Curray, Joseph R; Moore, David G (2005): Smear slide analysis of Hole 64-474A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230911
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Vacquier, Victor; Simoneit, Bernd R T; Schrader, Hans-Jürgen; Saunders, Andrew D; Rueda-Gaxiola, Jaime; Niemitz, Jeffrey W; Molina-Cruz, Adolfo; Matoba, Y; Lyle, Mitchell W; Kelts, Kerry; Kastner, Miriam; Guerrero-Garcia, Jose; Gieskes, Joris M; Fornari, Daniel J; Einsele, Gerhard; Aubry, Marie-Pierre; Aguayo, J Eduardo; Curray, Joseph R; Moore, David G (1982): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LXIV, 507 pp + 1303 pp, https://doi.org/10.2973/dsdp.proc.64.1982
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.959300 * Longitude: -108.978000
Date/Time Start: 1978-12-02T00:00:00 * Date/Time End: 1978-12-02T00:00:00
Minimum DEPTH, sediment/rock: 163.77 m * Maximum DEPTH, sediment/rock: 545.00 m
Event(s):
64-474A * Latitude: 22.959300 * Longitude: -108.978000 * Date/Time: 1978-12-02T00:00:00 * Elevation: -3022.0 m * Penetration: 626 m * Recovery: 290.1 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 453 m cored; 9.5 m drilled; 64 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
14 | Calcareous spicules | Calc spic | % | Smear slide analysis | ||
15 | Bryozoa | Bryozoa | % | Smear slide analysis | ||
16 | Chalcedony | Chalcedony | % | Smear slide analysis | ||
17 | Siliceous microfossils | Silic foss | % | Smear slide analysis | ||
18 | Radiolarians | Rad | % | Smear slide analysis | ||
19 | Diatoms | Diatoms | % | Smear slide analysis | ||
20 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
21 | Spiculae | Spiculae | % | Smear slide analysis | ||
22 | Quartz | Qz | % | Smear slide analysis | ||
23 | Feldspar | Fsp | % | Smear slide analysis | ||
24 | Zeolite | Zeo | % | Smear slide analysis | ||
25 | Mica | Mica | % | Smear slide analysis | ||
26 | Biotite | Bt | % | Smear slide analysis | ||
27 | Clay minerals | Clay min | % | Smear slide analysis | ||
28 | Opaque minerals | Opaque | % | Smear slide analysis | ||
29 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
30 | Iron | Fe | % | Smear slide analysis | ||
31 | Heavy minerals | HM | % | Smear slide analysis | ||
32 | Augite | Aug | % | Smear slide analysis | ||
33 | Zircon | Zrn | % | Smear slide analysis | ||
34 | Apatite | Ap | % | Smear slide analysis | ||
35 | Epidote | Ep | % | Smear slide analysis | ||
36 | Hornblende | Hbl | % | Smear slide analysis | ||
37 | Pyroxene | Pyrox | % | Smear slide analysis | ||
38 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
39 | Basalt | Basalt | % | Smear slide analysis | ||
40 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
41 | Organic matter | OM | % | Smear slide analysis | organic debris | |
42 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
43 | Micronodules | Micronod | % | Smear slide analysis | ||
44 | Detritus | Detritus | % | Smear slide analysis | detrital material |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5047 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Lamellibranchiata [%] | 14 Calc spic [%] | 15 Bryozoa [%] | 16 Chalcedony [%] | 17 Silic foss [%] | 18 Rad [%] | 19 Diatoms [%] | 20 Silicoflag [%] | 21 Spiculae [%] | 22 Qz [%] | 23 Fsp [%] | 24 Zeo [%] | 25 Mica [%] | 26 Bt [%] | 27 Clay min [%] | 28 Opaque [%] | 29 Py [%] | 30 Fe [%] | 31 HM [%] | 32 Aug [%] | 33 Zrn [%] | 34 Ap [%] | 35 Ep [%] | 36 Hbl [%] | 37 Pyrox [%] | 38 Volc glass [%] | 39 Basalt [%] | 40 Rock fragm [%] | 41 OM [%] | 42 Terr [%] | 43 Micronod [%] | 44 Detritus [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
163.77 | 64-474A-1-1,27 | 10 | 30 | 60 | Lower pleistocene | Dominat lithology; numerical abundance | 15 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 1 | 10 | 10 | 0 | 2 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 75 | 0 | 0 | |
163.82 | 64-474A-1-1,32 | 1 | 70 | 30 | Lower pleistocene | CLAYEY NANNO-OOZE | relative abundance | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
165.80 | 64-474A-1-2,80 | 0 | 20 | 80 | Lower pleistocene | NANNO BEARING SILTY CLAY | Dominat lithology; numerical abundance | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 3 | 5 | 5 | 0 | 2 | 0 | 50 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
