pig farms in America consolidated into 114,000, with 80 percent of the production on factory farms. According to the Worldwatch Institute, 74 percent of the world's poultry, 43 percent of beef, and 68 percent of eggs are produced this way. Famines however continued to sweep the globe through the 20th century.
However these were also eventually abolished and their units amalgamated into CINCFLEET. At the same time, the commands established to manage individuals naval bases were replaced in 1969 after the post of Commander-in-Chief, Plymouth was merged with that of Commander-in-Chief, Portsmouth to form Naval Home Command. As overseas bases continued to be reduced, the Navy's shore establishments became more concentrated in the UK, under Naval Home Command.
The company's difficulties were attributed in part to changes in the North American office supply market overall. Distribution became more concentrated as stores consolidated through mergers and acquisitions and new superstores became more important players. Competition was intense between the large distributors, and prices overall were forced down. By 1993, Esselte Pendaflex had a smaller pool of customers than in past years, though the customers on the whole were larger.
Hurricane Javier probably originated from a tropical wave that left Africa on July 17. While it showed some signs of organization off the west coast of Africa, most of the convection dissipated by time it was near the Lesser Antilles. Around the time it entered the Pacific on July 27, thunderstorm activity increased and became more concentrated. By July 30, the cloud pattern began to organize, though it was initially elongated.
By July 11, dry air and unfavorable wind shear prevented the convection from developing near the center. The low became elongated, though on July 12 the overall convection became more concentrated as it turned to a northeast drift. An approaching mid-level trough caused the system to accelerate northeastward across Florida Panhandle, though upon doing so the thunderstorm activity quickly diminished. On July 13, forecasters expected the system to be absorbed by the approaching trough.
A strong pulse in the Madden–Julian oscillation—a propagating climate pattern associated with increased tropical cyclogenesis—may have aided in creating favorable conditions for further development. Moving south of the Gulf of Tehuantepec on October 18, the system consolidated and developed a small, defined circulation. Associated convection became more concentrated around its center. Another gap wind event soon impacted the system, temporarily delaying development of the disturbance into a tropical depression.
The slow-moving disturbance tracked towards the south and southeast, steered by a broad area of high pressure. On November 23, 01F attained tropical depression status. Supported by the stout outflow of air at the upper-levels of the troposphere, shower activity became more concentrated around the center of circulation. The depression reached tropical cyclone intensity by 06:00 UTC on November 24 near the Santa Cruz Islands, earning the name Rita.
On April 30, Météo-France (MFR) classified the system as a zone of disturbed weather. It slowly organized, prompting the Joint Typhoon Warning Center (JTWC) to issue a tropical cyclone formation alert late on May 2, around the time that MFR classified it as Tropical Disturbance 14. The thunderstorms became more concentrated around an increasingly well-defined center, and with minimal wind shear, the system strengthened into Tropical Depression 14 on May 3.
A tropical wave moved off the west coast of Africa on August 14. A ridge of high pressure to its north caused the wave to move quickly westward. An area of convection developed along the wave axis to the south of the Cape Verde islands, and on August 15, meteorologists began classifying the system with the Dvorak technique. The thunderstorm activity became more concentrated, and narrow spiral rainbands began to develop around a center of circulation.
A tropical wave moved off the coast of Africa on August 14. Under the influence of a ridge of high pressure to its north, the wave tracked quickly westward. An area of convection developed along the wave axis to the south of the Cape Verde islands, and on August 15 meteorologists began classifying the system with the Dvorak technique. The thunderstorm activity became more concentrated, and narrow spiral rainbands developed around a developing center of circulation.
Festival Republic is a UK music promoter. It was founded as Mean Fiddler Group in 1982 by Irish-born chairman John Vincent Power, as a venue-management and music-promotion group. After the group was taken over by Hamsard Ltd in 2005, the focus became more concentrated on festivals, and in 2007 the venues along with the Mean Fiddler name were sold on, with the remaining company being renamed Festival Republic. Melvin Benn is the current managing director.
