HO-759 Patapsco State Park Architectural Survey File This is the architectural survey file for this MIHP record. The survey file is organized reverse- chronological (that is, with the latest material on top). It contains all MIHP inventory forms, National Register nomination forms, determinations of eligibility (DOE) forms, and accompanying documentation such as photographs and maps. Users should be aware that additional undigitized material about this property may be found in on-site architectural reports, copies of HABS/HAER or other documentation, drawings, and the “vertical files” at the MHT Library in Crownsville. The vertical files may include newspaper clippings, field notes, draft versions of forms and architectural reports, photographs, maps, and drawings. Researchers who need a thorough understanding of this property should plan to visit the MHT Library as part of their research project; look at the MHT web site (mht.maryland.gov) for details about how to make an appointment. All material is property of the Maryland Historical Trust. Last Updated: 02-07-2013 CAPSULE SUMMARY Patapsco Valley State Park MIHP # AA-2290, BA-3003, CARR-1662, HO-759 Elkridge to Sykesville Anne Arundel, Baltimore, Carroll, and Howard Counties, Maryland Park =1907 Public Patapsco Valley State Park encompasses 14,250 acres in Anne Arundel (992 acres), Baltimore (4,541 acres), Howard (6,011 acres), and Carroll (2,706 acres) counties (Maryland Department of Natural Resources (MdDNR) 2002). The park land stretches approximately 26 miles along the Patapsco River from west of Sykesville to just east of Baltimore Harbor. The river courses through the lengthy Fall Line zone that extends from approximately the villages of Alberton to Elkridge. East of Elkridge, the river becomes a broad, slow, relatively shallow stream that is affected by tidal action. As a park, the property has been assembled from 1907 through the 1990s. The first acquisition was a 40-acre donation in the Hilton area. Until 1950, land acquisition was focused on the valley south of Ellicott City. During the 1950s, the park was expanded to incorporate lands north of Ellicott City and west to Sykesville. Most of the park is open space and forests. Recreation areas within the park have been designed as distinct, independent areas that support a wide-range of activities and park operations, but the recreation areas are not linked to form a unified entity. Thus, the park boundaries do not establish an identifiable entity that would qualify as a district for listing in the National Register of Historic Places. The buildings that transferred with the land represent a disparate group of buildings that are unrelated to each other historically or aesthetically by plan or physical development. The resources most intimately coimected with the Patapsco River are the industrial buildings and sites that required waterpower or water resources to make their products. Most industrial resources located within park boundaries are archeological sites that have not been evaluated applying National Register Criteria for Evaluation. Agricultural resources contained within the park boundaries are not related to each other. Agriculture was not a significant theme in Patapsco River valley, but in the upland areas bordering the river. Any agricultural buildings located within the park boundaries are actually on the edges of agriculturally productive areas. While the built resources located within the boundaries of Patapsco Valley State Park do not qualify as a district, many possess the qualities of significance and integrity for listing in the National Register of Historic Places individually or in complexes as detailed in the accompanying table. Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form 1. Name of Property (indicate preferred name) historic Patapsco Valley State Park BA-3003, CARR-1662, HO-759 other 2. Location street and number 8020 Baltimore National Pike not for publication city, town Elllicott City vicinity county AA, BA, CARR, HO 3. Owner of Property (give names and mailing addresses of all owners) name Maryland Department of Natural Resources street and number 580 Tawes Avenue, E-3 telephone 410-260-1864 city, town Amiapolis state MD zip code 21401 4. Location of Legal Description courthouse, registry of deeds, etc. Multiple tax map and parcel: city, town Multiple liber folio 5. Primary Location of Additional Data Contributing Resource in National Register District X Contributing Resource in Local Historic District Determined Eligible for the National Register/Maryland Register Determined Ineligible for the National Register/Maryland Register Recorded by HABS/HAER Historic Structure Report or Research Report Other 6. Classification Category Ownership Current Function Resource Count X district X agriculture landscape Contributing Noncontributing X public building(s) private commerce/trade X recreation/culture buildings defense religion sites structure both X domestic social structures site education transportation objects object funerary work in progress Total government unknown 268 health care vacant/not in use Number of Contributing Resources industry other previously listed in the Inventory 140 7. Description inventory NO. AA-2290 BA-3003 