Pennsylvania's colonial ironmasters forged iron and a revolution that had both
& V5 T6 @8 A" }+ d# `" ? industrial and political implications. The colonists in North America wanted the right to2 g2 i7 h h0 t& V# J
the profits gained from their manufacturing. However, England wanted all of the
% d6 Z' e! f. I3 ]7 C+ c Line colonies' rich ores and raw materials to feed its own factories, and also wanted the
2 H1 h4 j8 M4 D1 ]6 R5 r (5) colonies to be a market for its finished goods. England passed legislation in 1750 to5 C$ O3 ^8 C! I$ `* [! J$ M
prohibit colonists from making finished iron products, but by 1771, when entrepreneur5 Z# ~4 {' O3 |6 [
Mark Bird established the Hopewell blast furnace in Pennsylvania, iron making had) \4 p0 _ S$ G( u" p$ A/ j
become the backbone of American industry. It also had become one of the major issues' j: N7 ]$ s# o; l. C" I* f3 }- v
that fomented the revolutionary break between England and the British colonies. By the" f' T8 L" Q; ]
(10) time the War of Independence broke out in 1776, Bird, angered and determined, was
! ~' M8 O( a6 w. V4 E. h7 R manufacturing cannons and shot at Hopewell to be used by the Continental Army.' S3 e2 Q1 r: P: n
After the war, Hopewell, along with hundreds of other "iron plantations," continued to
9 a" r( _. K0 u& s* ~ form the new nation's industrial foundation well into the nineteenth century. The rural5 j! y' ~2 F) n9 K% E
landscape became dotted with tall stone pyramids that breathed flames and smoke,
- Z3 \: D; l0 n( a9 g' P, P! z (15) charcola-fueled iron furnaces that produced the versatile metal so crucial to the nation's2 C/ n( M9 P* n) L+ c
growth. Generations of ironmasters, craftspeople, and workers produced goods during
: g1 P* l7 P8 {# y2 S8 L war and peace-—ranging from cannons and shot to domestic items such as cast-iron
! l( Q) \( ], P% j9 \. z stoves, pots, and sash weights for windows.. W- M% _+ w( r# p
The region around Hopewell had everything needed for iron production: a wealth of
* O1 W- I) I3 J' y (20) iron ore near the surface, limestone for removing impurities from the iron, hardwood' M; k4 H. a# ]5 k! ~/ y
forests to supply the charcoal used for fuel, rushing water to power the bellows that
/ V* w: F K. K0 f9 d pumped blasts of air into the furnace fires, and workers to supply the labor. By the
1 j$ C3 X3 V" j 1830's, Hopewell had developed a reputation for producing high quality cast-iron stoves,' E+ j7 U; i' H4 L, t* \# b
for which there was a steady market. As Pennsylvania added more links to its
0 D5 Q3 J, M* S6 o (25) transportation system of roads, canals, and railroads, it became easier to ship parts made6 m' `- l# e G) t- i0 j
by Hopewell workers to sites all over the east coast. There they ware assembled into
( C3 T( Z3 S3 `- `" O" b stoves and sold from Rhode Island to Maryland as the "Hopewell stove". By the time the# @9 E( G& j ^+ @7 Y
last fires burned out at Hopewell ironworks in 1883, the community had produced some
& u T: }' p' M. [7 ~ t 80,000 cast-iron stoves.
4 Y0 {* L$ p0 _' Q& g% u' `$ l 5. Pennsylvania was an ideal location for the Hopewell ironworks for all of the following reasons EXCEPT
9 @& Y, \4 f) K8 R9 S (A) Many workers were available in the area
/ z. K5 D6 q Y/ u (B) The center of operations of the army was nearby3 E$ z# Y0 y: Q/ w2 G: Y9 J" N" }6 ] e C
(C) The metal ore was easy to acquire* p8 f8 j: z4 D* I' a
(D) There was an abundance of wood/ [5 W2 f8 H6 C# z! v+ B2 h* J
答案:B3 z) l( w8 W% S# ~7 W9 w
Under the Earth's topsoil, at various levels, sometimes under a layer of rock, there are! Y" b* A" f1 p" ^9 [4 e( J% q$ L
deposits of clay. Look at cuts where highways have been built to see exposed clay beds;1 v# D @( P7 l q
or look at a construction site, where pockets of clay may be exposed. Rivers also reveal
8 m' X T9 {4 x' w6 c Line clay along their banks, and erosion on a hillside may make clay easily accessible.
K4 o2 y8 G4 a. C. w2 u# k (5) What is clay made of? The Earth's surface is basically rock, and it is this rock that
, A6 S8 u+ l T gradually decomposes into clay. Rain, streams, alternating freezing and thawing, roots of) Y9 W8 {& J U- y& V: V" }% G; a
trees and plants forcing their way into cracks, earthquakes, volcanic action, and glaciers6 n6 [0 y! O+ U
—all of these forces slowly break down the Earth's exposed rocky crust into smaller and& |" g# ^/ `0 } D; s7 Z8 I- s
smaller pieces that eventually become clay.6 m+ Z, O. |& V- E- j& |. c, i, E
(10) Rocks are composed of elements and compounds of elements. Feldspar, which is the
0 m) @% A8 q; l- a6 Z9 O9 i most abundant mineral on the Earth's surface, is basically made up of the oxides2 P4 G9 B4 L5 @& y
silica and alumina combined with alkalis like potassium and some so-called impurities
$ W$ X/ p- F0 V such as iron. Feldspar is an essential component of granite rocks, and as such it is the8 p; k+ m6 N1 w) N5 x: v
basis of clay. When it is wet, clay can be easily shaped to make a variety of useful
5 F7 P4 X0 n( n. o- j1 X (15) objects, which can then be fired to varying degrees of hardness and covered with% ?! g! l1 u% A. n! f$ y2 B
impermeable decorative coatings of glasslike material called glaze. Just as volcanic
& D/ T0 P# S/ t" @6 v1 B action, with its intense heat, fuses the elements in certain rocks into a glasslike rock" T/ _6 ?: P# d$ d
called obsidian, so can we apply heat to earthen materials and change them into a hard,
+ o( y: r) O3 k8 }& ]4 E dense material. Different clays need different heat levels to fuse, and some, the low-fire
+ R+ T* a& P* J. ?9 G (20) clays, never become nonporous and watertight like highly fired stoneware. Each clay can% A9 `' y; m1 T4 e/ z. H
stand only a certain amount of heat without losing its shape through sagging or melting.& _! i; d# `$ `
Variations of clay composition and the temperatures at which they are fired account for
, {1 l# ?5 u+ z w the differences in texture and appearance between a china teacup and an earthenware t8 f" X6 s& r/ m# d
flowerpot.% B3 U& ? G4 Y: w, L0 O
2. It can be inferred from the passage that clay is LEAST likely to be plentiful in which of the following areas?/ z1 o& v$ {* v5 Z5 d
(A) in desert sand dunes
3 {, j% c& }/ _2 R- [% T# X: I (B) in forests2 c3 s' D- B8 T% M4 f/ C% [
(C) on hillsides
, g3 h7 j4 i# d) |/ ]0 o (D) near rivers3 d( R/ R. w8 r( L( F
答案:A |