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22" x 20" - ceramic, a variety of glass, stones, dinnerware, and millefiore on a custom built substrate.
Still seawater in these shallow mud flats and sandy substrate closer to shore. There's a reef structure/habitat classification and coral zonation from shore to deep ocean. [Some small fish traveling in schools were churning the water surface but it can be barely seen in this photo.]
Info: Reef flat
Shoreward of the reef crest there is a strong environmental gradient on the shallow reef flats of south Moloka‘i. The seaward edge of the reef flat is subjected to breaking waves over the reef crest and strong currents. Small carbonate rock outcrops surrounded by coral rubble characterize the seaward reef flat. Depth diminishes shoreward of the reef crest. Wave energy is dissipated as the water decreases in depth, moving toward the shoreline (Denny, 1988). Moving shoreward, the substrate becomes sandy with scattered rock. Near the shoreline the sand grades into mud. > cramp.wcc.hawaii.edu/Watershed_Files/Molokai/WS_Molokai_m...
Jänesvaabik + seltsiv tindik.
Lattakääpä + parvimustesieni.
Substrate: Populus tremula.
Kantküla, Lääne-Virumaa.
The substrate glass culture!
From bottom to top.
Charcoal, moss, coarse pine bark and fine pine bark.
So simple.
Found in various coral reef habitats from estuaries to outer reef lagoons to about 20 m depth, but usually more common on shallow reef flat at the 6 m mark. Cryptic usually on corals and sponges of isolated outcrops. Oviparous. Eggs are demersal and adhesive , and are attached to the substrate via a filamentous, adhesive pad or pedestal. Larvae are planktonic, often found in shallow, coastal waters. Lembeh Strait, North Sulawesi, Indonesia