Having asserted that during the culmination4 of a frigid5 period the ice-sheets spread over a portion of the lands of the tropical zone, I will give my views, with those of several writers, on the spread of ice-sheets within the now temperate latitudes7; and meanwhile I will repeat a portion of my former essays on the subject. Professor Hitchcock, in his lectures on the early history of North America, says that “the history opens with igneous8 agency in the ascendant, aqueous and organic forces become conspicuous9 later on, and ice has put on the finishing touches to the terrestrial contours.” But there appear to be various opinions held by geologists10 respecting the changes brought about on the earth’s surface during the glacial period. Some think that glaciers have never been an important geological agent, while others assert that during the glacial epoch11 heavy ice-sheets covered the elevated portions of Western63 North America as far south as the thirty-sixth parallel of latitude6, and Eastern North America was overspread with ice-sheets, which attained12 a depth of five or six thousand feet, and were able to move their débris over wide lands of little declivity13 toward the sea, their immense deposits forming the lands of Cape14 Cod15, and also the islands of Nantucket and Martha’s Vineyard.
But it is now said that this implied magnitude of the glacial deposits on the lands skirting the New England coast is without foundation, since the larger bulk of these islands consists of upturned Cretaceous and Tertiary strata16, which are only thinly covered with glacial débris, such as bowlders, gravel17, clay, and sand, from the eroded18 shores of the mainland of New England. But it appears that the dislocated and folded cretaceous strata which underlie19 the glacial drift of Nantucket and Martha’s Vineyard were during an early period deposited on the bottom of a shallow sea, which then covered the Vineyard Sound, Buzzard’s Bay, and their surrounding lowlands. Thus the ice-sheets of the frigid age which moved over New England displaced the yielding stratified deposits of the shallow sea, and forced them southward in a disturbed condition to the position which they now occupy.
Still, it is apparent that only a small portion of the glacial drift is found on these islands, which, according to appearances, must have been eroded and moved southward from the rocky lands of New England during the ice age; but there is sufficient to show that large quantities of such débris were carried over the islands into the Atlantic. And, judging from the eroded rocky New England lands, there must have been sufficient glacial drift moved over Nantucket and Martha’s Vineyard into the ocean beyond to far exceed in bulk the deranged20 Tertiary and Cretaceous deposits which now form so large a portion of the islands.
For, when we look over lands bearing traces of the ice age, where the glaciers did not move their drift into the sea, so the64 terminal moraines of such glaciers can be better estimated, we can realize the great work that has been performed by the ice-sheet that overran New England during a frigid age.
Professor James Geikie states, in his discussion on the glacial deposits of Northern Italy, that the deposits from Alpine21 glaciers of a frigid period “rise out of the plains of Piedmont as steep hills to a height of fifteen hundred feet, and in one place to nearly two thousand feet. Measured along its outer circumference22, this great morainic mass is found to have a frontage of fifty miles, while the plain which it encloses extends some fifteen miles from Andrate southward.” And it is reported that there are found on the southern flank of the Jura numerous scattered23 bowlders, all of which have been carried from the Alps across the intervening plains, and left where they now rest. Many contain thousands of cubic feet, and not a few are quite as large as cottages.
Such blocks are found on the Jura, at a height of no less than two thousand feet above the Lake of Neuchatel. The Jura Mountains being formed of limestone24, it is easy to distinguish the débris deposited by Alpine glaciers; and, from what I can learn of extensive glacial work, it appears that intervening plains, lakes, and sounds are so often found separating the source of ancient glaciers from their deposits that their existence becomes almost necessary to represent the general outlines of disturbance25 performed during an ice period. In consideration of such facts and the foregoing statements of reliable observers, I am prompted to offer my views on glacial work performed on a portion of the Pacific shores of North America, which seems to me to be much more extensive than hitherto supposed.
Professor Whitney describes the coast mountains of California as being made up of great disturbances26, which have been brought about within geologically recent times; and this statement I found to be so obvious in my travels over that region that it appears to me that the coast ranges originated in a different65 manner from the older Sierras. The western sides of the latter mountains everywhere show the great eroding27 power of ancient glaciers; and, when I considered their favorable position for the accumulation of snow during a glacial period, I was led to seek for the glacial deposits adequate to represent the great gathering28 of ice which an age of frigid temperature would produce.
