Author: Daniel T. Snyder, Dorie L. Brownell
Publisher:
ISBN:
Category :
Languages : en
Pages : 60
Book Description
Hydrogeologic Setting and Preliminary Estimates of Hydrologic Components for Bull Run Lake and the Bull Run Late Drainage Basin
Author: Daniel T. Snyder, Dorie L. Brownell
Publisher:
ISBN:
Category :
Languages : en
Pages : 60
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 60
Book Description
Seismic Maps Foster Landmark Legislation
Author:
Publisher:
ISBN:
Category : Earthquake engineering
Languages : en
Pages : 2
Book Description
Publisher:
ISBN:
Category : Earthquake engineering
Languages : en
Pages : 2
Book Description
New Publications of the Geological Survey
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 836
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 836
Book Description
Quake Forecasting--an Emerging Capability
Creating an Effective Fact Sheet
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Earth sciences
Languages : en
Pages : 2
Book Description
Publisher:
ISBN:
Category : Earth sciences
Languages : en
Pages : 2
Book Description
The New U.S. Geological Survey
Volcanic Ash
Hydrologic Setting of Wetlands in the Cottonwood Lake Area, Stutsman County, North Dakota
Author: Thomas C. Winter
Publisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 52
Book Description
Because of growing interest in the role of lakes and wetlands in the hydrology of the prairie environment, a group of wetlands in the Cottonwood Lake area, Stutsman County, N. Dak., are being instrumented for long-term hydrologic studies. The study site is on a regional topographic high near the eastern edge of the Missouri Coteau and is underlain by more than 400 feet of glacial drift, largely silty, clayey till. Long-term climatic data indicate the study area is in a water deficient area--mean annual evaporation exceeds mean annual precipitation by about 18 inches. Different methodologies are being used to compare measurements and estimates of each hydrologic component interacting with the lakes and wetlands. For example, for a 3-month period in 1979, estimates of precipitation for the study site using data collected at National Weather Service stations differed from that measured by a recording gage at the study site by several tenths of an inch for 14-day totals and differed by more than half an inch for individual storms. Numerical simulation analysis of regional groundwater flow systems shows the study site is situated in a regional recharge area, but local groundwater flow systems can discharge to lakes and wetlands within the recharge area. Instrumentation at the study site shows a complex interrelation of wetlands and groundwater. Based on data for 1979 only, some wetlands appear to recharge groundwater, some wetlands are flow-through types where groundwater enters one side and surface water seeps to groundwater on the other side, and some wetlands are discharge points for groundwater. Further, these interrelations vary throughout the year.
Publisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 52
Book Description
Because of growing interest in the role of lakes and wetlands in the hydrology of the prairie environment, a group of wetlands in the Cottonwood Lake area, Stutsman County, N. Dak., are being instrumented for long-term hydrologic studies. The study site is on a regional topographic high near the eastern edge of the Missouri Coteau and is underlain by more than 400 feet of glacial drift, largely silty, clayey till. Long-term climatic data indicate the study area is in a water deficient area--mean annual evaporation exceeds mean annual precipitation by about 18 inches. Different methodologies are being used to compare measurements and estimates of each hydrologic component interacting with the lakes and wetlands. For example, for a 3-month period in 1979, estimates of precipitation for the study site using data collected at National Weather Service stations differed from that measured by a recording gage at the study site by several tenths of an inch for 14-day totals and differed by more than half an inch for individual storms. Numerical simulation analysis of regional groundwater flow systems shows the study site is situated in a regional recharge area, but local groundwater flow systems can discharge to lakes and wetlands within the recharge area. Instrumentation at the study site shows a complex interrelation of wetlands and groundwater. Based on data for 1979 only, some wetlands appear to recharge groundwater, some wetlands are flow-through types where groundwater enters one side and surface water seeps to groundwater on the other side, and some wetlands are discharge points for groundwater. Further, these interrelations vary throughout the year.
The Water Resources Research Program of the U.S. Geological Survey
Author: Geological Survey (U.S.). Water Resources Research Program
Publisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 252
Book Description
Publisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 252
Book Description