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In J. Charles Delbeek's article Your First Reef Aquarium, [2] he states, The use of live rock immediately introduces into the aquarium numerous algae, bacteria and small invertebrates all of which contribute to the overall quality of the aquarium water. Live rock has just as much, if not more, surface area for bacteria than a trickle filter.
Sea Life Michigan Aquarium is the state's largest aquarium [citation needed] with over 250 species and 2,000 creatures including sharks, rays, and green sea turtles. Exhibits include freshwater lakes, coral reef, shipwreck, an interactive touch pool and a 180 degree underwater ocean tunnel.
With over 11 million gallons, the largest aquarium in the United States is the Georgia Aquarium. [1] [2] This is a list of existing public aquariums [3] in the United States, some of which are unaccredited. For zoos, see List of zoos in the United States.
Sacred Rock is an Engadine-dolomite boulder, [1] now 20 feet long by 8 feet wide and 6 feet high, on the shore of Lake Huron in Northern Lower Michigan. It is located 6 miles north of Rogers City, Michigan , approximately 0.5 miles north of P.H. Hoeft State Park .
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The Berlin method requires large amounts of live rock in the aquarium. The rule of thumb is 1/2–1 lb. per 1 US gallon (0.2–0.4 kg per 4 liters). Many marine aquariums include a sump, which is an external container connected to the main aquarium with a water pump.
Basalt (UK: / ˈ b æ s ɒ l t,-ɔː l t,-əl t /; [1] [2] US: / b ə ˈ s ɔː l t, ˈ b eɪ s ɔː l t /) [3] is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon.
Serpentine subgroup is a set of common rock-forming hydrous magnesium iron phyllosilicate ((Mg,Fe) 3 Si 2 O 5 4) minerals, resulting from the metamorphism of the minerals that are contained in mafic to ultramafic rocks. [6] They may contain minor amounts of other elements including chromium, manganese, cobalt or nickel.
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