Seldom-Found Projectile Point from North Carolina’s Piedmont

Two Fountain Creek projectile points from Chatham County, North Carolina, shown above a centimeter and inch scale.

by Peter G. Murphy and Alice J. Murphy, St. Johns, Michigan

More than a hundred years of archaeological research and information garnered from well documented amateur collections have made it possible to identify and date many of the more distinctive projectile points found in North America. Over a thousand types have been described in journals and reference books. But other points, especially the less common types and those with transitional characteristics, present classification challenges even to the professional archaeologist. The two points in Fig. 1 present such a challenge. Of the 1,279 identifiable projectile points we surface-collected over a three-year period from 83 cultivated-field sites in six counties of North Carolina’s Piedmont, only two (Fig. 1) appeared to be of the Fountain Creek type first described in 1978 by Floyd Painter in The Chesopiean. He described the point as rare and estimated that fewer than 75 were known to have been found, mainly in southeastern Virginia and northeastern North Carolina.

Painter (1978) provided dimensional data for 24 examples of his proposed Fountain Creek type and illustrations of six points, but the illustrations are somewhat stylized drawings rather than photographs of actual points. Based largely on form, he believed Fountain Creek is related to, or a variant of, the Early Archaic Palmer type first described by Coe (1964) in North Carolina. In his guide to projectile points of Virginia and the Carolinas, Peck (1993) does not make reference to Fountain Creek points, but one of the three Palmer points he illustrates clearly resembles Painter’s Fountain Creek type. The same is true for one or two of the 21 Palmer points pictured in Barnard’s (1988) guide to Southeastern points.

Both of the points in Fig. 1 have Fountain Creek characteristics, but the point on the left, with the deep serrations, is most similar to Painter’s illustrations. Further, the two points in Fig. 1 are similar to six of the ten examples pictured in Overstreet (2011). Interestingly, Overstreet did not include Fountain Creek points in his 1st edition (1989), but by the 3rd edition (1993) four examples were pictured. Substantive information on the point is very limited and only a few other publications make any mention at all, among them Dragoo (1993) and Hranicky (2011). In the comprehensive survey of 30,164 identifiable North Carolina points reviewed by McReynolds (2005), Fountain Creek is not among the 35 recognized types.

The characteristics that define Fountain Creek points include 2–7 deep serrations or notches on each blade margin, a ground and slightly curved (convex) base, and length of 27–55 mm (Painter 1978). The width-to-length ratio of Fountain Creek points shown in Overstreet (2011) averages 1:2.3; our two examples average 1:2.4. The similarities between the two points in Fig. 1, found at a site in Chatham County, are somewhat subtle. Both have ground, rounded bases (unlike the straight or slightly concave bases of most Palmer points), blades with relatively straight, serrated edges, and both are made of the same type of metavolcanic stone with similar patination. The serrations are largely worn down on the smaller point.

Figure 1. Two Fountain Creek points from a site in Chatham County of the North Carolina Piedmont. The point on left is 45 mm long.


Although Painter perceived a connection between Fountain Creek and Palmer, Overstreet (2011) suggests a similarity with Kirk Stemmed points. As discussed in Murphy and Murphy (2012), Palmer and Kirk are sometimes considered to be elements of an Early Archaic complex of point types, rather than distinct entities, although Palmer is considered the earlier of the two types. The site from which we collected the points in Fig. 1 yielded a wide variety of Archaic Period points, including Palmer and Kirk. If Fountain Creek points are indeed of the Early Archaic Period, they would fall within the age range of approximately 10,000–7,000 B.P. But we have seen no record of them being found in controlled excavations with actual evidence of age or relationships to other point types. Coe (1964) shows one point with Fountain Creek traits among a group of excavated Palmers, but he represents it as just another Palmer. His Palmer points tend to fall into two basic categories; those that are fairly broad relative to their length (width-to-length ratio 1:1.3) and those that are more slender (width-to-length ratio 1:2.3). Relative to Palmer, the 24 Fountain Creek points described by Painter (1978) tend to be intermediate (1:1.8) in width-to-length ratio.

Until good examples of Fountain Creek points are found in controlled excavations of stratified sites, their age and relationship to other points, such as Palmer or Kirk, will remain speculative. Painter’s (1978) suggestion of a relationship with Palmer appears entirely valid. The points share characteristics that can make it difficult to distinguish between the two and they occur in the same region. However, until further evidence is acquired it may be most reasonable to consider Fountain Creek points as components of a Palmer-Kirk complex. It remains to be seen whether they deserve to be recognized as a separate type rather than a variant of a more established type. Whatever the case, points of the form shown in Fig. 1 are uncommon even in their apparent main region of occurrence, Virginia and North Carolina. They present engaging questions concerning their proper classification relative to other points of the Southeast.

References

Barnard, Frank K.
1988. How to Find and Identify Arrowheads and Other Indian Artifacts (Southeastern United States). F.K. Barnard, Rt. 6, Box 511, Chapel Hill, North Carolina. 53 pgs.

Coe, Joffre L.
1964. The Formative Cultures of the Carolina Piedmont. Transactions of the American Philosophical Society New Series 54(5). 130 pgs.

