- geology, a
syncline is a fold with
younger layers closer to the
center of the structure,
whereas an
anticline is the
inverse of a
syncline. A synclinorium...
- The Prüm
Syncline, Prüm
Limestone Basin (German: Prümer Kalkmulde) or Prüm
Basin (Prümer Mulde) is a
landscape unit of the
southern Limestone Eifel in...
- The
Tetapaga Syncline, also
known as the Lake
Tetapaga Syncline, is a
northeasterly trending syncline in
Northeastern Ontario, Canada,
located in Strathy...
- The
Micheldever Syncline is one of a
series of
parallel east-west
trending folds in the
Cretaceous chalk of Hampshire. It lies at the
western end of the...
- The
Southland Syncline is a
major geological structure located in the
Southland Region of New Zealand's
South Island. The
syncline folds the
Mesozoic greywackes...
- The Alderbury-Mottisfont
Syncline is an east–west
trending fold in the
Cretaceous chalk of Hampshire. It lies to the
north of the Dean Hill
Anticline and...
-
Syncline Mountain is a 7,560-foot (2,300-metre)
mountain summit located on the
shared border between Okanogan County and
Whatcom County in
Washington state...
- that is an arch-like
shape and has its
oldest beds at its core,
whereas a
syncline is the
inverse of an anticline. A
typical anticline is
convex up in which...
- part of the
great shallow syncline known as the
London Basin. The beds dip in a south-easterly
direction towards the
syncline's lowest point roughly under...
-
landscape features. The
lineament lies
along the axis of the
Central Wales Syncline, both
following the
generally northeast–southwest
Caledonide trend though...
