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depth (m)<br />

10<br />

20<br />

30<br />

40<br />

osit is thinnest<br />

3, the smallest<br />

lake clay was<br />

f the lake clay<br />

to Site 3, the<br />

30<br />

glacial<br />

till<br />

F. increases. 40<br />

G. remains the same.<br />

H. first increases and then decreases.<br />

J. decreases.<br />

Figure 3In<br />

Figure 2, the key shows us that the glacial till is indicated with stripes. As we<br />

move left from Grand Forks to Site 3, we see that the area of the glacial till gets<br />

thinner. So the thickness of the glacial till decreases.<br />

9. According to Figure 2, which of the following graphs<br />

best represents the elevations, in m above sea level, of<br />

the top of the glacial till layer at Sites 1, 2, and 3 ?<br />

A.<br />

B.<br />

lake<br />

clay<br />

18 16<br />

___________________________<br />

O/ O of groundwater Answer: sample J.<br />

18 16<br />

O/ O of standard water sample<br />

y, and T. W. D. Edwards, “Isotopic Composition of Old Ground Water from Lake Agassiz:<br />

by the American Association for the Advancement of Science.<br />

elevation<br />

(m above sea level)<br />

elevation<br />

(m above sea level)<br />

225<br />

200<br />

175<br />

150<br />

225<br />

200<br />

175<br />

150<br />

1<br />

1<br />

depth (m)<br />

O = – 1 × 1,000<br />

2<br />

Site<br />

2<br />

Site<br />

3<br />

3<br />

10<br />

20<br />

C.<br />

D.<br />

elevation<br />

(m above sea level)<br />

elevation<br />

(m above sea level)<br />

225<br />

200<br />

175<br />

150<br />

225<br />

200<br />

175<br />

150<br />

1<br />

1<br />

lake<br />

clay<br />

2<br />

Site<br />

2<br />

Site<br />

10. Precipitation that falls at Sites 1, 2, and 3 soaks into<br />

Answer: the soil C. until it reaches the groundwater table about<br />

3 m below the surface. Based on Figure 3, and assuming<br />

no alteration of the precipitation, the δ<br />

Notice that the word elevation appears in italics in this question. In previous<br />

questions about Figure 2, we’ve been look at the thickness of different layers.<br />

Whoever wrote the question wants to make sure that we pay attention to elevation<br />

instead of thickness.<br />

18 O value of<br />

present-day precipitation in the study area is closest to:<br />

F. −26.<br />

G. −23.<br />

H. −20.<br />

J. −15.<br />

In Figure 2, the elevation of a layer is shown with numbers along the vertical axis<br />

labeled “elevation GO (m ON above TO sea THE level)”. NEXT So, PAGE. for example, the top of the glacial till is<br />

45 230 m at Winnipeg and 200 m at Site 1. Looking at sites 1, 2, and 3, we see that the<br />

elevation of the top of the glacial till is highest at Site 2 and lowest at Site 3, so C is<br />

the only possible answer.<br />

10. Precipitation that falls at Sites 1, 2, and 3 soaks into the soil until it reaches the groundwater table about<br />

3 m below the surface. Based on Figure 3, and assuming no alteration of the precipitation, the δ18Ο value<br />

of present-day precipitation in the study area is closest to:<br />

F. −26.<br />

3<br />

3

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