エピスの授業ではこんなことをやっています。



Summarize the passage in 100 words.

【The Extreme Geography of Death Valley】

Death Valley, situated in the Basin and Range province of the Mojave Desert, is a dramatic
study in geological extremes. It is defined by its rugged topography, characterized by
deep, narrow basins and soaring, steep mountain ranges, most notably the Panamint and
Amargosa mountains. The valley’s defining feature is Badwater Basin, which drops to 282
feet below sea level—the lowest point in North America.

This landscape is the direct result of tectonic forces pulling the Earth’s crust apart over
millions of years. Acting as a "graben"—a depressed block of crust bounded by parallel
faults—the valley floor continues to subside. Seismic activity along these fault systems
maintains the valley’s stark, vertical relief, often resulting in high-altitude peaks like
Telescope Peak rising sharply above the basin floor.

Hydrology and extreme aridity further shape the surface. With less than two inches of
annual rainfall, the valley functions as a closed basin where evaporation far outpaces
precipitation. When rare, intense storms occur, water rushes down from the surrounding
canyons, carrying sediments and dissolved minerals onto the floor. As this water
evaporates, it leaves behind vast, crystalline salt flats that stretch for miles. Alluvial fans,
formed at the mouths of steep canyons, offer further evidence of these powerful,
infrequent flood events. The combination of intense heat, extreme low elevation, and
ongoing tectonic deformation makes Death Valley a premier laboratory for understanding
the Earth’s crustal evolution.



みなさんはどうまとめますか？？

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小手先のテンプレート学習ではなく、英語圏の大学への出願でも通用する英語の力を身につけたい方は、ぜひ一度体験にいらしてください！


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