1 DOUGLAS HOT SPRINGS - ntlis.nt.gov.au

RailwayStation

KINTORECAVES

Revisions and updates have been made since the initial publicationof this map in May 2007

Mt Thomas

Neds Knob

Prospect Hill

Mt BriggsMt Muriel

Mt Pleasant Plateau Pt

Mt Freda

Mt Armstrong

Limestone Hill

Mt Pearce

Mt Compton

Crocker Hill

Mt Bowman

Mullens Ridge

Dead Horse Hill

Gallery Hill

Bondi Ridge

Beasley Pillar

Mt Todd

Zed Hill

Foelsche Headland

Far View Peak

Mt Mueller

Mt Colton

RomulaKnob

TinkerHill

Leliyn(Edith Falls)

Maryfield

Birdum

Western

CreekCreek

Maranboy

KATHERINE

KATHERINE RIVERKING

Limestone

Mathison

Battle

REYNOLD

DOUGLAS

SandyC

Middle Creek

Austral

Y RIVER

Lilyarba

Camp CkSalt

Trough

Copperfield

FERGUSSON

MileCk

Driffield Creek

EDITHRIVER

Granite

CkYujullowan

Native Cat

FERGUSSON

KATHERINE

RIVERFERGUSSON

KATHERINE

RIVERFERGUSSON

FERGUSSON

DOUGLAS

KATHERINE

Oolloo Springs

Rainbow Spring

Fig TreeSpring

Bitter Springs (See note 3)

DouglasHot Springs(See note 1)

FloraRiver

Spring

(see note 2)

KatherineHot

Springs

2200622006

2942929429

75957595

2171721717

RN22397RN22397

Delamere RangeFacil i ty

Mataranka

BamyiliKATHERINE

Dunmarra

Larrimah

DalyWaters

PineCreek

TopSprings

Daly Waters

Mataranka

BamyiliKATHERINE

Larrimah

PineCreek

Daly Waters

Mataranka

BamyiliKATHERINE

Larrimah

PineCreek

HayesCreek

MargaretDowns

Tipperary

Dorisvale

Douglas

Claravale

Delamere

Florina

Jindare

Maranboy

Kalala

Maryfield

Tarlee

Gorrie

Wyworrie

Blood Downs

Birdum Creek

Maryfield(ruins)

WesternCreek

SundayCreek

Fergusson River

Scott Creek Mataranka Homestead

Middle Creek

Dry River

LewinSprings

Banatjarl

Werenbun

Jodetluk

Dillinya

Douglas DalyExperimental

Station

Djarrung

BishopsBore

Jomet(Urpalarwn)

Binjari

Jilkminggan

Daly Waters

Pine Creek

Larrimah

Kybrook Farm

Mataranka

Rockhole

Nauiyu

Barunga

Katherine

KATHERINE

Douglas Crossing

Oolloo Crossing

BeeboomCrossing

ROPER HIGHWAY

Daly River

Fleming

Centra

Arnhem

BUNTINE

STUART

Florina

VICTORIA

WAY STUART

HIGHWAYSTU

STUART

BUCHANAN

CARPENTARIA

STUART

CARPENTARIA

STUART

HIGHWAY

STUART

TARLEEWESTERN CK

GILNOCKIE

GORRIE

LARRIZONA

DRY RIVER

MANBULLOO

INNESVALE

DORISVALE

TIPPERARY

FLORINA

CLARAVALE

JINDARE

BONROOK

DOUGLAS

KALALA

MARYFIELD

VERMELHA

BIRDUM CKMIDDLE CK

COW CREEK

WYWORRIE

LAKEFIELDELSEY

EAST MATHISON

SCOTT CREEK

WESTMATHISON

MARYRIVERWEST

BLOODWOODDOWNS

SUNDAYCREEK

MARGARETDOWNS

FLORARIVER

LITCHFIELD

DALY RIVER(Mt. Nancar)

TJUWALIYN

UMBRAWARRAGORGE

STRAYCREEK

DOUGLAS RIVER/ DALY RIVER

NITMILUK(Katherine

Gorge)

STRAYCREEK

DALY BASIN

WISOBASIN

HWY.ROPER

ROPERRIVERMataranka

KATHERINE

KATHERINE HWY.