But it seemed to me that such deposits could not be found in the foot-hills of the Sierras, which contain the moraine of inferior ice-sheets that terminated at the base of the mountains.
Under these conditions I came to the conclusion that during the earlier ice period the immense glaciers which must have formed on the western slopes of the Sierra range moved their gigantic accumulation of débris so far seaward as to form the range of hills now existing next the coast line, and perhaps the islands abreast29 the Santa Barbara coast, the Contra Costa, or eastern range, being formed during a subsequent ice period, in the same manner as the hills next the coast line.
Still, it may be that neither of the coast ranges was the work of a single cold epoch; but the western range must necessarily have been the earliest deposit. Although the coast ranges differ from the Sierras in their make up, yet it does not disagree with the glacial origin of the former inferior mountains, from the fact that the ice-sheets, while moving their bulk westward30, displaced the deposits of such bays, lakes, rivers, and marshes31 as lay abreast of the Sierra slopes. The advancing ice-sheets, thousands of feet in depth, moving from a lofty and steep incline, pressed and ploughed below the somewhat superficial cretaceous and alluvial32 strata which lay in their course. The disturbed strata, while forced along in confused heaps in front of the ice, were amassed33 in ridges34 sufficient to form the hills of the coast ranges. The bowlders found imbedded in several of the coast hills must have been moved by the ice from the Sierras on account of the coast ranges not having a rocky core of sufficient firmness to give shape to such bowlders. Moreover,66 the temperature of the Pacific waters would not be favorable for glaciers to form on the coast ranges, with the ice-sheets of the Sierras terminating at the foot-hills.
The Sacramento and San Joaquin Valleys are now covered by recent river deposits. Therefore, the glacial drift which should be traced from the Sierras to the coast ranges is concealed35.
Yet the abraded36 appearance of exposed solid rocks at the base of the foot-hills, and also the scattered bowlders which gradually disappear beneath the diluvial deposits of the plains, indicate that the Sierra ice-sheets could not have ended at the foot-hills, but must have moved further westward, while gathering immense accumulations in their front, sufficient to form the coast hills, the débris thus amassed being able to arrest the further movement of the ice seaward.
The coast ranges in several places have been subject to igneous action, which may have been brought about through heat generated from pressure exerted on the interior masses after the ice had melted away, the heat thus produced being sufficient to cause outbursts of lava37, where the nature of the material favored combustion38. The low plains, lakes, and bays which separate the Sierras from the coast hills are in a position similar to the shallow sounds which separate Nantucket, Martha’s Vineyard, and Long Island from the inferior slopes of the mountains of New England. Therefore, while agreeing with glacialists, who believe that great geological changes have been wrought39 by ice-sheets in Italy and New England, it appears to me that the ancient glaciers of the Sierra Nevada have accomplished40 more extensive work, owing to the Sierras being situated41 in a more favorable position to receive the humidity of the ocean.
Hence, with a low temperature, vast quantities of snow must have collected on their lofty sides; and at the same time their great height and declivity would cause the ice to move down their steeps with greater force than the glaciers which passed67 over New England. Writers who have given the subject considerable study think that the deep valleys of the Sierra Nevada were produced by disruptive rather than erosive agencies. This conclusion has been formed from the lack of large accumulations of débris about their lower extremities42, which would not be the case if such valleys were the result of glacial erosion. But, should the coast ranges be attributed to glacial action, as has been stated, we can well account for the débris that should accumulate from the erosion of the deep valleys.
