People v. Rindge

164 P. 633, 174 Cal. 743, 1917 Cal. LEXIS 860
California Supreme Court·Decided April 7, 1917·No. L. A. No. 3752.·Published·Cited by 2 cases

Opinion

HENSHAW, J.

This action was brought to abate alleged nuisances maintained by defendants upon and across a public highway in the county of Los Angeles. The nuisances were gates and fences. The purpose of the litigation is to obtain a decree declaring that a public highway exists through the Malibu ranch along the shore of the Pacific Ocean. The Malibu ranch is about twenty-two miles long and contains about thirteen thousand acres. Thus it is quite narrow, varying in width from one mile and a half to two miles and a half. Its length is easterly and westerly. Its southern front is bounded and washed by the waters of the Pacific Ocean. The inland boundary line extends along the southerly slope of a fugged, inhospitable mountain chain, cut by deep ravines and canyons. At the foot of these mountains is a stretch of country narrow and comparatively level and known as mesa lands. The “shore of the Pacific” along which it is declared this highway extends is a shore characteristic of many hundreds of miles of California’s littoral. Nearest to the ocean is a gradually sloping sandy beach between the lines of high and low tide. At low tide this beach is uncovered, and the sand wet and compacted affords a firm passageway for footmen and vehicles. Above this is a stretch of loose shifting sand, washed and blown above the line of ordinary high tide. This sand is dry and passage over it, though possible, is difficult. The footman sinks to his ankles, the horse to his fetlocks, the *745 vehicle which he is dragging half way or more to the hubs. Beyond this loose sand is a bluff varying in height from thirty to one hundred feet. Eroded from this bluff and lying at the foot of it is the talus. This bluff marks the seaward end of the comparatively level mesa lands of which we have spoken. These mesa lands in turn are channeled by ravines or arroyos, in winter carrying the mountain waters down the gulches to the ocean. In summer they are dry. Their banks usually are quite precipitous. The beach, of course, is likewise pierced in places by these short mountain streams, although in summer when these streams are not flowing the ocean frequently restores the sand washed away by the winter torrents. Still further the beach is broken by small promontories and rocky headlands jutting out into the ocean and by rocky outcrops here and there along its line. As is well known to anyone at all conversant with the primitive life of California, these beaches afforded the customary routes of travel up and down the coast. They were smooth and level, as compared with the mesa lands which were cut by numerous gullies, difficult of descent and equally difficult of ascent. Thus travel sought the beach and followed along the line of the hard sand uncovered by the ebbing tide. As a promontory was approached the traveler was compelled to leave the beach, climb to the mesa uplands, cross the promontory, descending to the beach on the farther side. Where the winter rains converted the- arroyos into torrential streams progress was impossible. When the rising tide covered the hard beach the traveler was compelled to make his laborious way through the soft sands above, or, as was usually the practice, he interrupted his journey and remained where he was until the tide had again ebbed. Little or no construction work was ever done upon these roads, if roads they could be called. The traveler, usually on horseback, when it became necessary to leave the beach, sought the least precipitous place in the bluffs up which he rode or led his horse. Where this was impossible, the earth bank of the bluff was graded down.

Such are the general characteristics- of many such ancient shoreways along the Pacific Ocean; such were the general characteristics of this ancient way. In those early days' the principal towns or pueblos to the north and west of that of Los Angeles were San Buena Ventura in Ventura County, and Santa Barbara in the county bearing the same name. *746 Both of these counties, like the county of Los Angeles, are coast counties. There were several routes of travel between Los Angeles and these northerly pueblos through the mountain passes, in addition to the shore route just described. This shore route, beginning at a settlement on the ocean near the mouth of Santa Monica Canyon, ran about five miles through another grant, Boca de Santa Monica; then entered upon the Malibu grant, ran along its coast line and a mile or two beyond it to a gulch known as Yerba Buena or Little Sycamore Canyon, when it struck inland up this gulch and over the mountains and so to the towns in Ventura County. Travel over the whole of this route was possible only to the footman or to the horseman. Wheeled vehicles could not be dragged over it, and indeed there were in those early days but few wheeled vehicles—carretas—clumsy carts with solid wooden wheels, drawn by oxen.

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People v. Rindge, 164 P. 633, 174 Cal. 743, 1917 Cal. LEXIS 860 (Cal. 1917).

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Related

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292 P. 157 (California Court of Appeal, 1930)
Rindge Co. v. County of Los Angeles
262 U.S. 700 (Supreme Court, 1923)