31 British Columbia

British Columbia is the third largest Canadian provinces, both in area and population. It is nearly 1.5 times as large as Texas, and extends 800 miles(1,280km) north from the United States border. It includes Canada's entire west coast and the islands just off the coast. 

Most of British Columbia is mountainous, with long rugged¹ ranges running north and south. Even the coastal² islands are the remains³ of a mountain range that existed thousands of years ago. During the last Ice Age, this range was scoured⁴ by glaciers⁵ until most of it was beneath the sea. Its peaks now show as islands scattered⁶ along the coast.

The southwestern coastal region has a humid mild marine⁷ climate. Sea winds that blow inland from the west are warmed by a current of warm water that flows through the Pacific Ocean. As a result, winter temperatures average above freezing and summers are mild. These warm western winds also carry moisture from the ocean.

Inland from the coast, the winds from the Pacific meet the mountain barriers of the coastal ranges and the Rocky Mountains. As they rise to cross the mountains, the winds are cooled, and their moisture begins to fall as rain. On some of the western slopes almost 200 inches (500cm) of rain fall each year.

More than half of British Columbia is heavily forested. On mountain slopes that receive plentiful⁸ rainfall, huge Douglas firs rise in towering columns. These forest giants often grow to be as much as 300 feet(90m) tall, with diameters up to 10 feet(3m). More lumber⁹ is produced from these trees than from any other kind of tree in North America. Hemlock¹⁰, red cedar¹¹, and balsam fir are among the other trees found in British Columbia.


32 Botany 

Botany, the study of plants, occupies a peculiar¹² position in the history of human knowledge. For many thousands of years it was the one field of awareness¹³ about which humans had anything more than the vaguest of insights. It is impossible to know today just what our Stone Age ancestors knew about plants, but form what we can observe of pre-industrial societies that still exist a detailed¹⁴ learning of plants and their properties must be extremely ancient. This is logical. Plants are the basis of the food pyramid for all living things even for other plants. They have always been enormously important to the welfare of people not only for food, but also for clothing, weapons, tools, dyes, medicines, shelter, and a great many other purposes. Tribes living today in the jungles of the Amazon recognize literally¹⁵ hundreds of plants and know many properties of each. To them, botany, as such, has no name and is probably not even recognized as a special branch of " knowledge" at all.

Unfortunately, the more industrialized we become the farther away we move from direct contact with plants, and the less distinct our knowledge of botany grows. Yet everyone comes unconsciously on an amazing amount of botanical knowledge, and few people will fail to recognize a rose, an apple, or an orchid¹⁶. When our Neolithic¹⁷ ancestors, living in the Middle East about 10,000 years ago, discovered that certain grasses could be harvested and their seeds planted for richer yields the next season the first great step in a new association of plants and humans was taken. Grains were discovered and from them flowed the marvel¹⁸ of agriculture: cultivated crops. From then on, humans would increasingly take their living from the controlled production of a few plants, rather than getting a little here and a little there from many varieties that grew wild- and the accumulated knowledge of tens of thousands of years of experience and intimacy¹⁹ with plants in the wild would begin to fade away.


33 Plankton²⁰浮游生物. / 'plжηktэn; `plжηktэn/

Scattered through the seas of the world are billions of tons of small plants and animals called plankton. Most of these plants and animals are too small for the human eye to see. They drift about lazily with the currents, providing a basic food for many larger animals.

Plankton has been described as the equivalent of the grasses that grow on the dry land continents, and the comparison is an appropriate one. In potential food value, however, plankton far outweighs²² that of the land grasses. One scientist has estimated that while grasses of the world produce about 49 billion tons of valuable carbohydrates²³ each year, the sea's plankton generates more than twice as much.

Despite its enormous food potential, little effect was made until recently to farm plankton as we farm grasses on land. Now marine scientists have at last begun to study this possibility, especially as the sea's resources loom²⁴ even more important as a means of feeding an expanding world population.

No one yet has seriously suggested that " plankton-burgers" may soon become popular around the world. As a possible farmed supplementary²⁵ food source, however, plankton is gaining considerable interest among marine scientists.

