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Research shows that a few organisms living in normal seawater can also be found in the halocline, as well as just below it-in the super-salty, no-oxygen area of the Deep Hypersaline Anoxic Basins (DHAB) that is found more than a mile from the surface of the water. In the proper setting, these salty layers are visible to the naked eye and will look fuzzy or hazy compared to the water around them. They are common in areas where freshwater and saltwater come together, such as in estuaries, seaside caves, fjords, and of course, the oceans, more so in colder regions where cold water with a lower salinity “floats” on top of the salty warm layer.
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Haloclines are found in many areas around the world. Specifically, a halocline has a different level of salinity than the surrounding body of water-usually higher than the layers above and below it. Haloclines are a type of chemocline, which means that the chemical makeup of the cline is what makes it different from the surrounding water. We’ll help you out by explaining them in this article. The most commonly known of the clines are thermoclines and haloclines, but they are often confused for one other. Clines are usually horizontal and are often vertically thin in comparison to the body of water around them. They may vary in temperature, salinity, density, or chemistry. What are Clines?Ĭlines are layers within water that have different properties than the surrounding water. If you’re a frequent diver, you’ve probably heard about “clines.” Not many know what it is, but this article will help explain and differentiate two types of clines you are likely to encounter while scuba diving.