| this, Dr. C. T. Jackson, of Boston, in his workon the Geology of New Hampshire, thus speaks:
  The Flume is a deep chasm, having muralprecipices of granite on each side, while a moun-
 tain torrent rushes through its midst, falling over
 precipitous crags and loose masses of rock.
 During the freshets of the spring season, and in
 early summer, it is not practicable to walk in the
 bed of the Flume. But in the driest season of
 the year, there is but little water in it, and the
 bottom of the ravine affords a good foot path.
  The direction of this rocky fisure is N. 80°E., and it appears to have resulted, not from the
 abrasion of the rocks by the action of running
 water, but to have been produced originally by
 a fracture of the uplifted rocks. The walls of
 the chasm on either hand exhibit proofs in favor
 of this opinion; for they are not water worn, but
 present surfaces of fracture, and the projecting
 ledges on each side are still comparatively sharp,
 and well defined in their outlines.
  One of the most remarkable objects in theFlume is an immense rounded block of granite,
 which hangs overhead, supported merely by
 small surfaces of contact against its sides. It
 appears to the traveller looking at it from below
 as if ready to fall upon him.''
 This Notch, in a remarkable manner, resemblesthe Great Notch, in its leading natural character-
 istics. Like that, it forms an extraordinary nat-
 ural avenue for a road, which connects the region
 of the upper Connecticut Biver with the seaboard.
 In the same manner, also, it has its river, taking
 its rise from a pond, called Ferrin's Pond, near
 the head of the Notch, and rapidly increasing as
 it flows onward, receiving perennial supplies from
 the mountain sides, and often swollen to a mad-
 dening torrent, by the rains which fall upon their
 broad and steep declivities. This river is the
 most N. branch of the Pemigewasset; and uniting
 with two other branches, from the E. and W., in
 the N. part of the town of Woodstock, forms
 one of the principal sources of the Merrimack,
 which, after performing such wonders of pro-
 ductive industry at Manchester, Lowell, Andover,
 and Lawrence, falls into the ocean at Newbury-
 port.
 Travellers visiting the White Mountains bythis route proceed by railroad from Boston to
 Concord, N. H., 76 miles ; thence by railroad to
 Plymouth, 51 miles; thence up the valley of the
 Pemigewasset, by railroad and stage to the Flume
 House, 24 miles; thence through the Notch, by
 the Old Man of the Mountain, to the Lafayette
 House, 5 miles farther; in all, 153 miles from
 Boston. From this the distance to Fabyan's
 White Mountain House, via Bethlem, is 16 miles.
 From the Lafayette House N. to Littleton is 12
 miles.
 GINGERCAKE ROCKS, N. C. This remarkable pile of rocks gives its nameto the mountain summit, upon the top of which
 it is seen. They are situated in the mountainous
 part of Burke co., amidst wild and romantic
 scenery. The pile consists of two rocks, of dif-
 ferent form and character, so poised as to stand
 firmly upon an exceedingly small base. The
 first or lower section, composed of a brittle slate
 stone, is in the form of the half of an inverted
 pyramid. Its truncated top, which, by its invert-
 ed position, becomes the base, upon which the
 whole is supported, is only 4 feet in diameter.
 
| The centre of gravity to this part of the pile,would fall much without the base upon which it
 rests, were it not most accurately balanced in its
 position by the second or superincumbent rock,
 which is a table of mountain granite, 32 feet in
 length, 18 in breadth, and 2 feet thick, resting
 horizontally upon the other with a sufficient ex-
 cess of its projection and weight, opposite to the
 preponderance of the inverted pyramid beneath,
 to produce a perfect counterpoise. The form and
 outline of this upper rock is as remarkable as that
 of the other, being as true in the proportions above
 given as if it had come from the hand of an artist.
 The lower section is about 29 feet high, which,
 being increased by the thickness of the upper sec-
 tion, makes the entire altitude 31 feet.
 A visitor to this curious freak of nature re-marks that  within the presence of this strange
 pile, the predominant feeling, after that of admi-
 ration, is fear. An attempt to reason one's self
 into a feeling of conscious security is utterly fu-
 tile. The argument that it has stood there per-
 haps for thousands of years, amid the raging
 winds and rocking earth, is met and opposed by
 the ocular fact of its standing before you almost
 upon nothing; and, approach it at what point
 you will, it appears leaning towards you.''
 As these rocks stand upon the summit of themountain, they can be seen, in a clear atmosphere,
 from a distance of many miles, looming up
 above the horizon, against the clear blue sky, in
 which they seem to float like a little fantastic
 cloud.
 The prospect from this mountain summit to-wards other distant points is also sublimely grand.
 Looking north, the eye runs down a ravine be-
 tween precipices from 800 to 1200 feet high, at
 the bottom of which the Linville Biver, one of the
 sources of the Catawba, dashes its pure waters
 along its rocky bed. From the top of one of the
 cliffs which overhangs this chasm is seen a shaft
 of rock shooting out over the gulf below, at the
 height of 1500 feet. This is known in the neigh-
 borhood by the name of the Hawk's Bill, from its
 resemblance to the beak of that bird.
 On the left of this, from the point of observa-tion, and about 5 miles distant, is the famous
 Table Rock, of Burke co., which rises, upon the
 verge of the Catawba valley, to the height of
 2500 feet. It appears, as seen from this point, to
 have the shape of a perfect cone.
 There are few mountain districts in which ispresented such a various display of the strange,
 the wild, the beautiful, and the grand, as here.
 GUILFORD POINT, CT., Situated in the old town of Guilford, on theshore of Long Island Sound, 15 miles E. of New
 Haven. The point runs out a short distance
 into the water, about one mile from the centre of
 the town. This has long been a place of resort,
 in the summer season, for the citizens of New
 Haven, Hartford, and other places, in pursuit of
 health and recreation. Good accommodations
 are found at the Point itself, and also at the ho-
 tels and boarding-houses in the village.
 HAMPTON BEACH, N. H. This beach is on the Atlantic coast, in Bock-ingham co., about 12 miles S. of Portsmouth, and
 about 7 miles S. W. from Exeter. It is little in-
 ferior to the celebrated Nahant Beach, near Bos
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