Geopolymers (GP) are a type of chemically-bonded ceramics whose chemical formula is centered around M 2 O•Al 2 O 3 •4SiO 2 •11H 2 O. They are refractory, inorganic polymers which can be made from calcined metakaolin clay of composition Al 2 O 3 •2SiO 2 . Geopolymers consist of both aluminate (AlO 4 − ) and silica (SiO 4 ) tetrahedral units, which are cross-polymerized under highly alkaline conditions (NaOH, KOH, or CsOH) at room temperature. They are a rigid, hydrated, alumino-silicate solid containing group I, chargebalancing cations. They are composed of an amorphous, nano-particulate, nanoporous, impervious, and acid-resistant structure. 1 When stoichiometric geopolymer is heated above 950-1050°C it crystallizes to form leucite (K 2 O•Al 2 O 3 •4SiO 2 ) or pollucite (Cs 2 O•Al 2 O 3 •4SiO 2 ), respectively. 2-5Basalt is the most common volcanic rock-type on earth. The sheer abundance of basalt, as well as its relatively inexpensive cost have been a reason it is extensively being researched as an alternative filler phase or reinforcement. [6][7][8] Many geopolymer composites have been made where the geopolymer matrix encapsulates a range of ceramic or biological reinforcements in the form of dispersed particulates, chopped fibers, uni-directional fibers, and fiber weaves. [9][10][11][12][13][14][15] Composites reinforced with fibers of carbon, alumina, mullite, and basalt have been reported. 1 The elevated temperature stability of both geopolymer and basalt suggest that they could be used as relatively inexpensive, intermediate temperature