publications > water resources investigations > report 00-4251 > appendix i > peacock park core
Peacock Park Core
| Depth (feet below land surface) |
Lithologic description |
|---|---|
| 0.0 - 1.0 | Quartz-sand-rich soil, dark-yellowish-brown 10YR 4/2; mainly clay and fine to medium grain size, ranges from clay to coarse; roots; 20 percent interparticle porosity; low hydraulic conductivity. |
| 1.0 - 2.0 | Rubble of oolitic lime grainstone, very pale orange 10YR 8/2; mainly medium grain size; 25 percent oomoldic and probable solution-channel porosity; high hydraulic conductivity. |
| 2.0 - 3.0 | Loose quartz sand, very pale orange 10YR 8/2, grayish orange 10YR 7/4; mainly fine to medium, ranges from fine to medium; 25 percent interparticle porosity; moderate hydraulic conductivity; bay sediments(?). |
| 3.0 - 4.0 | No recovery. |
| 4.0 - 5.0 | Silty mudstone, very pale orange 10YR 8/2, pale-yellowish-brown 10YR 6/2, brownish gray 5YR 4/1; mainly clay to silt; roots; 5 percent interparticle porosity; very low hydraulic conductivity; bay sediments(?). |
| 5.0 - 5.5 | Peat; black N1; mainly clay to silt; roots; 25 percent interparticle porosity; very low hydraulic conductivity; bay sediments(?). |
| 5.5 - 8.5 | Loose quartz sand, pale-yellowish-brown 10YR 6/2, light gray N7; mainly fine to medium grain size, ranges from very fine to coarse; caved grains; 25 percent interparticle porosity; moderate hydraulic conductivity; mainly caved quartz sand (?). |
| 8.5 - 9.0 | Calcretized oolitic lime grainstone, very pale orange 10YR 8/2, pale-yellowish-brown 10YR 6/2; medium grain size; 25 percent oomoldic and solution-channel porosity; high hydraulic conductivity. |
| 9.0 - 11.0 | No recovery. |
| 11.0 - 13.0 | Loose quartz sand, very light gray N7; mainly fine to medium grain size, ranges from fine to coarse; caved particles and roots; 25 percent interparticle porosity; moderate hydraulic conductivity. |
| 13.0 - 13.8 | Rubble of oolitic lime grainstone, very pale orange 10YR 8/2; mainly fine grain size; ranges from fine to pebble; mollusks and branching bryozoans 25 percent oomoldic and solution-channel porosity; high hydraulic conductivity. |
| 13.8 - 15.0 | Rubble of oolitic lime grainstone, very pale orange 10YR 8/2, grayish orange 10YR 7/4, moderate yellowish brown 10 YR 5/4; mainly fine grain size; ranges from fine to pebble; mollusks and branching bryozoans 25 percent oomoldic and solution-channel porosity; high hydraulic conductivity. |
| 15.0 - 16.0 | Loose quartz sand, very light gray N7; mainly fine to medium grain size, ranges from fine to coarse; 25 percent interparticle porosity; moderate hydraulic conductivity. |
| 16.0 - 18.0 | Rubble of oolitic lime grainstone, very pale orange 10YR 8/2, grayish orange 10YR 7/4, moderate yellowish brown 10YR 5/4; mainly fine grain size, ranges from fine to medium; 25 percent oomoldic and solution-channel porosity; high hydraulic conductivity. |
| 18.0 - 23.2 | No recovery. |
| 23.2 - 24.0 | Rubble of sandstone cemented with calcite and oolitic lime grainstone, sample is probably cave, very pale orange 10 YR 8/2, grayish orange 10YR 7/4, moderate yellowish brown 10YR 5/4; mainly fine grain size, ranges from fine to medium; 25 percent oomoldic, interparticle and vuggy porosity; high hydraulic conductivity. |
| 24.0 - 25.0 | No recovery. |
| 25.0 - 25.5 | Rubble of oolitic lime grainstone, very pale orange 10YR 8/2, grayish orange 10YR 7/4; mainly fine grain size, ranges from fine to pebble; branching bryozoans and mollusks; 25 percent oomoldic porosity; high hydraulic conductivity. |
| 25.5 - 30.0 | No recovery. |
| 30.0 - 30.8 | Skeletal-fragment lime grainstone, very pale orange 10YR 8/2, grayish orange 10YR 7/4, dark-yellowish-orange 10YR 6/6; mainly fine to medium grain size, ranges from very fine to granule; 35 percent vuggy, moldic, interparticle and solution-channel porosity; very high hydraulic conductivity; probable exposure surface between 25.5 and 30 feet. |
