publications > water resources investigations > report 00-4251 > appendix i > deering estate park no. 1 core
Deering Estate Park No. 1 Core
| Depth (feet below land surface) |
Lithologic description |
|---|---|
| 0.0 - 1.5 | Oomoldic lime grainstone, white N9; medium grain size, ranges from fine to medium; well rounded; sparry calcite; 10 percent oomoldic and interparticle porosity; moderate hydraulic conductivity. |
| 1.5 - 2.0 | No recovery. |
| 2.0 - 2.3 | Shell fragment-rich clay lime mudstone, pale-yellowish-brown 10YR 6/2; clay grain size, ranges from clay to medium; 10 percent quartz sand; less than 5 percent interparticle porosity; very low hydraulic conductivity. |
| 2.3 - 4.5 | Quartz sand, pale-yellowish-brown, 10YR 6/2 grayish orange 10YR 7/4; fine to medium grain size, ranges from clay to medium; 5 percent clay, 3 percent skeletal fragments, 2 percent organic material (Holocene roots); 5 percent interparticle porosity, low hydraulic conductivity. |
| 4.5 - 5.5 | Rubble; oolitic-peloid lime grainstone, very pale orange 10YR 8/2 grayish orange 10YR 7/4; fine to medium grain size, ranges from fine to medium; 10 percent oomoldic porosity, pelmoldic and interparticle porosity; moderate hydraulic conductivity. |
| 5.5 - 8.0 | Oolitic-peloid lime grainstone, very pale orange 10YR 8/2 grayish orange 10YR 7/4; fine to medium grain size, ranges from fine to medium; 20 percent oomoldic and pelmoldic porosity; moderate hydraulic conductivity. |
| 8.0 - 10.0 | No recovery. |
| 10.0 - 12.0 | Oolitic-peloid lime grainstone, very pale orange 10YR 8/2; fine to medium grain size, ranges from fine to medium; mollusks and gastropods; 20 percent oomoldic and pelmoldic porosity; high hydraulic conductivity. |
| 12.0 - 15.0 | No recovery. |
| 15.0 - 15.3 | Bryozoan framestone, very pale orange 10YR 8/2; pebble grain size; skeletal fragments; 15 percent interparticle porosity; moderate hydraulic conductivity. |
| 15.3 - 15.5 | Laminate calcrete (exposure surface); moderate yellowish brown 10YR 5/4; clay grain size; micrite; less than 5 percent porosity; very low hydraulic conductivity. |
| 15.5 - 16.7 | Skeletal lime floatstone with a matrix of quartz sand-rich, peneroplid, peloid, skeletal fragment lime grainstone, very pale orange 10YR 8/2; fine to coarse grain size, ranges from fine to coarse; 15 percent interparticle and vuggy porosity; moderate hydraulic conductivity. |
| 16.7 - 20.0 | No recovery. |
| 20.0 - 20.5 | Skeletal-fragment lime grainstone, very pale orange 10YR 8/2; fine to medium grain size, ranges from very fine to coarse; 30 percent very fine to fine quartz sand; 25 percent vuggy porosity, riddled with solution channels; very high hydraulic conductivity. |
| 20.5 - 21.8 | No recovery. |
| 21.8 - 22.2 | Skeletal fragment, quartz-sand-rich lime grainstone, very pale orange 10YR 8/2; fine to medium grain size, ranges from very fine to coarse; 5 percent very fine to medium quartz sand; 20 percent vuggy porosity; high hydraulic conductivity. |
| 22.2 - 23.5 | Monastrea lime framestone, very pale orange 10YR 8/2; cobble grain size; 25 percent intraparticle porosity; very high hydraulic conductivity. |
| 23.5 - 25.0 | No recovery. |
| 25.0 - 25.5 | Monastrea lime framestone, very pale orange 10YR 8/2; cobble grain size; 25 percent intraparticle porosity; very high hydraulic conductivity. |
| 25.5 - 26.5 | No recovery. |
| 26.5 - 27.0 | Rubble of limestone. |
| 27.0 - 27.5 | Quartz sand-rich, skeletal-fragment lime packstone, very pale orange 10YR 8/2; clay and fine to medium grain size; ranges from clay to pebble; 10 percent very fine to fine quartz sand; 25 percent vuggy porosity, riddled with solution channels; very high hydraulic conductivity. |
| 27.5 - 28.2 | Skeletal-fragment lime floatstone with matrix of mollusk, miliolid, quartz-sand-rich lime packstone and wackestone; very light gray N8; clay and fine to medium grain size, ranges from clay to pebble; 10 percent very fine to fine quartz sand; 10 percent vuggy porosity; low hydraulic conductivity. |
| 28.2 - 31.0 | No recovery. |
| 31.0 - 32.7 | Lime-mud-rich quartz sandstone; very light gray N8; clay and fine to medium grain size, ranges from clay to granule; 60 percent very fine to medium quartz sand; 15 percent lime mud; 25 percent mollusks and skeletal fragments; 20 percent vuggy porosity, riddled with solution channels; very high hydraulic conductivity. |
| 32.7 - 35.0 | Lime-mud-rich queers sandstone, very light gray N8; clay and very fine to medium grain size, ranges from clay to granule; 60 percent very fine to medium quartz sand, 15 percent lime mud, 25 percent mollusks and skeletal fragments; 15 percent vuggy porosity; minor solution channels; high hydraulic conductivity. |
