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TABLE 4.1 CLASSIFICATION OF MARINE SEDIMENTS Campistion SourtesOrigin DiatrlhutiovMaln looations where sedimentoirently foms Rvars; coastal arosion; landsides Continantal shelt Fock tragments Quartz sand Quartr sit Ciay Giaciers Continantal shelt in high atitudes Turbidly curents Contnantal skopa and rta; ocaan basin margins Qartz sit Clay Wird biown dust; rivars Abysal plains and other regors of the dasp-ocean basirs Volcanic ash Vocanic eruptiors Coccolthophores (algoe) Foraminitars (proturcars) Law-latibude regiore, saa foor above CCD; abng mis- Dcaan ridges and the tops of sutmarine volcanic pasks Calcareous care (microscopic) Macroscopic shel pratucing ogantams Continantal shelt; baches Shels and coral fragments (macroscopic) Shallow low lalitude regbrs Coral rosts Hgh-latitude regbns; sea fcar below CCD; upwelling areas where cold, deep watar rises to the surtace, espacialy that caused by surface current divergence near the equator Dartoms (alga) Radiolarians (protomans) Sicenus oze Mangorese nodules (marganea, ron, coppar, nickel cobalt) Abysal plain Phosphorite (phosphoroLE) Continantal shalt Preciptation of dissovad matarials direciy tom saawatar due to chemicalShalow sher in low latitude regiors Colas (Cacoa) Matal sufides (ron, nickel, copper, anc, siver) raactiors Hydrothermalvents at mid-ccean ridges Shalow restricted basirs where avaparation is high in law-katihude regjors In vary small proportins mixed with all ypes of Evaporites (ay peum, halte, other salts) Iron-nickel spheruks Taktles (sica gess) Space dust adiment and in al marine environments Iron-nickel metearites Metaors Localiked near metaor impact structures Fusugue agruogre unp

TABLE 4.1 CLASSIFICATION OF MARINE SEDIMENTS Campistion SourtesOrigin DiatrlhutiovMaln looations where sedimentoirently foms Rvars; coastal arosion; landsides Continantal shelt Fock tragments Quartz sand Quartr sit Ciay Giaciers Continantal shelt in high atitudes Turbidly curents Contnantal skopa and rta; ocaan basin margins Qartz sit Clay Wird biown dust; rivars Abysal plains and other regors of the dasp-ocean basirs Volcanic ash Vocanic eruptiors Coccolthophores (algoe) Foraminitars (proturcars) Law-latibude regiore, saa foor above CCD; abng mis- Dcaan ridges and the tops of sutmarine volcanic pasks Calcareous care (microscopic) Macroscopic shel pratucing ogantams Continantal shelt; baches Shels and coral fragments (macroscopic) Shallow low lalitude regbrs Coral rosts Hgh-latitude regbns; sea fcar below CCD; upwelling areas where cold, deep watar rises to the surtace, espacialy that caused by surface current divergence near the equator Dartoms (alga) Radiolarians (protomans) Sicenus oze Mangorese nodules (marganea, ron, coppar, nickel cobalt) Abysal plain Phosphorite (phosphoroLE) Continantal shalt Preciptation of dissovad matarials direciy tom saawatar due to chemicalShalow sher in low latitude regiors Colas (Cacoa) Matal sufides (ron, nickel, copper, anc, siver) raactiors Hydrothermalvents at mid-ccean ridges Shalow restricted basirs where avaparation is high in law-katihude regjors In vary small proportins mixed with all ypes of Evaporites (ay peum, halte, other salts) Iron-nickel spheruks Taktles (sica gess) Space dust adiment and in al marine environments Iron-nickel metearites Metaors Localiked near metaor impact structures Fusugue agruogre unp

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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Using Table 4.1, list and describe the characteristics of the four main types of marine sediment.
TABLE 4.1 CLASSIFICATION OF MARINE SEDIMENTS Campistion SourtesOrigin DiatrlhutiovMaln looations where sedimentoirently foms Rvars; coastal arosion; landsides Continantal shelt Fock tragments Quartz sand Quartr sit Ciay Giaciers Continantal shelt in high atitudes Turbidly curents Contnantal skopa and rta; ocaan basin margins Qartz sit Clay Wird biown dust; rivars Abysal plains and other regors of the dasp-ocean basirs Volcanic ash Vocanic eruptiors Coccolthophores (algoe) Foraminitars (proturcars) Law-latibude regiore, saa foor above CCD; abng mis- Dcaan ridges and the tops of sutmarine volcanic pasks Calcareous care (microscopic) Macroscopic shel pratucing ogantams Continantal shelt; baches Shels and coral fragments (macroscopic) Shallow low lalitude regbrs Coral rosts Hgh-latitude regbns; sea fcar below CCD; upwelling areas where cold, deep watar rises to the surtace, espacialy that caused by surface current divergence near the equator Dartoms (alga) Radiolarians (protomans) Sicenus oze Mangorese nodules (marganea, ron, coppar, nickel cobalt) Abysal plain Phosphorite (phosphoroLE) Continantal shalt Preciptation of dissovad matarials direciy tom saawatar due to chemicalShalow sher in low latitude regiors Colas (Cacoa) Matal sufides (ron, nickel, copper, anc, siver) raactiors Hydrothermalvents at mid-ccean ridges Shalow restricted basirs where avaparation is high in law-katihude regjors In vary small proportins mixed with all ypes of Evaporites (ay peum, halte, other salts) Iron-nickel spheruks Taktles (sica gess) Space dust adiment and in al marine environments Iron-nickel metearites Metaors Localiked near metaor impact structures Fusugue agruogre unp
Transcribed Image Text:TABLE 4.1 CLASSIFICATION OF MARINE SEDIMENTS Campistion SourtesOrigin DiatrlhutiovMaln looations where sedimentoirently foms Rvars; coastal arosion; landsides Continantal shelt Fock tragments Quartz sand Quartr sit Ciay Giaciers Continantal shelt in high atitudes Turbidly curents Contnantal skopa and rta; ocaan basin margins Qartz sit Clay Wird biown dust; rivars Abysal plains and other regors of the dasp-ocean basirs Volcanic ash Vocanic eruptiors Coccolthophores (algoe) Foraminitars (proturcars) Law-latibude regiore, saa foor above CCD; abng mis- Dcaan ridges and the tops of sutmarine volcanic pasks Calcareous care (microscopic) Macroscopic shel pratucing ogantams Continantal shelt; baches Shels and coral fragments (macroscopic) Shallow low lalitude regbrs Coral rosts Hgh-latitude regbns; sea fcar below CCD; upwelling areas where cold, deep watar rises to the surtace, espacialy that caused by surface current divergence near the equator Dartoms (alga) Radiolarians (protomans) Sicenus oze Mangorese nodules (marganea, ron, coppar, nickel cobalt) Abysal plain Phosphorite (phosphoroLE) Continantal shalt Preciptation of dissovad matarials direciy tom saawatar due to chemicalShalow sher in low latitude regiors Colas (Cacoa) Matal sufides (ron, nickel, copper, anc, siver) raactiors Hydrothermalvents at mid-ccean ridges Shalow restricted basirs where avaparation is high in law-katihude regjors In vary small proportins mixed with all ypes of Evaporites (ay peum, halte, other salts) Iron-nickel spheruks Taktles (sica gess) Space dust adiment and in al marine environments Iron-nickel metearites Metaors Localiked near metaor impact structures Fusugue agruogre unp
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