In the medieval city of Veridia, all civic buildings constructed before 1300 CE utilized locally quarried limestone, a highly porous material. Highly porous stone degrades rapidly when exposed to continuous freeze-thaw cycles. Historical climate records indicate that Veridia did not experience continuous freeze-thaw cycles until a localized mini-ice age began in 1350 CE, a climate pattern that persists to this day. Interestingly, most of the pre-1300 civic buildings in Veridia that survive intact to the present day underwent extensive structural reinforcement during the 15th century. It is an architectural fact that no building constructed purely of unreinforced porous limestone can survive more than two centuries of continuous freeze-thaw cycles without catastrophic degradation.
Based on the information above, which of the following statements are most strongly supported? (Select all that apply)
- At least some civic buildings in Veridia have been subjected to continuous freeze-thaw cycles for more than two centuries.Cevap
- Any civic building in Veridia constructed before 1300 CE that currently survives intact has undergone some form of structural reinforcement.Cevap
- CThe primary reason the pre-1300 civic buildings were structurally reinforced in the 15th century was to protect them from the degrading effects of the mini-ice age.
- DCivic buildings in Veridia constructed after 1350 CE were generally not built using locally quarried limestone.
- EIf a building in Veridia is constructed of a material that is not highly porous, it will not experience catastrophic degradation from continuous freeze-thaw cycles.