Hydrologic Atlas最新文献_第8页

Backwater at bridges and densely wooded flood plains, Tenmile Creek near Elizabeth, Louisiana 桥上的回水和树木繁茂的洪泛平原，路易斯安那州伊丽莎白附近的Tenmile溪

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA606

G. J. Arcement, B. Colson, C. Ming

引用次数: 1

Availability of ground water in the Oak Level quadrangle, Kentucky 肯塔基州Oak Level四合院地下水的可用性

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA116

J. Morgan

引用次数: 1

Reconnaissance of ground-water resources of the Jackson Purchase region, Kentucky 肯塔基州杰克逊购买地区地下水资源的勘测

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA13

L. M. Maccary, T. W. Lambert

引用次数: 9

Water resources of the River Raisin basin, southeastern Michigan 密西根州东南部Raisin河流域的水资源

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA356

R. L. Knutilla, W. B. Allen

{"title":"Water resources of the River Raisin basin, southeastern Michigan","authors":"R. L. Knutilla, W. B. Allen","doi":"10.3133/HA356","DOIUrl":"https://doi.org/10.3133/HA356","url":null,"abstract":"The accompanying tables summarize some physiographic data for selected subbasins in the River Raisin basin having about 2 or more square miles of drainage area. Selected subbasins of the major streams include area above mouths of tributaries, and points of interest such as highways, towns, gaging stations, or dams, and below the confluence of the main stream and a tributary so as to include both drainage areas. Similar criteria were used for tributary streams, except where the tributary was too small to merit further dividing. Most subbasins are shown on the basin map, sheet 1. To help locate the tabulated areas on the map, each subbasin is assigned a number and numbers for selected subbasins are shown on the map at the downstream end of the subbasins. Also shown are names of main roads and river miles, at 5-mile intervals, for the River Raisin and two of its main tributaries. Basin divides were outlined on the latest 7Vi-or 15minute topographic maps, scale 1:24,000 or 1:62,500, respectively, and drainage areas determined in accordance with the standards set forth by the Committee on Hydrology, Water Resources Council (formerly the Subcommittee on Hydrology, Inter-Agency Committee on Water Resources). Similarly, river miles were determined in accordance with the Committee's standards. Mile zero is considered to be the mouth of the stream. The source of a stream is considered to be the upper end of the stream, whether or not it is perennial. A defined channel which may be inferred from topographic maps to carry water occasionally is, therefore, included in the stream length. A stream that has its beginning at the confluence of two tributaries is considered to be a continuation of the longer tributary and to have as its source the source of that tributary. Its average slope is determined by treating the stream and tributary as one. Beaver Creek (number 253), for example, is considered to be the continuation of Slater Creek. In the table Slater Creek has been parenthetically noted as being the headwaters of Beaver Creek. Other tributary streams, in tl ;s classification, are likewise noted. Altitudes shown for site and source are f:~om topographic maps and represent the altitude of the water surface at approximately normal river stage, the datum being mean sea level. Average slopes were computed from the mileage between and differences in altitude of site and source and represent the fall of the stream in feet per mile. Streams are listed in a downstream order along the main stem, with tributary streams entered above the next main-stem location. A similar order if followed for listing streams of first rank, second ran) or other rank. To indicate the rank, and the stream to which it is tributary, the stream name is indented, each indentation representing one rank. The st\"aam rank is further identified by numbers in th* column heading with stream name and location. Number 1 applies to River Raisin. Principal tributaries are under number 2, their tribu","PeriodicalId":304802,"journal":{"name":"Hydrologic Atlas","volume":"104 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117194154","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 11

Geology and hydrology of alluvial deposits along the Ohio River between Newport and Warsaw Kentucky 肯塔基州纽波特和华沙之间俄亥俄河沿岸冲积沉积物的地质学和水文学

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA98

W. Price

引用次数: 1

Floods in McHenry Quadrangle, Northeastern Illinois 伊利诺伊州东北部麦克亨利四合院发生洪水

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA255

R. T. Mycyk, G. Walter

引用次数: 1

Geohydrologic systems in Kansas physical framework of the lower aquifer unit in the western interior plains aquifer system 地质水文系统在堪萨斯州的物理框架下的含水层单位在西部内陆平原含水层系统

Hydrologic Atlas Pub Date : 1900-01-01 DOI: 10.3133/HA722D

C. Hansen, J. Spinazola, E. Underwood, R. Wolf