One may make the trip on horseback, or in a carriage, even; for a good level road may be found all the way round, by Shasta Valley, Sheep Rock, Elk8 Flat, Huckleberry Valley, Squaw Valley, following for a considerable portion of the way the old Emigrant9 Road, which lies along the east disk of the mountain, and is deeply worn by the wagons10 of the early gold-seekers, many of whom chose this northern route as perhaps being safer and easier, the pass here being only about six thousand feet above sea level. But it is far better to go afoot. Then you are free to make wide waverings and zigzags11 away from the roads to visit the great fountain streams of the rivers, the glaciers12 also, and the wildest retreats in the primeval forests, where the best plants and animals dwell, and where many a flower-bell will ring against your knees, and friendly trees will reach out their fronded14 branches and touch you as you pass. One blanket will be enough to carry, or you may forego the pleasure and burden altogether, as wood for fires is everywhere abundant. Only a little food will be required. Berries and plums abound16 in season, and quail17 and grouse18 and deer—the magnificent shaggy mule19 deer as well as the common species.
As you sweep around so grand a center, the mountain itself seems to turn, displaying its riches like the revolving20 pyramids in jewelers' windows. One glacier13 after another comes into view, and the outlines of the mountain are ever changing, though all the way around, from whatever point of view, the form is maintained of a grand, simple cone21 with a gently sloping base and rugged22, crumbling23 ridges24 separating the glaciers and the snowfields more or less completely. The play of colors, from the first touches of the morning sun on the summit, down the snowfields and the ice and lava25 until the forests are aglow26, is a never-ending delight, the rosy27 lava and the fine flushings of the snow being ineffably28 lovely. Thus one saunters on and on in the glorious radiance in utter peace and forgetfulness of time.
Yet, strange to say, there are days even here somewhat dull-looking, when the mountain seems uncommunicative, sending out no appreciable29 invitation, as if not at home. At such time its height seems much less, as if, crouching30 and weary, it were taking rest. But Shasta is always at home to those who love her, and is ever in a thrill of enthusiastic activity—burning fires within, grinding glaciers without, and fountains ever flowing. Every crystal dances responsive to the touches of the sun, and currents of sap in the growing cells of all the vegetation are ever in a vital whirl and rush, and though many feet and wings are folded, how many are astir! And the wandering winds, how busy they are, and what a breadth of sound and motion they make, glinting and bubbling about the crags of the summit, sifting32 through the woods, feeling their way from grove33 to grove, ruffling34 the loose hair on the shoulders of the bears, fanning and rocking young birds in their cradles, making a trumpet35 of every corolla, and carrying their fragrance36 around the world.
In unsettled weather, when storms are growing, the mountain looms37 immensely higher, and its miles of height become apparent to all, especially in the gloom of the gathering38 clouds, or when the storm is done and they are rolling away, torn on the edges and melting while in the sunshine. Slight rainstorms are likely to be encountered in a trip round the mountain, but one may easily find shelter beneath well-thatched trees that shed the rain like a roof. Then the shining of the wet leaves is delightful39, and the steamy fragrance, and the burst of bird song from a multitude of thrushes and finches and warblers that have nests in the chaparral.
The nights, too, are delightful, watching with Shasta beneath the great starry40 dome41. A thousand thousand voices are heard, but so finely blended they seem a part of the night itself, and make a deeper silence. And how grandly do the great logs and branches of your campfire give forth42 the heat and light that during their long century-lives they have so slowly gathered from the sun, storing it away in beautiful dotted cells and beads43 of amber44 gum! The neighboring trees look into the charmed circle as if the noon of another day had come, familiar flowers and grasses that chance to be near seem far more beautiful and impressive than by day, and as the dead trees give forth their light all the other riches of their lives seem to be set free and with the rejoicing flames rise again to the sky. In setting out from Strawberry Valley, by bearing off to the northwestward a few miles you may see
"...beneath dim aisles45, in odorous beds,
The slight Linnaea hang its twin-born heads,
And [bless] the monument of the man of flowers,
Which breathes his sweet fame through the northern bowers46."
This is one of the few places in California where the charming linnaea is found, though it is common to the northward47 through Oregon and Washington. Here, too, you may find the curious but unlovable darlingtonia, a carnivorous plant that devours48 bumblebees, grasshoppers50, ants, moths51, and other insects, with insatiable appetite. In approaching it, its suspicious-looking yellow-spotted hood52 and watchful53 attitude will be likely to make you go cautiously through the bog54 where it stands, as if you were approaching a dangerous snake. It also occurs in a bog near Sothern's Station on the stage road, where I first saw it, and in other similar bogs55 throughout the mountains hereabouts.
The "Big Spring" of the Sacramento is about a mile and a half above Sisson's, issuing from the base of a drift-covered hill. It is lined with emerald algae56 and mosses57, and shaded with alder58, willow59, and thorn bushes, which give it a fine setting. Its waters, apparently60 unaffected by flood or drouth, heat or cold, fall at once into white rapids with a rush and dash, as if glad to escape from the darkness to begin their wild course down the canyon61 to the plain.