| 35.0 - 35.4 | Mollusk lime floatstone with a matrix of skeletal fragment, quartz-rich lime packstone, very pale orange 10YR 8/2; clay and very fine to medium grain size, ranges from clay to pebble; 30 percent very fine to medium quartz sand, mollusks, gastropods and dasyclad algae; 15 percent moldic and root-mold porosity; moderate hydraulic conductivity; abundant millimeter- wide root molds suggest an exposure surface at 35 feet. |
| 35.4 - 35.6 | Skeletal fragment floatstone with a matrix of skeletal-fragment-rich quartz sand, very light gray N8; clay and very fine to medium grain size, ranges from very fine to pebble; very fine to medium quartz sand; 20 percent vuggy porosity; high hydraulic conductivity. |
| 35.6 - 37.5 | Skeletal lime floatstone with matrix of skeletal, quartz-sand-rich lime packstone, very pale orange 10YR 8/2; clay and coarse to pebble grain size, ranges from clay to pebble; 10 percent very fine to medium quartz sand, gastropods, mollusks and peneroplids; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 37.5 - 37.8 | Branching Porites lime rudstone with matrix of skeletal lime grainstone; very pale orange 10YR 8/2; fine to medium and pebble to cobble grain size, ranges from clay to cobble; 10 percent very fine to medium quartz sand; 20 percent interparticle porosity; moderate hydraulic conductivity. |
| 37.8 - 38.8 | Skeletal-fragment lime packstone, very pale orange 10YR 8/2; clay and coarse to pebble grain size, ranges from clay to pebble; 15 percent very fine to medium quartz sand; mollusks, peneroplids and miliolids; 20 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 38.8 - 39.2 | Skeletal fragment floatstone with matrix of skeletal-fragment quartz sandstone; very light gray N8; clay and very fine to medium grain size, ranges from clay to pebble; |
| 39.2 - 39.8 | Gastropod lime floatstone with matrix of gastropod and mollusk lime packstone, very pale orange 10YR 8/2; clay and very fine to fine and pebble grain size, ranges from clay to pebble; 10 percent very fine to fine quartz sand, gastropods and mollusks; 25 percent moldic porosity; moderate hydraulic conductivity; probable lacustrine environment. |
| 39.8 - 39.9 | Peneroplid-rich floatstone with matrix of quartz sandstone, very pale orange 10YR 8/2; clay and very fine to medium and pebble grain size; ranges from clay to pebble; 80 percent very fine to medium quartz sand, peneroplids; 20 percent vuggy and interparticle porosity; high hydraulic conductivity. |
| 39.9 - 40.0 | Laminated calcrete, pale-yellowish-brown 10YR 6/2; clay grain size, ranges from clay to very fine; 10 percent silt to very fine quartz grains; 5 percent porosity; very low hydraulic conductivity; exposure surface at 39.9 feet. |
| 40.0 - 41.0 | Skeletal lime floatstone with matrix of skeletal-fragment lime grainstone; very pale orange 10YR 8/2; medium to granule grain size, ranges from very fine to pebble; peneroplids, mollusks and gastropods; 25 percent interparticle and vuggy porosity; high hydraulic conductivity. |
| 41.0 - 45.0 | Skeletal floatstone with matrix of quartz sandstone, very pale orange 10YR 8/2; very fine to medium grain size, ranges from very fine to pebble; mollusks and dasyclad algae; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 45.0 - 49.0 | No recovery. |
| 49.0 - 49.5 | Mollusk floatstone with matrix of skeletal fragment quartz sandstone, very light gray N8; fine to medium grain size, ranges from silt to pebble; 70 percent very fine to fine quartz sand, mollusks, benthic foraminifers and branching Porites; 20 percent moldic and vuggy porosity; high hydraulic conductivity. |
| 49.5 - 50.5 | Skeletal, quartz-sand-rich lime grainstone, very pale orange 10YR 8/2; very fine to medium grain size, ranges from silt to pebble; 30 percent very fine to medium sand, mollusks and gastropods; 15 percent moldic porosity; moderate hydraulic conductivity. |
| 50.5 - 55.0 | No recovery. |
| 55.0 - 57.5 | Skeletal fragment floatstone with matrix of skeletal-fragment-rich quartz sandstone, very light gray N8; very fine to fine grain size, ranges from very fine to pebble; 50 percent very fine to fine quartz grains, mollusks and gastropods; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 57.5 - 58.7 | Skeletal floatstone with matrix of skeletal-fragment-rich quartz sandstone, very light gray N8; very fine to fine grain size, ranges from very fine to pebble; 60 percent very fine to fine quartz grains, mollusks, dasyclad algae, benthic foraminifers and bryozoans; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 58.7 - 61.0 | No recovery. |
