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Updated: June 17, 2025
Remains of them have been found in badly explored graves in northern Korea. 4 The Neolithic age In the period that now followed, northern China must have gradually become arid, and the formation of loess seems to have steadily advanced. There is once more a great gap in our knowledge until, about 4000 B.C., we can trace in North China a purely Mongoloid people with a neolithic culture.
Loess of the Danube. Oscillations in the Level of the Alps and lower Country required to explain the Formation and Denudation of the Loess. More rapid Movement of the Inland Country. The same Depression and Upheaval might account for the Advance and Retreat of the Alpine Glaciers. Himalayan Mud of the Plains of the Ganges compared to European Loess.
She started walking down the road, over hillocks of buried rubble, around snags of wall jutting up out of the loess, past buildings still standing, some of them already breached and explored, and across the brush-grown flat to the huts. There were ten people in the main office room of Hut One when she entered.
After visiting the spot in 1846, I described the geological position of the bones, and discussed their probable age, with a stronger bias, I must confess, as to the antecedent improbability of the contemporaneous entombment of Man and the mastodon than any geologist would now be justified in entertaining. Modern alluvium of the Mississippi. 2. Loam or loess. 3, f. Eocene. 4.
In European river-loams we occasionally observe isolated pebbles and angular pieces of stone which have been floated by ice to the places where they now occur; but no such coarse materials are met with in the plains of Egypt. In some parts of the valley of the Rhine the accumulation of similar loam, called in Germany "loess," has taken place on an enormous scale.
The bluffs before alluded to often consist of a terrace of gravel, from 30 to 40 feet in thickness, covered by an older loess, which is continuous as we ascend the valley to Liege. In the suburbs of that city patches of loess are seen at the height of 200 feet above the level of the Meuse.
Worms appear to act in the same manner in New Zealand as in Europe; for Professor J. von Haast has described a section near the coast, consisting of mica-schist, "covered by 5 or 6 feet of loess, above which about 12 inches of vegetable soil had accumulated."
This plain is composed of modern loess, undistinguishable in mineral character from that of higher antiquity, before alluded to, and entirely without signs of successive deposition and devoid of terrestrial or fluviatile shells. It is extensively worked for brick-earth to the depth of about 8 feet.
Lu-fêng-hsien and its bridge. Magnificence of mountains towards the capital. Opportunity for Dublin Fusiliers. Characteristic climbing. Crockery crash and its sequel. Mountain forest. Changeableness of climate. Wayside scene and some reflections. Is your master drunk? Babies of the poor. Loess roads. Travelers, and how they should travel. Wrangling about payment at the tea-shop.
The position of the loess between Basle and Bonn is such as to imply that the great valley of the Rhine had already acquired its present shape, and in some places, perhaps more than its actual depth and width, previously to the time when it was gradually filled up to a great extent with fine loam.
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