23
North Lowther Energy Initiative: Appendix 4.1 Borrow Pit Assessment Prepared by Mouchel Morrison House Lanark Court Ellismuir Way Tannochside Business Park Uddingston Glasgow G71 5PW T 01698 802850 W www.mouchel.com

North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

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Page 1: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nor

th L

owth

er E

nerg

y In

itiat

ive:

A

ppen

dix

4.1

Bor

row

Pit

Ass

essm

ent

Pre

pare

d by

M

ouch

el

Mor

rison

Hou

se

Lana

rk C

ourt

El

lism

uir W

ay

Tann

ochs

ide

Busi

ness

Par

k U

ddin

gsto

n G

lasg

ow

G71

5PW

T

016

98 8

0285

0 W

ww

w.m

ouch

el.c

om

Page 2: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

ii

Doc

umen

t Con

trol S

heet

Pr

ojec

t Titl

e N

orth

Low

ther

Ene

rgy

Initi

ativ

e R

epor

t Titl

e Bo

rrow

Pit

Asse

ssm

ent

Rev

isio

n 3

Stat

us

Fina

l C

ontro

l Dat

e 09

/05/

2017

R

ecor

d of

Issu

e Is

sue

Stat

us

Auth

or

Dat

e C

heck

D

ate

Auth

oris

ed

Dat

e

1 D

raft

I Mur

ch

K Zu

k 28

/03/

17

G M

cGov

ern

31/0

3/17

B

Seed

hous

e S

Bone

04

/04/

17

07/0

4/17

2 D

raft

I Mur

ch

K Zu

k S

Bone

04/0

5/17

S

Bone

04

/05/

17

S Bo

ne

04/0

5/17

3 Fi

nal

I Mur

ch

K Zu

k S

Bone

08/0

5/17

S

Bone

08

/05/

17

S Bo

ne

09/0

5/17

Dis

trib

utio

n O

rgan

isat

ion

Con

tact

C

opie

s La

nd U

se C

onsu

ltant

s Ka

te W

igle

y 1

2020

Ren

ewab

les

Ian

Sim

ms

1 Th

is re

port

is p

rese

nted

to L

and

Use

Con

sulta

nts

(ref

erre

d to

from

this

poi

nt a

s LU

C) i

n re

spec

t of N

orth

Low

ther

E

nerg

y In

itiat

ive

and

may

not

be

used

or

relie

d on

by

any

othe

r pe

rson

or

by th

e cl

ient

in r

elat

ion

to a

ny o

ther

m

atte

rs n

ot c

over

ed s

peci

fical

ly b

y th

e sc

ope

of th

is re

port.

Not

with

stan

ding

any

thin

g to

the

cont

rary

con

tain

ed in

the

repo

rt, M

ouch

el L

td is

obl

iged

to e

xerc

ise

reas

onab

le

skill,

car

e an

d di

ligen

ce in

the

perfo

rman

ce o

f the

ser

vice

s re

quire

d.

LUC

and

Mou

chel

Ltd

sha

ll no

t be

liab

le

exce

pt to

the

exte

nt th

at th

ey h

ave

faile

d to

exe

rcis

e re

ason

able

ski

ll, c

are

and

dilig

ence

, and

this

repo

rt sh

all b

e re

ad a

nd c

onst

rued

acc

ordi

ngly

.

This

repo

rt ha

s be

en p

repa

red

by M

ouch

el L

td.

No

indi

vidu

al is

per

sona

lly li

able

in c

onne

ctio

n w

ith th

e pr

epar

atio

n of

this

repo

rt. B

y re

ceiv

ing

this

repo

rt an

d ac

ting

on it

, the

clie

nt o

r any

oth

er p

erso

n ac

cept

s th

at n

o in

divi

dual

is

pers

onal

ly li

able

whe

ther

in c

ontra

ct, t

ort,

for b

reac

h of

sta

tuto

ry d

uty

or o

ther

wis

e.