Muir's Peak, a few miles to the north of the spring, rises about three thousand feet above the plain on which it stands, and is easily climbed. The view is very fine and well repays the slight walk to its summit, from which much of your way about the mountain may be studied and chosen. The view obtained of the Whitney Glacier should tempt62 you to visit it, since it is the largest of the Shasta glaciers and its lower portion abounds63 in beautiful and interesting cascades64 and crevasses65. It is three or four miles long and terminates at an elevation66 of about nine thousand five hundred feet above sea level, in moraine-sprinkled ice cliffs sixty feet high. The long gray slopes leading up to the glacier seem remarkably67 smooth and unbroken. They are much interrupted, nevertheless, with abrupt68, jagged precipitous gorges70, which though offering instructive sections of the lavas71 for examination, would better be shunned72 by most people. This may be done by keeping well down on the base until fronting the glacier before beginning the ascent73.
The gorge69 through which the glacier is drained is raw-looking, deep and narrow, and indescribably jagged. The walls in many places overhang; in others they are beveled, loose, and shifting where the channel has been eroded74 by cinders75, ashes, strata76 of firm lavas, and glacial drift, telling of many a change from frost to fire and their attendant floods of mud and water. Most of the drainage of the glacier vanishes at once in the porous77 rocks to reappear in springs in the distant valley, and it is only in time of flood that the channel carries much water; then there are several fine falls in the gorge, six hundred feet or more in height. Snow lies in it the year round at an elevation of eight thousand five hundred feet, and in sheltered spots a thousand feet lower. Tracing this wild changing channel-gorge, gully, or canyon, the sections will show Mount Shasta as a huge palimpsest, containing the records, layer upon layer, of strangely contrasted events in its fiery-icy history. But look well to your footing, for the way will test the skill of the most cautious mountaineers.
Regaining78 the low ground at the base of the mountain and holding on in your grand orbit, you pass through a belt of juniper woods, called "The Cedars," to Sheep Rock at the foot of the Shasta Pass. Here you strike the old emigrant road, which leads over the low divide to the eastern slopes of the mountain. In a north-northwesterly direction from the foot of the pass you may chance to find Pluto's Cave, already mentioned; but it is not easily found, since its several mouths are on a level with the general surface of the ground, and have been made simply by the falling-in of portions of the roof. Far the most beautiful and richly furnished of the mountain caves of California occur in a thick belt of metamorphic limestone80 that is pretty generally developed along the western flank of the Sierra from the McCloud River to the Kaweah, a distance of nearly four hundred miles. These volcanic81 caves are not wanting in interest, and it is well to light a pitch pine torch and take a walk in these dark ways of the underworld whenever opportunity offers, if for no other reason to see with new appreciation82 on returning to the sunshine the beauties that lie so thick about us.
Sheep Rock is about twenty miles from Sisson's, and is one of the principal winter pasture grounds of the wild sheep, from which it takes its name. It is a mass of lava presenting to the gray sage83 plain of Shasta Valley a bold craggy front two thousand feet high. Its summit lies at an elevation of five thousand five hundred feet above the sea, and has several square miles of comparatively level surface, where bunchgrass grows and the snow does not lie deep, thus allowing the hardy84 sheep to pick up a living through the winter months when deep snows have driven them down from the lofty ridges of Shasta.
From here it might be well to leave the immediate85 base of the mountain for a few days and visit the Lava Beds made famous by the Modoc War. They lie about forty miles to the northeastward, on the south shore of Rhett or Tule 7 Lake, at an elevation above sea level of about forty-five hundred feet. They are a portion of a flow of dense86 black vesicular lava, dipping northeastward at a low angle, but little changed as yet by the weather, and about as destitute87 of soil as a glacial pavement. The surface, though smooth in a general way as seen from a distance, is dotted with hillocks and rough crater88-like pits, and traversed by a network of yawning fissures89, forming a combination of topographical conditions of very striking character. The way lies by Mount Bremer, over stretches of gray sage plains, interrupted by rough lava slopes timbered with juniper and yellow pine, and with here and there a green meadow and a stream.
This is a famous game region, and you will be likely to meet small bands of antelope90, mule deer, and wild sheep. Mount Bremer is the most noted91 stronghold of the sheep in the whole Shasta region. Large flocks dwell here from year to year, winter and summer, descending92 occasionally into the adjacent sage plains and lava beds to feed, but ever ready to take refuge in the jagged crags of their mountain at every alarm. While traveling with a company of hunters I saw about fifty in one flock.