Tropical Storm Agatha originated from an area of convection, or thunderstorms, that developed on May 24, off the west coast on Costa Ricaam. At the time, there was a trough in the region that extended into the southwestern Caribbean Sea, associated with the Intertropical Convergence Zone. The system drifted northwestward, and conditions favored further development. On May 25, the convection became more concentrated, and the National Hurricane Center (NHC) noted the potential for a tropical depression to develop.
It is thought there was pottery manufacture of coarse ware in Goldenhill during the 16th century. At the beginning of the 19th century there were six potteries works. During the century pottery manufacture became more concentrated in Tunstall, which had 13 potteries by 1834, compared with two in Goldenhill; in 1863 there were 19 potteries in Tunstall and one in Goldenhill, which closed soon afterwards. There was coal mining on a small scale in the 1700s.
The size of the building on top of the mound also shows how power became more concentrated and centralized over time. The governing body became smaller; structures three and two present this notion. The mound could have been built as a display of power and prestige, for practical purposes, or both. However, in the search for the existence of political power of governing persons, Mound 6 at Paso de la Amada provides evidence and allows for discussion and speculation.
On July 6, a tropical wave moved off the coast of Africa. Moving westward, the disturbance gradually organized until July 10, at which point convection became more concentrated, and it is estimated Tropical Depression Five formed in the central tropical Atlantic that evening. Late on July 11, it strengthened and was named Tropical Storm Emily. Initially forecast to strengthen rapidly and move west-northwest through the Greater Antilles, Emily instead moved almost due west toward the Windward Islands, remaining a moderate tropical storm.
Chrysoberyl forms as a result of pegmatitic processes. Melting in the Earth's crust produces relatively low-density molten magma which can rise upwards towards the surface. As the main magma body cools, water originally present in low concentrations became more concentrated in the molten rock because it could not be incorporated into the crystallization of solid minerals. The remnant magma thus becomes richer in water, and also in rare elements that similarly do not fit in the crystal structures of major rock-forming minerals.
The system drifted westward, and early on October 14 the convection became more concentrated and a little better organized as upper- level wind shear lessened slightly. Later on October 14, the system became much better defined, with increasingly organized shower and thunderstorm activity, as conditions in the upper levels of the atmosphere became significantly more favorable. It was then that the National Hurricane Center first indicated that it was possible for a tropical depression to develop in the area. Dvorak classifications were initiated on October 15.
On September 9, a tropical depression formed in the South China Sea in the west Pacific basin. Two days later, the system struck Vietnam and progressed westward through Indochina. The remnants entered the Bay of Bengal around September 13, accompanied by increasing convection. Moving to the west-northwest, the system resembled a monsoon depression at times, although the thunderstorms gradually became more concentrated. On September 16, the system developed into a depression, and on the same day the JTWC classified it as Tropical Cyclone 01B.
The tropical depression originated from a tropical wave off the southern coast of Mexico in late May 2006\. An area of convection was associated with the wave, and forecasters at the National Hurricane Center (NHC) remarked that environmental conditions favored gradual development. The system, which was enhanced by the Intertropical Convergence Zone (ITCZ), drifted northward with an anticyclone to its east and west. On June 1, the convection became more concentrated, and by early the next day it developed a low pressure area; by that time, it began a steady northwestward track.
As a result of industrialization, the population became more concentrated into urban areas. By 1900, the Twin Cities were becoming a center of commerce, led by the Minneapolis Grain Exchange and the foundation of the Federal Reserve Bank with its ninth district in Minneapolis. Many of the businessmen who had made money in the railroad, flour milling, and logging industries lived in the Twin Cities and personified the gilded age. They started to donate money for cultural institutions such as the Minneapolis Symphony Orchestra (now the Minnesota Orchestra).
Shortly thereafter, the Joint Typhoon Warning Center (JTWC) followed suit by initiating advisories on Tropical Depression 17W, and the Hong Kong Observatory (HKO) followed suit early on August 3. Initially, it moved generally to the west-northwest, owing to a mid-level ridge over eastern China. The convection became more concentrated, and the JMA upgraded the depression to Tropical Storm Kammuri late on August 3, to the south of Hong Kong. An upper-level low connected to a trough weakened the ridge over China, allowing Kammuri to move slowly northward.