The only thing that could prevent the ice from gathering on the Sierra Nevada range during an ice period in greater masses than on any mountains in the northern hemisphere would be the lack of cold; for, with a low temperature, the fall of snow would be enormous. This is shown by the great snow-fall during the short mild winters of to-day. Therefore, with ice-sheets covering a large portion of the lands of the high northern latitudes, and with the Japanese current which tempers the north Pacific waters made cold in the manner described in the foregoing pages, and while the sea along the north-west coast of America was strewn with icebergs43 launched from Alaska and British Columbia, it seems that California must also have obtained a frigid climate during the ice age. Therefore, on account of its exposure to the ocean winds, and the consequent heavy snow-fall, the accumulation of ice on its lands must have been immense. For, when it is considered that the glaciers of North America extended southward even into the torrid zone sufficient to cover a large portion of Central America, it is unreasonable44 to suppose that any portion of California could escape being covered by heavy ice-sheets during the glacial epoch. The comparatively scant45 fall of rain and snow over Greenland is known to form ice-sheets hundreds of feet in thickness.
Therefore, what must have been the depth of ice over the high lands of the Pacific coast north of California at the culmination of a frigid period? The descriptions given by Dr.68 Dawson and others, of glacial phenomena46 along that coast, favor the impression that an immense ice-sheet at one time deeply covered the whole region from the top of the mountain range to the ocean.
Thus all the deep channels were filled and all the islands deeply overrun with ice, while the immense bergs launched from the shore and carried by the winds and currents southward were probably not melted until they reached the tropical latitudes. Thus, when the whole circulation of the Pacific waters are taken into account, it will be seen that their temperature during the ice age must have been considerably47 lowered. The movement of ice-sheets on the Pacific slope was probably local in character, and not connected with the movement of ice on the eastern sides of the mountains.
From what I have seen of the vast territory lying between the Sierra Nevada and the Rocky Mountains it appears that it obtained much heavier ice-fields than generally supposed. Professor Geikie in his lectures says of this region that during the glacial age, “in the Second Colorado Canyon48, the sides were completely glaciated from bottom to top. These walls are from 800 to 1,000 feet high, and at the thickest point the glacier2 was 1,700 feet thick”; and he says that “the country around Salt Lake was covered with ice, for the rocks about there show the action of ice, and that the bones of the musk-ox are found there.” This vast area of ancient ice, although subject to little movement in its interior basin, still, in whatever movement it may have had, must have found its main outlet49 through the Grand Canyon of the Colorado.
For in no other way can we account for the erosive forces necessary to excavate50 that immense chasm51. Not even the mighty52 torrent53 that carried off the waters of the melting ice-sheets that covered the interior portion of the continent could accomplish work of such magnitude.
According to Professor Geikie’s observations the Second Colorado Canyon was filled with glaciers during the ice age.69 Therefore, it seems that these glaciers must have flowed down into the Grand Canyon, and there united with glaciers flowing from more northern regions.
An account of a collecting expedition to Lower California by G. Eison, in 1895, describes ancient moraines at the extremity54 of the peninsula as being prominent, large, and steep. This region lies under the tropic of Cancer, and 8° south of the mouth of the Colorado River where it empties into the Gulf55 of California. Hence it appears that the temperature of that portion of North America during the ice age was favorable for the great glacier of the Colorado Canyon to have flowed into the Gulf of California.
The wide, shallow basins of Utah and Nevada were filled with the water from the melting ice-sheet on the breaking up of the ice period, and the lakes so caused remained for a considerable time after the disappearance56 of the ice. But, owing to the great evaporation57 and light rain-fall of that region, the lakes gradually shrank away, the filling and emptying of the lake basins being governed by the cold and mild epochs.
The conglomerate58 deposits in the Appalachian district of North America are known as occurring on a large scale. Professor Shaler is inclined to attribute them to glacial action, because he knows of no other force that could bring together such masses of pebbles59 from a wide-spread surface. In Eastern Kentucky and East Tennessee these deposits are found to be several hundred feet in thickness. Such accumulations of apparent glacial origin are to be found from New Brunswick to Alabama.
Hence it seems that the ice during a frigid period followed down the Alleghany range even so far south as Georgia and Alabama; and for a time, when the ice attained its greatest spread, it flowed over the central portion of the Gulf States. For how else can we account for the clay mixed with gravel and pebbles and stony60 fragments being spread broadcast over that region?
