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22 Sentences With "seawaters"

How to use seawaters in a sentence? Find typical usage patterns (collocations)/phrases/context for "seawaters" and check conjugation/comparative form for "seawaters". Mastering all the usages of "seawaters" from sentence examples published by news publications.

Scientists, who said climate change was warming seawaters, did not expect this level of damage for another 30 years.
It is more interesting to see how climate change opposition plays out in Republican-controlled states facing the brunt of rising seawaters.
The best part of how they'll put the phone in our heads is that when the seawaters all rise, the phone will be the last part of us to get wet.
The new straws, targeted to go on sale in the second quarter of 2019, are made of wood and natural binders that can be recycled via industrial composting, and they biodegrade should they end up in seawaters.
While the United Nations warned of mass wildfires, food shortages and dying coral reefs as soon as 22050, Mr. Trump discussed his successful Supreme Court battle rather than how rising seawaters are already flooding Miami on sunny days.
These cuts come at a time when experts are warning that if we do not act immediately to lower dangerous gas emissions, runaway climate change could cause worldwide food shortages, droughts, rising seawaters, heatwaves and conflict, threatening the economy and security of the world.
Mountain building raised the Ancestral Rockies in Colorado, Utah, and Wyoming. Seawaters left the interior of the country. Densely vegetated swamps were widespread. The largest insects in geologic history lived during the Pennsylvanian.
Davidson, Myers & Weiss 2004, p. 1025 Since the industrial Revolution, mercury levels have tripled in many near-surface seawaters, especially around Iceland and Antarctica.New Scientist August 2014, p. 4 Dutch Boy white lead paint advertisement, 1912.
It was a little smaller than Asian elephants averaging to . It lived in forest which mixed subarctic conifers and cool-temperate deciduous trees. The ancestor of Palaeoloxodon naumanni moved from the Eurasian continent to Japan via a land bridge; it subsequently evolved independently and spread throughout Japan after the land bridge was covered by rising seawaters. Palaeoloxodon naumanni was hunted by the inhabitants of the time.
According to Djakonov it has been collected at depths of 5-96m. It is found in the littoral zone from the east in the seas around Japan, west to the Sea of Japan and further to the Yellow Sea, and north through the Peter the Great Gulf (Primorsky Krai) to off the coast of De-Kastri in Khabarovsk Krai. It is among the most common starfish of Chinese seawaters.
The remains of the oldest settlement at the site of modern Acre were found at a tell (archaeological mound) located east of the modern city of Acre. Known as Tel Akko in Hebrew and Tell el- Fukhar in Arabic, its remains date to about 3000, during the Early Bronze Age. This farming community endured for only a couple of centuries, after which the site was abandoned, possibly after being inundated by rising seawaters.
Even more different than usual brines, in acid saline systems the amount of Al is magnitudes higher than that of Ca. Some of the most concentrated Al is at 8000mg/L, which is much higher than that of acid mine waters or seawaters. Other trace ions are present in these lakes in large amounts as well. On average, strontium (Sr) values can get up to 65mg/L and increase with salinity. 59% of the sampled waters have detectable amounts of Mn (>46 mg/L) and Cu (<9.5 mg/L).
Fluoride accumulates in the bone tissues of fish and in the exoskeleton of aquatic invertebrates. The mechanism of fluoride toxicity in aquatic organisms is believed to involve the action of fluoride ions as enzymatic poisons. In soft waters with low ionic content, invertebrates and fishes may suffer adverse effects from fluoride concentration as low as 0.5 mg/L. Negative effects are less in hard waters and seawaters, as the bioavailability of fluoride ions is reduced with increasing water hardness Seawater contains fluoride at a concentration of 1.3 mg/L.
Known in the past for its vast timberlands and, for the present, with its over six thousand hectares of government- irrigated lands, it has seawaters in the east, mountains in the west, north and south. The plains have navigable rivers known as Carac-an, Union, Cantilan, Consuelo, Benoni, Bun-ot, Adlayan, Lancogue and some smaller ones. The extent of creeks and wetlands or lowlands and swamps were main landmarks and features of its old topography. The conversions and developments of the lowlands into rice paddies began in the 18th century when the friars were stationed therein.
The lake is the likely point of origin of the landlocked salmon, stated in the species' scientific name (Salmo salar sebago). At one point, the entire watershed was under seawater, and the first populations of these marine animals became established as the land rose and seawaters retreated. Other game fish that can be found in the lake include lake trout, brook trout, brown trout, largemouth bass,(particularly on the lake's West Side) and northern pike. Some of these are stocked by the state, either in the lake directly or in connected bodies of water, while others were introduced illegally.