167.43 | 64-474A-1-3,93 | 0 | 40 | 60 | Lower pleistocene | NANNO BEARING SILTY CLAY | Dominat lithology; numerical abundance | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | 10 | 2 | 0 | 0 | 5 | 0 | 60 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.60 | 64-474A-1-CC,0 | 0 | 0 | 0 | Lower pleistocene | SPONGE SPICULES | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
169.60 | 64-474A-1-CC,0 | 0 | 60 | 40 | Lower pleistocene | CLAYEY SILTSTONE, FINE GRAINED INDURAT.M QTZ 45,CLAY 40,HVY.MINS TR,CARB | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
174.20 | 64-474A-2-11,120 | 50 | 40 | 10 | Lower pleistocene | QUARTZOSE SILTY SAND | Dominat lithology; numerical abundance | 19 | 0 | 4 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 3 | 25 | 6 | 0 | 19 | 0 | 0 | 5 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 |
179.60 | 64-474A-2-5,60 | 0 | 55 | 45 | Lower pleistocene | MUDDY SILT | Dominat lithology; numerical abundance | 2 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 1 | 2 | 20 | 10 | 0 | 0 | 0 | 30 | 0 | 1 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
181.55 | 64-474A-2-61,105 | 0 | 0 | 0 | Lower pleistocene | COARSE ARKOSE | Minor lithology; numerical abundance | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 33 | 33 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 11 | 0 | 0 | 0 | 0 |
183.00 | 64-474A-3-1,50 | 0 | 60 | 40 | Lower pleistocene | NANNO BEARING SILICEOUS MUD CLAYEY SILTM QTZ 10,FEL 15,MICA 3,CLAY 30,PY | Dominat lithology; numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
186.89 | 64-474A-3-31,139 | 90 | 0 | 0 | Lower pleistocene | YELLOW SAND, NOT SIEVED | Minor lithology; numerical abundance | 11 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 67 | 17 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
189.89 | 64-474A-3-51,139 | 85 | 10 | 5 | Lower pleistocene | QTZ SAND W/SHALLOW WATER DEBRIS | Minor lithology; numerical abundance | 46 | 0 | 0 | 6 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 34 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
189.92 | 64-474A-3-51,142 | 5 | 25 | 70 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 30 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 5 | 0 | 0 | 5 | 0 | 40 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
189.93 | 64-474A-3-51,143 | 5 | 30 | 65 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 10 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 2 | 15 | 5 | 0 | 5 | 0 | 45 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
197.25 | 64-474A-4-4,75 | 2 | 38 | 60 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 2 | 25 | 0 | 0 | 0 | 0 | 58 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
202.25 | 64-474A-5-1,75 | 10 | 40 | 50 | Lower pleistocene | (CALCAREOUS) SILTY CLAY | Dominat lithology; numerical abundance | 10 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 25 | 2 | 0 | 10 | 0 | 25 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
211.55 | 64-474A-6-1,55 | 1 | 19 | 80 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 3 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 5 | 1 | 0 | 2 | 0 | 65 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
211.75 | 64-474A-6-1,75 | 2 | 28 | 70 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 5 | 0 | 25 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 3 | 10 | 2 | 0 | 2 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
211.95 | 64-474A-6-1,95 | 5 | 30 | 65 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 5 | 0 | 25 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 15 | 0 | 0 | 2 | 0 | 40 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
212.05 | 64-474A-6-11,105 | 0 | 60 | 40 | Lower pleistocene | NANNO BEARING CLAYEY SILT | numerical abundance | 12 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 2 | 10 | 5 | 2 | 5 | 0 | 40 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
212.25 | 64-474A-6-11,125 | 10 | 45 | 45 | Lower pleistocene | Dominat lithology; numerical abundance | 0 | 0 | 15 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 3 | 40 | 3 | 0 | 6 | 0 | 16 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | |
