Mexico and the Pacific

Author(s):  
Edward R. Slack

Called “Mar del Sur” [South Sea] when first spotted by Balboa in 1513 and dubbed “Mar Pacifíco” [Peaceful Calm Sea] by Ferdinand Magellan in 1520, the historical relationship between the Pacific Ocean and the people of Mexico is multilayered and dynamic. During the Spanish colonial era (1521–1821), the viceroyalty of New Spain (Nueva España) supervised the Asian and Polynesian colonies of the Philippines and Guam (and briefly Taiwan and the Spice island of Ternate) across the Pacific. Acapulco became a mythical emporium of exotic luxury supplied by the galleons from Manila that for 250 years tied Asia to the Iberian New World. Beyond this famous port, littoral native communities dotting the Pacific coast, from Oaxaca in the south to the forty-second parallel of Alta California in the north, gradually fell under Spanish secular and religious control. The enormous coastline measured approximately 5,400 miles, more than double the length of seaside territory facing the Gulf of Mexico. Following the War of Mexican Independence (1810–1821), the United Mexican States (Estados Unidos Mexicanos) emerged. For the next fifty years, Mexico experienced domestic political instability exacerbated by wars against the United States (Mexican-American War, 1846–1848) and France (1862–1867). When political order was finally established under the regime of Porfirio Díaz (1876–1910), regionalism was confronted by the centrifugal power of a modernizing, technocratic state. Despite losing 840 miles of California coastline, and a lucrative trade route with Manila, in the Mexican-American War, Mexico’s Pacific littoral in the south grew to incorporate the formerly Guatemalan territory of Chiapas, and a new shipping network evolved. Traditional research on pueblos, cities, or states along the Pacific coast emphasizes purely local or regional contexts within the colonial or independent Mexican state; or it is grouped thematically into studies about the galleon trade or California mission settlements. Recent scholarship is encouraging a more balanced approach, accentuating the many threads that wove a rich tapestry of Mexico’s unique relationship with the “Pacific World” (as opposed to the more popular “Atlantic World”); not only in a nationalist framework, but with inter-American and trans-Pacific or global dimensions.

2021 ◽  
Vol 33 (2) ◽  
pp. 382-411
Author(s):  
Chris Madsen

Henry Eccles, in classic studies on logistics, describes the dynamics of strategic procurement in the supply chain stretching from home countries to military theatres of operations. Naval authorities and industrialists concerned with Japanese aggression before and after Pearl Harbor looked towards developing shipbuilding capacity on North America’s Pacific Coast. The region turned into a volume producer of merchant vessels, warships and auxiliaries destined for service in the Pacific and Indian Oceans. Shipbuilding involved four broad categories of companies in the United States and Canada that enabled the tremendous production effort.


1969 ◽  
Vol 7 (2) ◽  
pp. 319-322
Author(s):  
Helen Kitchen

The membership of the African Studies Association now numbers 1,731— 734 fellows, 618 associates, and 379 student associates. Some 700 of these participated in the eleventh annual meeting of the Association. Although attendance was considerably below the 1,300 registered at the New York Hilton in 1967 and the nearly 1,000 who made their way to the University of Indiana in 1966, there is no indication that this reflects a declining interest in African studies in the United States. Rather, the A.S.A. custom of bringing its annual meetings in turn to scholars in the north-east, on the Pacific coast, and in the Middle West results in predictable fluctations in registration.


2004 ◽  
Vol 1 (6) ◽  
pp. 8-11 ◽  
Author(s):  
Udgardo Juan L. Tolentino

The Philippines, known as the Pearl of the Orient, is an archipelago of 7107 islands, bounded on the west by the South China Sea, on the east by the Pacific Ocean, on the south by the Sulu and Celebes Sea, and on the north by the Bashi Channel. The northernmost islands are about 240 km south of Taiwan and the southernmost islands approximately 24 km from Borneo. The country has a total land area of some 300 000 km2. It is divided into three geographical areas: Luzon, Visayas and Mindanao. It has 17 regions, 79 provinces, 115 cities, 1495 municipalities and 41 956 barangays (the smallest geographic and political unit). It has over 100 ethnic groups and a myriad of foreign influences (including Malay, Chinese, Spanish and American).


