Jeffrey L Howard
Biographic Data
| ID | 5637623 |
|---|---|
| NAME | Jeffrey L Howard |
| GIVEN NAMES | Jeffrey L |
| FAMILY NAME | Howard |
| SIGNATURE | HOWARD J L |
| AFFILIATIONS | Wayne State University |
| ORCID | 0000-0001-8841-7182 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 9 |
| AUTHOR COUNT | 5 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1993 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 2 |
Soils of Urban and Human‐Impacted Landscapes
Anthropogenic soils (referred to here as anthrosoils) are soils that have been influenced, modified, or created by human activity. They are found worldwide in urban and other human‐impacted landscapes. Four distinct types of anthrosoils can be distinguished based on geographical setting and historical context: (i) agricultural, (ii) archaeological, (iii) mine‐related, and (iv) urban. Most anthrosoils found in agricultural and archaeological setti…
Soils of Urban and Human‐Impacted Landscapes
Soils of urban and human‐impacted landscapes (Anthrosols) differ from soils normally found in natural settings in that they have been modified so profoundly by human activity that they have characteristics outside the range of native soil series and require reclassification as a different type of soil. Anthrosols are widely distributed in agricultural, archaeological, mine‐related, and urban geographical settings. Agricultural Anthrosols are form…
Artifact preservation and post-depositional site-formation processes in an urban setting
Proposal to add anthrostratigraphic and technostratigraphic units to the stratigraphic code for classification of anthropogenic Holocene deposits
Anthropogenic surficial deposits are formed from Holocene and older deposits that have been so modified by human activity that their original form is unrecognizable. Because their characteristics are fundamentally different from those of natural origin, the creation of special stratigraphic categories seems justified. Two new material categories are proposed for the stratigraphic classification of anthropogenic deposits. An anthrostratigraphic un…
Alluvial Soil Chronosequence in the Inner Coastal Plain, Central Virginia
A chronological sequence of soils formed on a series of alluvial depositional surfaces ranging in age from late-middle Miocene to late Pleistocene was characterized to clarify soil-geomorphic relations and provide a basis for allostratigraphic subdivision of the inner Coastal Plain. On Quaternary river terraces, Ultic Hapludalfs containing abundant weatherable mineral species and clast types are estimated to have formed in 60,000-120,000 yr, wher…
Artifact preservation and post-depositional site-formation processes in an urban setting
Proposal to add anthrostratigraphic and technostratigraphic units to the stratigraphic code for classification of anthropogenic Holocene deposits
Anthropogenic surficial deposits are formed from Holocene and older deposits that have been so modified by human activity that their original form is unrecognizable. Because their characteristics are fundamentally different from those of natural origin, the creation of special stratigraphic categories seems justified. Two new material categories are proposed for the stratigraphic classification of anthropogenic deposits. An anthrostratigraphic un…
Alluvial Soil Chronosequence in the Inner Coastal Plain, Central Virginia
A chronological sequence of soils formed on a series of alluvial depositional surfaces ranging in age from late-middle Miocene to late Pleistocene was characterized to clarify soil-geomorphic relations and provide a basis for allostratigraphic subdivision of the inner Coastal Plain. On Quaternary river terraces, Ultic Hapludalfs containing abundant weatherable mineral species and clast types are estimated to have formed in 60,000-120,000 yr, wher…
Artifact preservation and post-depositional site-formation processes in an urban setting
Proposal to add anthrostratigraphic and technostratigraphic units to the stratigraphic code for classification of anthropogenic Holocene deposits
Anthropogenic surficial deposits are formed from Holocene and older deposits that have been so modified by human activity that their original form is unrecognizable. Because their characteristics are fundamentally different from those of natural origin, the creation of special stratigraphic categories seems justified. Two new material categories are proposed for the stratigraphic classification of anthropogenic deposits. An anthrostratigraphic un…
Soils of Urban and Human‐Impacted Landscapes
Soils of urban and human‐impacted landscapes (Anthrosols) differ from soils normally found in natural settings in that they have been modified so profoundly by human activity that they have characteristics outside the range of native soil series and require reclassification as a different type of soil. Anthrosols are widely distributed in agricultural, archaeological, mine‐related, and urban geographical settings. Agricultural Anthrosols are form…
Soils of Urban and Human‐Impacted Landscapes
Anthropogenic soils (referred to here as anthrosoils) are soils that have been influenced, modified, or created by human activity. They are found worldwide in urban and other human‐impacted landscapes. Four distinct types of anthrosoils can be distinguished based on geographical setting and historical context: (i) agricultural, (ii) archaeological, (iii) mine‐related, and (iv) urban. Most anthrosoils found in agricultural and archaeological setti…
Archaeology (4 works) · Archaeology and ancient environmental studies (4 works) · Geography (4 works) · Environmental Science (3 works) · Heavy metals in environment (3 works) · Soil Science (3 works) · Soil water (3 works) · Agriculture (2 works) · Amazonian Archaeology and Ethnohistory (2 works) · Geochemistry (2 works)