212.45 | 64-474A-6-11,145 | 20 | 50 | 30 | Lower pleistocene | FORAM NANNO BEARING SANDY SILTY | Dominat lithology; numerical abundance | 1 | 0 | 8 | 8 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 19 | 19 | 0 | 1 | 0 | 38 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.55 | 64-474A-6-2,5 | 60 | 20 | 20 | Lower pleistocene | SILTY SAND FORAM BEARING | numerical abundance | 0 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 40 | 10 | 0 | 10 | 0 | 10 | 0 | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.62 | 64-474A-6-2,12 | 100 | 0 | 0 | Lower pleistocene | COARSE SAND LAYER AT BASE OF TURBIDITE | numerical abundance | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 20 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
212.63 | 64-474A-6-2,13 | 100 | 0 | 0 | Lower pleistocene | BASE TURBIDITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 37 | 37 | 0 | 0 | 15 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
213.27 | 64-474A-6-2,77 | 2 | 33 | 65 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 10 | 0 | 15 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 4 | 10 | 2 | 0 | 5 | 0 | 25 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
222.50 | 64-474A-7-2,50 | 1 | 49 | 50 | Lower pleistocene | Dominat lithology; numerical abundance | 5 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 5 | 20 | 10 | 0 | 2 | 0 | 25 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | |
233.75 | 64-474A-8-3,75 | 10 | 70 | 20 | Lower pleistocene | CLAYEY SILT | Dominat lithology; relative abundance | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 5 | 25 | 25 | 0 | 1 | 0 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 75 | 0 | 0 |
236.40 | 64-474A-8-5,40 | 85 | 0 | 0 | Lower pleistocene | IN GRAY SAND, AT BASE OF 1 CYCLE-MUDDY | Minor lithology; numerical abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 20 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
236.68 | 64-474A-8-5,68 | 1 | 39 | 60 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 10 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 5 | 15 | 0 | 0 | 4 | 0 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
241.81 | 64-474A-9-2,81 | 5 | 40 | 55 | Lower pleistocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 25 | 1 | 10 | 10 | 0 | 0 | 2 | 0 | 15 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
243.40 | 64-474A-9-3,90 | 3 | 12 | 85 | Lower pleistocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 5 | 0 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 10 | 1 | 2 | 10 | 0 | 0 | 4 | 0 | 45 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
244.77 | 64-474A-9-4,77 | 2 | 43 | 55 | Lower pleistocene | Dominat lithology; numerical abundance | 15 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 1 | 0 | 5 | 0 | 1 | 0 | 45 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 3 | 0 | |
244.77 | 64-474A-9-4,77 | 0 | 25 | 75 | Lower pleistocene | SILICEOUS SILTY CLAY | Minor lithology; numerical abundance | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
249.60 | 64-474A-10-1,60 | 10 | 60 | 30 | Lower pleistocene | CLAYEY SILTSTONE | Dominat lithology; numerical abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 1 | 20 | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
252.60 | 64-474A-10-3,60 | 10 | 30 | 60 | Lower pleistocene | Dominat lithology; numerical abundance | 15 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 1 | 2 | 20 | 0 | 0 | 1 | 0 | 40 | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | |
254.10 | 64-474A-10-4,60 | 20 | 20 | 50 | Lower pleistocene | CALCAREOUS SILTY CLAYSTONE | Dominat lithology; numerical abundance | 20 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 25 | 1 | 0 | 3 | 0 | 36 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
259.60 | 64-474A-11-11,110 | 0 | 30 | 70 | Lower pleistocene | DIATOM BEARING CLAYEY SILTSTONE | Dominat lithology; relative abundance | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 20 | 20 | 0 | 2 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.71 | 64-474A-11-2,71 | 85 | 15 | 0 | Lower pleistocene | GRAY SAND, HEAVY MINERAL SAND | Minor lithology; numerical abundance | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 46 | 23 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 | 2 | 6 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.89 | 64-474A-11-31,139 | 15 | 35 | 20 | Lower pleistocene | CALCAREOUS SILTY CLAYSTONE | Dominat lithology; numerical abundance | 20 | 0 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 1 | 20 | 20 | 0 | 3 | 0 | 10 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