CARR-1662 HO-759C ondition excellent deteriorated good ruins X fair altered Prepare both a one paragraph summary and a comprehensive description of the resource and its various elements as it exists today. RESOURCE COUNT National Register Listed resources = 15 MHT DOE Not eligible resources = 5 Recommended National Register eligible resources = 63 Recommended Not National Register eligible resources =119 Unevaluated resources = 53 TOTAL = 255D SUMMARY Patapsco Valley State Park encompasses approximately 14,250 acres in Anne Arundel (992 acres), Baltimore (4,541 acres), Howard (6,011 acres), and Carroll (2,706 acres) counties (Maryland Department of Natural Resources (MdDNR) 2002). The park derives its name from the Patapsco River, a 52-mile long river that drains a watershed of approximately 375,000 acres (approximately 540 sq mi) and forms the boundary line between the counties. The park is oriented along 32 miles of the Patapsco River and extends from west of Sykesville to just east of the mouth of the river at Baltimore Harbor. During its course, the Patapsco River traverses two major physiographic provinces, the piedmont and the Atlantic coastal plain. The river's headwaters originate in the piedmont, an area of rolling and hilly terrain. Throughout the piedmont, the river traverses a narrow valley flanked by relatively steep bluffs. The river courses through the lengthy Fall Line zone that extends from approximately the villages of Alberton to Elkridge. Water power generated at the Fall Line was harnessed historically to power a variety of industries. East of Elkridge, the river enters the Atlantic coastal plain and becomes a broad, slow, relatively shallow stream that is affected by tidal action. The nucleus of Patapsco Valley State Park was established in 1907 through a donation of approximately 40 acres near Hilton by John M. Glenn. Land acquisition between 1907 and 1950 focused on the area between Ellicott City and Elkridge. During the 1950s, the park was greatly expanded and property began to be acquired north of Ellicott City and westwards towards Sykesville. During the 1950s, Hollofield and McKeldin recreation areas were established and new recreational support structures were added to the Glen Artney, Orange Grove, and Hilton areas. The lands acquired for Patapsco Valley State Park historically were associated with two primary uses: industry and agriculture. The Patapsco River Valley was the site of Maryland's industrial revolution, and was an important area of industrial activity between the late eighteenth century until the Civil War. Mills, mill races, and dams were constructed along the river from north of Elkridge up to Alberton. Agricultural areas generally were located in the uplands above the river. Patapsco Valley State Park contains 255 resources comprising 60 sites, 116 buildings, 72 structures, 3 objects, and 4 districts that date before 1960. These resources include prehistoric and historic archeological sites, as well as industrial sites and buildings, agricultural complexes, individual dwellings, and recreational facilities constructed from 1930 through 1960. As properties were transferred to MdDNR, the agency has implemented a variety of strategies to manage buildings contained on the properties. In some cases, properties have been transferred with life-tenancy clauses, which allow former owners to occupy the buildings until their removal or death. Some buildings are rented to keep them in active use. Other buildings are managed under the curatorship program. In 1983, MdDNR established a statewide program of curatorships to maintain historic buildings located on MdDNR-owned lands. As of 2002, 14 properties located within the boundaries of Patapsco Valley State Park were enrolled in the curatorship program. Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 1 METHODOLOGY The overall purpose of this project is to provide the Maryland Historical Trust (MHT) and the Maryland Department of Natural Resources (MdDNR) with consistent data on the cultural resources contained within the MdDNR-owned land unit. The survey area consisted of MdDNR-owned lands within the boundaries of Patapsco Valley State Park as of April 2003. These boundaries were based on a review of property maps verified by knowledgeable MdDNR personnel. No property leased by MdDNR was surveyed as part of this project. Resources on property owned by other private entities or state agencies were excluded from this investigation; these entities included the State Highway Administration, CSX Corporation, private entities, or county maintained facilities, such as ball fields, recreation centers, or museums on state land. Historical Research The Maryland Inventory of Historic Properties forms and the archeological site files on file at MHT and MdDNR provided the base-line data for historical research for the MdDNR-owned land unit. An analysis of the property types and occupation periods provided supported the identification of historic themes/historic contexts appropriate to evaluate the historic resources in the park. The development of historic contexts that encompassed the history of each unit prior to state ownership was synthesized Irom the architectural and archeological forms and expanded to