Pleasant Hill, Cass Co., Missouri, USAi
| Regional Level Types | |
|---|---|
| Pleasant Hill | Hill |
| Cass Co. | County |
| Missouri | State |
| USA | Country |
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Key
Latitude & Longitude (WGS84):
38° 47' 15'' North , 94° 16' 9'' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Pleasant Hill | 8,289 (2017) | 0.0km |
| Lake Winnebago | 1,144 (2017) | 9.1km |
| Strasburg | 142 (2017) | 9.4km |
| Greenwood | 5,569 (2017) | 9.6km |
| Lone Jack | 1,124 (2017) | 12.4km |
In creek valley
Regions containing this locality
| North America Plate | Tectonic Plate |
Select Mineral List Type
Standard Detailed Strunz Dana Chemical ElementsDetailed Mineral List:
| ⓘ Calcite Formula: CaCO3 Reference: Sherwood, M. D., & Williams, G. A. (1998). Missouri mineral locality index. Rocks & Minerals, 73(2), 98-117. |
| ⓘ Vivianite Formula: Fe2+3(PO4)2 · 8H2O Reference: Sherwood, M. D., & Williams, G. A. (1998). Missouri mineral locality index. Rocks & Minerals, 73(2), 98-117. |
List of minerals arranged by Strunz 10th Edition classification
| Group 5 - Nitrates and Carbonates | |||
|---|---|---|---|
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Vivianite | 8.CE.40 | Fe2+3(PO4)2 · 8H2O |
List of minerals arranged by Dana 8th Edition classification
| Group 14 - ANHYDROUS NORMAL CARBONATES | |||
|---|---|---|---|
| A(XO3) | |||
| ⓘ | Calcite | 14.1.1.1 | CaCO3 |
| Group 40 - HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES | |||
| A3(XO4)2·xH2O | |||
| ⓘ | Vivianite | 40.3.6.1 | Fe2+3(PO4)2 · 8H2O |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Vivianite | Fe32+(PO4)2 · 8H2O |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Vivianite | Fe32+(PO4)2 · 8H2O |
| O | ⓘ Calcite | CaCO3 |
| P | Phosphorus | |
| P | ⓘ Vivianite | Fe32+(PO4)2 · 8H2O |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Vivianite | Fe32+(PO4)2 · 8H2O |
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