lake clay वाक्य
उदाहरण वाक्य
मोबाइल
- Lake Clay has public access at two public boat ramps.
- Lake Clay Drive surrounds three-fourths of Lake Clay.
- Lake Clay Drive surrounds three-fourths of Lake Clay.
- In the streams lower reaches, this is underlain by glacial lake clays.
- The landscape is dominated by deposits of till, boulder clays and glacial lake clays.
- The Holderness landscape is dominated by deposits of till, boulder clays and glacial lake clays.
- In the stream's lower reaches, some of the till is underlain by glacial lake clays.
- The city slopes gently from the northwest to southeast on a till plain composed largely of glacial and lake clay.
- Wisconsinan Till occurs along the stream's valley throughout its length and is underlain by glacial lake clays in some reaches.
- Further upstream, the surficial geology consists of Wisconsinan Till and alluvial fan, some of which is underlain by glacial lake clays.
- Slightly further upstream, there is a till known as Wisconsinan Till, which is underlain with glacial lake clays in some reaches.
- In the stream's upper reaches, alluvium is present as well and some of the Wisconsinan Till is underlain by glacial lake clays.
- One is on the east side of the lake, at 1650 Lake Clay Drive, and the other is on the west side, at 1300 Lake Clay Drive.
- One is on the east side of the lake, at 1650 Lake Clay Drive, and the other is on the west side, at 1300 Lake Clay Drive.
- Many of the soils of the immediate Laguna area are classified as Clear Lake clay; these soils are associated with regions of poor drainage, and are underlain by alluvium and sedimentary rock.
- Further upstream, in the middle and upper reaches, there is a till known as Wisconsinan Till, which is underlain by glacial lake clays in the vicinity of the stream's middle reaches.
- "' Ventifact Knobs "'( ) are minor knobs, 3 to 6 m high, composed of lake clay covered by glacial drift . The glacial drift has cobbles that are well polished by the wind and cut into ventifacts.
- The Lower Shiawassee is bordered by a low-relief till plain overlain by relatively impermeable and are poorly-drained fine-grained glacial lake clays and relict beach deposits that were deposited over a several thousand-year period when glacial Lake Saginaw covered much of the area, after the most recent retreat of the ice at the end of the Wisconsin glaciation.
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