The Van Bremer brothers, after whom the mountain is named, told me that they once climbed the mountain with their rifles and hounds on a grand hunt; but, after keeping up the pursuit for a week, their boots and clothing gave way, and the hounds were lamed93 and worn out without having run down a single sheep, notwithstanding they ran night and day. On smooth spots, level or ascending94, the hounds gained on the sheep, but on descending ground, and over rough masses of angular rocks they fell hopelessly behind. Only half a dozen sheep were shot as they passed the hunters stationed near their paths circling round the rugged summit. The full-grown bucks96 weigh nearly three hundred and fifty pounds.
The mule deer are nearly as heavy. Their long, massive ears give them a very striking appearance. One large buck95 that I measured stood three feet and seven inches high at the shoulders, and when the ears were extended horizontally the distance across from tip to tip was two feet and one inch.
From the Van Bremer ranch15 the way to the Lava Beds leads down the Bremer Meadows past many a smooth grassy97 knoll98 and jutting99 cliff, along the shore of Lower Klamath Lake, and thence across a few miles of sage plain to the brow of the wall-like bluff100 of lava four hundred and fifty feet above Tule Lake. Here you are looking southeastward, and the Modoc landscape, which at once takes possession of you, lies revealed in front. It is composed of three principal parts; on your left lies the bright expanse of Tule Lake, on your right an evergreen101 forest, and between the two are the black Lava Beds.
When I first stood there, one bright day before sundown, the lake was fairly blooming in purple light, and was so responsive to the sky in both calmness and color it seemed itself a sky. No mountain shore hides its loveliness. It lies wide open for many a mile, veiled in no mystery but the mystery of light. The forest also was flooded with sun-purple, not a spire102 moving, and Mount Shasta was seen towering above it rejoicing in the ineffable103 beauty of the alpenglow. But neither the glorified104 woods on the one hand, nor the lake on the other, could at first hold the eye. That dark mysterious lava plain between them compelled attention. Here you trace yawning fissures, there clusters of somber105 pits; now you mark where the lava is bent106 and corrugated107 in swelling108 ridges and domes109, again where it breaks into a rough mass of loose blocks. Tufts of grass grow far apart here and there and small bushes of hardy sage, but they have a singed110 appearance and can do little to hide the blackness. Deserts are charming to those who know how to see them—all kinds of bogs, barrens, and heathy moors111; but the Modoc Lava Beds have for me an uncanny look. As I gazed the purple deepened over all the landscape. Then fell the gloaming, making everything still more forbidding and mysterious. Then, darkness like death.
Next morning the crisp, sunshiny air made even the Modoc landscape less hopeless, and we ventured down the bluff to the edge of the Lava Beds. Just at the foot of the bluff we came to a square enclosed by a stone wall. This is a graveyard112 where lie buried thirty soldiers, most of whom met their fate out in the Lava Beds, as we learn by the boards marking the graves—a gloomy place to die in, and deadly-looking even without Modocs. The poor fellows that lie here deserve far more pity than they have ever received. Picking our way over the strange ridges and hollows of the beds, we soon came to a circular flat about twenty yards in diameter, on the shore of the lake, where the comparative smoothness of the lava and a few handfuls of soil have caused the grass tufts to grow taller. This is where General Canby was slain113 while seeking to make peace with the treacherous114 Modocs.
Two or three miles farther on is the main stronghold of the Modocs, held by them so long and defiantly115 against all the soldiers that could be brought to the attack. Indians usually choose to hide in tall grass and bush and behind trees, where they can crouch31 and glide116 like panthers, without casting up defenses that would betray their positions; but the Modoc castle is in the rock. When the Yosemite Indians made raids on the settlers of the lower Merced, they withdrew with their spoils into Yosemite Valley; and the Modocs boasted that in case of war they had a stone house into which no white man could come as long as they cared to defend it. Yosemite was not held for a single day against the pursuing troops; but the Modocs held their fort for months, until, weary of being hemmed117 in, they chose to withdraw.
It consists of numerous redoubts formed by the unequal subsidence of portions of the lava flow, and a complicated network of redans abundantly supplied with salient and re-entering angles, being united each to the other and to the redoubts by a labyrinth118 of open and covered corridors, some of which expand at intervals119 into spacious120 caverns121, forming as a whole the most complete natural Gibraltar I ever saw. Other castles scarcely less strong are connected with this by subterranean122 passages known only to the Indians, while the unnatural123 blackness of the rock out of which Nature has constructed these defenses, and the weird124, inhuman125 physiognomy of the whole region are well calculated to inspire terror.
Deadly was the task of storming such a place. The breech-loading rifles of the Indians thrust through chinks between the rocks were ready to pick off every soldier who showed himself for a moment, while the Indians lay utterly126 invisible. They were familiar with byways both over and under ground, and could at any time sink suddenly out of sight like squirrels among the loose boulders127. Our bewildered soldiers heard them shooting, now before, now behind them, as they glided128 from place to place through fissures and subterranean passes, all the while as invisible as Gyges wearing his magic ring. To judge from the few I have seen, Modocs are not very amiable-looking people at best. When, therefore, they were crawling stealthily in the gloomy caverns, unkempt and begrimed and with the glare of war in their eyes, they must have seemed very demons129 of the volcanic pit.