262.89 | 64-474A-11-31,139 | 5 | 65 | 55 | Lower pleistocene | CLAYEY SILTSTONE | Dominat lithology; numerical abundance | 45 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 20 | 3 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
269.65 | 64-474A-12-2,15 | 5 | 50 | 45 | Lower pleistocene | CALCAREOUS, QTZ CLAYEY SILT | numerical abundance | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 25 | 25 | 0 | 0 | 0 | 30 | 0 | 5 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
273.10 | 64-474A-12-4,60 | 50 | 20 | 30 | Lower pleistocene | MUDDY SAND | numerical abundance | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 40 | 20 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
281.36 | 64-474A-13-3,86 | 0 | 80 | 20 | Lower pleistocene | QUARTZOSE CLAYEY SILT | Dominat lithology; numerical abundance | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 0 | 0 | 0 | 10 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
282.06 | 64-474A-13-4,6 | 0 | 40 | 60 | Lower pleistocene | Dominat lithology; numerical abundance | 20 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 40 | 0 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
283.06 | 64-474A-13-41,106 | 30 | 60 | 10 | Lower pleistocene | QUARTZOSE SANDY SILT | Dominat lithology; numerical abundance | 13 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 35 | 0 | 5 | 0 | 0 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
287.39 | 64-474A-14-1,39 | 10 | 80 | 10 | Lower pleistocene | QUARTZOSE SILTSTONE | Dominat lithology; relative abundance | 12 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 35 | 0 | 0 | 0 | 5 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
290.79 | 64-474A-14-3,79 | 30 | 50 | 20 | Lower pleistocene | CLAYEY SILTSTONE | Dominat lithology; relative abundance | 5 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 10 | 15 | 0 | 15 | 0 | 20 | 0 | 10 | 0 | 1 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
293.80 | 64-474A-14-5,80 | 10 | 20 | 70 | Lower pleistocene | QUARTZOSE NANNO OOZE | Dominat lithology; relative abundance | 5 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 10 | 10 | 0 | 10 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
307.03 | 64-474A-16-11,103 | 0 | 40 | 60 | Lower pleistocene | CLAYSTONE LITH | Dominat lithology; numerical abundance | 5 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 18 | 5 | 0 | 5 | 0 | 40 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
309.77 | 64-474A-16-3,77 | 15 | 50 | 35 | Lower pleistocene | IN THE MIDDLE OF A SILTY MUD TURBIDITE | Dominat lithology; numerical abundance | 2 | 0 | 15 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 15 | 5 | 0 | 15 | 0 | 40 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
310.01 | 64-474A-16-31,101 | 0 | 20 | 80 | Lower pleistocene | CLAYSTONE | Dominat lithology; relative abundance | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 5 | 0 | 0 | 0 | 60 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
316.15 | 64-474A-17-1,65 | 2 | 28 | 70 | Lower pleistocene | SILTY CLAYSTONE W/NANNOS | Dominat lithology; numerical abundance | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 5 | 0 | 65 | 0 | 2 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
320.60 | 64-474A-17-4,60 | 2 | 40 | 58 | Lower pleistocene | SILTY CLAYSTONE WITH NANNOS | relative abundance | 10 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 2 | 15 | 15 | 0 | 0 | 0 | 50 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 |
321.76 | 64-474A-17-5,26 | 0 | 55 | 45 | Lower pleistocene | Minor lithology; relative abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 15 | 15 | 0 | 20 | 0 | 40 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | |
326.10 | 64-474A-18-11,110 | 0 | 35 | 65 | Lower pleistocene | SILTY CLAYSTONE(QUARTZOSE) W/15% NANNOSM QTZ 20,FEL 15,MICA 10,HVY.MINS | Dominat lithology; relative abundance | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
327.90 | 64-474A-19-1,90 | 0 | 40 | 60 | Lower pleistocene | QUARTZOSE SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 10 | 0 | 60 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