incorporate information contained in historic maps and other secondary sources, such as published county and local histories, and National Register documentation. Research in primary archival materials, such as deed research or genealogical materials available in local historical societies, was not conducted for this project. Historical research also was undertaken to document the history of the MdDNR land unit. Research was conducted at MdDNR to provide an overview history of the park and its subsequent evolution and development. The purpose of this research was to determine the reasons behind the establishment of land unit and subsequent management practices. Sources examined in this research effort included MdDNR real estate acquisition files, land unit files, personnel interviews, park master plans, and relevant secondary sources on the development of parks in the state of Maryland. Field Survey Archeological reconnaissance survey focused on the relocation of archeological sites recorded in the archeological site files maintained by MHT. The data in the archeological site files was augmented through review of published literature and unpublished reports available at the MHT library. The mapped or reported location of each recorded site was visited and its condition was assessed, based on surface conditions, (e.g., undisturbed, plowed, eroded, graded/contoured, collected, vandalized, dredged, or other). No archeological survey was conducted for reported ruins not previously identified in the MHT archeological site files. The archeological survey was conducted in April-May 2003. Architectural field survey focused on built resources constructed prior to 1960, the landscape elements associated with the individual resources, and the overall landscape of the MdDNR-owned land unit. The list of built resources included in the survey was compiled from the Maryland Inventory of Historic Properties forms, the CIS database maintained at MHT, and the Detailed Maintenance List (DMI) provided by the MdDNR. The DMI, compiled during the late 1990s, contained information about building materials and components, as well as information on location, estimated construction date, dates of renovations, and an assessment of condition. The list of built resources for survey was refined through a review of 1:600 scale maps provided by MdDNR and through interviews with MdDNR personnel. Reported ruins not previously identified on MIHP forms were not systematically surveyed as part of this investigation. The locations of reported ruins are evident on project maps, but no additional survey was undertaken. If a MIHP form reported a resource as a site, no additional research was conducted on the resource. A few Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 2 resources previously documented on MIHP forms are no longer extant, including the Flynn House and grave site (Tivis Adventure) (MIHP # CARR-240) located in the McKeldin Area and the Paris House and Bam (MIHP # CARR-236, CARR-236A) in Freedom Park. Architectural field investigations were conducted on the exteriors of all pre-1960 buildings and structures. Properties owned by other state agencies were not included in the survey. For example, bridges owned by the Maryland State Highway Administration and recreation facilities maintained by county recreation departments were excluded from the current survey. Field survey was undertaken to verify the character-defining features and materials recorded on MIHP forms and to assess the integrity and overall physical conditions of the exterior of the resources. No additional architectural data or photographs were collected for pre-1960 MdDNR-owned buildings that are pending demolition for which MdDNR has completed consultations with MHT or MHT Determinations of Eligibility classifying the resource as not eligible. The architectural survey was conducted June through September 2003. Exterior building conditions were assigned ratings of excellent, good, fair, poor, or ruin based on the condition of the resource at the time of the site investigation. The building classifications do not necessarily reflect those condition assessments recorded in the MdDNR's DMI. For the purposes of this survey, excellent was defined as the overall absence of conditions requiring maintenance or minor repairs. Good classifications were assigned to resources with building systems and materials appeared to be sound with minimal deterioration. Buildings with minor cosmetic conditions, such as minor paint failure due to age of paint or minor deterioration in wood elements, were classified as good condition. A rating of fair condition was used for buildings exhibiting deterioration in several types of exterior materials or systems, such as deterioration in wood elements in several systems, that could be corrected through maintenance, but without apparent structural damage. A rating of poor denoted large-scale problems in several materials, such as large sections of missing siding or roofing, often resulting in evidence of structural failure. Ruin was used to classify buildings or structures that were no longer usable in their current condition. DESCRIPTIONS The following descriptions are for all recorded archeological resources and all