70 I know that such statements do not agree with the views of glacialists who have written on the subject, and have drawn61 the glacial boundary from seven to ten degrees further north, where a line of bowlders with other glacial débris is plainly traced. Still, it appears to me that a line of bowlders deposited by an ice-sheet spreading over a continent and across many degrees of latitude cannot be compared to the moraines of inferior mountain glaciers of the temperate latitudes of the present age.
An ice-sheet moving from a high latitude to a lower would, while in the colder latitude, freeze firmly to the rocky ledges62, and hold them so strong in its frigid grasp as to break off the weaker portions of the rocks, and drag them toward a milder region, as far as the freezing grip of the ice-sheet would permit; but, on gaining lower and milder latitudes, the holding and dragging power of the ice would be lost on account of the increased warmth of the earth over which the glacier must pass, and also because of the ice-sheet having lost a portion of the low temperature acquired in the higher latitudes. Therefore, on such lines the bowlders would be released, while the ice-sheet would still move on, although largely deprived of its eroding power.
This is the probable reason why a line of glacial débris, largely composed of bowlders, is found to extend across the Middle and Western States, and so generally supposed to be the glacial boundary of a frigid period. But there is no reason to suppose that an ice-sheet, although deprived of its eroding power, was arrested in its southern movement on the line of its stony débris, because there could be no sudden change of temperature in a particular latitude on the eastern lands of North America to cause an abrupt63 ending of the ice-sheets. And there appears to be nothing to hinder the ice from gathering and flowing over lands warm enough to loosen its implements64 of erosion; for there is much to show that the ice-sheets flowed much further southward, even into the middle portion of the71 Gulf States, and there spread the clay mixed with gravel and pebbles, with now and then a bowlder, over the land. The scattered bowlders, found in numerous instances many miles south of the bowlder line, were so deeply imbedded in the ice-sheet that they could not be dropped on the usual releasing ground. The ice-sheet, when deprived of its rocky, eroding implements, would, while flowing over the land, leave few or no imprints65 on the rocks; but it would probably move and spread a large amount of clay, gravel, pebbles, and sand over its wide course, especially if the ice moved from a region abounding66 with such material.
Should we place the glacial boundary on the line of the rocky débris, how could we account for the glaciated stones found on the hills and plains situated far southward of the bowlder-strewn regions of the Middle and Western States? The clay mixed with gravel and sand, and spread so broadcast over a large portion of Georgia and even into Northern Florida, makes it appear that the ice of a cold period must have covered that southern region.
Moreover, it seems to have been through the great abrasion67 which only ice-sheets could perform that the sands of the Florida peninsula were produced; for on examination they seem to have resulted from the abrasion and weathering of crystalline rocks.
The worn remnants of such rocks are now found in the southern Appalachian range. In fact, the hills and mountains of that region at the present time are supposed to be a small remnant of the ancient highlands. Thus, on consideration, it appears that the sands caused by the action of glaciers were, on the disappearance of ice-sheets, blown by the strong north-west winds toward the Florida peninsula as fast as the receding68 waters of the ocean which flowed the lowlands on the breaking up of the ice age would permit; and in this way the sand was spread over the lowland region, which was largely composed of coral sea shells and other marine69 matter. And it72 seems that the sand must have been blown over large areas in Florida soon after the ending of the frigid period, because the sand, in order to be moved by the winds, must have spread over a country nearly destitute70 of vegetation; and such would be the condition of that region during times which succeeded the ice period and the subsequent brief flowage of the lowlands on the ending of the frigid age, which would not be the case if such sands resulted entirely71 from water erosion and weathering, because with such a state of things the country would be covered with forests and grasses, which would prevent the sand from being moved by the winds to any great extent.