330.35 | 64-474A-19-3,35 | 15 | 40 | 45 | Lower pleistocene | CLAYEY SILTSTONE (QUART RICH) | Minor lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 25 | 0 | 0 | 0 | 45 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
344.83 | 64-474A-21-1,83 | 1 | 14 | 85 | Lower pleistocene | CALCAREOUS MARLSTONE | Dominat lithology; relative abundance | 50 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
345.84 | 64-474A-21-2,34 | 5 | 30 | 65 | Lower pleistocene | Dominat lithology; relative abundance | 20 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 4 | 0 | 2 | 0 | 60 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | |
350.06 | 64-474A-21-5,6 | 70 | 20 | 10 | Lower pleistocene | SILTY FINE SANDSTONE | Dominat lithology; numerical abundance | 7 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 10 | 0 | 15 | 0 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
350.90 | 64-474A-21-5,90 | 80 | 15 | 5 | Lower pleistocene | SILTY FINE SANDSTONE (ARKOSE) | Dominat lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 40 | 10 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
355.60 | 64-474A-22-2,60 | 2 | 38 | 60 | Lower pleistocene | SILTY CLAY | Dominat lithology; numerical abundance | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 1 | 0 | 2 | 0 | 55 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
369.85 | 64-474A-23-5,85 | 5 | 35 | 60 | Lower pleistocene | SILTY CLAYSTONE | numerical abundance | 15 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 1 | 0 | 45 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
372.93 | 64-474A-24-1,43 | 0 | 30 | 70 | Lower pleistocene | NANNO RICH SILTY QTZ CLAY | Minor lithology; relative abundance | 5 | 0 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 70 |
382.77 | 64-474A-25-1,77 | 2 | 28 | 70 | Lower pleistocene | Dominat lithology; numerical abundance | 15 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 2 | 0 | 35 | 0 | 3 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
383.68 | 64-474A-25-2,18 | 5 | 75 | 20 | Lower pleistocene | QUARTZOSE CLAYEY SILT | Dominat lithology; relative abundance | 30 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 5 | 0 | 1 | 0 | 20 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
385.77 | 64-474A-25-3,77 | 0 | 40 | 60 | Lower pleistocene | SILTY CLAY | Dominat lithology; relative abundance | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 1 | 0 | 60 | 0 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
388.40 | 64-474A-25-5,40 | 0 | 0 | 0 | Lower pleistocene | SAND IN A MUDDY TURBIDITE BASE | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 16 | 16 | 0 | 66 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
388.41 | 64-474A-25-5,41 | 5 | 30 | 65 | Lower pleistocene | Dominat lithology; numerical abundance | 10 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 2 | 0 | 5 | 0 | 20 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | |
392.55 | 64-474A-26-11,105 | 5 | 35 | 60 | Lower pleistocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 10 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 2 | 0 | 3 | 0 | 25 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
393.78 | 64-474A-26-2,78 | 0 | 70 | 30 | Lower pleistocene | CLAYEY SILT | Dominat lithology; numerical abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 3 | 0 | 25 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
402.86 | 64-474A-27-2,36 | 0 | 40 | 60 | Lower pleistocene | Dominat lithology; numerical abundance | 15 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 3 | 0 | 4 | 0 | 15 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
403.54 | 64-474A-27-21,104 | 5 | 50 | 45 | Lower pleistocene | Dominat lithology; numerical abundance | 10 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 40 | 4 | 0 | 3 | 0 | 8 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
404.72 | 64-474A-27-3,72 | 0 | 10 | 30 | Lower pleistocene | Dominat lithology; numerical abundance | 10 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 1 | 0 | 1 | 0 | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | |
404.72 | 64-474A-27-3,72 | 50 | 20 | 90 | Lower pleistocene | Dominat lithology; numerical abundance | 20 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 2 | 0 | 75 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
