Answer:
As a result, the majority of deep marine deposits are of siliceous ooze, which lithifies as chert. Chert is an amorphous hydrous silica that is characteristic of deep marine depositional environments.
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Answer:
As a result, the majority of deep marine deposits are of siliceous ooze, which lithifies as chert. Chert is an amorphous hydrous silica that is characteristic of deep marine depositional environments.