A long valley profile shows the cross-sectional view of a valley from its headwaters to its mouth. It typically displays the variations in elevation and slope along the length of the valley, often revealing features such as V-shaped valleys, interlocking spurs, and river meanders. This profile is useful for analyzing the geological and geomorphological history of a valley.
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
A stream-carved valley typically has a V-shape with a narrower and deeper profile due to the erosive force of flowing water. In contrast, a glacial-carved valley has a U-shape with a wider and shallower profile due to the movement of glaciers scooping out the landscape.
Valley glaciers form when ice and snow accumulate in a mountain valley due to the accumulation of snow exceeding the rate of melting. Over time, the ice flows downhill, shaping the valley and creating a distinct U-shaped profile.
The major city closest to Long Valley Caldera is Mammoth Lakes in California. It is located about 12 miles southeast of the caldera.
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
The Long Valley was created in 1938.
u shaped
I would say the waterfall and the rapids are the most prominent features of a narrow V - Shaped valley where the stream profile drops rapidly.
how long will ittake for a valley toform
The address of the Long Valley Branch Jackson County Library is: Po Box 27, Long Valley, 57547 0027
A glaciated mountain valley typically has a U-shaped profile with steep, smooth walls and a flat bottom due to the scouring action of the glacier. In contrast, a mountain valley that was not glaciated usually has a V-shaped profile with more rugged and uneven walls, shaped primarily by flowing water and tectonic forces.
The address of the Wash. Twsp. Pub. Lib.- Long Valley - is: 37 E. Springtown Road, Long Valley, 07853 9303
how long did it take for Kagan valley toform
Yes, it has a long O (oh), a long i (eye), and a silent E. Profile is pronounce PROH-fyl. (rhymes with go-style)
Valley glaciers melt and it make a U shaped profile (cirque) ~W