Dragoo, Don W.
1993. Projectile Points of the Archaic Period, Eastern North America. Institute for Human History, Gloucester, Virginia. 36 pgs.

Hranicky, Wm Jack
2011. Prehistoric Projectile Points Found Along the Atlantic Coastal Plain. Universal Publishers, Boca Raton, Florida. 282 pgs.

McReynolds, Theresa E.
2005. Spatial and Temporal Patterning in the Distribution of North Carolina Projectile Points. North Carolina Archaeology 54:1-33.

Murphy Peter G. and Alice J. Murphy
2012. Palmer Points Reflect On-Going Change in the Early Archaic Southeast and Demonstrate the Complexities Inherent in Point Classification. Central States Archaeological Journal 59(3):149-151.

Overstreet, Robert M.
2011. Official Overstreet Identification and Price Guide to Indian Arrowheads. House of Collectibles. 1264 pgs.

Painter, Floyd
1978. The Fountain Creek Projectile Point. The Chesopiean 16(1-3):32-33.

Peck, Rodney M.
1993. Indian Projectile Point Types from Virginia and the Carolinas. Piedmont Archaeological Society of N.C. and S.C., Inc., 2121 Quail Drive, Harrisburg, North Carolina. 43 pgs.

Big Sandy and Rowan Projectile Points of the Archaic Piedmont: Classification Issues

by Peter G. Murphy and Alice J. Murphy, St. Johns, Michigan

July 2014 Central States Archaeological Journal

Five Big Sandy projectile points from North Carolina Piedmont displayed on red background showing variation in size shape and side notching
Figure 1. Five points of the Big Sandy type from Durham and Bunner Counties of the North Carolina Piedmont. Longest point, 70 mm.

The structural distinctions between named point types are often far from clear. As in all classification systems, the classifiers tend to fall into one of two categories, “lumpers” or “splitters.” Personal judgment is always a factor and can be very subjective, especially when it comes to minor or subtle differences among objects being classified. Distinctive side-notched points of the general type shown in Figures 1–2 are represented in most collections from the North Carolina Piedmont. Approximately five percent of the 1,279 identifiable points we found at 83 North Carolina Piedmont sites were of this general type. In the past, most such points found in the Southeast were readily classified as Big Sandy, a point commonly considered to be of Early Archaic age. Barnard (1988) shows an excellent selection of 25 Big Sandy points that illustrates the range of variability for the Piedmont region. The auriculate form of Big Sandy, in which the basal auricles, or tangs, flare outward and usually slightly downward, was first described in 1931 by Claflin, based on specimens from the Stallings Island Mound, Columbia County, Georgia (Claflin 1931). A second variant of Big Sandy, the so-called notched form, was described in 1956 by Kneberg based on specimens from the Big Sandy site, Tennessee (Kneberg 1956). Most references describe Big Sandy points as being found widely in the lower, more eastern portions of the Midwest and through the Southeast. Notched points, generally, are considered to be one of five main projectile point types, along with lanceolate, stemmed, bifurcate and triangle (Hranicky 2011). There is great variability in the side-notched variety and in some regions generally similar forms are given other names, such as Otter Creek, Bolen and Taylor, among many others. Beasley (2011) described the similarity between Big Sandy and Bolen as an enigma.

Whereas Big Sandy had become a generally recognized designation for points of the type in Figures 1–2 from the North Carolina Piedmont, the situation evolved in 1970. Peter Cooper, in the pages of this journal, described what he considered to be a Big Sandy look-alike and named it Rowan (Cooper 1970). His work was based largely on points that he referred to as dart points, found in North Carolina’s Rowan County in the central-westerly Piedmont about 160 km to the west of the sites that were the source of our points (Figs. 1 and 2). Other points that Cooper studied were from Granville County, just to the east of our sites. The naming of a new point, Rowan, has led to some confusion, especially among amateur archaeologists and artifact collectors, some of whom began to call virtually all points of this general form Rowan rather than Big Sandy. There seems to have been an assumption that there had been an overall name change, from Big Sandy to Rowan, at least for points of the type found in the Piedmont. But in reality, this is not the case. Cooper defined and described Rowan points as a separate type, with features that he considered sufficient to be named a previously unrecognized type. According to Cooper, Rowan points occur widely in relatively small numbers through the Southeast, into Tennessee, and at some sites occur together with Big Sandy points. Specific age data for Rowan points are unavailable, but based on association with other types they are assumed to be Early Archaic, possibly B.P. 9,500–8,000. Big Sandy has been estimated at B.P. 8,500 (auriculate type) and B.P. 9,500 (notched type). Cooper (1970) and more recently Overstreet (2013) suggest that Rowan is “believed” to be derived from Dalton, Quad, Greenbrier or Hardaway and was a predecessor, possibly by as much as a thousand years according to Hranicky (2011), of Big Sandy and other later side-notched types.