| 30.8 - 31.7 | Skeletal-fragment lime rudstone with skeletal-fragment lime grainstone matrix; very pale orange 10YR 8/2, grayish-orange 10YR 7/4, dark-yellowish-orange 10 YR 6/6; mainly fine to granule grain size; 35 percent vuggy, moldic, interparticle and solution-channel porosity; very high hydraulic conductivity. |
| 31.7 - 32.7 | Skeletal-fragment lime rudstone with skeletal-fragment lime grainstone matrix; very pale orange 10YR 8/2, grayish-orange 10YR 7/4, dark-yellowish-orange 10 YR 6/6; mainly medium to pebble grain size; 35 percent vuggy, moldic, interparticle and solution-channel porosity; very high hydraulic conductivity. |
| 32.7 - 34.0 | Monastrea lime framestone, very pale orange 10YR 8/2; mainly cobble grain size; 25 percent intraparticle porosity; very high hydraulic conductivity. |
| 34.0 - 35.0 | No recovery. |
| 35.0 - 36.0 | Rubble of coral lime framestone, very pale orange 10YR 8/2; mainly clay and pebble and cobble, ranges from clay to cobble; 25 percent intraparticle porosity; very high hydraulic conductivity. |
| 36.0 - 40.8 | No recovery. |
| 40.8 - 41.8 | Rubble of skeletal lime packstone, very pale orange 10YR 8/2, grayish orange 10YR 7/4; mainly clay to pebble; ranges from clay to pebble; 20 percent moldic and vuggy porosity; high hydraulic conductivity; possible cave. |
| 41.8 - 43.0 | Friable calcareous quartz sandstone; very pale orange 10YR 8/2, pale-yellowish-orange 10YR 6/6; grayish-orange 10YR 7/4; mainly very fine to fine grain size, ranges from very fine to medium; 20 percent interparticle porosity; moderate hydraulic conductivity. |
| 43.0 - 45.5 | Rubble of skeletal lime grainstone and packstone and oolitic lime grainstone, very pale orange 10YR 8/2, grayish-orange 10YR 7/4; mainly clay to pebble grain size, ranges from clay to pebble; 20 percent moldic, vuggy and interparticle porosity; high hydraulic conductivity; at least some of the rubbly limestone is cave (oolitic lime grainstone). |
| 45.5 - 51.0 | No recovery. |
| 51.0 -51.5 | Rubble of caved limestone. |
| 51.5 - 52.0 | Diplora coral lime framestone, very pale orange 10YR 8/2; mainly cobble grain size; 30 percent intraparticle porosity; very high hydraulic conductivity. |
| 52.0 - 61.0 | Rubble of caved limestone. |
| 61.0 - 62.5 | Skeletal fragment lime wackestone, packstone and grainstone, mottled combination of very pale orange 10YR 8/2, pale-yellowish-orange 10YR 8/6, grayish orange 10YR 7/4, and very light gray N7; mainly clay to medium grain size; ranges from clay to pebble; peloids, mollusks, gastropods and echinoid spines; 25 percent moldic, root-mold and minor solution-channel porosity; high hydraulic conductivity; mottled colors, root molds and solution channels suggest exposure surface between 52 and 61 feet. |
| 62.5 - 71.0 | No recovery. |
| 71.0 - 71.5 | Rubble of skeletal fragment lime wackestone, packstone and grainstone, mottled combination of very pale orange 10YR 8/2, pale-yellowish-orange 10YR 8/6, grayish orange 10YR 7/4, and very light gray N7; mainly clay to medium grain size; ranges from clay to pebble; peloids, mollusks, gastropods and echinoid spines; 25 percent moldic, root-mold and minor solution-channel porosity; high hydraulic conductivity. |
| 71.5 - 72.0 | Skeletal fragment lime wackestone and packstone, mottled combination of very pale orange 10YR 8/2, pale-yellowish-orange 10YR 8/6, grayish orange 10YR 7/4, and very light gray N7; mainly clay to medium grain size; ranges from clay to pebble; peloids, mollusks, miliolids and gastropods; 25 percent moldic, root-mold and minor solution-channel porosity; high hydraulic conductivity. |
| 72.0 - 73.0 | Red algae, skeletal fragment, quartz-sand-rich lime grainstone; very pale orange 10YR 8/2; light gray N8; mainly very fine to coarse grain size. ranges from very fine to pebble; 10 percent fine to medium quartz sand; red algae and mollusks; 20 percent moldic and interparticle porosity; moderate hydraulic conductivity. |