| 61.0 - 61.7 | Rubble of skeletal floatstone with matrix of skeletal-fragment-rich quartz sandstone; very light gray N8; very fine to fine grain size, ranges from very fine to pebble; 60 percent very fine to fine quartz sand, mollusks, dasyclad algae, benthic foraminifers and bryozoans; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 61.7 - 67.0 | Skeletal-fragment lime floatstone with matrix of quartz-sand-rich skeletal lime packstone, very pale orange 10YR 8/2; very fine to fine grain size, ranges from very fine to pebble; 10 to 20 percent very fine to fine quartz sand, mollusks and gastropods; 15 percent moldic porosity, minor vugs; moderate hydraulic conductivity. |
| 67.0 - 68.0 | Rubble of skeletal-fragment-rich quartz sandstone, very light gray N8; very fine to fine grain size, ranges from very fine to pebble; 15 percent vuggy porosity; moderate hydraulic conductivity. |
| 68.0 - 70.8 | Mollusk skeletal lime floatstone with matrix of skeletal-fragment lime grainstone, very pale orange 10YR 8/2; very fine to medium grain size, ranges from very fine to pebble; 10 percent very fine to fine quartz sand, mollusks, gastropods, branching Porites, bryozoans and sand dollars; 20 percent moldic and vuggy porosity, high hydraulic conductivity. |
| 70.8 - 70.8 | Laminate calcrete, grayish orange 10YR 7/4; clay to silt grain size, ranges from clay to silt; less than 5 percent porosity; very low hydraulic conductivity; 1-millimeter-thick calcrete, exposure surface at 70.8 feet. |
| 70.8 - 73.0 | Mollusk, skeletal-fragment lime floatstone with matrix of skeletal-fragment lime grainstone, very pale orange 10YR 8/2 and very light gray N8; very fine to medium grain size, ranges from very fine to pebble; 10 percent very fine to fine quartz sand, mollusks and gastropods; 20 percent moldic and vuggy porosity; high hydraulic conductivity. |
| 73.0 - 75.0 | No recovery. |
| 75.0 - 75.5 | Mollusk floatstone with matrix of skeletal-fragment-rich quartz sandstone, very light gray N8; very fine to fine grain size, ranges from very fine to pebble; 70 percent very fine to fine quartz sand; mollusks and gastropods; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 75.5 - 84.0 | No recovery. |
| 84.0 - 85.0 | Skeletal-fragment lime packstone and mollusk, skeletal-fragment lime floatstone with matrix of skeletal lime packstone; very pale orange 10YR 8/2; clay to pebble grain size, ranges from clay to pebble; 20 percent very fine to fine quartz sand, red algae, mollusks and gastropods; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity; root molds, possible exposure surface at 84 feet. |
| 85.0 - 87.0 | No recovery. |
| 87.0 - 88.0 | Skeletal-fragment lime floatstone with matrix of skeletal-fragment lime grainstone, very pale orange 10YR 8/2; fine to medium grain size, ranges from very fine to pebble; 10 percent very fine quartz sand, red algae; 15 percent interparticle and moldic porosity; moderate hydraulic conductivity. |
| 88.0 - 90.0 | Skeletal-fragment lime floatstone with matrix of skeletal fragment, quartz-sand-rich lime packstone, very pale orange 10YR 8/2; clay to pebble grain size, ranges from clay to pebble; 10 percent very fine quartz sand, mollusks and gastropods; 20 percent moldic and vuggy porosity; high hydraulic conductivity. |
| 90.0 - 91.3 | Mollusk, skeletal-fragment lime rudstone with matrix of skeletal fragment, quartz-sand-rich lime packstone, very pale orange 10YR 8/2; clay to pebble grain size, ranges from clay to pebble; 10 percent very fine to very coarse quartz sand, mollusks and gastropodes; 20 percent moldic and vuggy porosity; high hydraulic conductivity. |
| 91.3 - 93.8 | No recovery. |
| 93.8 - 95.5 | Mollusk, skeletal fragment lime floatstone with matrix of quartz-sand-rich, skeletal-fragment lime packstone and wackestone, very pale orange 10YR 8/2; clay to pebble grain size, ranges from clay to pebble; 20 percent very fine to fine quartz sand; 15 percent moldic and vuggy porosity; moderate hydraulic conductivity. |
| 95.5 - 98.8 | Quartz-sand-rich skeletal lime packstone and wackestone, very pale orange 10YR 8/2; clay to granule grain size, ranges from clay to pebble; 20 percent very fine to coarse quartz sand; 10 percent moldic porosity; low hydraulic conductivity. |
| 98.8 - 101.0 | No recovery. |
Go back to Appendix I (cont'd): Lithologic description of St. Hugh's School Core |
Go ahead to Appendix I (cont'd): Lithologic description of Deering Estate Park No. 2 Core
U.S. Department of the Interior, U.S. Geological Survey
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Last updated: 20 January, 2005 @ 01:23 PM (KP)