built resources constructed before 1960. The descriptions are organized by property types. The property classifications were assigned based on the primary historic function of the property as defined by the National Register of Historic Places (U.S. Department of Interior, National Park Service 1997). In general, within each property type, the discussion of the resources is organized geographically progressing from south to north and west in the following order: resources located east of Elkridge (maps 1 and 2), Elkridge to Hollofield (maps 3, 4, and a portion of map 5), Hollofield to Woodstock (map 5 and one half of map 6), and Woodstock west (maps 7 and 8 and one half of map 6). The resources are discussed as entities. The descriptions of agricultural complexes include the farmhouse and all associated buildings. Likewise, discussions of former industrial complexes include the mill buildings and all associated buildings and structures. All resources constructed to support park functions are grouped in their respective geographical areas. PREHISTORIC AND MULTI-COMPONENT ARCHEOLOGICAL RESOURCES BIG HOLLY BRANCH (18AN20) is a prehistoric site that was occupied primarily during the Archaic period, with limited occupation occurring also during the Late Woodland period. The site is situated on a low riverine terrace, approximately 121.9 m (400 ft) west of Holly Branch and 152.4 m (500 ft) south of the Patapsco River. Nursery Road (Route 168) bounds the site on the south; Lakeview Avenue forms the western boundary of the site. Richard Steams initially identified Big Holly Branch in 1949 (McNamara 1977:16). Tyler Bastian of the Maryland Geological Survey, Archeology Division later visited the site in 1969 and conducted a non-systematic surface survey and surface collection (MHT Site Files). The northem portion of Big Holly Branch lies within the boundaries of Patapsco Valley State Park and encompasses a low-lying, wooded wetland area and pond. Vegetation Maryland Historical Trust Inventory No. AA-2290 BA-3003 .Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 3 included mixed deciduous trees and wetland plants. This portion of the site was not visibly disturbed. The portion of the site lying beyond the park boundaries is located within the northern extent of a residential subdivision and appears to have been at least partially disturbed by construction and landscaping activities. The extent of disturbance cannot be assessed without testing. The overall condition of the site is unknown. RIVER ROAD (18 AN21) is an Archaic period lithic scatter that is located on a narrow stretch of land between the Patapsco River and River Road, along the southern side of the river. Situated on a low riverine terrace, the site is bound by River Road on the south and the Patapsco River on the north. The intersection of River Road and Nursery Road is located approximately 182.9 m (600 ft) east of the site area. A railroad bed no longer in use and associated access road crosses through the site area. Richard Steams first identified the River Road site in 1949 (McNamara 1977:17). Wayne E. Clark visited the site in 1970 and conducted a non-systematic surface survey (McNamara 1977:17; MHT Site Files). The River Road site is currently maintained as a wooded area of mixed deciduous trees that includes the abandoned railroad bed, access road, and a small quarry pit now filled with water. The quarry pit, which appears on the USGS 1957 Relay quadrangle map (USGS 1957 photo revised 1966, 1974), has destroyed the southwestern portion of the site. The railroad bed and access road have disturbed the southern portion of the site. The site condition is considered poor, with disturbance to the site assessed as major (60-99 per cent). PATAPSCO LAKES (18AN24) is an Archaic and Woodland period artifact scatter situated within a swampy area near the confluence of an unnamed tributary and the Patapsco River. The site area includes numerous small ponds that have formed between the river, the tributary and River Road, located less than 100 m (328.1 ft) south of the site. Hammonds Ferry Road is located approximately 243.8 m (800 ft) east. Richard Steams identified Patapsco Lakes in 1949 (McNamara 1977:18). Wayne Clark visited the site in 1970 and conducted a non-systematic surface survey (McNamara 1977:18; MHT Site Files). Previous disturbance was reported to include gravel mining, which had destroyed the majority of the site. Patapsco Lakes is currently maintained in a combination of open grass fields and wooded wetland areas. A series of ponds within the wetland areas may be the remnants of gravel mining activity. The overall topography slopes gradually down to the south. Included within the site area is the northem extent of a high terrace along River Road that appears to have been partially extended by the addition of fill soils. Given the extent of past gravel mining activity and the presence of possible overburden deposits (fill soils), it is likely that the site has been impacted. ELKRIDGE (18AN30) is a village site that includes occupation components dating from the Early Archaic through the Late Woodland. The site is located on a high terrace adjacent to the Patapsco River. The site is bound by 1-195 to the South; the