STUART

VICTORIA

Mathison

R I V E R

RIVERDOUGLAS

BambooCreek

BitterSprings Rainbow

Spring

DALYBASIN

GEORGINABASIN

WISO BASIN

100 -100

100 50

-200-300

-400-500

-200 -100 0

DALYRIVER

ADELAIDERIVER

FINNISS RIVER

G8140411G8140411G8140001G8140001

G8140410G8140410G8140409G8140409

G8140312G8140312G8140408G8140408

G8140222G8140222G8140407G8140407

G8140535G8140535

G8140003G8140003

G8140008G8140008G8140038G8140038

G8140040G8140040 G8140042G8140042

G8140044G8140044

G8140060G8140060

G8140063G8140063

G8140067G8140067

G8140098G8140098

G8140157G8140157

G8140161G8140161

G8140169G8140169

G8140205G8140205

G8140538G8140538

G8170008G8170008

G8140011G8140011

G8140022G8140022

G8140025G8140025

G8140068G8140068

G8140086G8140086

G8140152G8140152

G8140158G8140158

G8140536G8140536

G9030001G9030001

G9030176G9030176

G8140159G8140159

750000mE

200000mE

300000mE

700000mE

200000mE 300000mE

8350000mN

800000mE

700000mE

8400000mN

750000mE

8450000mN

8500000mN

800000mE

8450000mN

8400000mN

250000mE

350000mE250000mE

8450000mN

200000mE

8300000mN

8400000mN

8500000mN

200000mE 300000mE 400000mE

8200000mN

200000mE 300000mE 400000mE

700000mE

200000mE 300000mE 400000mE 500000mE

500000mE

200000mE 300000mE

300000mE200000mE

200000mE

700000mE

200000mE

800000mE700000mE

Zone 52 Zone 53

800000mE

Zone 52 Zone 53

800000mE700000mE

Zone 52 Zone 53

750000mE 800000mE

800000mE700000mE 750000mE

700000mE 800000mE

800000mE700000mE

Zone 52 Zone 53

MGA Zone 53MGA Zone 52

200000mE195000mE 205000mE 210000mE

Tindall Water Level TindallWater Level

Cretaceous Sand/Clay CretaceousSand/Clay Cretaceous

Sand/Clay

TindallLimestone

Tindall Water Level

JinduckinWater Level

CretacousSand/Clay

Cretacous Sand/Clay

Oolloo Water Level

DISTANCE (kilometres)0 50

BasaltBasalt

Basalt

SECTION E - F

TindallLimestone

SandstoneJinduckinFormation

TindallLimestone

JinduckinWater Level

)SECTION A - B

DISTANCE (kilometres) 50

TindallLimestone

Siltstone / Sandstone / Granite

Siltstone/

Sandstone / Granite

Jinduckin Formation

Oolloo Dolostone

DISTANCE (kilometres)0 50

SECTION C - D

Cretacous Sand/Clay

Florina Formation

Oolloo Dolostone"Massive Unit"

Tindall

L imestone

Basalt

BasaltJ induck in

Formation

TindallWater Level

OollooDolostone

This product and all material forming part of it is copyright belonging to the Northern Territory of Australia. You may use this material foryour personal, non-commercial use or use it within your organisation for non-commercial purposes, provided that an appropriateacknowledgement is made and the material is not altered in any way. Subject to the fair dealing provisions of the Copyright Act 1968, youmust not make any other use of this product (including copying or reproducing it or part of it in any way) unless you have the writtenpermission of the Northern Territory of Australia to do so.The Northern Territory of Australia does not warrant that the product or any part of it is correct or complete and will not be liable for anyloss damage or injury suffered by any person as a result of its inaccuracy or incompleteness.

C Northern Territory of Australia

This map was producedon the Geocentric Datum

of Australia 1994 (GDA 94)

The Daly, Wiso and Georgina Basins are sedimentary basins. The boundariesbetween them are defined by ridges in the underlying bedrock. This diagramshows the topography of the basin floor and the relationship between the basins.

