The Origin of the Name “California” and the Island Myth

Nicholas de Fer's map of 1705 showing California as an island. It is titled "Cette Carte De Californie et Du Nouveau Mexique." Image provided courtesy http://www.RareMaps.com — Barry Lawrence Ruderman Antique Maps Inc.

The Origin of the Name “California”

“There ruled on that island of California, a queen great of body, very beautiful for her race, at a flourishing age, desirous in her thoughts of achieving great things, valiant in strength, cunning in her brave heart, more than any other who had ruled that kingdom before her. . .Queen Calafia.”

—Garcia Ordonez de Montalvo, “The Adventures of Esplandián” (1510)

The name “California” derives from a novel written by Garcia Ordonez de Montalvo in the 16th century titled, “Las Sergas del muy esforzado caballero Esplandian, hijo del excelente rey Amandis de Gaula.” It was the fifth book in a series of Spanish romance novels.

The story tells of a mythical island called “California” ruled by Queen Calafia and warrior women “of vigorous bodies and strong and ardent hearts and of great strength.” The queen and her warriors venture forth on forays, where they seize and kill men they come upon. Any man found in their domain they eat. And although sometimes they have children from those they make peace with they keep only daughters and murder sons. It is a land near the Terrestrial Paradise, where the only metal in existence is gold. A land where griffons abound, which the women take as pets and feed to them the men they capture and the sons they bear.

Where Montalvo got the idea for the name remains unknown, but several plausible theories exist. One idea holds that it stems from an Islamic term for leader, which is “caliph.” The Spanish equivalent being “Calif.” In Montalvo’s novel Queen Calafia is a sovereign ruler who is allied with infidels against Muslims. Thus the name “California” is a logical designation for the land she ruled over.

Montalvo’s novels were popular reading material and the legend of California island was not unknown to New World explorers of the time. But like much in history no definitive understanding informs us today of the events surrounding the actual naming of the land that is now part of the United States. “No clear account has come down to us,” Dora Beale Polk writes, “about how the name was chosen, where, when, or by whom. All we have to date are tantalizing scraps of information.” What is understood is that the name was first applied in some manner to the Baja peninsula. Either the headland known today as Land’s End near where Cabo San Lucas is located or in reference to the entire peninsula itself.

The Island of California Myth

“A general tendency of geography and romance prevailing in those days was to locate in an insular landscape the scene of adventures and the place of wonders and marvels.”

Leonardo Olschki Storia letteraria delle scoperte geografiche (1937)

Spanish explorers of the 16th century thought California was an island. It was a myth that ebbed and flowed through the centuries based on the reports of various maritime explorers of different nationalities. Despite occasional doubt cast upon the legend and contrary evidence, the mistake was reflected on maps for a couple hundred years and became one of the great cartographic errors of all-time.

Upon landing on the Baja California peninsula in 1535, Hernán Cortés believed he had found an island. In describing his discovery as insular he is credited as the originator of the island theory. Cortés thought the body of water later named in his honor, the Sea of Cortés, was actually a strait separating mainland Mexico from the island of California. In 1539, he sent an expedition led by Francisco de Ulloa to circumnavigate the imagined island and it was Ulloa that named the Gulf of California in Cortés’ honor. Ulloa, however, was unable to lay the myth to rest and correct Cortes’ erroneous belief. The legend lived on.

Yet, as early as 1542, the notion of California being an island was largely dismissed and cartographers began showing the region attached to the mainland. Despite the change in general sentiment, though, all views remained at most “ambiguous or fence-straddling theories,” Polk writes. The myth proved hard to kill.

Maps drawn in subsequent years, such as the one featured here from 1705, resurrected the island myth. It was not until 1747 that the true nature of California was finally settled. In that year, Spanish monarch Ferdinand VI issued a royal proclamation based on the exploration of the Jesuit missionary, Fernando Consag, and informed the world that “California is not an island.” There was finally too much evidence for myth and fantasy to outweigh empirical facts on the balance of reason. At long last the uncertainty was over.

A detail showing the “Canal of Santa Barbara” as thought to exist in 1705. It was a place name later mentioned by Richard Henry Dana, Jr. in 1835. Today it is better known as the Santa Barbara Channel.

Bibliography:

Dora Beale Polk, The Island of California: A History of the Myth (1991)

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2×2 Bucks

I was out wandering around the woods up in San Luis Obispo County on Sunday and saw a number of deer. I walked up on two doe and one small buck that were remarkably unafraid. I watched them for about 20 minutes sometimes getting as close as 10 to 15 yards away. I never startled them and eventually I just walked away leaving them nibbling away on grass. Then later I happened across an older buck with a larger rack of antlers that was a bit more wary and wouldn’t let me get close to him, as he stood behind a tree watching me intently.

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Canoe Campin’ and Fishin’ in Minnesota

Clint Elliott plying the waters far from home.

Northern Pike

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Clint Sliding Down Mono Dam

Clint in Costa Rica Cliff Diving Montezuma Falls

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Hankins Falls

Hankins Falls as seen last March from Old San Marcos Pass.

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Rocky Peak Park, Santa Susana Mountains

The bedrock plated, boulder strewn hills of Rocky Peak northeast of Simi Valley are made of the Chatsworth Formation, a 6000 foot thick sandstone deposit formed at the bottom of the ocean at the time of the dinosaurs.

The sand that makes up the rocks of today was washed off mountain slopes 70 to 75 million years ago during the late Cretaceous period. Rivers carried the sediment to the ocean and currents pushed it offshore. It settled to the sea floor accumulating in delta-like fans in submarine canyons thousands of feet deep and it was these deposits that fused into stone creating the Chatsworth Formation. Shifting climates, sea levels and fault lines would eventually leave the sandstone high and dry and form new mountains.

Over the last several million years a bend has developed in the San Andreas fault, which has forced the Pacific Plate and the Continental Plate to collide into each other, in addition to sliding past one another. The resulting compression has rippled the land south of the fault in Southern California and formed a series of hills and valleys or anticlines and synclines. Simi Valley, for example, is located in a syncline while nearby Big Mountain Ridge is an anticline.

The tectonic folding of earth’s crust from the pressure of the bending fault line fractured the Chatsworth Formation and thrust it skyward, where it weathered into the tan- and pink-tinged rocks of today. The busted up formation is riddled with caves, overhangs and tunnels providing hikers with the opportunity for hours of recreation exploring the range.

Here I am poking my way through one of the many tunnels in the sandstone. During periods of heavy rain, runoff flows through this channel. In other areas seasonal runnels appear and disappear falling into underground caves.

Along the west end of the Hummingbird Trail, in a section that crosses through a convenient gap in a prominent outcrop, there is a remarkably long cave that is about 100 feet long. Scrambling through the hollow is akin to what an ant must feel like crawling through a deep crack in a sidewalk, where a tree root has split and uplifted the slab. The sequence of photos below shows the cave as I made my way through from one end to the other.

Looking back at the entrance.

Looking down the throat of the cave from the same spot as the last photo.

Looking back at the entrance on the left, as seen from a little further down.

Continuing down the cave.

A shot of me.

The bottom exit hole on the right.

What that exit looks like from the outside. The lower opening of the cave seen here as the darkened area at the bottom center of the photo.

Looking over the giant crack in the sandstone plate where the cave is located.

Bibliography:

Patricia Havens, Simi Valley: A Journey Through Time (1997)

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