Patapsco River to the west and north; and by the Penn Central railway to the east. Currently listed on the National Register of Historic Places, the site has been examined on at least three occasions. Wayne E. Clark first visited the site in 1967, returning later that same year to conduct limited test excavations (MHT Site Files). Additional excavations were undertaken in 1968, with assistance from the Maryland Academy of Sciences, which identified a possible prehistoric hearth and an early twentieth century historic hearth (Clark 1970). Recovered artifacts included lithic debitage, projectile points, and ceramic artifacts, including textile- impressed, incised, cord-impressed and plain sherds. These artifacts were recovered from stratified contexts up to 40.6 cmbs (16 inbs). The Elkridge site was listed on the National Register of Historic Places in 1978. Carol Ebright, of the Maryland Geological Survey, Division of Archeology, conducted a limited investigation in 1987, excavating a single Ix Im (3.3 x 3.3 ft) test unit that produced 816 artifacts (Ebright 1988). The test unit was located 12 m (39.4 ft) fi-om the terrace edge and yielded artifacts from intact, stratified contexts, up to a depth of 100 cmbs (39.4 inbs). Diagnostic ceramic artifacts included Accokeek, Mockley, and Potomac Creek, indicating occupation during the Early, Middle, and Late Woodland periods. Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 4 Robert Wall conducted limited test excavations at the site in 1996 as part of the Archeological Society of Maryland's annual field school. Wall returned in 2003 to conduct additional investigations, also as part of the ASM field school (Wall personal communication 2003). These investigations were in progress during the current archeological assessment and included the excavation of at least 20 test units, including a 2 x 2 m (6.6 x 6.6 ft) test unit placed around a large looter hole. A second large looter hole was located a few meters north of the current excavation. Pedestrian reconnaissance of the terrace identified an additional area of disturbance that may be related to looting activity. The site area is currently wooded, with a sparse understory of mixed deciduous species. Although looting and past archeological excavations have impacted an unknown percentage of the site area, the site condition is good and the Elkridge site is regarded as one of the few undisturbed, stratified prehistoric sites along the Patapsco River. PUMPHREY LAKES (18AN246) is a prehistoric lithic scatter that potentially dates from the Late Archaic period. Situated on a low terrace along the southern bank of the Patapsco River, the site is located approximately 250 m (820.2 ft) north of Belle Grove Road (Route 170) and 640 m (2,99.7 ft) east of Route 648. The landform on which the site is located currently consists of a narrow isthmus surrounded by ponds that feed into the river. Wayne E. Clark visited the site in 1972 and conducted a non- systematic surface survey (MHT Site Files). The site is currently maintained as a wooded lot adjacent to an overhead power line corridor. The concrete footer for one tower is located immediately south of the site area, which is vegetated with mixed hardwoods and exhibits dense understory growth. Although the site was not visibly disturbed, construction of the utility-line may have impacted portions of the site. The extent of disturbance carmot be assessed without testing. The overall condition of the site is unknown. POWER LINE (18AN253) is an Early to late Woodland short-term resource procurement camp located on a low terrace along the eastern side of Stony Run, a tributary of the Patapsco River. A higher terrace is located east of the site and extends to the railroad. The old Emmitsburg road bisects the site; the Pennsylvania Central railway line is located less than 50 m (164 ft) east of the site. All-terrain vehicle (ATV) trails parallel Stony Run and define the western and southern boundaries of the site. An artificial drainage ditch is located along the northern edge of the site, extending from the railroad bed toward Stony Run. The Baltimore Washington Parkway is located about 850 m (2,788.7 ft) south of the Power Line site; the Patapsco River is located approximately 1,100 m (3,608.9 ft) to the north. Lewis Phelps initially identified the Power Line site in 1972 (Clark 1973:1). The Anne Arundel County Archeological Society, under the direction of Wayne Clarke and Lewis Phelps, conducted a non-systematic surface survey and limited test excavations at the site in 1974 (Clark 1975). Accokeek Net impressed ceramics and shell tempered ceramics; lithic debitage; a projectile point; a biface; and fire-cracked rock were recovered from a narrow remnant of the site that had not been disturbed by gravel mining activities or soil erosion. Fred Kinsey re-located the site in 1978 during a Phase 1 cultural resources survey in advance of the construction of I-195 (Kinsey 1978). Kinsey conducted limited shovel testing and determined the site would not be adversely affected by construction of the power line; no fiirther work was recommended. Currently, the only intact portion of the site is a narrow wooded section of the terrace between the old Emmitsburg road and