Total Dissolved Solids is a measure of the mineral salts dissolved inwater. The main constituents in Daly Basin groundwaters are calcium,magnesium and bicarbonate ions. They are derived from the host rockwhich is made up of the minerals dolomite (calcium/magnesiumcarbonate) and calcite (calcium carbonate). The TDS is controlled by therate of recharge and the nature of the rock that hosts the aquifer.

STANDING WATER LEVELWater levels in observation bores vary with time. The levels show an annual cycle; they rise in the wet when the aquifers are recharged and fall during the dry as they drain.Longer term fluctations are related to changes in rainfall. Current groundwater levels are mostly very high, reflecting above average rainfalls experienced since the mid 1970’s.

W A T E R Q U A L I T YMany bores in the rural subdivisionsalong Florina Road tap aquifers in theJinduckin Formation and have elevatedlevels of sodium, chloride and sulphate.This makes some of the waterunsuitable for human consumption. Thesource of these salts are the mineralshalite (sodium chloride) and anhydrite(calicum sulphate) which wereincorporated into the rock when it waslaid down.

NOTES:

1 DOUGLAS HOT SPRINGS - This spring issues from a sandstone aquifer that underlies the Daly Basin and is brought to the surfaceby faulting. The recharge area is some 15km to the north east where the sandstone outcrops. The high temperature of the spring water (50^C)suggests that it comes from a greater depth than other springs in the basin. It also has a low hardness and low Total Dissolved Solids contentindicating that the aquifer does not contain limestone.

2 KATHERINE HOT SPRINGS - On a Dry season morning when the air temperature can drop to 15^C or less, the spring water at 32?Cfeels hot and steam can rise from the water. It is not a true thermal spring however, as the ambient temperature of shallow groundwatersthroughout the region is also about 32^C. Other springs in the basin range between 32^C to 35^C.

3 BITTER SPRINGS - The slightly bitter taste of these waters is due to a higher than normal content of salts of sulphate. The oxygen poorenvironment beneath the surrounding swamp converts some of the sulphate to hydrogen sulphide (rotten egg gas) which can often be smelt in thespring area.

Black numbered lines are 20000 metre intervals of the Map Grid of Australia (MGA)Zones 52 & 53 Universal Transverse Mercator Projection

Horizontal Datum GDA 94

0 10 20 30 40

kilometres50

kilometres10

END OF DRY SEASON FLOWSThe lowest river flow recorded each year occurs just before the first substantial rains of the wet season, typically in October or November. At that time all of the water is sourcedfrom groundwater, via springs and seepage into the river bed. This graph shows how flows progressively increase as the river passes across the Daly Basin. It also shows thatthe flows are directly related to rainfall and that flows over the past 30 years are probably higher than the long term average.

For further information contact:Water Resources, Department of Land Resource Management

4th Floor Goyder Centre, 25 Chung Wah Terrace,Palmerston, Northern Territory.

T: (08) 8999 4455 Email: waterresources@nt.gov.auPO Box 496, Palmerston, NT 0831

Water Bore

Water Level Monitoring Bore

Stream gauging station

Spring

Line of Cross-section

End of Dry Season River Flows

0.01 to 0.1 cumecs

0.1 to 1.0 cumecs

1.0 to 10.0 cumecs

BASurfacewater Catchment - Name / Boundary

G9030176

DALY BASIN AQUIFERS

FLORINA FORMATIONFractured rock local aquifers, yields to 20 L/s.Moderate sucess rate. Limestones locallycavernous. Limestone and glauconiticsandstone

OOLLOO DOLOSTONE

Fractured and cavenous aquifer, yields up to50 L/s. Moderate success rate. The aquifer isconfined by Jinduckin Formation in this zone.The inner margin approximates the pointswhere the limestone is 150 metres belowground level. Shallow aquifers in the JinduckinFormation may also be present.

Fractured and cavenous aquifer, yields up to50 L/s. Moderate to high success rate. Theaquifer is largely unconfined in this zone

Fractured rock local aquifers, yields up to 5 L/s.Minor interbedded limestone, fractured andcavenous aquifers, yields up to 20 L/s.Moderate to low success rate.