Page 3: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

iii

Con

tent

s D

ocum

ent C

ontr

ol S

heet

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.. ii

Con

tent

s iii

Phot

ogra

phs

iii

Tabl

es

iii

1 In

trod

uctio

n ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

1

2 Pr

ojec

t Met

hod .

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 1

3 D

esk

Stud

y ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

. 2

3.1

Geo

logy

.....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

2

Drif

t Geo

logy

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 2

B

edro

ck G

eolo

gy ...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

2 St

ruct

ural

Geo

logy

.....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

. 2

Min

eral

Dep

osits

and

wor

king

s ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

2

3.2

Hyd

roge

olog

y ...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.....

2

3.3

Peat

Sta

bilit

y an

d La

ndsl

ide

Susc

eptib

ility .

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.....

2

3.4

Suita

bilit

y of

Bed

rock

as

Aggr

egat

e ...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

. 2

4 En

gine

erin

g G

eolo

gy W

alko

ver S

urve

y ...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

... 3

4.1

BP01

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 3

4.2

BP02

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 4

4.3

BP03

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 5

4.4

BP04

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 6

4.5

BP05

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 7

5 As

sess

men

t of P

oten

tial B

orro

w P

it Lo

catio

ns ..

......

......

......

......

......

......

......

......

......

......

......

......

......

......

... 8

5.1

Intro

duct

ion .

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.....

8

5.2

Acce

ss A

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 8

Asse

ssm

ent o

f BP0

1 ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

..... 8

As

sess

men

t of B

P02 .

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.. 8

5.3

Acce

ss B

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 9

Asse

ssm

ent o

f BP0

3 ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

..... 9

As

sess

men

t of B

P04 .

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.. 9

Asse

ssm

ent o

f BP0

5 ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

..... 9

6 C

oncl

usio

ns a

nd R

ecom

men

datio

ns ..

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

10

7 G

eote

chni

cal R

isk

Reg

iste

r ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.. 11

8 R

efer

ence

s ...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

13

Appe

ndix

A:

Figu

res

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

... 1

4

Phot

ogra

phs

Phot

ogra

ph 1

. Ph

otog

raph

look

ing

north

wes

t sho

win

g po

tent

ial b

orro

w p

it lo

catio

n (B

P01)

.....

......

......

......

......

......

. 3

Phot

ogra

ph 2

. Ph

otog

raph

sho

win

g to

psoi

l with

sub

angu

lar g

rave

l (BP

01) ..

......

......

......

......

......

......

......

......

......

......

3 Ph

otog

raph

3.

Phot

ogra

ph lo

okin

g no

rthw

est s

how

ing

com

pete

nt b

edro

ck a

rea

and

ram

p of

wor

ked

mat

eria

l po

ssib

ly s

uita

ble

for u

se (B

P02)

.....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

... 4

Phot

ogra

ph 4

. Ph

otog

raph

indi

catin

g co

nditi

on w

here

stro

ng a

nd v

ery

stro

ng g

reyw

acke

is e

ncou

nter

ed (B

P02)

.. 4

Phot

ogra

ph 5

. Ph

otog

raph

look

ing

wes

t sho

win

g co

mpe

tent

bed

rock

are

a (B

P03)

. ....

......

......

......

......

......

......

......

.. 5

Phot

ogra

ph 6

. Ph

otog

raph

indi

catin

g de

taile

d vi

ew a

nd th

e si

ze o

f gre

ywac

ke ru

bble

(BP0

3). .

......

......

......

......

......

5 Ph

otog

raph

7.

Phot

ogra

ph lo

okin

g w

est s

how

ing

expo

sed

bedr

ock

(BP0

4). ..

......

......

......

......

......

......

......

......

......

.... 6

Ph

otog

raph

8.

Phot

ogra

ph s

how

ing

back

s sc

arp

and

deta

iled

view

of g

reyw

acke

(BP0

4). ..

......

......

......

......

......

......

6 Ph

otog

raph

9.

Phot

ogra

ph lo

okin

g no

rthw

est s

how

ing

expo

sed

bedr

ock

(BP0

5). ..

......

......

......

......

......

