Sentence examples for lost streams from inspiring English sources

When the terms of the new agreement were originally announced in February 2013, Johnson Matthey indicated that it expected commission income from the two lost streams to be £35m in the year ending March 2013.

Many rivers and streams flowing from the north side of the plain sink into the aquifer instead of flowing into the Snake River, a group of watersheds called the lost streams of Idaho.

Several species of frogs are common in the "lost streams" basin and the northeasternmost part of the Snake River watershed, including the inland tailed frog, northern leopard frog, western toad, Columbia spotted frog, long-toed salamander, spadefoot toad.

Pronghorn and bighorn sheep are common in the area drained by the "lost streams of Idaho", several rivers and large creeks that flow south from the Rocky Mountains and disappear into the Snake River Aquifer.

Twitter lost streaming rights NFL Thursday Night Football games to Amazon this season, in a deal valued at around $50 million – up from the $10 million Twitter had paid previously.

Water from the surface drains directly into an aquifer through features like sinks and losing streams and may discharge at the surface only at seeps and springs.

Concurrent application of the stream radon method, transient storage modelling of injected tracer breakthrough curves and hydraulic methods is recommended to capture the full spectrum of hyporheic exchange in losing streams.

Spring water and groundwater from two wells dominantly receiving diffuse and conduit flow (termed diffuse site and conduit site, respectively) in the Barton Springs segment of the Edwards aquifer (central Texas, USA) and surface water from losing streams that recharge the aquifer were sampled every 3 4 weeks during November 2008 March 2010.

Karst systems are often characterized by substantial groundwater surface water connections via processes such as aquifer recharge by losing streams, fracture and conduit connections between surface water and groundwater, and spring flow contributions to surface water (e.g., Katz et al. 1997; Musgrove et al. 2010).

Water availability in dry regions is primarily limited by the very small amounts of meteoric precipitation that re-supply below-ground resources and snowmelt from nearby mountainous regions which is, in some regions, the primary source of recharge to aquifers through losing streams and rivers.

They form losing streams flowing to the sea, while springs of lower yield dry up during summer.