Question: the Goddard coin can be found at a prehistoric archaeological site in which city in Maine?
Context: The Brockway Site, designated Site 90.3 by the Maine Archaeological Survey, is a prehistoric archaeological site in Milo, Maine.  Long known to local amateur archaeologists, the site was formally tested in 1986, yielding evidence of a well-stratified site containing thousands of artifacts dating as far back as c. 2000 BCE.  These types of sites are rare in the interior of Maine.  The site was listed on the National Register of Historic Places in 1987. The Maine penny, also referred to as the Goddard coin, is a Norwegian silver coin dating to the reign of Olaf Kyrre King of Norway (1067–1093 AD).  It was discovered in Maine in 1957 and it has been suggested as evidence of Pre-Columbian trans-oceanic contact. The Spiller Farm Paleoindian Site, designated Site 4.13 by the Maine Archaeological Survey, is a prehistoric archaeological site in Wells, Maine.  Located overlooking a stream on the Spiller Farm property on Branch Road, it is an extensive site at which a fine collection of stone artifacts has been found, dating to c. 8,000 BCE.  The site was listed on the National Register of Historic Places in 2003. Key Marco was an archaeological site (8CR48) consisting of a large shell works island next to Marco Island, Florida.  A small pond on Key Marco, now known as the "Court of the Pile Dwellers," (8CR49) was excavated in 1896 by the Smithsonian Institution's Pepper-Hearst Expedition, led by Frank Hamilton Cushing.  Cushing recovered more than 1,000 wooden artifacts from the pond, the largest number of wooden artifacts from any prehistoric archaeological site in the eastern United States.  These artifacts are described as some of the finest prehistoric Native American art in North America.  The Key Marco materials are principally divided between the University of Pennsylvania Museum of Archaeology and Anthropology, University of Pennsylvania; the Department of Anthropology, National Museum of Natural History, Smithsonian Institution; and the Florida Museum of Natural History, University of Florida.  The original pond was completely excavated and refilled.  It is now covered by a housing subdivision.  Excavations of small parts of the site were also conducted in 1965 and 1995. Brinsfield I Site, or Brinsfield I Prehistoric Village Site, is an archaeological site near Cambridge in Dorchester County, Maryland.  The site was first identified in 1955 by Perry S. Flegel of the Sussex Society of Archaeology & History.  It is a late prehistoric archaeological site characterized by shell-tempered pottery and triangular projectile points.  The site may provide evidence of prehistoric life on the eastern shore of Maryland during the Late Woodland period, c. 900-1500. The Eddington Bend Site, designated Site 74-8 by the Maine Archaeological Survey, is a prehistoric archaeological site in Eddington, Maine.  Located near the banks of the Penobscot River, the site includes both evidence of habitation, and of funerary remains.  The stratified site has dated elements as old as 3,000 BCE, and undated finds that are probably older.  The site was listed on the National Register of Historic Places in 1988. The Wilson Mounds and Village Site is a prehistoric archaeological site located in and around the Marshall Ferry Cemetery in Rising Sun, White County, Illinois.  The site includes twelve burial mounds and a village site.  The site was inhabited by Hopewell peoples from approximately 400 B.C. to 400 A.D. Excavations at the site began in the 1940s; the first formal investigations were conducted the following decade by the Illinois State Museum and the University of Chicago.  The site was part of a trade network which spanned much of the eastern United States, as resources from as far away as North Carolina and the Lake Superior region have been found at the site.  Two different skeletal types have been recovered from the site, indicating the presence of multiple cultures at the village.  The site also includes a prehistoric cemetery in addition to burial mounds, suggesting that burials were organized based on social status. The Gavin Watson Site, designated Site 59.8 by the Maine Archaeological Survey, is a prehistoric archaeological site in Sullivan, Maine.  Located on the shore of Flanders Bay, an inlet off Frenchman Bay in Down East Maine, the site is a refuse midden that is (unusually for the region) free of shells.  An important regional multicomponent site with artifacts spanning thousands of years, it was listed on the National Register of Historic Places in 1987. The Goddard Site is a prehistoric archaeological site in Brooklin, Maine.  The site is notable for the large number of stone artifacts found, most of which were sourced at locations well removed from the area, and for the presence of worked copper artifacts.  It is most widely known as the claimed location at which the Maine penny, a Norse coin dating to the reign of Olaf Kyrre (1067–1093 AD) was found.  The site was listed on the National Register of Historic Places in 1979. The Atkinson-Koskinen Site, designated 45.13 by the Maine Archaeological Survey, is a prehistoric archaeological site in or near Steuben, Maine.  Its main feature is a non-shell refuse midden, a rarity on the coast of eastern Maine.  Along with the Goddard Site in Brooklin, it is important in analyzing land use and subsistence patterns during the Late Ceramic period (1000-1400 CE).  The site was listed on the National Register of Historic Places in 1984.
Answer: Brooklin