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| Feature | Description | |---------|-------------| | | Longitudinal splitting crack | | Orientation | Parallel to the reinforcing bar | | Typical Location | Along the bar path, often at corner bars or where cover is minimal | | Associated Phenomenon | Loss of bond, potential rebar slip, reduced service life |
The Toh Rebar Crack is believed to have formed as a result of the Indian tectonic plate's movement, which led to the creation of the [mountain range/plateau] region. Over time, the rocks were subjected to immense stress, causing them to fracture and split apart. Weathering and erosion then took over, widening and deepening the crack into its current form. toh rebar crack