The composition of exports shows that whereas in 1963 processed and semi-processed manufactured exports accounted for only 5% of total exports, in 1974 their share had reached 29%. In the 1968–73 period, personal income became more concentrated and regional disparities became greater. Industrial expansion took place more vigorously in the Center-South Region, which had benefited most from the import substitution industrialization strategy. Its per-capita income considerably exceeded the national average, its infrastructure was more developed, and it had an adequate supply of skilled workers and professionals.
Enrique formed from a westward-moving tropical wave that crossed the Atlantic from June 30 to July 8. A short-lived cyclonic circulation center within the wave was detected on satellite imagery when the system was over the eastern Atlantic. However, persistent deep convection did not occur until the wave neared the Gulf of Tehuantepec in the eastern Pacific Ocean on July 11. On July 12, the convection became more concentrated about south of Acapulco, near a mid-level vortex within the wave; however, it had diminished the next day.
A tropical wave moved off the coast of Africa on September 10, with evidence of a low-level circulation and convective banding. It moved west-northwestward, located south of a subtropical ridge. Based on satellite imagery, it is estimated the system organized into Tropical Depression Nine by 1200 UTC on September 11 to the south of the Cape Verde islands. Upon its formation, the center was poorly defined, with restricted easterly outflow due to easterly wind shear. After about 24 hours of remaining somewhat disorganized, the convection became more concentrated on September 12 as banding features and outflow improved.
Ford's River Rouge assembly plant 1941 As a result of industrialization, the population became more concentrated into urban areas. In part to balance democratic representation against the economic and political power of these corporations, the region hosted industrial labor organization, consolidated agricultural cooperatives and state educational systems. The Big Ten Conference memorializes the nation's first region in which every state sponsored major research, technical-agricultural, and teacher-training colleges and universities. The Congress of Industrial Organizations grew out of the region's coal and iron mines; steel, automobile and rubber industries; and breakthrough strikes and contracts of Ohio, Indiana, and Michigan.
The combination of vertical wind shear and the wave's proximity to land impeded further development. Convection increased along the northern portion of the wave on July 24, although by the following day the NHC expected no significant redevelopment. Early on July 26, the thunderstorms along the tropical wave became more concentrated to the south of Cuba, in association with a low- pressure area. The system continued to organize, and by 0600 UTC on July 27, the surface circulation became defined enough for it to be classified as a tropical depression about 60 mi (95 km) northeast of Cancún, Mexico.
Long before the Holocaust, antisemitism threatened Eastern European Jews. Many Jews immigrated to the region after having been expelled from Western Europe during the 15th and 16th centuries, and their communities only became more concentrated when the Russian government confined them to the area, specifically the nations of modern-day Latvia, Lithuania, Poland, Belarus, Ukraine, Slovakia, and parts of northern Hungary. Once they were settled, the Jews still weren't safe. A never-before-seen film shot in the 1920s reveals the aftermath of a pogrom, where Cossacks tore through Jewish neighborhoods raping, maiming, killing, and looting.
The low moved north-northeastward, and gradually became better organized despite high amounts of vertical wind shear. The deep convection became more concentrated near the center, and it is estimated the system developed into a tropical depression at 1200 UTC on June 1 just to the northwest of the western tip of Cuba. Operationally, it was not classified until eleven hours later. Animated radar image from Tampa of Tropical Storm Barry passing through Florida on June 2 The depression developed a large area of squalls, and organized enough to warrant a Hurricane Hunters flight into the area.
A tropical wave moving westward off the African coast on October 1, 2001 entered the tropical Atlantic. The wave's organization changed little until October 4 as it moved westward, when curved banding features began to increase. However, little improvement in the wave's organization occurred until October 6 after continuing to move westward for two days, when an area of low pressure was identified by the National Hurricane Center. Afterward, the cloudiness became more concentrated, and the system organized into a tropical depression by noon on October 6, shortly after the first advisory from the NHC was issued at 11 a.m. AST.
Hurricane Leslie near its initial peak intensity on 3 October Soon after being re- classified, Leslie moved to the due west under the interactions with the subtropical ridge to the west and a large deep-layer low that formed to the east. On 29 September, the storm turned to the southwest as it embedded to the deep-layer low, and Leslie's deep convection became more concentrated near the center. This signified its transition into a tropical cyclone. Later that day, Leslie developed an anti-cyclonic outflow to its northeast and southeast, and it developed a warm core structure.