......

......

......

.. 7

Phot

ogra

ph 1

0.Ph

otog

raph

sho

win

g de

taile

d vi

ew o

f gre

ywac

ke (B

P05)

. ....

......

......

......

......

......

......

......

......

......

......

. 7

Tabl

es

Tabl

e 1.

Pro

spec

tive

borro

w p

it lo

catio

ns ..

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 1

Ta

ble

2. G

eolo

gica

l site

sum

mar

y ....

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.. 2

Tabl

e 3.

Ind

icat

ive

BP01

Dim

ensi

ons

and

Extra

ctio

n Vo

lum

es ...

......

......

......

......

......

......

......

......

......

......

......

......

......

8 Ta

ble

4. I

ndic

ativ

e BP

02 D

imen

sion

s an

d Ex

tract

ion

Volu

mes

......

......

......

......

......

......

......

......

......

......

......

......

......

... 8

Tabl

e 5.

Ind

icat

ive

BP03

Dim

ensi

ons

and

Extra

ctio

n Vo

lum

es ...

......

......

......

......

......

......

......

......

......

......

......

......

......

9 Ta

ble

6. I

ndic

ativ

e BP

04 D

imen

sion

s an

d Ex

tract

ion

Volu

mes

......

......

......

......

......

......

......

......

......

......

......

......

......

... 9

Tabl

e 7.

Ind

icat

ive

BP05

Dim

ensi

ons

and

Extra

ctio

n Vo

lum

es ...

......

......

......

......

......

......

......

......

......

......

......

......

......

9 Ta

ble

8 G

eote

chni

cal R

isk

Eval

uatio

n M

atric

es...

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

......

.... 1

1

Page 4: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

1

1 In

trodu

ctio

n Th

is re

port

form

s an

App

endi

x to

Cha

pter

4: S

chem

e D

escr

iptio

n fo

r Nor

th L

owth

er E

nerg

y In

itiat

ive

(LU

C, 2

017)

an

d sh

ould

be

read

with

refe

renc

e to

this

cha

pter

.

Nor

th L

owth

er E

nerg

y In

itiat

ive

(NLE

I) (th

e D

evel

opm

ent)

is a

join

t ven

ture

bet

wee

n 20

20 R

enew

able

s Li

mite

d an

d Bu

ccle

uch

Esta

tes

Lim

ited

and

is p

ropo

sing

to d

evel

op a

35

turb

ine

win

d fa

rm o

n la

nd o

wne

d by

Buc

cleu

ch

Esta

te.

The

prop

osed

Dev

elop

men

t is

situ

ated

on

the

Low

ther

Hills

in D

umfri

es a

nd G

allo

way

. The

site

is lo

cate

d be

twee

n Sa

nquh

ar a

nd W

anlo

ckhe

ad. T

he s

ite c

ompr

ises

an

area

par

tially

cov

ered

by

fore

stry

in th

e no

rthw

est o

f the

site

an

d m

oorla

nd w

ith s

teep

-sid

ed h

ills a

nd v

alle

ys in

the

rem

aind

er. F

igur

e 4.

1.1

incl

uded

in A

ppen

dix

A pr

ovid

es th

e pr

opos

ed a

rrang

emen

t of t

he D

evel

opm

ent.

Ther

e ar

e 3

spin

e tra

cks

prop

osed

pro

vidi

ng a

cces

s to

the

win

dfar

m. A

cces

s A

prov

ides

acc

ess

to th

e tw

o no

rther

n ar

rays

. The

nor

th m

ost t

rack

pro

vide

s ac

cess

to T

urbi

ne 3

2 to

35,

the

cent

ral t

rack

Tur

bine

s 10

to 3

1. A

cces

s B

prov

ide

acce

ss to

Tur

bine

1 to

9 in

the

sout

h of

the

site

.

