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Rancho Suscol

1843 establishments in MexicoCalifornia ranchosRanchos of Napa County, CaliforniaRanchos of Solano County, California

Rancho Suscol was an 84,000-acre (340 km2) Mexican land grant in present day Sonoma County, California, Napa County, California, and Solano County, California, given in 1843 by Governor Manuel Micheltorena to General Mariano Guadalupe Vallejo. In a significant land law decision, the land claim was rejected by the US Supreme Court in 1862. Rancho Suscol extended from Rancho Petaluma on the west, south down to the San Francisco Bay and Mare Island and Carquinez Strait, and then to Rancho Suisun on the east. It included present day cities of Vallejo and Benicia.

Excerpt from the Wikipedia article Rancho Suscol (License: CC BY-SA 3.0, Authors).

Rancho Suscol
Ramal Road,

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Latitude Longitude
N 38.22 ° E -122.38 °
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Ramal Road

Ramal Road

California, United States
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1898 Mare Island earthquake

The 1898 Mare Island earthquake occurred in Northern California on March 30 at 23:43 local time with a moment magnitude of 5.8–6.4 and a maximum Mercalli intensity of VIII–IX (Severe–Violent). Its area of perceptibility included much of northern and central California and western Nevada. Damage amounted to $350,000 (about $10,700,000 inflation adjusted to 2018) and was most pronounced on Mare Island, a peninsula in northern San Francisco Bay. While relatively strong effects there were attributed to vulnerable buildings, moderate effects elsewhere in the San Francisco Bay Area consisted of damaged or partially collapsed structures, and there were media reports of a small tsunami and mostly mild aftershocks that followed. The mechanism of the shock is unknown, but several independent investigations focused on different aspects to gain a better understanding of the intensity, magnitude, source fault, and epicenter of this pre-instrumental event. Most investigators placed it under or to the north of San Pablo Bay, though two earthquake catalogs gave specific coordinates that place it within the confines of the San Pablo Bay National Wildlife Refuge. One of the numerous strike-slip faults of the San Andreas Fault System in the North Bay are most often named as the source fault, but one seismologist's paper detailed how an unnamed dip-slip fault may have been responsible. Several more recent studies gave alternate perspectives that named specific faults as the origin.