Counties, states, countries, continents, or oceans | |
Chittenden | county |
Vermont | state |
United States | country |
North America | continent |
Land | continent |
Map quadrangles, from USGS or Canadian NTS | |
Mount Philo | quadrangle 1:24,000 scale |
Lake Champlain South | quadrangle 1:100,000 scale |
Lake Champlain | quadrangle 1:250,000 scale |
Watershed boundaries (USGS hydrologic units) | |
Winooski | hydrologic unit |
Richelieu | hydrologic accounting unit |
Richelieu | hydrologic subregion |
Mid Atlantic | hydrologic region |
Unit | State | Lithology |
---|---|---|
Danby Formation | VT | Upper Cambrian |
Clarendon Springs Formation | VT | Upper Cambrian |
Cutting Dolostone | VT | Lower Ordovician |
Shelburne Marble | VT | Lower Ordovician |
ID | Data type | Description |
---|---|---|
Vermont Regional | M-Dz | Vermont Regional 1190 line km with spacing 3.20 km over parts of VT |
Lake Champlain Detail | M/R-D | Lake Champlain Detail 1255 line km with spacing 2.00 km over parts of NY-VT |
Lake Champlain | M/R-D | Lake Champlain 906 line km with spacing 10.00 km over parts of NY-VT-NH |
Tract | Deposit Type | Mineralization age |
---|---|---|
NA18 | Sandstone-hosted Pb-Zn | Cambrian - Ordovician |
NA22 | Mississippi Valley, Appalachian Zn | Cambrian - Ordovician |
NA20 | Sedimentary exhalative Zn-Pb | Cambrian - Ordovician |
Domain | Crust type | Region |
---|---|---|
Laurentides | Passive margin | Southeastern Laurentia and Appalachians |
Sample ID | Date collected | Sample type |
---|---|---|
5322303 | 1977-09-22 | Stream sediment sample from flowing stream, sieved to less than 149 microns (-100 mesh) and dried at less than or equal to 110øC. |
Sample ID | Date collected | Sample type |
---|---|---|
1259037 | 1977-09-22 | Stream water sample filtered through a 0.8 micron filter at the site. |
Tract name | Deposit type | Geology |
---|---|---|
Pacific Margin | porphyry copper | Cretaceous through middle Tertiary volcanic and intrusive rocks representing a series of continental- and island-arc systems accreted and superimposed onto the paleomargin of northeast Asia. |