A tropical wave moved off the coast of Africa on July 11. It moved westward and quickly developed two areas of convection along the wave axis. One of the areas nearly developed into a tropical depression after moving northwestward, though it failed to organize further and dissipated. The southern area continued westward and ultimately entered the eastern Pacific Ocean on July 21. Thunderstorms along the wave axis became more concentrated a few hundred miles south of the Gulf of Tehuantepec, and the system developed into Tropical Depression Five-E on July 24 while located 500 mi (800 km) southwest of Manzanillo, Mexico.
The second named storm of the season originated from a slow-moving area of increasing cloudiness over the Gulf of Tehuantepec on June 14. Moving little, a broad area of low pressure formed within the mass, but the low remained disorganized, although a tropical wave moved through on June 16. However, another tropical wave moved through on June 18, and the area of cloudiness gradually became more concentrated, and post-storm analysis indicated that a tropical depression formed on June 18 near Huatulco, as banding increased. A report of tropical storm-force winds from a ship was issued, and the depression was quickly upgraded to Tropical Storm Beatriz.
On October 11, a fast-moving tropical wave moved off the coast of Africa, and traversed the Atlantic without development. By October 20, the disturbance emerged into the Pacific Ocean. The next day, a weak surface circulation developed in response to a Gulf of Tehuantepec wind gap event. Organization continued further over the next two days, and after deep convection became more concentrated and the low became better defined, it is estimated that Tropical Depression Twenty-E formed around 06:00 UTC on October 23 about south of Manzanillo, Mexico, later strengthening into a tropical storm six hours later and assigned the name Seymour, accordingly.
In addition there were other places that specialized in the salt extraction, providing a precious trading commodity, especially for groups that lived inland. Skill in multi-colored ceramic art reached an advanced level; new colors and styles became available to local ceramic artisans, clearly inspired by Mesoamericana. In the heart of Costa Rica populations became more concentrated in organized economic and political centers, that would form living and ceremonial groups. The most well-known archeological site of this kind is Guayabo in Turrialba, which contains raised mounds with walls of stone, access ramps and pedestals, as well as aqueducts, elevated platforms, circular and rectangular foundations, paved walkways and other structures.
A westward-moving tropical wave entered the Pacific Ocean in mid-May. Convection within the disturbance became more concentrated and organized on May 19 while the wave was located a short distance south of the Gulf of Tehuantepec. The deep convection concentrated around a low-level circulation with expanding outflow, and the system developed into Tropical Depression One-E on May 21, while located about 400 mi (645 km) south of Manzanillo, Mexico. Initially the depression was forecast to strengthen to reach winds of 55 mph (90 km/h) as it moved westward under the influence of a high-pressure system to its north.
Under the influence of a mid- to upper-level ridge to its north, the depression tracked west-northwestward. Convection became more concentrated as outflow organized further, and 18 hours after the depression first developed, it intensified into Tropical Storm Darby. Located in an area conducive to further development, Darby attained hurricane status on July 24, subsequent to the development of a 17-mile (27 km)-wide eye. The eye became more distinct while surrounded by an area of deep convection, and on July 25 the hurricane reached peak winds of 115 mph (185 km/h) about 850 miles (1370 km) southwest of Cabo San Lucas.
The new disturbance then turned towards Hispaniola and Puerto Rico, at which point the National Hurricane Center began to monitor the disturbance for possible tropical cyclogenesis. On November 7, convection increased as it passed to the northeast of Hispaniola; however, surface pressures were still relatively high. By early on November 8, showers and convection became more concentrated around the area of low pressure, and there was indications that the disturbance was producing gale-force winds in squally bands that were short-lived. It is estimated that Tropical Depression Twelve formed at around 18:00 UTC, after further organization occurred, while located north of the Turks and Caicos Islands.