One type of plankton that seems to have great harvest possibilities is a tiny shrimp-like creature called krill. Growing to two or three inches long, krill provides the major food for the great blue whale, the largest animal to ever inhabit the Earth. Realizing that this whale may grow to 100 feet and weigh 150 tons at maturity²⁶, it is not surprising that each one devours²⁷ more than one ton of krill daily.


34 Raising Oysters²⁹

In the oysters were raised in much the same way as dirt farmers raised tomatoes- by transplanting them. First, farmers selected the oyster²⁸ bed, cleared the bottom of old shells and other debris³⁰, then scattered clean shells about. Next, they "planted" fertilized³¹ oyster eggs, which within two or three weeks hatched into larvae³². The larvae drifted until they attached themselves to the clean shells on the bottom. There they remained and in time grew into baby oysters called seed or spat³³. The spat grew larger by drawing in seawater from which they derived³⁴ microscopic³⁵ particles of food. Before long, farmers gathered the baby oysters, transplanted them once more into another body of water to fatten³⁶ them up.

Until recently the supply of wild oysters and those crudely farmed were more than enough to satisfy people's needs. But today the delectable³⁷ seafood³⁸ is no longer available in abundance. The problem has become so serious that some oyster beds have vanished entirely³⁹.

Fortunately, as far back as the early 1900's marine biologists realized that if new measures were not taken, oysters would become extinct or at best a luxury food. So they set up well-equipped hatcheries and went to work. But they did not have the proper equipment or the skill to handle the eggs. They did not know when, what, and how to feed the larvae. And they knew little about the predators⁴⁰ that attack and eat baby oysters by the millions. They failed, but they doggedly⁴¹ kept at it. Finally, in the 1940's a significant breakthrough was made.

The marine biologists discovered that by raising the temperature of the water, they could induce oysters to spawn⁴² not only in the summer but also in the fall, winter, and spring. Later they developed a technique for feeding the larvae and rearing them to spat. Going still further, they succeeded in breeding new strains that were resistant⁴³ to diseases, grew faster and larger, and flourished in water of different salinities and temperatures. In addition, the cultivated oysters tasted better!


35.Oil Refining

An important new industry, oil refining, grew after the Civil war. Crude oil, or petroleum⁴⁴ - a dark, thick ooze⁴⁵ from the earth - had been known for hundreds of years, but little use had ever been made of it. In the 1850's Samuel M. Kier, a manufacturer in western Pennsylvania, began collecting the oil from local seepages and refining it into kerosene⁴⁶. Refining, like smelting⁴⁷, is a process of removing impurities⁴⁸ from a raw material.

Kerosene was used to light lamps. It was a cheap substitute for whale oil, which was becoming harder to get. Soon there was a large demand for kerosene. People began to search for new supplies of petroleum.

The first oil well was drilled by E.L. Drake, a retired⁴⁹ railroad conductor. In 1859 he began drilling in Titusville, Pennsylvania. The whole venture seemed so impractical⁵⁰ and foolish that onlookers⁵¹ called it " Drake's Folly⁵²". But when he had drilled down about 70 feet(21 meters), Drake struck oil. His well began to yield 20 barrels of crude oil a day.

News of Drake's success brought oil prospectors⁵³ to the scene. By the early 1860's these wildcatters were drilling for " black gold" all over western Pennsylvania. The boom rivaled the California gold rush of 1848 in its excitement and Wild West atmosphere. And it brought far more wealth to the prospectors than any gold rush.

Crude oil could be refined into many products. For some years kerosene continued to be the principal one. It was sold in grocery stores and door-to-door. In the 1880's refiners learned how to make other petroleum products such as waxes and lubricating oils. Petroleum was not then used to make gasoline or heating oil.


36.Plate Tectonics and Sea-floor Spreading

The theory of plate tectonics describes the motions of the lithosphere⁵⁴, the comparatively rigid⁵⁵ outer layer of the Earth that includes all the crust and part of the underlying⁵⁶ mantle⁵⁷. The lithosphere(n.[地]岩石圈)is divided into a few dozen plates of various sizes and shapes, in general the plates are in motion with respect to one another. A mid-ocean ridge⁵⁸ is a boundary between plates where new lithospheric⁵⁹ material is injected from below. As the plates diverge⁶⁰ from a mid-ocean ridge they slide on a more yielding layer at the base of the lithosphere.