Cooper describes Rowan points as differing from Big Sandy in a number of ways and feels they are best distinguished by a constellation of traits that include: overall length of 38–55 mm, ground and beveled bases and notches, elongated notches with asymmetrical tangs that are pointed or rounded and ground thin, and blades beveled on one or both edges. These are traits that can be very variable and often subtle on weather-worn and eroded points, certainly not obvious to those who have not handled a variety of both types. In our experience, which includes the examination of well over a thousand points from the Piedmont of North Carolina (Murphy and Murphy 2009), the differences often blur. It is fair to ask whether Rowan really deserves to be named as a distinct type, rather than a variant of Big Sandy peculiar to the region studied by Cooper. Opinions will differ on questions of this sort.

Side-notched Big Sandy (Rowan variation) projectile point from Durham County North Carolina with beveled blade edge and weathered surface
Figure 2. A point of the Big Sandy (Rowan variation) type from Durham County of the North Carolina Piedmont. One blade edge is beveled. Length, 54 mm.

One way of addressing this issue is to look at the extent to which the Rowan type has been accepted in the published archaeological literature. Of 18 standard reference books and identification guides that focus on the eastern and southeastern portions of the United States published over the period 1983–2013, we found that only four make reference to or describe Rowan points and three of those four include Big Sandy as well. Eight refer to points of the general type (Figs. 1 and 2) as Big Sandy with no mention of Rowan. Six mention neither type. Only one reference (Peck 1993) describes Rowan but not Big Sandy.

A Michigan Hi-Lo Point

by George Jachim, Grand Rapids, Michigan

Volume 65, Number 1, January 2018 Central States Archaeological Journal

Michigan Hi-Lo projectile point made of Bayport chert, showing broad blade, concave base with light grinding, and Late Paleo-Early Archaic workmanship from Ottawa County, Michigan.

Figures 1 & 2. The Hi-Lo point found in two parts in Ottawa County, Michigan.

On June 20, 2017 I was walking a favorite field of mine in Ottawa County, Michigan. Ottawa County is due west of Kent County, in west central Michigan. Grand Rapids lies within Kent County. As I was walking the rows of corn I came across the base portion of a point. At the time I knew it was much different from what I normally find. However, I did not think much more of it. It was only another broken part of a point. When I got back home, I followed my usual routine. I checked all broken pieces against pieces I had previously found. BINGO!!

No doubt about it; I had the perfect mate. What you see pictured here are the obverse and reverse of a Michigan Hi-Lo point (Figs. 1,2). It measures 1 ½ inches long, 13/16ths at the widest part of the shoulder and ¼ inch thick. The break is more prominent on the reverse. Noel D. Justice places this type point in the Late Paleo/Early Archaic time period. This was in the Great Lakes area; 8000 to 6000 B.C. The point type is named for the Hi-Lo site which is located in Ionia County, Michigan. This point was made from Bayport chert; a common lithic material found here in Michigan. Light grinding is found in the concave base. It is present on the ears and shoulder area as well. One shoulder has somewhat more grinding than the other.

Once I had taken the time to fully study my point, I knew I had found something special. At least, it was special by my standards. Next was to get another opinion. On June 22, 2017 I visited with Dr. Janet Brasher, Professor and Curator of Anthropology at Grand Valley State University. GVSU is the largest university in the greater Grand Rapids area. It has one campus in downtown Grand Rapids. Another campus is located in Allendale, Michigan. Dr. Brasher was very comfortable with this point being of the Hi-Lo type. She also agreed that Bayport chert was the stone of choice. Dr. Brasher also showed me two other Hi-Lo type points. They are part of the collection that GVSU has, so we could do some comparisons. My point is on the small side. Dr. Brasher has been a good friend for a number of years and has always made herself available to me. This is certainly one example of a fine working relationship between the professional and the avocational archaeologist. I have come to appreciate the knowledge and expertise that Dr. Brasher has shared with me. It is also worth noting that in the summer of 2014 Dr. Brasher and a team of GVSU students conducted some field work at this same site. My point was found there. However, their work was in a different area of the site.

This is not the first point found at this site. I have found about 60 artifacts found there. Lamoka and Brewerton are more common with scrapers, drills, hafted scrapers and blades also found. This point happens to be the earliest in the historical time line that I have found there.

This property is presently owned by a large farming operation out of Allendale. The owner has graciously allowed me a window of time in late spring. During this period, I can continue to walk this property and retrieve pieces of history. I originally learned of this site in May of 1994 when I met the original farmer and his family. They had already been working the farm for many years and he was a collector as well. I was able to view his personal collection on two occasions and it was impressive. We shared a common love for prehistoric artifacts. Because of this, he allowed me to walk his property. Eventually, the property changed to the current ownership.

This is the second Hi-Lo type point I have found; all items in my collection are personal finds. I feel very fortunate to have salvaged this part of history. Locating sites, finding pieces and documenting information relative to each piece all make for an excellent learning experience. Piecing together our historical past is fascinating and enjoyable. Here is another piece to the puzzle – or should I say two.

References:

Justice, Noel D.
1987 Stone Age Spear and Arrow Points of the Midcontinental and Eastern United States. Indiana University Press, Bloomington, IN.

Brasher, Dr. Janet
Personal communication.
Professor and Curator of Anthropology @ Grand Valley State University.