1969 ◽  
Vol 1 (1) ◽  
pp. 30-36
Author(s):  
Kenneth L. Holmes

Francis Drake's circumnavigation of the world (1577-1581) marks the first certain approach of Europeans to what later became known as the Northwest Coast of America. Historical research on this voyage has stemmed from Great Britain and the United States. British scholars concerned with the subject as part of English maritime activity have included Richard Hakluyt, James Anthony Froude, E. G. R. Taylor, James A. Williamson and A. L. Rowse. The latest British scholar to inquire into the motives and events of the great voyage is Kenneth R. Andrews. These writers have generally given little space to Drake's experiences on the Northwest Coast. However, the late California scholar Henry Raup Wagner published a monumental study of the subject in 1926. This work and two volumes published by the Hakluyt Society provide most of the documents relating to the voyage.The pertinent passages describing Drake's activities in the North Pacific are as follows: From Guatulco [a village near Acapulco on the Mexicanwest coast] we departed the day following, viz. April 16.setting our course directly into the sea: whereon we sayled500. leagues in longitude, to get a winde: and between thatand June 3. 1400. leagues in all, till we came into 42. deg.of North latitude. ….The land in that part of America, bearing farther out into the West, then we before imagined, we were neerer on it than wee were aware; and yet the neerer still wee came unto it, the more extremitie of cold did sease upon us. The 5. day of June, wee were forced by contrary windes, to run in with the shoare, which we then first descried; and cast anchor in a bad bay, the best roade we could for the present meete with: where wee were not without some danger, by reason of the many extreme gusts, and flawes that beate upon us; which if they ceased and were still at any time, immediately upon their intermission, there followed most vile, thicke, and stinking fogges; against which the sea prevailed nothing, till the gusts of wind were againe remowed them, which brought with them, such extremitity and violence when they came, that there was no dealing or resisting against them.


1988 ◽  
Vol 25 (6) ◽  
pp. 844-852 ◽  
Author(s):  
Garry C. Rogers

The active tectonic setting of the southwest coast of Canada and the Pacific northwest coast of the United states is dominated by the Cascadia subduction zone. The zone can be divided into four segments where oceanic lithosphere is converging independently with the North American plate: the Winona and the Explorer segments in the north, the larger Juan de Fuca segment that extends into both Canada and the United States, and the Gorda segment in the south. The oceanic lithosphere entering the Cascadia subduction zone in all segments is extremely young, less than 10 Ma. Of the other six zones around the Pacific where young (< 20 Ma) lithosphere is being subducted, five have had major thrust earthquakes (megathrust events) on the subduction interface in historic time. An estimation based on potential area of rupture gives maximum possible earthquake magnitudes along the Cascadia subducting margin of 8.2 for the Winona segment, 8.5 for the Explorer segment, 9.1 for the Juan de Fuca segment, and 8.3 for the South Gorda segment. Repeat times for maximum earthquakes, based on the ratios of seismic slip to total slip observed in other subduction zones, are predicted to be up to several hundred years for each segment, well beyond recorded history of the west coast, which began about 1800. Thus the lack of historical seismicity information provides a few constraints on the assessment of the seismic potential of the subduction zone.


2021 ◽  
Vol 57 (03) ◽  
Author(s):  
HURNG-YU CHEN

After Japan occupied Taiwan from the Quin Dynasty in 1895, the Japanese government immediately held talks with Spain to delimit the sea boundary between Spain and Japanese Taiwan. According to the Convention between Japan and Spain in 1895, the sea boundary of both countries was in the middle of the navigable channel of Bashi. For it did not refer to the longitude and latitude, thus it resulted in confusion when the United States negotiated a peace treaty with Spain. What is the meaning of “in the middle of the navigable channel of Bashi?” In the Treaty of Paris between the United States and Spain in 1898, Spain ceded the Philippines archipelagoes to the south of 20∘ North latitude to the United States. In fact, the Batanes Islands are located at 20–21∘ North latitudes. Geographically, the Batanes Islands were not included in the Treaty of Paris. This paper will focus on the reasons why did not Spain cede the territory to the north of 20∘ North latitude to the United States? And, it also discussed the problems of the legal status of the Batanes Islands and the rights of claim by Taiwan.


1944 ◽  
Vol 9 (3) ◽  
pp. 265-270 ◽  
Author(s):  
H. G. Barnett

Semi-Subterranean houses with an entrance through the roof are a well known feature of the interior of British Columbia, having been described for the Thompson, the Chilcotin, the Shuswap and others of the upper Fraser River valley. They have, in fact, an even wider distribution east of the Coast and Cascade Ranges, extending south over the Plateau and into northern California. Although this type of dwelling existed among the Aleuts, it appears that the coastal people to the south of them, even in Alaska, were either unfamiliar with the pattern or rejected it in favor of others. Sporadically, along the Pacific Coast all the way from California to Bering Sea, house floors were excavated to varying depths, sometimes even to two levels; but, everywhere, the houses characteristically lack the roof entrance and, except for sweathouses in the south and Bering Sea Eskimo dwellings in the north, even the idea of an earth covering is absent. In view of this fundamental divergence, it is interesting that subterranean structures do appear in several places on the coast of British Columbia.


Author(s):  
Simon Young

The study brings together fourteen landscape place names with the element ‘mermaid’ from the West Indies. The locations range from a coastal cave in Bermuda, in the north, to an inland pool in Trinidad, in the south. Some of these names are linked to regional folklore; some are arguably confected names invented, for instance, to encourage tourism. The author asks what markers can help us distinguish between folklore and confected names and ends with a list of other mermaid place names in Africa, the Pacific and America that might have their origins in indigenous or colonial era folklore.


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