OBJECTID|MapUnit|Name|FullName|Age|Description|LegendDescription|HierarchyKey|ParagraphStyle|Label|Symbol|AreaFillPatternDescription|DescriptionSourceID|GeoMaterial|GeoMaterialConfidence|DescriptionOfMapUnits_ID|AreaFillRGB
|1||Postglacial deposits|Postglacial deposits||||001|Heading2||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0001|
2|f|Fill|Fill|Holocene|Consists of various materials including gravel, sand, silt, and clay.|Consists of various materials including gravel, sand, silt, and clay.|001-001|standaloneunit|f|f||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|"Made" or human-engineered land|high|DMU0002|219,198,145
3|h|Hillslope sediment|Hillslope sediment|Holocene|Primarily sand, silt, and clay eroded from adjacent upland areas; usually composed of till of the Kirby Lake Member of the Kewaunee Formation; typically 1 to 2 m thick.|Primarily sand, silt, and clay eroded from adjacent upland areas; usually composed of till of the Kirby Lake Member of the Kewaunee Formation; typically 1 to 2 m thick.|001-002|standaloneunit|h|h||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Colluvium and other widespread mass-movement sediment|high|DMU0003|193,183,155
4||Peat|Peat||||001-003|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0004|
5|p|Peat|Peat|Holocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|001-003-001|subunit|p|p||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Peat and muck|high|DMU0005|185,151,116
6|pg|Peat over sandy till|Peat over sandy till|Holocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|Peat overlying sandy till of the Horicon Member of the Holy Hill Formation.|001-003-002|subunit|pg|pg||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Peat and muck|low|DMU0006|214,174,146
7|po|Peat over lake sediment|Peat over lake sediment|Holocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|usually only occurs at elevations less than 800 ft above sea level; may be beach sediment near margins of wetland|001-003-003|subunit|po|po||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Peat and muck|low|DMU0007|168,168,192
8|ps|Peat over stream sediment|Peat over stream sediment|Holocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|Peat overlying postglacial or meltwater stream sediment consisting of silty and sandy sediment and some channel sand and silt.|001-003-004|subunit|ps|ps||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Peat and muck|low|DMU0008|214,143,136
9|s|Stream sediment|Stream sediment|Holocene|Typically consists of sand and silt that was deposited on floodplains adjacent to modern streams; typically 1 to 15 m thick; most of this sediment was probably deposited during the Holocene.|Typically consists of sand and silt that was deposited on floodplains adjacent to modern streams; typically 1 to 15 m thick; most of this sediment was probably deposited during the Holocene.|001-004|standaloneunit|s|s||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Alluvial sediment|high|DMU0009|249,192,203
10||Glacial deposits|Glacial deposits||||002|Heading2||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0010|
11||Lake sediment|Lake sediment||||002-001|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0011|
12|l|lake sediment|lake sediment|Pleistocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|002-001-001|subunit|l|l||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Lacustrine sediment|high|DMU0012|144,172,203
13|lf|Glacial Lake Fond du Lac sediment|Glacial Lake Fond du Lac sediment|Pleistocene|Organic-rich sediment consisting of decomposed plant matter occupying low-lying, flat to low-relief surfaces; thickness varies, but is typically 1 to 3 m thick.|Usually between elevations of 830 and 850 ft above sea level; largely silt and clay where deposited in deeper water grading to sand near the shoreline; typically 1 to 3 m thick; sediment deposited near the shoreline may include windblown sediment, washed h|002-001-002|subunit|lf|lf||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Lacustrine sediment, mostly fine-grained|medium|DMU0013|173,197,231
14||Meltwater-stream sediment|Meltwater-stream sediment||Sand and gravel deposited by streams originating from the margins of the Green Bay and Lake Michigan Lobes; commonly 1 to 30 m thick.|Sand and gravel deposited by streams originating from the margins of the Green Bay and Lake Michigan Lobes; commonly 1 to 30 m thick.|002-002|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0014|
15|sa|Meltwater-stream sediment in fans or deltas|Meltwater-stream sediment in fans or deltas|Pleistocene|Sand and gravel deposited by streams originating from the margins of the Green Bay and Lake Michigan Lobes; commonly 1 to 30 m thick.|Sediment deposited in an alluvial fan or delta immediately adjacent to a moraine or ice-contact face.|002-002-001|subunit|sa|sa||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Ice-contact and ice-marginal sediment, mostly coarse-grained|high|DMU0015|252,223,236
16|su|Meltwater-stream sediment|Meltwater-stream sediment|Pleistocene|Sand and gravel deposited by streams originating from the margins of the Green Bay and Lake Michigan Lobes; commonly 1 to 30 m thick.|Sediment deposited in proglacial river channels.|002-002-002|subunit|su|su||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Ice-contact and ice-marginal sediment, mostly coarse-grained|high|DMU0016|250,190,175
17|sc|Collapsed metlwater-stream sediment|Collapsed metlwater-stream sediment|Pleistocene|Sand and gravel deposited by streams originating from the margins of the Green Bay and Lake Michigan Lobes; commonly 1 to 30 m thick.|Collapsed meltwater-stream sediment deposited in alluvial fans, deltas, and proglacial river channels.|002-002-003|subunit|sc|sc|"hummock" pattern - fill is overlaid by irregular mesh of fill color plus 10% -20% black (FGDC pattern 523-DO)|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Ice-contact and ice-marginal sediment, mostly coarse-grained|high|DMU0017|250,191,186
