" An ultraslow ballad about closeness and intimacy, "Braid," concludes with Mr. Hadreas's voice braided into close harmonies, singing, "Every harm is lovingly washed away.
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The album is not beholden to radio formats or presold by a single; fans are likely to explore the whole album, streaming every track and hearing how far afield — a brass band, stomping blues-rock, ultraslow avant-R&B — Beyoncé is willing to go.
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The Beebe vent field is located in the very near vicinity of the spreading center, which has been described as an ultraslow ridge at a rate of to per year. The area is primarily basalt, with metal-sulfide mounds and talus sourced from hydrothermal activity.
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The P30 Pro's camera modes have been carried over to the Mate 30 Pro. Night Mode has been improved, and the Mate 30 Pro can take 4K HDR Plus time- lapse and ultraslow-motion video, shooting 720p at 7680 frames per second. Like its predecessor, the Mate 30 series uses Leica optics.
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Kankan Bhattacharyya is a modern non-linear laser spectroscopy scientist. His main interest is in femtosecond dynamics in nano-confined systems that include biological assemblies. His primary discovery is the ultraslow nature of biological water. He was the director and chair professor of Indian Association for the Cultivation of Science (IACS), Kolkata, the oldest centre for scientific research in Asia.
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The spreading rate of the North Atlantic Ocean is ~ 25 mm/yr, while in the Pacific region, it is 80–145 mm/yr. The highest known rate is over 200 mm/yr in the Miocene on the East Pacific Rise. Ridges that spread at rates <20 mm/yr are referred to as ultraslow spreading ridges (e.g., the Gakkel Ridge in the Arctic Ocean and the Southwest Indian Ridge).
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This site is located on the 110 km long, ultraslow spreading Mid- Cayman Rise within the Cayman Trough. In early 2013, the deepest known hydrothermal vents were discovered in the Caribbean at a depth of almost . Oceanographers are studying the volcanoes and hydrothermal vents of the Juan de Fuca mid ocean ridge where tectonic plates are moving away from each other. Hydrothermal vents and other geothermal manifestations are currently being explored in the Bahía de Concepción, Baja California Sur, Mexico.
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There is a strong resemblance between the Terceira Rift and other ultra- or super- slow spreading ridges, such as the Gakkel Rift and the Southwest Indian ridges. In particular, high obliquity values of 40°-65°, and a magmatic segmentation wavelength of 100 km, are similar to other very slow rifts. Rift valleys present along the rift are 1000–2200 m deep, and 30–60 km wide, similar to the Mid-Atlantic Ridge median valley. However, the amplitude of the Terceira Rift along-strike topography is 2000–4000 m, which is much larger than expected for ultraslow spreading ridges.
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The estimate has declined over time with a most recent estimate of ~1800 Gt carbon. A large part of this uncertainty is due to our knowledge gap in sources and sinks of methane and the distribution of methane clathrates at the global scale. For example, a relatively newly discovered source of methane was discovered in an ultraslow spreading ridge in the Arctic. Some climate models suggest that today's methane emission regime from the ocean floor is potentially similar to that during the period of the Paleocene–Eocene Thermal Maximum (PETM) around 55.5 million years ago, although there are no data indicating that methane from clathrate dissociation currently reaches the atmosphere.
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