We study partially ordered monoids over which a class of free (over sets and over posets), projective, and (strongly, weakly) flat partially ordered polygons is axiomatizable, complete, or model complete. Similar issues for polygons were dealt with in papers by V. , classes of free, projective, and (strongly, weakly) flat polygons were explored in relation to their axiomatizability, completeness, and model completeness. In the present paper, we look into the same issues, but now for classes of partially ordered polygons. Here, the concept of a left perfect monoid is carried over the case of a partially ordered monoid, and certain conditions equivalent to this concept are formulated. We furnish a description of partially ordered monoids with an axiomatizable class of partially ordered flat, weakly flat, and strongly flat polygons. This result is similar to the appropriate result for polygons (see [2,3]). As in the unordered case, for a commutative partially ordered monoid, it is proved that completeness of a class of strongly flat partially ordered polygons over the monoid is equivalent to the class being model complete, categorical, and to the monoid being a partially ordered Abelian group. It is known that a partially ordered polygon is strongly flat iff it satisfies conditions (P < ) and (E < ) (see [4]).Here we study partially ordered monoids with axiomatizable, complete, model complete, and categorical classes of partially ordered polygons satisfying (P < ) or (E < ). The results obtained for axiomatizable, complete, model complete, and categorical classes of partially ordered projective polygons free over a set are similar to corresponding results for polygons (see [1,2]). Again, we describe partially ordered monoids with finitely many different right ideals over which a class of partially ordered polygons free over a poset is axiomatizable, and remark that there does not exist a partially ordered monoid for which this class is axiomatizable and complete.The results presented in Sec. 3 are due to Stepanova; Theorem 2.6 was proved jointly by the two authors; other results are due to Pervukhin.