18||Kewaunee Formation|Kewaunee Formation||||003|Heading2||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0018|
19||Kirby Lake Member|Kirby Lake Member||||003-001|Heading3||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0019|
20||Till|Till||Red, clayey silt with some gravel deposited by the Green Bay Lobe during its first readvance; generally at least 3 m thick.|Red, clayey silt with some gravel deposited by the Green Bay Lobe during its first readvance; generally at least 3 m thick.|003-001-001|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0020|
21|gk|Till of the Kirby Lake Member with nondescript topography|Till of the Kirby Lake Member of the Kewaunee Formation with nondescript topography|Pleistocene|Red, clayey silt with some gravel deposited by the Green Bay Lobe during its first readvance; generally at least 3 m thick.|Low-relief nondescript glacial topography; till generally draped over pre-existing topography.|003-001-001-001|subunit|gk|gik||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly clayey|high|DMU0021|153,212,192
22|gkl|Till of the Kirby Lake Member with nondescript topography and thin glacial Lake Oshkosh sediment|Till of the Kirby Lake Member of the Kewaunee Formation with nondescript topography and thin glacial Lake Oshkosh sediment|Pleistocene|Red, clayey silt with some gravel deposited by the Green Bay Lobe during its first readvance; generally at least 3 m thick.|Similar to gk but covered with thin patches of glacial Lake Oshkosh sediment that are typically less than 2 m thick. The Kirby Lake Member is located west of Lake Winnebago and the Fond du Lac River.|003-001-001-002|subunit|gkl|gkl|Hatching, bottom left to top right (208,233,218)|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly clayey|medium|DMU0022|153,212,192
23||Chilton Member|Chilton Member||||003-002|Heading3||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0023|
24||Till|Till||Red, clayey silt with some gravel deposited by the Lake Michigan Lobe during its first readvance; generally at least 3 m thick.|Red, clayey silt with some gravel deposited by the Lake Michigan Lobe during its first readvance; generally at least 3 m thick.|003-002-001|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0024|
25|gc|Till of the Chilton Member with nondescript topography|Till of the Chilton Member of the Kewaunee Formation with nondescript topography|Pleistocene|Red, clayey silt with some gravel deposited by the Lake Michigan Lobe during its first readvance; generally at least 3 m thick.|Low-relief nondescript glacial topography; till generally draped over pre-existing topography.|003-002-001-001|subunit|gc|gc||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly clayey|high|DMU0025|97,184,180
26|gcl|Till of the Chilton Member with nondescript topography and glacial Lake Oshkosh sediment|Till of the Chilton Member of the Kewaunee Formation with nondescript topography and glacial Lake Oshkosh sediment|Pleistocene|Red, clayey silt with some gravel deposited by the Lake Michigan Lobe during its first readvance; generally at least 3 m thick.|Similar to gc but covered with thin patches of glacial Lake Oshkosh sediment that are typically less than 2 m thick. The Chilton Member is located east of Lake Winnebago and the Fond du Lac River.|003-002-001-002|subunit|gcl|gcl|Hatching, bottom left to top right (208,233,218)|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly clayey|medium|DMU0026|97,184,180
27||Holy Hill Formation|Holy Hill Formation||||004|Heading2||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0027|
28||Horicon Member|Horicon Member||||004-001|Heading3||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0028|
29||Till|Till||Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay and Lake Michigan Lobes; generally at least 3 m thick.|Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay and Lake Michigan Lobes; generally at least 3 m thick.|004-001-001|superunit||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0029|
30|ghr|Till of the Horicon Member with rolling topography|Till of the Horicon Member of the Holy Hill Formation with rolling topography|Pleistocene|Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay and Lake Michigan Lobes; generally at least 3 m thick.|Generally rolling topography lacking drumlins.|004-001-001-001|subunit|ghr|ghr|"till" pattern - fill is overlaid by irregular stripes of fill color plus 10%-20% black (FGDC pattern 524-K)|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly sandy|high|DMU0030|206,230,193
31|ghs|Till of the Horicon Member with streamlined topography|Till of the Horicon Member of the Holy Hill Formation with streamlined topography|Pleistocene|Brown to reddish-brown, gravelly, clayey, silty sand deposited by the Green Bay and Lake Michigan Lobes; generally at least 3 m thick.|Rolling topography that was subglacially molded; contains streamlined landforms including drumlins and flutes.|004-001-001-002|subunit|ghs|ghs|"till" pattern - fill is overlaid by irregular stripes of fill color plus 10%-20% black (FGDC pattern 524-K)|FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Glacial till, mostly sandy|high|DMU0031|181,219,174
32||Bedrock|Bedrock||||005|Heading2||||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|||DMU0032|
33|r|Bedrock|Bedrock|Pre-Pleistocene|Dolomite, sandstone, quartzite, or granite; glacially scoured areas of bedrock near the ground surface are covered by less than 2 m of various sediment such as the sandy till of the Holy Hill Formation or sand and gravel.|Dolomite, sandstone, quartzite, or granite; glacially scoured areas of bedrock near the ground surface are covered by less than 2 m of various sediment such as the sandy till of the Holy Hill Formation or sand and gravel.|005-001|standaloneunit|r|r||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Rock|high|DMU0033|218,215,207
34|w|Water|Water|Pre-Pleistocene|Water|Water|006|standaloneunit||w||FondDuLac_Quaternary_Mode_Hooyer_Rawling_2021|Water or ice|high|DMU0034|200,222,238