Since the size of the Earth is essentially⁶¹ constant, new lithosphere can be created at the mid-ocean ridges⁶² only if an equal amount of lithospheric material is consumed elsewhere. The site of this destruction is another kind of plate boundary: a subduction zone. There one plate dives under the edge of another and is reincorporated into the mantle. Both kinds of plate boundary are associated with fault systems, earthquakes and volcanism, but the kinds of geologic⁶³ activity observed at the two boundaries are quite different.

The idea of sea-floor spreading actually preceded the theory of plate tectonics. In its original version, in the early 1960's, it described the creation and destruction of the ocean floor, but it did not specify⁶⁴ rigid lithospheric plates. The hypothesis was substantiated⁶⁵ soon afterward⁶⁶ by the discovery that periodic reversals of the Earth's magnetic field are recorded in the oceanic crust. As magma rises under the mid-ocean ridge, ferromagnetic⁶⁷ minerals in the magma become magnetized in the direction of the magma become magnetized in the direction of the geomagnetic field. When the magma cools and solidifies⁶⁸, the direction and the polarity of the field are preserved in the magnetized volcanic⁶⁹ rock. Reversals of the field give rise to a series of magnetic stripes running parallel to the axis⁷⁰ of the rift²¹. The oceanic crust thus serves as a magnetic tape recording⁷¹ of the history of the geomagnetic field that can be dated independently; the width of the stripes indicates the rate of the sea-floor spreading.


37 Icebergs⁷²

Icebergs are among nature's most spectacular creations, and yet most people have never seen one. A vague air of mystery envelops⁷³ them. They come into being ----- somewhere ------in faraway, frigid⁷⁴ waters, amid thunderous noise and splashing turbulence⁷⁵, which in most cases no one hears or sees. They exist only a short time and then slowly waste away just as unnoticed.

Objects of sheerest beauty they have been called. Appearing in an endless variety of shapes, they may be dazzlingly white, or they may be glassy blue, green or purple, tinted⁷⁶ faintly of in darker hues⁷⁷. They are graceful⁷⁸, stately, inspiring ----- in calm, sunlight seas.

But they are also called frightening and dangerous, and that they are ---- in the night, in the fog, and in storms. Even in clear weather one is wise to stay a safe distance away from them. Most of their bulk is hidden below the water, so their underwater parts may extend out far beyond the visible top. Also, they may roll over unexpectedly, churning the waters around them.

Icebergs are parts of glaciers that break off, drift into the water, float about awhile, and finally melt. Icebergs afloat today are made of snowflakes that have fallen over long ages of time. They embody⁷⁹ snows that drifted down hundreds, or many thousands, or in some cases maybe a million years ago. The snows fell in polar regions and on cold mountains, where they melted only a little or not at all, and so collected to great depths over the years and centuries.

As each year's snow accumulation lay on the surface, evaporation⁸⁰ and melting caused the snowflakes slowly to lose their feathery points and become tiny grains of ice. When new snow fell on top of the old, it too turned to icy grains. So blankets of snow and ice grains mounted layer upon layer and were of such great thickness that the weight of the upper layers compressed the lower ones. With time and pressure from above, the many small ice grains joined and changed to larger crystals, and eventually the deeper crystals merged⁸² into a solid mass of ice.


38 Topaz

Topaz is a hard, transparent⁸³ mineral. It is a compound of aluminum⁸⁴, silica, and fluorine. Gem⁸⁵ topaz is valuable. Jewelers call this variety of the stone "precious topaz". The best-known precious topaz gems⁸⁶ range in color from rich yellow to light brown or pinkish red. Topaz is one of the hardest gem minerals. In the mineral table of hardness, it has a rating of 8, which means that a knife cannot cut it, and that topaz will scratch quartz⁸⁷.

The golden variety of precious topaz is quite uncommon⁸⁸. Most of the world's topaz is white or blue. The white and blue crystals of topaz are large, often weighing thousands of carats. For this reason, the value of topaz does not depend so much on its size as it does with diamonds and many other precious stones, where the value increases about four times with each doubling of weight. The value of a topaz is largely determined⁸⁹ by its quality. But color is also important: blue topaz, for instance, is often irradiated to deepen and improve its color.