Captain Jack's cave is one of the many somber cells of the castle. It measures twenty-five or thirty feet in diameter at the entrance, and extends but a short distance in a horizontal direction. The floor is littered with the bones of the animals slaughtered130 for food during the war. Some eager archaeologist may hereafter discover this cabin and startle his world by announcing another of the Stone Age caves. The sun shines freely into its mouth, and graceful131 bunches of grass and eriogonums and sage grow about it, doing what they can toward its redemption from degrading associations and making it beautiful.
Where the lava meets the lake there are some fine curving bays, beautifully embroidered132 with rushes and polygonums, a favorite resort of waterfowl. On our return, keeping close along shore, we caused a noisy plashing and beating of wings among cranes and geese. The ducks, less wary133, kept their places, merely swimming in and out through openings in the rushes, rippling134 the glassy water, and raising spangles in their wake. The countenance135 of the lava beds became less and less forbidding. Tufts of pale grasses, relieved on the jet rocks, looked like ornaments136 on a mantel, thick-furred mats of emerald mosses appeared in damp spots next the shore, and I noticed one tuft of small ferns. From year to year in the kindly137 weather the beds are thus gathering beauty—beauty for ashes.
Returning to Sheep Rock and following the old emigrant road, one is soon back again beneath the snows and shadows of Shasta, and the Ash Creek138 and McCloud Glaciers come into view on the east side of the mountain. They are broad, rugged, crevassed cloudlike masses of down-grinding ice, pouring forth streams of muddy water as measures of the work they are doing in sculpturing the rocks beneath them; very unlike the long, majestic139 glaciers of Alaska that riverlike go winding140 down the valleys through the forests to the sea. These, with a few others as yet nameless, are lingering remnants of once great glaciers that occupied the canyons141 now taken by the rivers, and in a few centuries will, under present conditions, vanish altogether.
The rivers of the granite142 south half of the Sierra are outspread on the peaks in a shining network of small branches, that divide again and again into small dribbling143, purling, oozing144 threads drawing their sources from the snow and ice of the surface. They seldom sink out of sight, save here and there in the moraines or glaciers, or, early in the season, beneath the banks and bridges of snow, soon to issue again. But in the north half, laden145 with rent and porous lava, small tributary146 streams are rare, and the rivers, flowing for a time beneath the sky of rock, at length burst forth into the light in generous volume from seams and caverns, filtered, cool, and sparkling, as if their bondage147 in darkness, safe from the vicissitudes148 of the weather in their youth, were only a blessing2.
Only a very small portion of the water derived149 from the melting ice and snow of Shasta flows down its flanks on the surface. Probably ninety-nine per cent of it is at once absorbed and drained away beneath the porous lava-folds of the mountain to gush150 forth, filtered and pure, in the form of immense springs, so large, some of them, that they give birth to rivers that start on their journey beneath the sun, full-grown and perfect without any childhood. Thus the Shasta River issues from a large lake-like spring in Shasta Valley, and about two thirds of the volume of the McCloud gushes151 forth in a grand spring on the east side of the mountain, a few miles back from its immediate base.
To find the big spring of the McCloud, or "Mud Glacier," which you will know by its size (it being the largest on the east side), you make your way through sunny, parklike woods of yellow pine, and a shaggy growth of chaparral, and come in a few hours to the river flowing in a gorge of moderate depth, cut abruptly152 down into the lava plain. Should the volume of the stream where you strike it seem small, then you will know that you are above the spring; if large, nearly equal to its volume at its confluence153 with the Pitt River, then you are below it; and in either case have only to follow the river up or down until you come to it.
Under certain conditions you may hear the roar of the water rushing from the rock at a distance of half a mile, or even more; or you may not hear it until within a few rods. It comes in a grand, eager gush from a horizontal seam in the face of the wall of the river gorge in the form of a partially154 interrupted sheet nearly seventy-five yards in width, and at a height above the riverbed of about forty feet, as nearly as I could make out without the means of exact measurement. For about fifty yards this flat current is in one unbroken sheet, and flows in a lacework of plashing, upleaping spray over boulders that are clad in green silky algae and water mosses to meet the smaller part of the river, which takes its rise farther up. Joining the river at right angles to its course, it at once swells155 its volume to three times its size above the spring.
The vivid green of the boulders beneath the water is very striking, and colors the entire stream with the exception of the portions broken into foam156. The color is chiefly due to a species of algae which seems common in springs of this sort. That any kind of plant can hold on and grow beneath the wear of so boisterous157 a current seems truly wonderful, even after taking into consideration the freedom of the water from cutting drift, and the constance of its volume and temperature throughout the year. The temperature is about 45 degrees, and the height of the river above the sea is here about three thousand feet. Asplenium, epilobium, heuchera, hazel, dogwood, and alder make a luxurious158 fringe and setting; and the forests of Douglas spruce along the banks are the finest I have ever seen in the Sierra.