407.66 | 64-474A-27-5,66 | 10 | 30 | 60 | Lower pleistocene | SILTY CLAY | Minor lithology; numerical abundance | 17 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 1 | 0 | 60 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
411.14 | 64-474A-28-1,64 | 2 | 30 | 68 | Lower pleistocene | (ORGANIC MATTER RICH) SILTY CLAYSTONE | Dominat lithology; relative abundance | 10 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 1 | 0 | 2 | 0 | 15 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
411.16 | 64-474A-28-1,66 | 10 | 0 | 90 | Lower pleistocene | ALTERED ASH, WHITE LAYER | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
415.28 | 64-474A-28-4,28 | 5 | 40 | 55 | Lower pleistocene | Dominat lithology; numerical abundance | 20 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 2 | 0 | 2 | 0 | 20 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
420.00 | 64-474A-29-1,0 | 0 | 30 | 70 | Lower pleistocene | SILTY CLAYSTONE | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 1 | 0 | 60 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
425.56 | 64-474A-29-41,106 | 0 | 0 | 0 | Cenozoic | COARSE SAND | Minor lithology; numerical abundance | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
425.57 | 64-474A-29-41,107 | 20 | 30 | 50 | Cenozoic | CEMENTED SAND LAYER | numerical abundance | 30 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 40 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
425.60 | 64-474A-29-41,110 | 0 | 0 | 0 | Cenozoic | WOOD FRAG FROM BASE OF TURBIDITE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
426.86 | 64-474A-29-5,86 | 0 | 80 | 20 | Cenozoic | CLAYEY SILTSTONE | Dominat lithology; relative abundance | 5 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 30 | 0 | 0 | 0 | 15 | 0 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
430.90 | 64-474A-30-11,140 | 15 | 25 | 60 | Cenozoic | Dominat lithology; numerical abundance | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 2 | 1 | 0 | 50 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | |
441.79 | 64-474A-31-21,129 | 2 | 10 | 78 | Cenozoic | SLIGHTLY SILTY CLAYSTONE | Dominat lithology; relative abundance | 12 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 1 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
442.54 | 64-474A-31-3,54 | 0 | 40 | 60 | Cenozoic | Dominat lithology; numerical abundance | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 10 | 2 | 0 | 0 | 55 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
455.20 | 64-474A-32-5,70 | 5 | 35 | 60 | Cenozoic | MUD SILTY CLAY | Dominat lithology; numerical abundance | 3 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 20 | 0 | 2 | 0 | 50 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 95 | 0 | 0 |
457.70 | 64-474A-32-7,20 | 0 | 50 | 50 | Upper pliocene | TYPICAL OF MORE SILTY MUD | Dominat lithology; numerical abundance | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 0 | 0 | 50 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
458.73 | 64-474A-33-1,73 | 0 | 35 | 65 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 15 | 0 | 5 | 0 | 40 | 0 | 10 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
462.80 | 64-474A-33-4,30 | 5 | 40 | 45 | Upper pliocene | SILTY CLAYSTONE W/NANNOS | Minor lithology; numerical abundance | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 15 | 0 | 5 | 0 | 35 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
469.40 | 64-474A-34-2,40 | 60 | 30 | 10 | Upper pliocene | SILTY SAND | Minor lithology; numerical abundance | 6 | 0 | 7 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 40 | 30 | 0 | 10 | 0 | 5 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
469.50 | 64-474A-34-2,50 | 0 | 25 | 75 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; relative abundance | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 20 | 0 | 3 | 0 | 40 | 0 | 5 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
480.48 | 64-474A-35-3,48 | 2 | 50 | 48 | Upper pliocene | CLAYEY SILT (BASE OF FINE GRAINED TURB)M QTZ 20,FEL 20,MICA 2,CLAY 40,PY | numerical abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