Blue topaz is often sold as aquamarine and a variety of brown quartz is widely sold as topaz. The quartz is much less brilliant and more plentiful than true topaz. Most of it is variety of amethyst⁹⁰: that heat has turned brown.

NOTE:
topaz / 'tэupжz; `topжz/ n (a) [U] transparent yellow mineral 黄玉（矿物）. 
(b) [C] semi-precious gem cut from this 黄玉; 黄宝石.


39 The Salinity⁹¹ of Ocean Waters

If the salinity of ocean waters is analyzed⁹², it is found to vary only slightly from place to place. Nevertheless, some of these small changes are important. There are three basic processes that cause a change in oceanic salinity. One of these is the subtraction⁹³ of water from the ocean by means of evaporation--- conversion⁹⁴ of liquid water to water vapor⁸¹. In this manner the salinity is increased, since the salts stay behind. If this is carried to the extreme, of course, white crystals of salt would be left behind.

The opposite of evaporation is precipitation, such as rain, by which water is added to the ocean. Here the ocean is being diluted⁹⁶ so that the salinity is decreased. This may occur in areas of high rainfall or in coastal regions where rivers flow into the ocean. Thus salinity may be increased by the subtraction of water by evaporation, or decreased by the addition of fresh water by precipitation or runoff.

Normally, in tropical regions where the sun is very strong, the ocean salinity is somewhat higher than it is in other parts of the world where there is not as much evaporation. Similarly, in coastal regions where rivers dilute⁹⁵ the sea, salinity is somewhat lower than in other oceanic areas.

A third process by which salinity may be altered is associated with the formation and melting of sea ice. When sea water is frozen, the dissolved materials are left behind. In this manner, sea water directly materials are left behind. In this manner, sea water directly beneath freshly formed sea ice has a higher salinity than it did before the ice appeared. Of course, when this ice melts, it will tend to decrease the salinity of the surrounding water.

In the Weddell Sea Antarctica, the densest⁹⁷ water in the oceans is formed as a result of this freezing process, which increases the salinity of cold water. This heavy water sinks and is found in the deeper portions of the oceans of the world.

NOTE：
salinity / sэ'linэti; sэ`linэti/ 
n [U] the high salinity of sea water 海水的高含盐量.
--->>>saline / 'seilain; US -li:n; `selin/ 
1.adj [attrib 作定语] (fml 文) containing salt; salty 含盐的; 咸的: 
* a saline lake 盐湖 * saline springs 盐泉 
* saline solution, eg as used for gargling, storing contact lenses, etc 盐溶液（如用于漱喉、存放隐形眼镜等）.
2. n [U] (medical 医) solution of salt and water 盐水.


40 Cohesion⁹⁸-tension Theory

Atmospheric pressure can support a column of water up to 10 meters high. But plants can move water much higher; the sequoia⁹⁹ tree can pump water to its very top more than 100 meters above the ground. Until the end of the nineteenth century, the movement of water in trees and other tall plants was a mystery. Some botanists¹⁰⁰ hypothesized that the living cells of plants acted as pumps. But many experiments demonstrated that the stems of plants in which all the cells are killed can still move water to appreciable¹⁰¹ heights. Other explanations for the movement of water in plants have been based on root pressure, a push on the water from the roots at the bottom of the plant. But root pressure is not nearly great enough to push water to the tops of tall trees. Furthermore, the conifers, which are among the tallest trees, have unusually low root pressures.

If water is not pumped to the top of a tall tree, and if it is not pushed to the top of a tall tree, then we may ask: how does it get there? According to the currently accepted cohesion-tension theory, water is pulled there. The pull on a rising column of water in a plant results from the evaporation of water at the top of the plant. As water is lost from the surface of the leaves, a negative pressure, or tension, is created. The evaporated water is replaced by water moving from inside the plant in unbroken columns that extend from the top of a plant to its roots. The same forces that create surface tension in any sample of water are responsible for the maintenance of these unbroken columns of water. When water is confined in tubes of very small bore, the forces of cohesion (the attraction between water molecules) are so great that the strength of a column of water compares with the strength of a steel wire of the same diameter. This cohesive¹⁰² strength permits columns of water to be pulled to great heights without being broken.

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