A tropical wave moved westward off the coast of Africa on July 14. After tracking steadily westward, an area of thunderstorms became more concentrated as its upper-level environment became more favorable, and late on July 19 the National Hurricane Center classified it as Tropical Depression Six while it was located about east of the Lesser Antilles. Upon being classified as a tropical cyclone, the depression maintained two ill- defined hooking bands to its north and south, and was originally forecast to attain hurricane status before passing through the Lesser Antilles. With warm waters and very light wind shear forecast, its environmental conditions met four out of five parameters for rapid intensification.
Initially, the disturbance's development was impeded by the trough aloft and adjacent land, though the National Hurricane Center (NHC) noted favorable conditions for tropical cyclogenesis over the Bay of Campeche, coupled with abating wind shear. On June 26, the disturbance moved inland over the Yucatán Peninsula, emerging into the bay the next day as it produced a surface low. Despite moderate shear, a Hurricane Hunters flight into the system revealed that a closed wind circulation had formed at sea level. Thunderstorm activity became more concentrated, and the NHC initiated advisories on Tropical Storm Arlene at midnight June 29, after the cyclone's surface winds increased to 40 mph (65 km/h) about 280 mi (450 km) south-southeast of Tampico, Tamaulipas.
The National Hurricane Center (NHC) began to monitor a tropical wave associated with a few showers and thunderstorms, moving westward off the coast of northern Central America on July 17. Four days later, thunderstorm activity became more concentrated; by July 22, the area of low-pressure became better organized. On July 23, the NHC noted that the system could become a tropical depression within the next two days; however, they also noted that wind shear could increase within a couple of days. Following an increase of deep convection developing near the center as well as the collection of ASCAT data showing an area of tropical storm-force winds, the NHC upgraded the system to Tropical Storm Genevieve on July 25.
Between the 15-16th century hemp culture and weaving expanded; and new crops such as mulberry, rice, and maize, were introduced. Landownership became more concentrated and sharecropping system consolidated, though the latter has been limited by the existence of Participants on a wide area. During the 16th century the Persiceto was overrun by foreign armies; the Agricultureal Attendance Institute "Partecipanza" was founded and a sharing of the common lands that took place every nine years was enhanced; the city centre underwent a process of impoverishment, whereas the weekly market on Wednesday kept flourishing thanks to old privileges. The local oligarchy of new families' faithful to the Church and subject to the Reggimento of Bologna and the Papal Legacy was established.
In early June 2006, an area of convection persisted across Central America and the western Caribbean in association with a broad, nearly stationary trough of low pressure. Thunderstorms increased and became more concentrated on June 8 after a tropical wave moved into the western Caribbean, and an upper-level low to its west increased outflow over the system. The disturbance moved slowly north-northwestward, and development was initially inhibited by marginally favorable upper-level winds and land interaction. The system gradually organized, and by June 10 a circulation formed with sufficiently organized convection for the National Hurricane Center to classify it Tropical Depression One. At this point the storm was located about 140 miles (225 km) south of the western tip of Cuba.
A tropical wave crossed Central America and entered the eastern Pacific Ocean on November 7. An area of convection along the wave tracked westward to the south of Central America and Mexico, and became more concentrated on November 12 while located about 400 miles (645 km) south of Acapulco. Later that day, Dvorak classification began on the disturbance, and the convection continued to organize. Early on November 13, the National Hurricane Center indicated the possibility of the system developing into a tropical depression. Thunderstorm activity briefly decreased, though late on November 13 the system acquired enough circulation and organized convection for it to be designated Tropical Depression Twenty- One-E while located about 460 miles (740 km) south of Manzanillo, Mexico.
In the earlier years of the trade, there were many owners and operators, sometimes just owning or operating on charter just one vessel. Owners of the 'sixty-milers', during this period, most typically were coal- mines (such as Coalcliff Colliery and Wallarah Colliery), or coal-shippers or merchants (such as Scott, Fell and Company, G.S.Yuill & Co. ), The southern coalfield collieries (Coalcliff Collieries, etc.) owned their own ships but most were chartered to the Southern Coal Owner's Agency, which operated the ships. Later companies that both owned coal mines and were also coal merchants (such as R.W.Miller and Howard Smith Ltd) owned ships and ownership became more concentrated. In the later years of the trade, one of the dominant owners was R.W. Miller and its successor companies.
