Sediments become rocks by lithification. 1  compaction-lithification occurs as the weight of overlying sediments and rocks squeeze the sediments together into rock. 2  cementation-precipitates from groundwater and the growth of secondary minerals between the fragments may cement the rock.ediments become rocks by lithification. 1  compaction-lithification occurs as the weight of overlying sediments and rocks squeeze the sediments together into rock. 2  cementation-precipitates from groundwater and the growth of secondary minerals between the fragments may cement the rock.
Weather in Mangrove Forests can ranges drastically because of their location in mainly tropical climates around the world. Most of the mangrove forestation is in the Indian Ocean, whether it be on the coasts of India or surrounding the islands of Indonesia (see Locations of Forests).
places that are too hot, too salty, too wet, and too exposed to wind, rain, tides, and storms for other. plants. The various species of mangroves have things in common, such as the ability to deal with excess salt. in their surroundings, and spreading root systems that allow trees to grow in anaerobic mud. But every species grows in a slightly different part of the wetland and has its own special adaptations.