Select each one of the 33 artifacts to learn more.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Fluted points from the Clovis culture in North America have various names to reflect regional changes. The Michaud-Neponset point is a variant of the fluted points that differs from the original Clovis type by the length of the flutes, the concave base and a slight inflection of the sides near the base.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Material from the state of Maine\’s centre north. It is 400-million-year-old Ordovician radiolarian chert. Its quality for cutting tools is exceptional.
Material from two known sources: Mount Jasper, near the city of Berlin, and near the Jefferson village area. It is intrusive rock whose size ranges from adequate to good.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Lance-shape points with parallel retouching were developed in the Early Palaeoindian period in the American West, of which the Agate Basin type is oldest from technological tradition associated with the Plano culture. The Agate Basin type was a contemporary of the fluted points of the Folsom culture.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Lance-shape points with parallel retouching were developed in the Early Palaeoindian period in the American West, of which the Agate Basin type is oldest from technological tradition associated with the Plano culture. The Agate Basin type was a contemporary of the fluted points of the Folsom culture.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Lance-shape points with parallel retouching were developed in the Early Palaeoindian period in the American West, of which the Agate Basin type is oldest from technological tradition associated with the Plano culture. The Agate Basin type was a contemporary of the fluted points of the Folsom culture.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Lance-shape points with parallel retouching were developed in the Early Palaeoindian period in the American West, of which the Agate Basin type is oldest from technological tradition associated with the Plano culture. The Agate Basin type was a contemporary of the fluted points of the Folsom culture.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Lance-shape points with parallel retouching were developed in the Early Palaeoindian period in the American West, of which the Agate Basin type is oldest from technological tradition associated with the Plano culture. The Agate Basin type was a contemporary of the fluted points of the Folsom culture.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
Material from the Moosehead Lake area of Maine. Green in colour, this material degrades over time and fades until it becomes white. It is intrusive rock whose size ranges from adequate to good.