This goes to show that the region of the Gulf States was so much affected72 by the cold of the glacial period, together with the submergence of the lowlands at its close, its flora73 and also its animals were exterminated74; for how else can we account for the abundant fossil remains75 of animals now found buried in the Florida sands? It appears also that, when Florida was being covered with drifting sands, many of the lake basins now formed did not exist, as the wind-blown sand could not have crossed a continuous chain of lakes like the St. John’s River; and it is an easy matter to-day to trace the beds of the ancient lakes that prevented the sands from drifting over certain lands now nearly destitute of it. And it is probable that the sea flowed the lowest lands during the period when the winds were drifting the greater portion of the sands over the peninsula. Therefore, regions which embrace the Everglades and portions of the Indian River territory are quite free from heavy sand deposits, and so also are the extensive flat woods of the peninsula.
Since the sands blew over the ancient desert of Florida, many lake basins have been formed because of the sinking of the ground. This sinking of the ground is a common occurrence in limestone regions, where a great amount of material is moved in solution, leaving caverns76 whose roofs often fall in. The great amount of sand blown upon Florida caused the73 marine strata to give way in the weaker places under its burden. The sinks thus formed, probably of frequent occurrence at one time, have now nearly ceased. Still, there are depressions to be seen to-day where the tops of large pine-trees, which grew on dry, sandy land, are barely above the surface of the water which partly fills the basins so recently formed. Yet I would not assert that all of the depressions where Florida lakes exist were caused by the sinking of the ground; for the winds may have caused shallow basins in the sand, where the decayed vegetation has formed mud sufficient to hold the water which now partly fills such basins.
The mobility77 of Florida sands can be seen to good advantage when exposed to a strong, dry north-west wind, where the ground happens to be destitute of vegetation. An observer can then realize what the result would be, should the whole land be deprived of vegetation and laid bare to the action of the winds.
Under such conditions, not only would the winds be much stronger than now, but the air near the ground would be filled with sand, moving like drifting snow in a Dakota blizzard78. And, furthermore, it is probable that the rainfall was very light while Florida was void of vegetation; and, even if shallow basins were formed, there would be a lack of rain to supply them with water.
The wide plains west of the Mississippi River, extending southward into Texas, during the frigid period must have been covered with a sheet of ice and snow. And it is probable that it was not wholly a product of more northern latitudes, but was mostly produced by the snow which fell on the plains during the long winters of that period, which could not be melted away during the cold summers of an ice age, when it is considered that an ice-sheet, with a temperature sufficiently79 low as to carry glacial drift, covered the lands of Missouri as far as latitude 38° south; and it may have been through the pressure from an ice-sheet in its south-eastern movement that we are to74 account for the numerous ore-bearing faulting fissures80 traversing the limestone strata.
The ice-sheet was also the probable cause of the erosion of the horizontal bedded stones, yet it appears that the ice did not greatly change the contour of the ground; for it is well known that glaciers do move over lands that are not frozen to the ice without causing much disturbance, especially where the gradient is small, and this was the probable condition of the Western plains during the ice age. Thus it seems that whatever disturbance this region has undergone could be partly attributed to ice-sheets without the presence of bowlder drift, because the temperature and texture81 of the ground in the limestone region were unfavorable for such accumulations; yet it may be owing to the action of ice that minerals once diffused82 are now found collected in fissures. The deep valleys through which the large rivers now pass on their way toward the sea were once filled with glaciers which flowed into them from their tributaries83. Thus the deep trenches84 of the plains are largely the work of glaciers. It is generally supposed that the driftless region of Wisconsin was free from ice during the frigid period. But it seems impossible for this region to have escaped being covered by ice and snow, with the great lakes filled with glaciers, and the regions on all sides of the driftless area covered with ice.
The reason why this territory escaped the drift from the north was on account of the hindrance85 which the drift-bearing ice-sheet encountered in the deep basin of Lake Superior. In this great depression the ice-sheet from the north was relieved of bowlders and other glacial drift, as well as obstructed86 in its southern movement.
Therefore, the snow and ice which gathered on the driftless region had little movement in any direction, while the temperature and consistency87 of the ground under the ice were not favorable for the production of bowlder drift; and, when we consider that the Mississippi valley was deprived of great75 sources of warmth during the culmination of a glacial period, we are forced to the conclusion that its wide lands were also covered with snow and ice.
