The South Yemen Landsat scene above extends over part of the Hadhramut Plateau, an uplifted section of Tertiary limestones and shales which experienced folding into a broad syncline (center) and two anticlines (top and bottom of image; not visibly evident). Typical dendritic drainage is developed as the Wadi al Masilah which, along with its tributaries, is a sometimes ephemeral stream (its valley is sand-filled) that obtains flow mostly after large storms but maintains enough water to support local farming. Much of this drainage was likely developed during a wet period before the regional climate shifted to its present arid state. Note the typical headwaters pattern for dendritic drainage in the system in the upper right. The drainage pattern near the coast has become trellis-like.

The above subscene (about 100 km [62 miles] wide) is located in West Virginia next to the Kentucky border. The Ohio River flows just to the north of the image top. The area is part of the Appalachian Plateau, an uplifted sector of the crust involved in the Appalachian orogeny that did not experience folding, so that the rocks remain horizontal. The drainage has reached a level referred to as mature, in which a distinctive high-density dissection has reduced divides to sharp ridges, with little of the earlier uplands remaining, and narrow valleys. Although this leads to maximum relief, the differences in elevation are seldom more than about 200 meters (675 ft).

In Section 4, we saw one example of a river delta so far, that being the bird's foot delta of the Mississippi River as it builds out into the Gulf of Mexico in Louisiana south of New Orleans. Here are two more classic examples:

This Landsat image shows about half (the western part) of the Ganges Delta in Bangledesh (India border near the left; Calcutta just at center edge). This is the world's largest delta, being more than 200 km (125 miles) in straight distance along the Bay of Bengal. The delta results from deposition of heavily silt-laden waters of the Ganges and the Brahmaputra Rivers, both transporting sediment from the Himalayas far to the north.

The present-day Ganges itself drains southward just off the image to the right; that segment is now the active delta region. In the scene above, we see the so-called abandoned delta which was formed in the past when the Ganges flowed in various positions as it shifted gradually eastward. Other rivers still flow into the Bay adding somewhat to the delta, as seen in the light blue sediment being carried out into marine waters. These quasi-distributaries become tidal channels that are much influenced by tidal currents. The dark red tones along the coast are mangrove forests and swamps. In the upper left quadrant, the area is part of the depauperate delta, where the clay soils now support sporadic agriculture (much of the forest once there have been removed by people seeking farmland). The entire region, especially the low flat areas near the coast, is vulnerable to frequent cyclones (hurricanes) that cause widespread damage and loss of life both because of high winds and tidal surges.

This next Landsat Band 7 (IR) image covers the central west coast of Alaska. Here the Yukon River flows into Norton Sound on the northeastern Bering Sea.

The main branch now carries sediment to the south end of a large semi-circular delta. It is actively extending the delta but an offshoot tributary is doing much of the deposition in the central part. This present delta is young (perhaps only a few thousand years since its start) that began with a major shift of the Yukon from a location not in this scene. Within and inland from the delta are numerous small lakes of ice origin. Along the coast at the bottom of the image are linear bands which are beach ridges developed when sea level was higher.

The two coastal landforms examples display special types that also fall into two general categories: coastlines of submergence and emergence.

The above scene lies in the Coast Ranges along the Pacific Ocean in the region where the Alaska Panhandle extends past Canada (near top of image); Juneau, Alaska's capital, is situated near the center. The region is tectonically active, with major faults separating individual crustal units known as terranes (see below). These faults and other structural features served as lines of weakness for erosional attack by streams and glaciers, which together had carved out deep valleys. Some present day glaciers are visible in the Glacier Bay National Park area northeast of Juneau and elsewhere. Since the close of the last major glaciation, melting glaciers are now in retreat to the extent that some large valleys downcut earlier by the ice to below sea level were then invaded by the ocean, effectively drowning them. The resulting landform is known as a fjord - a Norwegian name assigned to submerged coastal valleys once occupied by ice.

The Atlantic seaboard, seen above, is generally now a coast of emergence associated with regional uplift. Over the past 50 million years or so, seas had lapped well onto the eastern North American continent, laying down thick, subhorizonatal sedimentary layers, but the ocean has been gradually retreating eastward. In the last few thousand years, a rise in sea level resulting from glacial ice melt has reversed this trend as marine waters drown coastal valleys (e.g., Chesapeake Bay) and push shorelines inland. Along much of the Atlantic coast from New Jersey to Florida, thin narrow lines of sand deposits built up above sea level by deposition from ocean waters encroaching shallow bottom slopes form barrier islands. The illustration is a photo taken by an Apollo 9 astronaut of the famed Outer Banks of North Carolina. The point farthest east is Cape Hatteras; the southern point is Cape Lookout. The wide stretch of water towards the mainland is Pamlico Sound which, with Albemarle Sound inland to the north, is termed a lagoon. Offshore, submerged sandbars - incipient islands - form hazards to shipping. Because of the irregular, cuspate coastline west of the barrier, geomorphologists argue that the island had already formed prior to current onlap by ocean waters, thus protecting the inner shores from wave erosion.

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