| 73.0 - 76.2 | No recovery. |
| 76.2 - 77.6 | Skeletal fragment, red algae, quartz-sand-rich lime grainstone; very light gray N7; light gray N8; mainly very fine to coarse grain size. ranges from very fine to pebble; 20 percent fine to medium quartz sand; mollusks; 15 percent moldic and interparticle porosity; moderate hydraulic conductivity. |
| 77.6 - 78.0 | Red algae lime floatstone with quartz-sand-rich, skeletal lime packstone matrix, mollusks, very pale orange 10YR 8/2, light gray N7; mainly clay to granule, ranges from clay to pebble; 20 percent fine to medium quartz sand, mollusks; 15 percent moldic, intergranular and vuggy porosity; moderate hydraulic conductivity. |
| 78.0 - 81.0 | No recovery. |
| 81.0 - 82.3 | Red algae, mollusk lime rudstone and floatstone with quartz-sand-rich, skeletal lime packstone matrix, light gray N7, very pale orange 10YR 8/2, grayish orange 10YR 7/4; mainly clay to pebble grain size, ranges from clay to pebble; 20 percent fine to medium quartz sand and minor coarse quartz sand; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 82.3 - 83.5 | Skeletal fragment, quartz-sand-rich lime grainstone, yellowish gray 5Y 8/1; mainly fine to medium grain size, ranges from very fine to medium; 15 to 25 percent very fine to fine quartz sand; mollusks, gastropods; 25 percent moldic and interparticle porosity; moderate hydraulic conductivity. |
| 83.5 - 84.9 | Lime mudstone, wackestone and packstone; very pale orange 10YR 8/2; mainly clay to very fine grain size, 10 percent very fine to fine quartz sand gastropods, mollusks; 15 percent moldic and root-mold porosity; low hydraulic conductivity; supratidal or intertidal environment, root molds, subaerial exposure surface at 83.5 feet. |
| 84.9 - 85.2 | Skeletal, quartz-sand-rich lime packstone; very pale orange 10YR 8/2; mainly clay to medium grain size; 20 percent very fine to fine quartz sand; 15 percent moldic porosity; moderate hydraulic conductivity. |
| 85.2 - 88.0 | No recovery. |
| 88.0 - 89.0 | Skeletal, quartz-sand-rich lime grainstone, very light gray N7, very pale orange 10YR 8/2; mainly very fine to medium grain size, ranges from very fine to coarse; 20 percent very fine to fine quartz sand, gastropods, mollusks; 20 percent moldic and interparticle porosity; moderate hydraulic conductivity. |
| 89.0 - 89.5 | Mollusk lime rudstone with quartz sand-rich, skeletal lime packstone matrix, very light gray N7, very pale orange 10YR 8/2; mainly clay to fine and pebble grain size, ranges from clay to pebble; 20 percent very fine to fine quartz sand; 15 percent moldic porosity; moderate hydraulic conductivity. |
| 89.5 - 91.0 | Skeletal, mollusk, quartz-sand-rich lime packstone and grainstone and minor lime floatstone with skeletal, quartz-sand-rich matrix; very light gray N7, very pale orange 10YR 8/2; mainly clay to medium grain size; ranges from clay to pebble; 30 percent very fine to fine quartz sand, mollusks, red algae; 15 percent moldic and interparticle porosity; moderate hydraulic conductivity. |
| 91.0 - 95.0 | No recovery. |
| 95.0 - 95.5 | Rubble of caved limestone. |
| 95.5 - 100.0 | Skeletal fragment, quartz-sand-rich lime grainstone and minor lime packstone, very light gray N7, very pale orange 10YR 8/2; mainly very fine to medium grain size, ranges from clay to pebble; 10 to 20 percent very fine to fine quartz sand and minor medium quartz sand, mollusks, gastropods, miliolids; 20 percent moldic, interparticle and vuggy porosity; moderate hydraulic conductivity. |
| 100.0 - 101.0 | No recovery. |
Go back to Appendix I (cont'd): Lithologic description of Mowry Canal Core |
Go ahead to Appendix II: Field Data Collected as Part of this Study
U.S. Department of the Interior, U.S. Geological Survey
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Last updated: 20 January, 2005 @ 01:23 PM (KP)