Ocean Thermal Energy Conversion (OTEC) uses the ocean thermal gradient between cooler deep and warmer shallow or surface seawaters to run a heat engine and produce useful work, usually in the form of electricity. OTEC can operate with a very high capacity factor and so can operate in base load mode. The denser cold water masses, formed by ocean surface water interaction with cold atmosphere in quite specific areas of the North Atlantic and the Southern Ocean, sink into the deep sea basins and spread in entire deep ocean by the thermohaline circulation. Upwelling of cold water from the deep ocean is replenished by the downwelling of cold surface sea water.
In the Kattegat, the salinity has a pronounced two-layer structure. The upper layer has a salinity between 18% and 26% and the lower layer – separated by a strong halocline at around – has a salinity between 32% and 34%. The lower layer consists of inflowing seawater from the Skagerrak, with a salinity on level with most other coastal seawaters, while the upper layer consists of inflowing seawater from the Baltic Sea and has a much lower salinity, comparable to brackish water, but still a great deal higher than the rest of the Baltic sea. These two opposing flows transport a net surplus of seawater from the Baltic to the Skagerrak every year.
Due to the fact it is a wide area, the square started being used as an entrance for the people of the provinces of Minho, Trás-os-Montes and Alto Douro, that arrived in Póvoa due to medical advice to cure several health problems, in which they plan to cure by diving in rich iodine seawaters, sunbathing and breathing sea-aroma air. By this, the square gained relevance and was where the coachwomen parked the cars. In 1897, when the streetcar tramline was expanded a shunting line is created that goes by the square reaching the Baths Beach.Planta das ruas por onde se pretende assentar a Linha do Americano (27 de Janeiro de 1903) - Arquivo Municipal da Póvoa de Varzim By then there were lodging needs, and to answer that, hotels were created.
In the beginning of the 18th century, Benedictine monks walked distances to take the "Baths of Póvoa", in search of iodine, considered invigorating, and cures for skin and bones problems throw sea and sun-baths. By the 19th century, the popularity increased with people from the provinces of Minho, Trás-os-Montes and Alto Douro that arrived by medical advice to cure several health problems, by breathing the air and diving in the rich iodine seawaters of Póvoa, in a popular movement that occurred in the European Atlantic coast since the 18th century, from Biarritz to Póvoa de Varzim. During the Belle Epoque, this popularity is especially noticeable amongst the wealthiest classes and, especially, between the Portuguese-Brazilians (the Brasileiros), leading to the appearance of high culture venues. Several casinos, theatres and hotels were raised.
Studies undertaken by marine biologists aim to verify the link between the waste generated by the salmon industry in the Chilean oceanic waters and the outbreak of the highly toxic red tide harmful algal blooms in the region. Following this outbreak, from 2016 and 2018, 40 thousand tons of salmon were lost following fatal health issues (0,9% of the total salmons cultivated in Chilean seawaters), but salmon producers deny the direct link between their activities and the red tide outbreak. Salmón Chile: Pérdidas por bloom de algas son mucho menores que en 2016, Cooperativa.cl, 15 February 2018 Evidence from Comau Fiord where a Harmful Algal Bloom caused a mass die of cold water coral reefs was directly linked to the eutrophic conditions causing HABs from the Salmon Farms in the area.
All of the remaining thorium isotopes have half-lives that are less than thirty days and the majority of these have half-lives that are less than ten minutes. In deep seawaters the isotope 230Th makes up to 0.04% of natural thorium. This is because its parent 238U is soluble in water, but 230Th is insoluble and precipitates into the sediment. Uranium ores with low thorium concentrations can be purified to produce gram-sized thorium samples of which over a quarter is the 230Th isotope, since 230Th is one of the daughters of 238U. The International Union of Pure and Applied Chemistry (IUPAC) reclassified thorium as a binuclidic element in 2013; it had formerly been considered a mononuclidic element. Thorium has three known nuclear isomers (or metastable states), 216m1Th, 216m2Th, and 229mTh.
Since 1725, the iodine-rich seawaters of Póvoa, due to the peculiar high quantities of seaweed, from the outlying kelp forests, that end up in Póvoa beaches, brought by ocean currents, lead that Benedictine monks choose to take sea-baths in Póvoa, in search of iodine (considered reinvigorating) and diving and sunbathing as a cure for skin and bone concerns. Some years later, but still in the 18th century, other people went to Póvoa with the same concerns.Projecto para a Construção de Pavilhões na Praia da Póvoa (Maio a Junho de 1924) - Arquivo Municipal da Póvoa de Varzim (2008) Largo do Café Chinês, one of the several gambling venues in 19th-century Póvoa. Since the 19th century, the touristic activity became even more significant especially among the wealthiest classes from the Entre-Douro-e-Minho province and wealthy Portuguese-Brazilians, the city took a cosmopolitan character, leading to the affirmation of the bourgeoisie in Póvoa de Varzim City Center and the development of entertainment venues.

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