bluff edge along the river. Although construction of the power-lines does not appear to have impacted the site, an extensively used ATV trail has impacted the southern portion of the site and a runoff gully has eroded the terrace on the northern side of the site. The deeply incised old Emmitsburg road, currently an unimproved two track that parallels the Penn Central railway, crosses through the eastern portion of the site. The overall condition of the site is unknown, but the site has the potential of major disturbance from soil erosion and recreational use of the area. DISNEY FARM (18AN264) is a Woodland period base camp located on a low terrace along the eastern bank of Deep Run Creek. The Baltimore Washington Parkway lies approximately 121.9 m (400 ft) east of the site; Race Road lies about the same distance to Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 5 the west. The intersection of Hanover Road and Race Road is located approximately 609.6 m (2,000 ft) south. Richard Steams initially identified the Disney Farm site in 1929 (McNamara 1977:23). Norma A. Baumgartner later conducted a non-systematic surface survey of the site in the 1970s (MHT Site Files). At that time, disturbances to the site included plowing and past mining activity. The site is currently situated within a wooded area, on a low terrace adjacent to Deep Run Creek. An unnamed tributary of Deep Run is included within in the southern portion of the site. Vegetation is mixed hardwoods with a sparse understory. The landform on which the site is located appears stable and no recent disturbance to the site was observed. The current condition of the site is unknown. INTERSECTION (18AN400) is a short-term resource procurement site that was occupied during the Late Archaic through the Late Woodland. The site is located on a low terrace along the eastern edge of Deep Run creek, immediately north of Hanover Road. Ray Korman identified the site in the early 1970s (MHT Site Files). Garrow & Associates re-identified the site in 1980 during a Phase I level cultural resources survey (Garrow et al. 1980). These surveys have yielded Late Archaic and Early Woodland projectile points. The site area is currently wooded and is located on a low terrace west of a residential area and south of an unnamed tributary of Deep Run. The area of the site was not visibly disturbed, but the terrace appears to be subject to flooding. The condition of the site is unknown. FIELD D (18AN405) is a Woodland period artifact scatter located on a high terrace between the Patapsco River and River Road and adjacent to a small pond. The intersection of River Road and Nursery Road is approximately 853.4 m (2,800 ft) to the east; the Patapsco River is approximately 426.7 m (1,400 ft) north of the center of the site. An abandoned railroad bed passes through the center of the site, along the boundary of Patapsco Valley State Park. The portion of the site lying on the southeastern side of the rail bed is located beyond the park boundaries. T. D. Jones first identified the site (MHT Site Files). Norma Baumgartner of the Maryland Geological Survey, Division of Archeology, conducted a non-systematic surface survey of the site in the 1970s (MHT Site Files). The site area is currently maintained as a wooded area adjacent to River Road. An abandoned railroad bed crosses through the central portion of the site and is the only visible disturbance. The artificial pond is depicted on the 1957 Relay, Maryland quadrangle, but is not depicted on the 1927 quadrangle and may be the result of gravel mining activity. With the exception of the presence of the railroad bed, the site is not visibly disturbed. The condition of the site is unknown. TDJ - FIELD X (I8BA154) is a prehistoric artifact scatter of unknown temporal affiliation. The site extends for approximately 1.6 km (1 mi) along the northern bank of the Patapsco River in the area of the Baltimore Beltway (1-695) and River Road. Both roadways cross through the site area. The Tunnel Thruway (1-895) extends along the northern edge of the site, while the Baltimore Washington Parkway (1-295) is located approximately 152.4 m (500 ft) east of the site. A small portion of the site extends to the north of the Thruway and is located beyond the current boundaries of Patapsco Valley State Park. Wades North (18BA90), a prehistoric lithic scatter, is located within the southwestern boundary of TDJ-Field X. Talbot Jones first identified TDJ-Field X in 1900, and reported a number of lithic and ceramic artifacts, including axes, gorgets, and mortars (McNamara 1977:27). K. Quinn and D. Schultz of the Baltimore County Office of Planning and Zoning visited the site in 1980 and conducted a non-systematic surface survey (MHT Site Files). TDJ-Field X is currently maintained as a combination of open fields and wooded areas that extend along a low riverine terrace between bank of the Patapsco River and the Harbor Tunnel Thruway. Numerous disturbances were identified within the site boundaries. An overhead power line corridor crosses through the northern portion of the site and is paralleled by an ATV trail, which extends beyond the site area. An artificial pond, most likely a relic gravel pit, is located immediately east of Hammonds