This edict against the erection of new temples is still in force in Japan, and while it is aided by a growing want of zeal in the hearts of the people, with a contempt for the priesthood, it may be broken through by the permission given to repair, or restore, or enlarge any temple already existing, however small it may be; and as a temple or shrine is standing upon nearly every knoll or eminence in Japan, there can be no difficulty, were the funds forthcoming, of raising such edifices as were raised of old by the zeal of fervent worshipers.
The Buddhist priesthood in 1720, by a great religious festival all over the empire, commemorated the eleventh centenary of the establishment of Buddhism.
The Japanese claim the discovery and settlement of the Bonin or Monin Islands in the year 1683. The name means “no men,” or uninhabited. Attempts were made to colonize the islands, but they seem to have failed; and some English and Americans, with Sandwich Islanders, male and female, succeeded them. But in 1862 the Japanese government fitted out a vessel and carried away all these adventurers, bringing them to Yokohama, and it seems to find the islands a convenient distance to which they can send vessels to train officers and men.
A work was commenced in 1786 which was expected to have proved of great advantage to Yedo. This was the cutting of a canal, and thereby joining several already existing channels, by which a through communication would have been opened up between Yedo, or the Bay of Yedo, and the Pacific Ocean on the east coast. The part of the province of Simosa between Yedo and the east coast is very low land, and it is generally believed that at one time the sea cut off the three provinces of Simosa, Kadsusa, and Awa, which then constituted a separate island; and that the detritus brought down, after a course of nearly two hundred miles, by the largest river in Japan, the Tonay, has filled up with alluvium the sea channel, leaving now only the passage for the fresh water of the river. In the course of the filling up, however, a large lake was left, the Een bang numa. About twenty miles above Yedo, the Tonay, coming down as one river from the Tonay district, divides into two. The one branch, receiving affluents from Hitatsi and the northern provinces, runs due east as the Bando taro, or “eldest son of Bando,” and enters the sea between Choshi and Itaku on the east coast. The other branch, running south, enters the sea to the east of the city of Yedo. The Okawa, or Great River, runs parallel with the Tonay, and passes through Yedo spanned by five bridges. Between the Okawa and Tonay, and running parallel to, and communicating by canals with both, is the Nakagawa or Middle River. By these cross canal communications the passage may be made from Yedo to the Pacific on the east, or to the northern provinces by running up to Seki Yedo, where the bifurcation takes place. It was proposed to deepen the lake, and cut through a passage from it into the Bay of Yedo.—The lower part of Yedo is so low that it is liable to be overflowed should the Tonay rise above its banks. To avert this danger, a large and important embankment, the Gongen do, has been made at Koori hashi. Should this give way, the whole of the lower parts of Yedo would be submerged, as happened, it is said, in 1844.
The town of Sakura first started the project, and commenced a canal, but did not finish the work. The Shiogoon, seeing the advantages of the proposed cut, ordered the Daimios to cut the remainder of this canal (of about fourteen miles in length), each cutting as his share about 360 feet. The work, which was immediately commenced, was in six months half completed, when orders were given to cease working at it. In 1843 the work was recommenced by orders of government, but when it was within three thousand yards of being finished it was again stopped, and it continues in that position to this day.
The river and canal communications in Japan are more ramified than the mountainous nature of the country would lead one to expect. It is said that Yedo might, by short canals, be put into water relations with Mito on the east coast and Negata on the north, as boats can go up the Tonay to Shimidzu, within eight miles of the navigable part of the Negata waters; while Miako might be joined by water to Tsurunga on the north and Owarri on the south. By private enterprise, in the year 1832, the Yodo ngawa between Miako and Osaka was deepened and improved by the removal of some rocks. It is said that the Katsura gawa, or Hozu kawa, now a large affluent of the Yodo gawa, formerly ran to the north through the province of Wakasa; but a private individual, Yodo yo, cut a channel by which this river now flows southward into the Osaka River. His family is permitted to levy tolls upon the new channel.
