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Goldberg, Edward D; Griffin, John J (1970): Mineralogy of northern Indian Ocean surface sediments and of suspended sediments of Indian rivers (Table 2 and 5) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.407959, Supplement to: Goldberg, ED; Griffin, JJ (1970): The sediments of the northern Indian Ocean. Deep-Sea Research and Oceanographic Abstracts, 17(3), 513-537, https://doi.org/10.1016/0011-7471(70)90065-3

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Abstract:
The solid phases from surface sediments, atmospheric dusts, and rivers of the Indian Ocean environment have been analyzed for their clay minerals and quartz. Such data have been used to delimit the transport paths and sources of the detrital minerals in the oceanic deposits. Diagnostic in distinguishing fluvial and eolian inputs to the northern Indian Ocean is a combination of the clay mineral assemblages and of their geographic distributions.
River borne solids are the primary components of the Bay of Bengal deposits. The eastern part receives its continental input through the Ganges-Brahmaputra river system, while drainage of the Indian Peninsula by rivers introduces solids to the western part. The former materials are characterized by high illite and chlorite in the clay mineral assemblages; the latter by montmorillonite. The winds over the Bay bear distinctive dust burdens based upon their directions. However, their contributions to the sediments are insignificant.
The eastern sector of the Arabian Sea receives major contributions of continental debris from the rivers and the high montmorillonite levels clearly indicate a source in the Indian Peninsula. The rest of the Sea appears to receive most of its land-derived materials from the north, perhaps the desert regions of northern India and West Pakistan, and they are wind-borne. These materials are also transported to the equatorial regions of the Indian Ocean.
A gradient in attapulgite, just north of the equator, may indicate an eolian contribution to the Arabian Sea from the African continent.
The halogenated hydrocarbon pesticides were assayed in the southwest monsoon winds and enter the Bay of Bengal at levels of a half ton per month, an amount comparable to those introduced by other wind and river systems to the marine environment.
Coverage:
Median Latitude: 15.624285 * Median Longitude: 75.176807 * South-bound Latitude: 1.275000 * West-bound Longitude: 47.117000 * North-bound Latitude: 24.500000 * East-bound Longitude: 94.367000
Date/Time Start: 1962-09-21T00:00:00 * Date/Time End: 1962-09-29T00:00:00
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
Ahmedabad (116)  * Latitude: 23.080000 * Longitude: 72.630000 * Elevation: 50.0 m * Location: Sabarmat, India, Asia * Campaign: Global River Discharge * Method/Device: River gauging station (RGS) * Comment: Area: 12950 km**2; Mapcode of UNESCO report: F6
CIRCE-21  * Latitude: 11.383000 * Longitude: 87.783000 * Elevation: -3308.0 m * Location: Bay of Bengal * Campaign: CIRCE * Basis: Melville * Method/Device: Gravity corer (GC)
CIRCE-22  * Latitude: 11.418300 * Longitude: 83.816700 * Elevation: -3456.0 m * Location: Bay of Bengal * Campaign: CIRCE * Basis: Melville * Method/Device: Gravity corer (GC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Sample code/labelSample labelGoldberg, Edward D
Latitude of eventLatitude
Longitude of eventLongitude
Elevation of eventElevationm
DEPTH, sediment/rockDepth sedmGeocode
MontmorilloniteMnt%Goldberg, Edward Din <2 µm fraction
IlliteIll%Goldberg, Edward Din <2 µm fraction
Kaolinite+ChloriteKln+Chl%Goldberg, Edward Din <2 µm fraction
10 KaoliniteKln%Goldberg, Edward Din <2 µm fraction
11 ChloriteChl%Goldberg, Edward Din <2 µm fraction
12 QuartzQz%Goldberg, Edward Din carbonate free sediment
13 QuartzQz%Goldberg, Edward Din total sample
Size:
345 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Sample label

Latitude

Longitude

Elevation [m]