The tropical waters of the North Atlantic were so much chilled by the floating icebergs of North-eastern America, Greenland, Iceland, and Northern Europe that the Caribbean Sea, its warmest reservoir, was reduced to a temperature so low that the easterly winds which blew over its waters were unable to prevent ice-sheets from gathering on Eastern Nicaragua.
Therefore, during such frigid times it appears that, with the waters of the Caribbean Sea and Gulf of Mexico reduced to a low temperature, it was impossible for the great Mississippi valley to escape glaciation, while being surrounded by cold seas and glaciated lands which extended even into the tropical latitudes. The broad, level lands of British America and Siberia during the ice age must have been thickly covered by the snow which fell on the deeply frozen plains, besides the large amount of snow that the cold westerly winds must have drifted over their icy surface from lands of greater snow-fall on their western borders. This snow during such freezing times could not be melted away.
The great ice-sheets thus formed over wide, level lands could have but little motion in any direction, certainly not sufficient to cause glacial drift of much magnitude; yet the ice-sheet, at one stage of its existence, probably served to widen and deepen the channels of the great rivers which empty into the Arctic Ocean from these vast regions, and the glacial débris from such erosion was deposited in the arctic seas.
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glaciers
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| 冰河，冰川( glacier的名词复数 ) | |
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glacier
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| n.冰川，冰河 | |
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temperate
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| adj.温和的，温带的，自我克制的，不过分的 | |
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culmination
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| n.顶点；最高潮 | |
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frigid
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| adj.寒冷的，凛冽的；冷淡的；拘禁的 | |
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latitude
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| n.纬度，行动或言论的自由(范围)，(pl.)地区 | |
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latitudes
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| 纬度 | |
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igneous
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| adj.火的，火绒的 | |
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conspicuous
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| adj.明眼的，惹人注目的；炫耀的，摆阔气的 | |
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geologists
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| 地质学家，地质学者( geologist的名词复数 ) | |
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epoch
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| n.(新)时代；历元 | |
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attained
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| （通常经过努力）实现( attain的过去式和过去分词 )； 达到； 获得； 达到（某年龄、水平、状况） | |
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declivity
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| n.下坡，倾斜面 | |
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cape
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| n.海角，岬；披肩，短披风 | |
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cod
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| n.鳕鱼；v.愚弄；哄骗 | |
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strata
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| n.地层（复数）；社会阶层 | |
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gravel
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| n.砂跞；砂砾层；结石 | |
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eroded
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| adj. 被侵蚀的，有蚀痕的 动词erode的过去式和过去分词形式 | |
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underlie
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| v.位于...之下，成为...的基础 | |
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deranged
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| adj.疯狂的 | |
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alpine
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| adj.高山的；n.高山植物 | |
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circumference
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| n.圆周，周长，圆周线 | |
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scattered
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| adj.分散的，稀疏的；散步的；疏疏落落的 | |
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limestone
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| n.石灰石 | |
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disturbance
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| n.动乱，骚动；打扰，干扰；(身心)失调 | |
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disturbances
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| n.骚乱( disturbance的名词复数 )；打扰；困扰；障碍 | |
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eroding
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| 侵蚀，腐蚀( erode的现在分词 )； 逐渐毁坏，削弱，损害 | |
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gathering
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| n.集会，聚会，聚集 | |
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abreast
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| adv.并排地；跟上(时代)的步伐，与…并进地 | |
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westward
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| n.西方，西部；adj.西方的，向西的；adv.向西 | |
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marshes
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| n.沼泽，湿地( marsh的名词复数 ) | |
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alluvial
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| adj.冲积的；淤积的 | |
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amassed
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| v.积累，积聚( amass的过去式和过去分词 ) | |
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ridges
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| n.脊( ridge的名词复数 )；山脊；脊状突起；大气层的)高压脊 | |
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concealed
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| a.隐藏的，隐蔽的 | |
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abraded
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| adj.[医]刮擦的v.刮擦( abrade的过去式和过去分词 )；（在精神方面）折磨（人）；消磨（意志、精神等）；使精疲力尽 | |
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lava
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| n.熔岩，火山岩 | |
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combustion
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| n.燃烧；氧化；骚动 | |
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wrought
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| v.引起；以…原料制作；运转；adj.制造的 | |