JINDUCKIN FORMATION

TINDALL LIMESTONE

Up to 0.01 cumecs

AQUIFERS

WATER RESOURCES FEATURES

Railway

Gas Pipeline

Property Boundary

Station Homestead

Powerline

MountainMt Bowman

Park or Reserve

GENERAL FEATURES

Major Aboriginal Community

Minor Aboriginal Community

Major Town

Minor Town

Roadhouse

Highway

Major road

Family Outstation

Minor Road - Sealed

Minor Road - Unsealed

ELEVATION of the FLOOR of the DALY BASIN

20 60 kmkm 0 40

100 Metres above / below sealevel AHD of the base

of the Tindall Limestone

20 60 kmkm 0 40

TINDALL AQUIFER GROUNDWATER ELEVATION

Daly Basin

Flow DirectionTindall Aquifer

Discharge Zone

Monitoring Bore

Oolloo Aquifer

Groundwater level(m AHD)110

OOLLOO AQUIFER GROUNDWATER ELEVATION TOTAL DISSOLVED SOLIDS in GROUNDWATER in theOOLLOO and TINDALL AQUIFERS

200 - 500 mg/L

500 - 800 mg/L

500 - 1500 mg/L

Daly Basin

Note: 1 cumec = 1000 litres/second

Daly Basin

Basin divide

Daly Basin

Flow Direction

Discharge Zone

Monitoring Bore

Oolloo Aquifer

Groundwater level (m AHD)

KATHERINE

NHULUNBUY

JABIRUDARWIN

NORTHERN

TERRITORY

TENNANT CREEK

ALICE SPRINGS

PINE CREEKSD 52-08

MOUNTEVELYN

SD 53-05

MOUNTMARUMBASD 53-06

FERGUSSONRIVER

SD 52-12

KATHERINESD 53-09

URAPUNGASD 53-10

DELAMERESD 52-16

LARRIMAHSD 53-13

HODGSON DOWNSSD 53-14

VICTORIARIVER DOWNS

SE 52-04

DALY WATERSSE 53-01

TANUMBIRINISE 53-02

MAPLOCALITY

Pastoral Station nameFLORINA

Hayes Creek

Dorisvale

Katherine

Pine Creek

Nauiyu

Binjari

Djarrung

INDEX TO 250KMAPSHEETS

10 30 kmkm 0 20

20 60 kmkm 0 40

SEEKATHERINE

REGION INSETFOR DETAIL

Minor porous sand aquifers but mostlyunsaturated. Sand and clay. Recharge to theunderlying Daly Basin is restricted whereclay is dominant.

Licensed Water Bore (as of 2011)

Oolloo Aquifer

Tindal Aquifer

KATHERINE REGION

WATER YEAR

RN 7595Confined by Cretaceuos Clays

OOLLOO AQUIFER - STANDING WATER LEVELRN 21717Unconfined

See main map for bore locations

WATER YEAR

TINDAL AQUIFER - STANDING WATER LEVELRN 29429Unconfined

See main map and Katherine Regionmap for bore locations

RN 22006Confined by Cretaceous Clays

RN 22397Confined by Jinduckin Formation

Rainfall; 2 yearmoving average

Daly River at Mount NancarG8140040

Daly River at Dorisvale CrossingG8140067

Katherine River at the old Railway BridgeG8140001

END of the DRY SEASON FLOWS in the DALY RIVER 1961 to 2010

Sedimentary Basin Boundary

Prepared and ProducedPrepared and Produced

APRIL 2016APRIL 2016

Hydrogeologist: S. Tickell,Water Resources Division, Department of Land Resource Management,

Northern Territory of Australia

Hydrogeologist: S. Tickell,Water Resources Division, Department of Land Resource Management,

Northern Territory of Australia

Revisions and updates have been made since the initial publicationof this map in May 2007

Major widespread cavernous aquifer. Yields to100 L/s. Moderate to high sucess rate.Dolostone.

Cartography: L. J. Fritz July 2016

Spatial Data & Mapping, Water Resources Division,

Department of Land Resource Management, Goyder Centre, Palmerston, Northern Territory

Internet: www.lrm.nt.gov.au/nrmapsnt Map Reference: Daly-Basin-Aquifers

1 DOUGLAS HOT SPRINGS - ntlis.nt.gov.au

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