From the spring you may go with the river—a fine traveling companion—down to the sportsman's fishing station, where, if you are getting hungry, you may replenish159 your stores; or, bearing off around the mountain by Huckleberry Valley, complete your circuit without interruption, emerging at length from beneath the outspread arms of the sugar pine at Strawberry Valley, with all the new wealth and health gathered in your walk; not tired in the least, and only eager to repeat the round.
Tracing rivers to their fountains makes the most charming of travels. As the life-blood of the landscapes, the best of the wilderness160 comes to their banks, and not one dull passage is found in all their eventful histories. Tracing the McCloud to its highest springs, and over the divide to the fountains of Fall River, near Fort Crook161, thence down that river to its confluence with the Pitt, on from there to the volcanic region about Lassen's Butte, through the Big Meadows among the sources of the Feather River, and down through forests of sugar pine to the fertile plains of Chico—this is a glorious saunter and imposes no hardship. Food may be had at moderate intervals, and the whole circuit forms one ever-deepening, broadening stream of enjoyment162.
Fall River is a very remarkable163 stream. It is only about ten miles long, and is composed of springs, rapids, and falls—springs beautifully shaded at one end of it, a showy fall one hundred and eighty feet high at the other, and a rush of crystal rapids between. The banks are fringed with rubus, rose, plum cherry, spiraea, azalea, honeysuckle, hawthorn164, ash, alder, elder, aster79, goldenrod, beautiful grasses, sedges, rushes, mosses, and ferns with fronds165 as large as the leaves of palms—all in the midst of a richly forested landscape. Nowhere within the limits of California are the forests of yellow pine so extensive and exclusive as on the headwaters of the Pitt. They cover the mountains and all the lower slopes that border the wide, open valleys which abound there, pressing forward in imposing166 ranks, seemingly the hardiest167 and most firmly established of all the northern coniferae.
The volcanic region about Lassen's Butte I have already in part described. Miles of its flanks are dotted with hot springs, many of them so sulphurous and boisterous and noisy in their boiling that they seem inclined to become geysers like those of the Yellowstone.
The ascent of Lassen's Butte is an easy walk, and the views from the summit are extremely telling. Innumerable lakes and craters168 surround the base; forests of the charming Williamson spruce fringe lake and crater alike; the sunbeaten plains to east and west make a striking show, and the wilderness of peaks and ridges stretch indefinitely away on either hand. The lofty, icy Shasta, towering high above all, seems but an hour's walk from you, though the distance in an air-line is about sixty miles.
The "Big Meadows" lie near the foot of Lassen's Butte, a beautiful spacious basin set in the heart of the richly forested mountains, scarcely surpassed in the grandeur169 of its surroundings by Tahoe. During the Glacial Period it was a mer de glace, then a lake, and now a level meadow shining with bountiful springs and streams. In the number and size of its big spring fountains it excels even Shasta. One of the largest that I measured forms a lakelet nearly a hundred yards in diameter, and, in the generous flood it sends forth offers one of the most telling symbols of Nature's affluence170 to be found in the mountains.
The great wilds of our country, once held to be boundless171 and inexhaustible, are being rapidly invaded and overrun in every direction, and everything destructible in them is being destroyed. How far destruction may go it is not easy to guess. Every landscape, low and high, seems doomed172 to be trampled173 and harried174. Even the sky is not safe from scath—blurred and blackened whole summers together with the smoke of fires that devour49 the woods.
The Shasta region is still a fresh unspoiled wilderness, accessible and available for travelers of every kind and degree. Would it not then be a fine thing to set it apart like the Yellowstone and Yosemite as a National Park for the welfare and benefit of all mankind, preserving its fountains and forests and all its glad life in primeval beauty? Very little of the region can ever be more valuable for any other use—certainly not for gold nor for grain. No private right or interest need suffer, and thousands yet unborn would come from far and near and bless the country for its wise and benevolent175 forethought.
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1 blessings | |
n.(上帝的)祝福( blessing的名词复数 );好事;福分;因祸得福 | |
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2 blessing | |
n.祈神赐福;祷告;祝福,祝愿 | |
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3 adventurous | |
adj.爱冒险的;惊心动魄的,惊险的,刺激的 | |
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4 bounties | |
(由政府提供的)奖金( bounty的名词复数 ); 赏金; 慷慨; 大方 | |
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5 compensate | |
vt.补偿,赔偿;酬报 vi.弥补;补偿;抵消 | |
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6 morbid | |
adj.病的;致病的;病态的;可怕的 | |
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7 solitudes | |
n.独居( solitude的名词复数 );孤独;荒僻的地方;人迹罕至的地方 | |
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8 elk | |
n.麋鹿 | |
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9 emigrant | |
adj.移居的,移民的;n.移居外国的人,移民 | |
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10 wagons | |
n.四轮的运货马车( wagon的名词复数 );铁路货车;小手推车 | |
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11 zigzags | |
n.锯齿形的线条、小径等( zigzag的名词复数 )v.弯弯曲曲地走路,曲折地前进( zigzag的第三人称单数 ) | |
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12 glaciers | |
冰河,冰川( glacier的名词复数 ) | |
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13 glacier | |
n.冰川,冰河 | |
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14 fronded | |
前移的 | |
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15 ranch | |
n.大牧场,大农场 | |
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16 abound | |
vi.大量存在;(in,with)充满,富于 | |
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17 quail | |
n.鹌鹑;vi.畏惧,颤抖 | |
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18 grouse | |
n.松鸡;v.牢骚,诉苦 | |
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19 mule | |
n.骡子,杂种,执拗的人 | |
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20 revolving | |
adj.旋转的,轮转式的;循环的v.(使)旋转( revolve的现在分词 );细想 | |
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21 cone | |
n.圆锥体,圆锥形东西,球果 | |
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22 rugged | |
adj.高低不平的,粗糙的,粗壮的,强健的 | |
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23 crumbling | |
adj.摇摇欲坠的 | |
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24 ridges | |
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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25 lava | |
n.熔岩,火山岩 | |
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26 aglow | |
adj.发亮的;发红的;adv.发亮地 | |
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27 rosy | |
adj.美好的,乐观的,玫瑰色的 | |
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28 ineffably | |
adv.难以言喻地,因神圣而不容称呼地 | |
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29 appreciable | |
adj.明显的,可见的,可估量的,可觉察的 | |
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30 crouching | |
v.屈膝,蹲伏( crouch的现在分词 ) | |
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31 crouch | |
v.蹲伏,蜷缩,低头弯腰;n.蹲伏 | |
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32 sifting | |
n.筛,过滤v.筛( sift的现在分词 );筛滤;细查;详审 | |
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33 grove | |
n.林子,小树林,园林 | |
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34 ruffling | |
弄皱( ruffle的现在分词 ); 弄乱; 激怒; 扰乱 | |
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35 trumpet | |
n.喇叭,喇叭声;v.吹喇叭,吹嘘 | |
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36 fragrance | |
n.芬芳,香味,香气 | |
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37 looms | |
n.织布机( loom的名词复数 )v.隐约出现,阴森地逼近( loom的第三人称单数 );隐约出现,阴森地逼近 | |
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38 gathering | |
n.集会,聚会,聚集 | |
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39 delightful | |
adj.令人高兴的,使人快乐的 | |
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40 starry | |
adj.星光照耀的, 闪亮的 | |
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41 dome | |
n.圆屋顶,拱顶 | |
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42 forth | |
adv.向前;向外,往外 | |
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43 beads | |
n.(空心)小珠子( bead的名词复数 );水珠;珠子项链 | |
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44 amber | |
n.琥珀;琥珀色;adj.琥珀制的 | |
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45 aisles | |
n. (席位间的)通道, 侧廊 | |
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46 bowers | |
n.(女子的)卧室( bower的名词复数 );船首锚;阴凉处;鞠躬的人 | |
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47 northward | |
adv.向北;n.北方的地区 | |
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48 devours | |
吞没( devour的第三人称单数 ); 耗尽; 津津有味地看; 狼吞虎咽地吃光 | |
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49 devour | |
v.吞没;贪婪地注视或谛听,贪读;使着迷 | |
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50 grasshoppers | |
n.蚱蜢( grasshopper的名词复数 );蝗虫;蚂蚱;(孩子)矮小的 | |
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51 moths | |
n.蛾( moth的名词复数 ) | |
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52 hood | |
n.头巾,兜帽,覆盖;v.罩上,以头巾覆盖 | |
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53 watchful | |
adj.注意的,警惕的 | |
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54 bog | |
n.沼泽;室...陷入泥淖 | |
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55 bogs | |
n.沼泽,泥塘( bog的名词复数 );厕所v.(使)陷入泥沼, (使)陷入困境( bog的第三人称单数 );妨碍,阻碍 | |
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56 algae | |
n.水藻,海藻 | |
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57 mosses | |
n. 藓类, 苔藓植物 名词moss的复数形式 | |
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58 alder | |
n.赤杨树 | |
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59 willow | |
n.柳树 | |
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60 apparently | |
adv.显然地;表面上,似乎 | |
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61 canyon | |
n.峡谷,溪谷 | |
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62 tempt | |
vt.引诱,勾引,吸引,引起…的兴趣 | |
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63 abounds | |
v.大量存在,充满,富于( abound的第三人称单数 ) | |
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64 cascades | |
倾泻( cascade的名词复数 ); 小瀑布(尤指一连串瀑布中的一支); 瀑布状物; 倾泻(或涌出)的东西 | |
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65 crevasses | |
n.破口,崩溃处,裂缝( crevasse的名词复数 ) | |
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66 elevation | |
n.高度;海拔;高地;上升;提高 | |
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67 remarkably | |
ad.不同寻常地,相当地 | |
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68 abrupt | |
adj.突然的,意外的;唐突的,鲁莽的 | |
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69 gorge | |
n.咽喉,胃,暴食,山峡;v.塞饱,狼吞虎咽地吃 | |
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70 gorges | |
n.山峡,峡谷( gorge的名词复数 );咽喉v.(用食物把自己)塞饱,填饱( gorge的第三人称单数 );作呕 | |
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71 lavas | |
n.(火山喷发的)熔岩( lava的名词复数 );(熔岩冷凝后的)火山岩 | |
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72 shunned | |
v.避开,回避,避免( shun的过去式和过去分词 ) | |
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73 ascent | |
n.(声望或地位)提高;上升,升高;登高 | |
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74 eroded | |
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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75 cinders | |
n.煤渣( cinder的名词复数 );炭渣;煤渣路;煤渣跑道 | |
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76 strata | |
n.地层(复数);社会阶层 | |
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77 porous | |
adj.可渗透的,多孔的 | |
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78 regaining | |
复得( regain的现在分词 ); 赢回; 重回; 复至某地 | |
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79 aster | |
n.紫菀属植物 | |
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80 limestone | |
n.石灰石 | |
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81 volcanic | |
adj.火山的;象火山的;由火山引起的 | |
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82 appreciation | |
n.评价;欣赏;感谢;领会,理解;价格上涨 | |
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83 sage | |
n.圣人,哲人;adj.贤明的,明智的 | |
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84 hardy | |
adj.勇敢的,果断的,吃苦的;耐寒的 | |
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85 immediate | |
adj.立即的;直接的,最接近的;紧靠的 | |
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86 dense | |
a.密集的,稠密的,浓密的;密度大的 | |
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87 destitute | |
adj.缺乏的;穷困的 | |
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88 crater | |
n.火山口,弹坑 | |
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89 fissures | |
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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90 antelope | |
n.羚羊;羚羊皮 | |
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91 noted | |
adj.著名的,知名的 | |
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92 descending | |
n. 下行 adj. 下降的 | |
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93 lamed | |
希伯莱语第十二个字母 | |
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94 ascending | |
adj.上升的,向上的 | |
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95 buck | |
n.雄鹿,雄兔;v.马离地跳跃 | |
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96 bucks | |
n.雄鹿( buck的名词复数 );钱;(英国十九世纪初的)花花公子;(用于某些表达方式)责任v.(马等)猛然弓背跃起( buck的第三人称单数 );抵制;猛然震荡;马等尥起后蹄跳跃 | |
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97 grassy | |
adj.盖满草的;长满草的 | |
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98 knoll | |
n.小山,小丘 | |
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99 jutting | |
v.(使)突出( jut的现在分词 );伸出;(从…)突出;高出 | |
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100 bluff | |
v.虚张声势,用假象骗人;n.虚张声势,欺骗 | |
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101 evergreen | |
n.常青树;adj.四季常青的 | |
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102 spire | |
n.(教堂)尖顶,尖塔,高点 | |
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103 ineffable | |
adj.无法表达的,不可言喻的 | |
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104 glorified | |
美其名的,变荣耀的 | |
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105 somber | |
adj.昏暗的,阴天的,阴森的,忧郁的 | |
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106 bent | |
n.爱好,癖好;adj.弯的;决心的,一心的 | |
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107 corrugated | |
adj.波纹的;缩成皱纹的;波纹面的;波纹状的v.(使某物)起皱褶(corrugate的过去式和过去分词) | |
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108 swelling | |
n.肿胀 | |
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109 domes | |
n.圆屋顶( dome的名词复数 );像圆屋顶一样的东西;圆顶体育场 | |
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110 singed | |
v.浅表烧焦( singe的过去式和过去分词 );(毛发)燎,烧焦尖端[边儿] | |
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111 moors | |
v.停泊,系泊(船只)( moor的第三人称单数 ) | |
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112 graveyard | |
n.坟场 | |
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113 slain | |
杀死,宰杀,杀戮( slay的过去分词 ); (slay的过去分词) | |
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114 treacherous | |
adj.不可靠的,有暗藏的危险的;adj.背叛的,背信弃义的 | |
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115 defiantly | |
adv.挑战地,大胆对抗地 | |
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116 glide | |
n./v.溜,滑行;(时间)消逝 | |
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117 hemmed | |
缝…的褶边( hem的过去式和过去分词 ); 包围 | |
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118 labyrinth | |
n.迷宫;难解的事物;迷路 | |
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119 intervals | |
n.[军事]间隔( interval的名词复数 );间隔时间;[数学]区间;(戏剧、电影或音乐会的)幕间休息 | |
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120 spacious | |
adj.广阔的,宽敞的 | |
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121 caverns | |
大山洞,大洞穴( cavern的名词复数 ) | |
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122 subterranean | |
adj.地下的,地表下的 | |
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123 unnatural | |
adj.不自然的;反常的 | |
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124 weird | |
adj.古怪的,离奇的;怪诞的,神秘而可怕的 | |
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125 inhuman | |
adj.残忍的,不人道的,无人性的 | |
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126 utterly | |
adv.完全地,绝对地 | |
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127 boulders | |
n.卵石( boulder的名词复数 );巨砾;(受水或天气侵蚀而成的)巨石;漂砾 | |
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128 glided | |
v.滑动( glide的过去式和过去分词 );掠过;(鸟或飞机 ) 滑翔 | |
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129 demons | |
n.恶人( demon的名词复数 );恶魔;精力过人的人;邪念 | |
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130 slaughtered | |
v.屠杀,杀戮,屠宰( slaughter的过去式和过去分词 ) | |
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131 graceful | |
adj.优美的,优雅的;得体的 | |
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132 embroidered | |
adj.绣花的 | |
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133 wary | |
adj.谨慎的,机警的,小心的 | |
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134 rippling | |
起涟漪的,潺潺流水般声音的 | |
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135 countenance | |
n.脸色,面容;面部表情;vt.支持,赞同 | |
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136 ornaments | |
n.装饰( ornament的名词复数 );点缀;装饰品;首饰v.装饰,点缀,美化( ornament的第三人称单数 ) | |
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137 kindly | |
adj.和蔼的,温和的,爽快的;adv.温和地,亲切地 | |
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138 creek | |
n.小溪,小河,小湾 | |
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139 majestic | |
adj.雄伟的,壮丽的,庄严的,威严的,崇高的 | |
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140 winding | |
n.绕,缠,绕组,线圈 | |
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141 canyons | |
n.峡谷( canyon的名词复数 ) | |
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142 granite | |
adj.花岗岩,花岗石 | |
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143 dribbling | |
n.(燃料或油从系统内)漏泄v.流口水( dribble的现在分词 );(使液体)滴下或作细流;运球,带球 | |
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144 oozing | |
v.(浓液等)慢慢地冒出,渗出( ooze的现在分词 );使(液体)缓缓流出;(浓液)渗出,慢慢流出 | |
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145 laden | |
adj.装满了的;充满了的;负了重担的;苦恼的 | |
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146 tributary | |
n.支流;纳贡国;adj.附庸的;辅助的;支流的 | |
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147 bondage | |
n.奴役,束缚 | |
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148 vicissitudes | |
n.变迁,世事变化;变迁兴衰( vicissitude的名词复数 );盛衰兴废 | |
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149 derived | |
vi.起源;由来;衍生;导出v.得到( derive的过去式和过去分词 );(从…中)得到获得;源于;(从…中)提取 | |
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150 gush | |
v.喷,涌;滔滔不绝(说话);n.喷,涌流;迸发 | |
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151 gushes | |
n.涌出,迸发( gush的名词复数 )v.喷,涌( gush的第三人称单数 );滔滔不绝地说话 | |
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152 abruptly | |
adv.突然地,出其不意地 | |
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153 confluence | |
n.汇合,聚集 | |
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154 partially | |
adv.部分地,从某些方面讲 | |
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155 swells | |
增强( swell的第三人称单数 ); 肿胀; (使)凸出; 充满(激情) | |
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156 foam | |
v./n.泡沫,起泡沫 | |
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157 boisterous | |
adj.喧闹的,欢闹的 | |
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158 luxurious | |
adj.精美而昂贵的;豪华的 | |
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159 replenish | |
vt.补充;(把…)装满;(再)填满 | |
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160 wilderness | |
n.杳无人烟的一片陆地、水等,荒漠 | |
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161 crook | |
v.使弯曲;n.小偷,骗子,贼;弯曲(处) | |
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162 enjoyment | |
n.乐趣;享有;享用 | |
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163 remarkable | |
adj.显著的,异常的,非凡的,值得注意的 | |
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164 hawthorn | |
山楂 | |
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165 fronds | |
n.蕨类或棕榈类植物的叶子( frond的名词复数 ) | |
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166 imposing | |
adj.使人难忘的,壮丽的,堂皇的,雄伟的 | |
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167 hardiest | |
能吃苦耐劳的,坚强的( hardy的最高级 ); (植物等)耐寒的 | |
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168 craters | |
n.火山口( crater的名词复数 );弹坑等 | |
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169 grandeur | |
n.伟大,崇高,宏伟,庄严,豪华 | |
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170 affluence | |
n.充裕,富足 | |
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171 boundless | |
adj.无限的;无边无际的;巨大的 | |
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172 doomed | |
命定的 | |
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173 trampled | |
踩( trample的过去式和过去分词 ); 践踏; 无视; 侵犯 | |
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174 harried | |
v.使苦恼( harry的过去式和过去分词 );不断烦扰;一再袭击;侵扰 | |
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175 benevolent | |
adj.仁慈的,乐善好施的 | |
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