The origins of Hurricane Olga were from the interaction of a cold front and a small weather disturbance in the north Atlantic Ocean, producing an extratropical low east of Bermuda on November 22\. The low gradually intensified and acquired subtropical characteristics, developing an area of convection east of the center and accompanied by a large area of gale-force winds. By 0000 UTC on November 24, the system organized enough to be classified as Subtropical Storm Two, while located about 900 mi (1450 km) east-southeast of Bermuda. Subsequently, the convection markedly increased and became more concentrated, with hints of an eye feature. Within 12 hours of becoming a subtropical, it is estimated the cyclone transitioned into Tropical Storm Olga; however, it was not purely tropical, due to being positioned beneath an upper-level low.
Findings by Ranere in 1975 support conclusions of Willey and McGimsey 23 years earlier that during initial occupation, the site was situated along the active shoreline of Parita Bay. Water-worn potsherds of the lowest layers indicate that both ridges were subject to flooding during spring tides, suggesting that occupation was not initially year-round. Later, the modern coastline “was established through the buildup of an offshore bar”, and the ridges of the site became surrounded by a water-filled lagoon. Hearths, post-holes, and pits became common, and shell, bone, pottery, charcoal, and stone tools became more concentrated, suggesting a more permanent occupation once the ridges were safe from flooding. Ranere and Hansell (1978) also argue that the abandonment of the site by its occupants later coincides with the lagoon’s being silted in and its conversion into a salt flat.
Important to the understanding of migrant community health is the increasingly stratified American society, manifested in residential segregation. Beginning in the 1970s, the low to moderate levels of income segregation in the United States began to degrade. As the rich became richer, so did their neighborhoods. This trend was inversely reflected in the poor, as their neighborhoods became poorer. As sociologist Douglas Massey explains, “As a result, poverty and affluence both became more concentrated geographically.” Professor of public administration and economics John Yinger writes that “one way for poor people to win the spatial competition for housing is to rent small or low-quality housing.” However, he continues, low-quality housing often features serious health risks such as lead paint and animal pests. Though lead-based paint was deemed illegal in 1978, it remains on the walls of older apartments and houses, posing a serious neurological risk to children.
Gold-bearing magma rising after being subducted under the continental crust. Geologic evidence indicates that over a span of at least 400 million years, gold that had been widely dispersed in the Earth's crust became more concentrated by geologic actions into the gold-bearing regions of California. Only gold that is concentrated can be economically recovered. Some 400 million years ago, rocks that would be accreted onto western North America to build California lay at the bottom of a large sea. Subsea volcanoes deposited lava and minerals (including gold) onto the sea floor; sometimes enough that islands were created. p. 167. Between 400 million and 200 million years ago, geologic movement forced the sea floor and these volcanic islands and deposits eastwards, colliding with the North American plate, which was moving westwards.Hill, Mary (1999), p. 168. Beginning about 200 million years ago, tectonic pressure forced the sea floor beneath the American continental mass.
The English Count de Rice, whose personal details remain unknown, bought from the Kornelimünster Abbey more than three hundred acres of the treeless Brand Heath (which is today the area around North Street (Nordstrasse) and Erberichshof Street, bounded by Eilendorf Street (Eilendorferstr.), and at the time included the estates of Gut Neuenhof, the Krummerrück, and the Hebscheider Hof), so that he could build homes and a horse racetrack. In 1789 the Count went bankrupt and the area was repossessed, but later it was given to the community of Brand, which still built the racetrack, along with a grandstand. Sculpture "Kit and Caboodle" ("Mit Kind und Kegle"), by Bonifatius Stirnberg In the 19th century, horse racing in Brand enjoyed great popularity after it had been initiated in 1830 by the industrialist James Cockerill and further expanded upon in 1870 by his grandchildren and respected gentlemen riders Otto and Henry Suermondt, who would later serve as the nucleus of the Aachen-Laurensberg Riding Club. After the turn of the 20th century, equestrian sports in the area became more concentrated in Soers, and so the wide-open area of Brand became a staging area for Aachen area flight pioneer and airplane builder Erich Lochner.

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