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accomplished
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| adj.有才艺的；有造诣的；达到了的 | |
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situated
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| adj.坐落在...的，处于某种境地的 | |
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extremities
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| n.端点( extremity的名词复数 )；尽头；手和足；极窘迫的境地 | |
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icebergs
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| n.冰山，流冰( iceberg的名词复数 ) | |
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unreasonable
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| adj.不讲道理的，不合情理的，过度的 | |
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scant
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| adj.不充分的，不足的；v.减缩，限制，忽略 | |
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phenomena
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| n.现象 | |
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considerably
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| adv.极大地；相当大地；在很大程度上 | |
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canyon
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| n.峡谷，溪谷 | |
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outlet
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| n.出口/路；销路；批发商店；通风口；发泄 | |
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excavate
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| vt.挖掘，挖出 | |
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chasm
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| n.深坑，断层，裂口，大分岐，利害冲突 | |
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mighty
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| adj.强有力的；巨大的 | |
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torrent
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| n.激流，洪流；爆发，(话语等的)连发 | |
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extremity
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| n.末端，尽头；尽力；终极；极度 | |
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gulf
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| n.海湾；深渊，鸿沟；分歧，隔阂 | |
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disappearance
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| n.消失，消散，失踪 | |
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evaporation
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| n.蒸发，消失 | |
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conglomerate
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| n.综合商社，多元化集团公司 | |
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pebbles
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| [复数]鹅卵石； 沙砾； 卵石，小圆石( pebble的名词复数 ) | |
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stony
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| adj.石头的，多石头的，冷酷的，无情的 | |
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drawn
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| v.拖，拉，拔出；adj.憔悴的，紧张的 | |
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ledges
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| n.（墙壁，悬崖等）突出的狭长部分( ledge的名词复数 )；（平窄的）壁架；横档；（尤指）窗台 | |
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abrupt
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| adj.突然的，意外的；唐突的，鲁莽的 | |
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implements
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| n.工具( implement的名词复数 )；家具；手段；[法律]履行（契约等）v.实现( implement的第三人称单数 )；执行；贯彻；使生效 | |
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imprints
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| n.压印( imprint的名词复数 )；痕迹；持久影响 | |
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abounding
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| adj.丰富的，大量的v.大量存在，充满，富于( abound的现在分词 ) | |
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abrasion
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| n.磨（擦）破，表面磨损 | |
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receding
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| v.逐渐远离( recede的现在分词 )；向后倾斜；自原处后退或避开别人的注视；尤指问题 | |
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marine
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| adj.海的；海生的；航海的；海事的；n.水兵 | |
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destitute
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| adj.缺乏的；穷困的 | |
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entirely
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| ad.全部地，完整地；完全地，彻底地 | |
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affected
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| adj.不自然的，假装的 | |
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flora
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| n.(某一地区的)植物群 | |
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exterminated
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| v.消灭，根绝( exterminate的过去式和过去分词 ) | |
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remains
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| n.剩余物，残留物；遗体，遗迹 | |
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caverns
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| 大山洞，大洞穴( cavern的名词复数 ) | |
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mobility
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| n.可动性，变动性，情感不定 | |
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blizzard
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| n.暴风雪 | |
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sufficiently
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| adv.足够地，充分地 | |
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fissures
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| n.狭长裂缝或裂隙( fissure的名词复数 )；裂伤；分歧；分裂v.裂开( fissure的第三人称单数 ) | |
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texture
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| n.(织物)质地；(材料)构造；结构；肌理 | |
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diffused
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| 散布的，普及的，扩散的 | |
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tributaries
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| n. 支流 | |
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trenches
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| 深沟，地沟( trench的名词复数 )； 战壕 | |
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hindrance
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| n.妨碍，障碍 | |
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obstructed
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| 阻塞( obstruct的过去式和过去分词 )； 堵塞； 阻碍； 阻止 | |
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consistency
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| n.一贯性，前后一致，稳定性；(液体的)浓度 | |
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