Sentence examples for seafloor temperature from inspiring English sources

(Hydrate Ridge is a cold seep, maintaining a typical seafloor temperature of about 37 degrees Fahrenheit).

For this reason, in this study, gas seepages were predicted by using HydrateResSim at different seafloor temperature increments varying from 1 to 5 °C and different sediment permeability values varying from 0.1 mD to 5mD in Thessaloniki mud volcano.

This is evidenced by changes in seafloor temperature that spanned from that of ambient seawater (22.1°C) to that of hydrothermal inputs (97.4°C).

The BSR depth variation in the convex-upward and convex-downward seafloor regions was investigated using two-dimensional thermal modeling in conjunction with topographic effects and seafloor temperature in the area where continuous BSRs were found.

The concentric zonation observed at Rocky Point and Speigelei suggests that seafloor coloration is qualitatively linked to seafloor temperature and associated mineralization, ranging from orange (high temperatures) to white (intermediate temperatures) and gray (lower temperatures) (Figure 7a).

The seafloor temperature was derived from the hydrographic data of the bottom water temperature from the Japan Oceanographic Data Center, which was then used in part to compute the geothermal gradient.

The water dissolves minerals deep in the Earth's crust before rising like a geyser from the seafloor at temperatures of up to 400°C.This mineral-laden fluid, if it is rich in iron and sulphur, emerges to create a plume of black "smoke", from which, when it meets cold bottom water, the minerals are precipitated.

Here, the team found holes in the seafloor "gushing high temperature fluids," and steaming sediments "laden with orange-colored oil and the rotten-egg stink of sulfide.

The analysis also notes that the extreme depths involved (~800 km to the rocky "seafloor") mean that temperatures at the bottom of a convective (adiabatic) ocean can be up to 40 K higher than those at the ice-water interface.

Our study shows that high-temperature seafloor vents produce high levels of acoustic radiation which can provide valuable information about geological and physical processes occurring within these systems, and may provide animals with information about the environment they inhabit.

In this study of the upper 20 cm of the Palaeochori seafloor sediment, δ34S and temperature data are consistent with partial isotopic exchange between vent H2S and subsurface anhydrite (Figure 14).