Checkpoint tanods allegedly beat the owner of a water refilling station over a dispute about whether mineral water is essential. The commotion erupted after a checkpoint manned by barangay tanods stopped an owner of a water refilling station. According to a GMA News article, tanods questioned the owner who was supposed to deliver his mineral water containers upon his entry. According to the victim, Jeffrey Mercado, the guards also debated whether mineral water was necessary. As Mercado exited at his vehicle, he was punched by a tanod at the checkpoint before he was punched by other barangay officials. Mercado suffers with a lump on his head, earned bruises, and knee swelling.
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In , M. Although this detail has no connection whatever with the real substance of what we are about to relate, it will not be superfluous, if merely for the sake of exactness in all points, to mention here the various rumors and remarks which had been in circulation about him from the very moment when he arrived in the diocese. True or false, that which is said of men often occupies as important a place in their lives, and above all in their destinies, as that which they do. Myriel was the son of a councillor of the Parliament of Aix; hence he belonged to the nobility of the bar. It was said that his father, destining him to be the heir of his own post, had married him at a very early age, eighteen or twenty, in accordance with a custom which is rather widely prevalent in parliamentary families. In spite of this marriage, however, it was said that Charles Myriel created a great deal of talk.
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Located in the Coachella and Imperial Valleys , it covered surface areas of 5, square kilometres 2, sq mi to a height of 12 metres 39 ft above sea level during the Holocene. During earlier stages of the Pleistocene , the lake reached even higher levels, up to 31—52 metres — ft above sea level. During the Holocene most of the water came from the Colorado River with little contribution from local runoff; in the Pleistocene local runoff was higher and it is possible that Lake Cahuilla was supported solely from local water sources during the Wisconsin glaciation. The lake formed several times during the Holocene, when water from the Colorado River was diverted into the Salton Trough.