480.48 | 64-474A-35-3,48 | 1 | 39 | 60 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 10 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 3 | 0 | 4 | 0 | 25 | 0 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
481.90 | 64-474A-35-4,40 | 0 | 20 | 60 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 2 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 1 | 0 | 30 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
481.90 | 64-474A-35-4,40 | 0 | 40 | 80 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 20 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 3 | 0 | 50 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
486.54 | 64-474A-36-1,4 | 0 | 0 | 0 | Upper pliocene | CALCITE CEMENTED QTZ FEL SANDSTONE | Minor lithology; numerical abundance | 40 | 0 | 0 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
489.47 | 64-474A-36-21,147 | 1 | 29 | 70 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 2 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
490.28 | 64-474A-36-3,78 | 5 | 25 | 25 | Upper pliocene | MUDDY SANDSTONE | Dominat lithology; numerical abundance | 10 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 2 | 0 | 2 | 0 | 25 | 0 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
490.28 | 64-474A-36-3,78 | 50 | 30 | 65 | Upper pliocene | SILTY CLAYSTONE | Minor lithology; numerical abundance | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 30 | 0 | 3 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
496.34 | 64-474A-37-1,34 | 0 | 0 | 0 | Upper pliocene | GRAI-SUPPORTED QTZ FEL SANDSTONE | Minor lithology; relative abundance | 40 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
497.95 | 64-474A-37-2,45 | 1 | 15 | 70 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 0 | 1 | 0 | 55 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
497.95 | 64-474A-37-2,45 | 2 | 30 | 84 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 10 | 0 | 2 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
506.20 | 64-474A-38-1,70 | 0 | 0 | 0 | Upper pliocene | POLYGENETIC COARSE SANDSTONE | Minor lithology; numerical abundance | 19 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 44 | 19 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 19 | 0 | 0 | 0 | 0 |
507.75 | 64-474A-38-2,75 | 0 | 40 | 60 | Upper pliocene | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 1 | 0 | 2 | 0 | 55 | 0 | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
515.70 | 64-474A-39-1,70 | 3 | 40 | 55 | SILTY CLAYSTONE (CALCAREOUS) | Dominat lithology; numerical abundance | 10 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 2 | 0 | 5 | 0 | 45 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | |
519.21 | 64-474A-39-31,121 | 0 | 5 | 95 | CALCAREOUS MARLSTONE | Dominat lithology; numerical abundance | 30 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
527.23 | 64-474A-40-21,123 | 0 | 0 | 0 | Lower pliocene | CALCITE CEMENTED ARKOSE | Minor lithology; numerical abundance | 40 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 10 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
529.40 | 64-474A-40-CC,6 | 10 | 40 | 50 | Lower pliocene | DOM LITH SILTY CLAY-SLIGHTLY CALC | Dominat lithology; numerical abundance | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 15 | 0 | 5 | 0 | 40 | 0 | 8 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
529.42 | 64-474A-40-CC,8 | 2 | 70 | 28 | Lower pliocene | Dominat lithology; relative abundance | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 2 | 0 | 3 | 0 | 28 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | |
534.80 | 64-474A-41-1,80 | 0 | 0 | 0 | COAL FRAGS (LIGNITE) | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
535.82 | 64-474A-41-2,32 | 5 | 50 | 45 | CLAYEY SILTSTONE, WHITE RADIAL | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
536.04 | 64-474A-41-2,54 | 2 | 60 | 38 | CLAYEY SILTSTONE (LIMESTONE) | Dominat lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
538.67 | 64-474A-41-4,17 | 0 | 0 | 0 | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | ||
541.28 | 64-474A-41-51,128 | 5 | 25 | 70 | SILTY CLAYSTONE (NEAR BASALT CONTACT) | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 7 | 0 | 0 | 0 | 65 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | |
545.00 | 64-474A-42-2,0 | 0 | 0 | 0 | MINS EXTRUDED FROM VESICLES IN BASALT | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |