问题 写作题

阅读下面的文字,按要求作文。

总有一些事、一些人让我们难以忘怀:或许只是一声轻轻的问候,就在自己的心头荡起了层层涟漪;或许只是琐屑到举手之劳,似乎不值一提,但走过多少个日子,依然温馨满怀……请以“那一次,让我铭记”为题,写一篇600字以上的记叙文。

要求:(1)立意正确,中心突出。(2)叙事具体,在记叙中有适当的抒情和议论。(3)文中不得出现真实的校名、人名。

答案

参考例文:

那一次,让我铭记

世界上有这么一种纯真美好的笑容,哪怕在最寒冷的冬天,也能送来初春的暖意。

她对于我,只能算陌生人,我甚至连她的名字都不知道!

我从小就爱跑,水泥地上跑,草地上跑,沙地上也跑……

大概是我二年级的时候,那时海天学校的大操场还没改建,我就经常在操场地疯跑。

有一回,我跑得正疯,没留意脚下碎石,一不小心就被一块有棱有角的大石头绊倒了。脚底下是沙地,一摔倒,破皮流血是难免的。腿受伤了,手受伤。沙子和一些小石子贴在伤口上,一开始只是火辣辣的痛,不一会儿就变成刺骨的痛。伤口的血溢开了,操场上却一人也没有,无助又年幼的我只能在原地大哭:“呜呜呜……”我害怕极了,虽然小,我也懂得死亡的含义,妈妈说血流多了就会死,我不会就这样死掉吧,我还没好好享受生活呢!想到这儿,我更伤心了,眼泪更是抑制不住地涌出来。

“咚——咚——”我突然听见了脚步声。“摔了就站起来呀。”我听见了一个柔和的女生。脚步声越来越近,最后停在我身边消失。我抬起满是泪痕的脸,朦胧中看到一个挺清秀的大姐姐。大姐姐弯下腰,轻轻递给我一张纸:“女孩子也不能这么娇气呀,摔伤了怕什么,回家擦药就好了。不可以再这么软弱地哭了,知道吗?”咦,回家擦药就好了吗?这个姐姐是谁呀?想着想着,我从哭泣变成抽咽,被泪水弄模糊的眼睛也开始明亮。大姐姐给了我一个甜甜的笑:“这就对了。”这一定是天使的笑容吧,简单美好,充满了善意,时间凝固在瞬间,笑容的温暖抚平了伤口,伤口似乎没有那么痛了……

我还沉侵在美好中,大姐姐就轻轻把纸巾放入我的掌心,留下一个轻轻的笑容,一转身,帅气地离开了我的视线……

那一次,让我铭记。我忘不掉那美好的笑,忘不掉这笑容带着的初春的暖。忘不掉那个姐姐,如果能再遇到她,我一定能认出她的笑容。

忘不掉的瞬间,就是那微笑的温暖!

题目分析:命题从学生的生活实际出发,贴近生活,立足于考察学生的生活积累,以及对生活的思考与感悟,也就是说对学生的生活是开放的。

这一题目继续坚持了鼓励考生写记叙文的导向,要求考生叙写真实的生活经历,抒发真挚的情感,表达真切的感受。可以写写人叙事类,也可以写成文质兼美的写景抒情、托物言志散文。

当然,这个命题看似简单平易,其中的限制也是不容忽视的。

“那一次,让我铭记”中的“一次”、“我”、“铭记”又起到了限制作用。无论选写什么文体,都要重点突出“铭记”在文中的作用,这次让我铭记的事情对自己的成长产生了怎样的影响,给了自己怎样的感悟和启示。考生要能做出真情的表达,深刻的阐述。“我”、“一次”在经历的主体上、数量上做出了要求。这一过程中需要落实具体的叙述、细致的描写。在考生的实际生活中有许多可以选用的素材,但是由于题目中的一些限定,还是要精心选择,谨慎运用的。

单项选择题 A1/A2型题
问答题


Directions: Read the following passage carefully and then translate the underlined sentences into Chinese and write your translation on the ANSWER SHEET.
Tsunamis are impulsively generated sea waves by a disturbance to or near the ocean.
21. Earthquakes, submarine volcanic explosions, landslides and the detonation of nuclear devices near the sea can give rise to such destructive sea waves. By far the most destructive tsunamis are generated from large shallow-focus earthquakes with an epicenter or fault line near or in the ocean. Vertical displacements of the earth’s crust along the rupture resulting from the ocean. Vertical displacements of the earth’s crust along the rupture resulting from such earthquakes can generate destructive tsunami waves which can travel across an ocean spreading destruction across their path. Similar displacements of the ocean floor can also be produced by volcanic eruptions and submarine avalanches or landslides. However, these sources are considered as point sources and, although the tsunami waves generated can be very destructive locally, the energy of the waves is rapidly dissipated as they travel across the ocean.
To forecast tsunamis and determine terminal run-up and destructiveness, one must be able to evaluate the parameters of the tsunami source mechanism in real time, often, from inadequate date. 22. Tsunami source mechanism analysis is difficult given the time constraints of a warning situation. It will suffice to say that forecasting the run-up and potential destructiveness of a tsunami at a distant shore will depend greatly on determining the seismic parameters of the source location such as magnitude of the earthquake, its depth, its orientation, the length of the fault line, the size of the crustal displacements, and depth of the water. 23. Refraction(折射) and diffraction(衍射) processes will affect the energy and height of the tsunami waves as they travel across the ocean. These effects must also be determined. Finally, terminal height, run-up, and inundation of the tsunami at a point of impact will depend upon the energy forcusing effect, the travel path of the waves, the coastal configuration, and the offshore bathymetry, only to name a few.
Tsunami run-up is the vertical distance between the maximum height reached by the water on shore and the mean-sea-level surface. 24. Contrary to meteorological predictions, tsunami run-up, the final product of earthquake and tsunami investigations is not possible to forecast with a great degree of accuracy. The reason for this inadequacy is that the Tsunami Warning System works in a real time frame of short duration, often with inadequate date and information. Problems of communication and lack of sufficient station density, often complicate the process. Forecasting tsunamis requires adequate understanding of the phenomenon, good and expeditious collection of earthquake and sea level date, and accruate and expeditious assessment and interpretation of this data.