The occurrence of fearful convulsions of nature is one of the most remarkable circumstances in these annals; and it may be presumed that only the most severe are noticed. But recent observations go to show that almost every day there is an observable motion of the earth at Yokohama from subterranean causes. The native accounts of these, with drawings, give an appalling idea of the suddenness and the severity of earthquakes. In the year 1707 a very severe earthquake shook the whole of the southern part of the island of Nippon, and simultaneously from the side of the mountain Fusiyama [Fusi—literally “not two,” or none such] issued an eruption of volcanic matter. This eruption continued for fifteen days; and at Yedo, a distance of seventy miles, dust fell to the depth of two feet. Fusiyama had not given any appearance of volcanic action for centuries. The projection on the smooth outline of the hill on the northwestern side marks the place where this action took place, and is known as Ho yay zan. At the same time the volcano Assama yama, in Sinano, broke out into violent action, by which the two adjacent provinces were laid under lava or dust. The same mountain broke out again in 1783, and of the destruction done at that time Titsingh gives a fearful account. He gives details of an earthquake which occurred in 1793 at Simabara, during which a large portion of the mountain was swallowed up; and the boiling sulphurous springs of Onzen, memorable during the persecutions of the Christians, were dried up. The fear of the inhabitants was quickened by the recollection of the eruption of Assama yama, in Sinano, only ten years before. The inhabitants, with their houses, were engulfed in the openings of the earth; they were carried away by boiling water issuing from the hill; they were killed by falling stones and enormous rocks; they were surrounded and burned by streams of fiery lava; they were drowned by the stoppage of rivers. Some were found suspended from trees, some on their knees, some on their heads in mud, the streets strewed with dead bodies. The falling houses immediately took fire, and the unfortunate inmates were burned, or were confined prisoners. The outline of the coast was completely altered, and the country converted into a desert. A number of vessels were sunk at their anchors, and those which tried to get away could hardly do so from dead bodies and floating wood. Fifty-three thousand are known to have perished in this earthquake in a comparatively thinly populated district.
In 1828 a tremendous earthquake and volcanic eruption took place in the province of Etsingo, during which, at Nadatchi, a large mountain was engulfed and disappeared. This province seems to be entirely undermined by fire. The volcano Taka yama is called the entrance to hell. Oil springs from the ground. Combustible gas issues in such quantity as to be used for cooking and lighting, by simply inserting pipes in the ground. Phosphorescent appearances are seen in many parts. Soda is found in the province in large quantities. Here many flint arrow and spear heads have been found, exactly similar in shape to those found in Europe.
The frequency of these earthquakes is a reason for nearly all the habitations of man being built of wood; and by long experience builders have arrived at certain modes of building, by which the great danger of a house coming down upon the inmates is in many cases obviated. They seem to depend upon the roof for weight; and the piles upon which this heavy roof rests are not fixed firmly into the ground, but some of them are fixed slightly into a square framework of wood, laid on stone, while the others stand simply each upon the surface of a large, round, hard, water-rolled stone, which has been firmly imbedded in broken-down sandstone. By this means the snap of a sudden shock is avoided, and some slight motion is allowed. Whatever be the principle upon which these houses are erected, it is wonderful to see buildings, which seem to be put up in a shape the most ready to topple over upon the least motion, withstand the shocks of earthquakes for ages. There are pagodas in many parts of the country of seven and even nine stories high. At Kamakura is a temple with a narrow circular neck, above which the eaves of a square roof project to about ten feet on every side, resembling the projection of a Chinaman’s hat. If it could withstand the wind, it could never be expected to resist an earthquake; and yet it is said to be two hundred years old, and seems as sound as when it was built.
The annals do not disdain to mention the visits of the Emperor to witness theatrical exhibitions, or proceedings of the Shiogoon in quest of sport.