Depth sed [m]

Mnt [%]
(in <2 µm fraction)

Ill [%]
(in <2 µm fraction)

Kln+Chl [%]
(in <2 µm fraction)
10 
Kln [%]
(in <2 µm fraction)
11 
Chl [%]
(in <2 µm fraction)
12 
Qz [%]
(in carbonate free sediment)
13 
Qz [%]
(in total sample)
Ahmedabad Sabaramathi river at Ahmedabad23.080072.630050018443726119
CIRCE-21 21G11.383087.7830-33080373514148
CIRCE-22 22G11.418383.8167-34560582012105
CIRCE-23 23G11.643381.1267-34960701010107
CIRCE-24 24G14.267080.8670-28450838547
CIRCE-25 25G15.300083.2833-314607711668
CIRCE-26 26G15.300087.3170-28310323814169
CIRCE-27 27G15.217091.233003630161810
CIRCE-28PB 28G15.350094.3670-3703132162133
CIRCE-30P 30G16.867092.5670-240303329182010
CIRCE-31G 31G19.700092.7670-590246203218
CIRCE-32 32G19.000091.533002046151912
CIRCE-33 33G19.080087.6800-214203636131513
CIRCE-34 34G20.866787.7417-4603038151755
CIRCE-36 36G20.333089.3170-43503438121615
CIRCE-37 37G17.550086.5833-254404828111311
CIRCE-38 38G13.483086.9000-30760443111138
CIRCE-39 39G9.791783.5000-36430601811115
CIRCE-40 40G7.991782.1917-379906017131110
CIRCE-41 41G8.000085.6417-37440442714146
CIRCE-42 42G6.917089.0330-37410343315176
CIRCE-44 44G4.183088.5830-40570403015157
CIRCE-45 45G1.700086.8083-43830184618196
CIRCE-46 46G1.918384.3033-472201852131610
CIRCE-47 47G1.275082.9050-44420165213197
CIRCE-48 48G4.346780.7667-4324070126105
Grand_Anicut_South Cauveri river at Trichi10.830078.8300580512821
Mancherial Godavary river18.830079.4500124081712
Paksay Ganges river at Allahabad24.080089.030014010583242820
PaksayGanges river at Nabadeep24.080089.0300140204338221621
Polavaram Godavary river at Rajahmundry16.920081.7800085610739
USN-02 U221.500069.50000751655
USN-03 U322.500068.500002648224
USN-07 U721.500060.500001646533
USN-08 U822.500060.500001446337
USN-16 U1623.450063.58330856234
USN-17 U1722.500063.500001651231
USN-18 U1821.550063.320001053532
USN-20 U2023.466765.516701452726
USN-22 U2224.500065.50000854929
USN-24 U2422.516766.400003440719
USN-26 U2621.550067.516704236428
USN-28 U2820.500061.500001653725
USN-29 U2920.500070.50000741555
USN-31 U3120.250072.48330622099
USN-32 U3219.516771.56670771455
USN-35 U3524.483362.433302581129
USN-37 U3724.500057.50000849<143
USN-38 U3824.500059.50000354<142
USN-40 U4020.500065.5000018541018
Vijayawada Krishna river at Vijaywada16.520080.620008758
ZEPHII-001G ZII-112.450047.1170-1814033352667
ZEPHII-005G ZII-512.417050.5500-24170343719107
ZEPHII-006G ZII-69.250054.1500-37010324414116
ZEPHII-008G ZII-89.283058.9670-31960274115175
ZEPHII-010G ZII-109.550061.4000-457902150141410
ZEPHII-011GA ZII-119.583063.1000-449801754111811
ZEPHII-012G ZII-129.800069.2500-4544030445219
ZEPHII-013G ZII-139.833071.8330-23720264017179
ZEPHII-014G ZII-149.933073.1330-19220343117179
ZEPHII-015G ZII-159.933074.8330-2286048202487