Ferry Road along the river edge. An earthen berm parallels the Hammonds Ferry Road to the east. The overall condition of the site is unknown, but there is high potential of major disturbance from gravel mining activities, road and utility construction, and general use of the area. Maryland Historical Trust Inventory No. AA-2290 BA-3003 Maryland Inventory of CARR-1662 HO-759 Historic Properties Form Name Patapsco Valley State Park Continuation Sheet Number 7 Page 6 TDJ-FIELDO (18BAI55) is a prehistoric lithic scatter of unknown temporal affiliation. The site extends for approximately 1.5 km (0.9 mi) along a low terrace located approximately 250 m (820.2 ft) north of the Patapsco River. The Harbor Tunnel Thruway (1-895) extends through the southern portion of the site. The part of the site lying north of the Thruway is located beyond the current boundaries of Patapsco Valley State Park. An industrial complex abuts the site on the north. Herbert's Run bounds the site on the west, while Transway Road forms the eastern boundary of the site. K.Quinn and D. Schultz visited this site in 1980 and conducted a non-systematic surface survey (MHT Site Files). Projectile points and lithic debitage, including jasper and rhyolite flakes, were observed. The portion of the site lying north of the Thruway has been destroyed by the construction of the Thruway and an adjacent industrial complex. To the south of the Thruway, the site is currently maintained in a combination of open fields and dense low scrub. This portion of the site consists of a narrow strip of land between the Thruway and an unnamed lake located north of the Patapsco River. Observed disturbances include a gravel two-track road and an overhead power-line that parallels the Thruway. WADES NORTH (18BA90) is a prehistoric lithic scatter that likely dates from the Late Archaic through the Woodland periods. Situated on the northern floodplain of the Patapsco River, the site extends to the east and west of the Baltimore Beltway (1-695), where that roadway crosses the Patapsco River. River Road is located along the eastern boundary of the site; the Patapsco River forms the southern boundary of the site. Wades North is located within the southwestern quadrant of prehistoric archeological site 18BA154 (TDJ-Field X), which was identified by Talbot Jones in 1900. Talbot Jones identified Wades North that same year and observed a number of ground stone tools and ceramic artifacts along the river bank (McNamara 1977:25). Richard Steams later visited the site. In 1980, K. Quinn and D. Shultz of the Baltimore County Office of Planning and Zoning re-visited the stie(MHT Site Files). Wades North is currently maintained as a wooded area that includes an area of wetland vegetation along the riverbank. Only the southwestern quadrant of the site, which lies west of the Baltimore Beltway (1-895) is located within the boundaries of Patapsco Valley State Park. The only visible disturbance within the park boundaries was a two-track road that paralleled the river, roughly bisecting the site. The portion of the site lying outside the park boundaries appears to be heavily disturbed from past construction activities, including interchange ramps between the Baltimore Beltway and the Harbor Tunnel Thruway. The condition of the site is unknown. HIGH HERBERT (18BA91) is a prehistoric lithic scatter of unknown temporal affiliation that is located at the confluence of Herbert Run and the Patapsco River. The site is situated on the southeastern terminus of a finger ridge that extends along the western side of Herbert Run. The Harbor Tunnel Thruway (1-895) is located less then 50 m (164 ft) north of the site. The Penn Central Railway crosses the Thruway approximately 243.8 m (800 ft) west of the site. Talbot Jones initially identified the site, which was later visited by Richard Steams (MHT Site Files). Wayne Clark visited High Herbert in 1971 and indicated the site had been destroyed by placement of a power line tower on the site location (McNamara 1977:26). K. Quinn and D. Shultz of the Baltimore County Office of Planning and Zoning later visited the site in 1980 (MHT Site Files). This site is mapped as located on the northern boundary of Patapsco Valley State Park and lies partially outside park boundaries. The site was not visited during the current assessment of previously identified archeological sites. The condition of the site is unknown. SCHULTZ FARM #1 (18HO203) is a multi-component prehistoric site that includes the location of a nineteenth-century dwelling. Paleo-lndian, Early Archaic and Early Woodland prehistoric occupation components have been identified at Shultz Farm, which has been characterized as a short-term resource procurement and transitory campsite dating from the Early to Middle Holocene (10,000 to 3,000 yrs B.P.) (Polglase et al. 1994). The site encompasses portions of the floodplain, terrace slope, and T2 terrace adjacent to Shallow Run, a tributary of Deep Run. The Baltimore Washington Parkway is located approximately 550 m (1,804.5 ft) southeast of the site. The intersection of Hanover Road and Race Road is located approximately 215 m (700 ft) east. The Baltimore and Ohio Railway crosses Hanover Road about 243.8 m (800 ft) northeast of the site.