Abstract
Most of the deposits occur as an irregular mantle of phosphate or phosphatic clay over and between bizarre pinnacles of raised limestone. Phosphatic solutions from bird droppings attacked the limestone; further weathering and solution produced the phosphatic mantle and shaped the pinnacles. However, the best deposits on Angaur are blanket deposits under swamps and apparently represent further alteration of deposits ofthe first type.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