To m

inim

ise

the

volu

me

of im

porte

d m

ater

ial b

roug

ht o

nto

the

site

and

any

sub

sequ

ent e

nviro

nmen

tal i

mpa

ct, s

ite-

won

agg

rega

te w

ill be

use

d fo

r co

nstru

ctio

n. A

ggre

gate

will

be r

equi

red

for

the

cons

truct

ion

of a

cces

s tra

cks,

tu

rbin

e ba

se b

ack-

fill,

com

poun

ds a

nd h

ards

tand

ing

area

s. I

t ha

s be

en c

alcu

late

d th

at t

he c

ut a

nd f

ill tra

ck

cons

truct

ion

met

hod

alon

e w

ill no

t ge

nera

te s

uffic

ient

agg

rega

te.

Ther

efor

e, t

here

is

a ne

ed f

or a

dditi

onal

ex

cava

tion

of a

ggre

gate

mat

eria

l. As

a re

sult,

11

borro

w p

it se

arch

are

as w

ere

prop

osed

, how

ever

site

con

stra

ints

re

sulte

d in

6 o

f th

e 11

loc

atio

ns b

eing

dee

med

uns

uita

ble

for

reas

ons

outli

ned

with

in T

able

2 i

n Se

ctio

n 4.

Th

eref

ore,

this

repo

rt fo

cuse

s on

the

5 pr

efer

red

site

s.

Mou

chel

Ltd

was

com

mis

sion

ed to

und

erta

ke a

bor

row

pit

asse

ssm

ent f

or th

is d

evel

opm

ent s

ite.

The

aim

s of

this

as

sess

men

t wer

e to

pro

vide

:

Pr

elim

inar

y as

sess

men

t of t

he s

uita

bilit

y of

the

bedr

ock

as a

road

bui

ldin

g m

ater

ial;

Po

tent

ial b

orro

w p

it lo

catio

ns;

In

dica

tive

borro

w p

it di

men

sion

s;

In

dica

tive

extra

ctio

n vo

lum

es;

Es

timat

es o

f ove

rbur

den

at b

orro

w p

it lo

catio

ns;

In

dica

tion

of p

oten

tial e

xtra

ctio

n m

etho

ds;

R

ecom

men

datio

ns fo

r geo

tech

nica

l tes

ting;

and

Pr

elim

inar

y bo

rrow

pit

re-in

stat

emen

t and

reha

bilit

atio

n pr

opos

als.

This

doc

umen

t ou

tline

s M

ouch

el’s

met

hod

for

borro

w p

it as

sess

men

t al

ong

with

the

ana

lysi

s un

derta

ken;

co

nclu

sion

s dr

awn

and

reco

mm

enda

tions

for b

orro

w p

it de

sign

and

loca

tions

.

It sh

ould

be

note

d th

at a

ll bo

rrow

pit

info

rmat

ion

prov

ided

with

in th

is re

port

is in

dica

tive

only

, and

is b

ased

on

desk

st

udy

and

reco

nnai

ssan

ce s

urve

y al

one.

No

intru

sive

inve

stig

atio

n ha

s be

en c

arrie

d ou

t, an

d co

nseq

uent

ly th

e su

itabi

lity

of th

e ro

ck, s

ugge

sted

ext

ract

ion

met

hods

and

vol

umes

are

bro

ad e

stim

ates

and

sho

uld

be tr

eate

d as

su

ch.

It is

sta

ndar

d pr

actic

e fo

r de

taile

d ge

otec

hnic

al s

ite in

vest

igat

ion

to c

onfir

m f

inal

des

ign

for

cons

truct

ion

to b

e un

derta

ken

post

-con

sent

and

prio

r to

con

stru

ctio

n an

d th

e in

form

atio

n pr

ovid

ed w

ithin

this

rep

ort i

s co

nsid

ered

su

ffici

ent f

or u

se a

t the

app

licat

ion

stag

e.

2 Pr

ojec

t Met

hod

The

proj

ect i

nvol

ved

a de

sk s

tudy

and

an

engi

neer

ing

geol

ogic

al w

alko

ver s

urve

y. T

he d

esk

stud

y co

nsis

ted

of a

re

view

of i

nfor

mat

ion

with

rega

rd to

the

iden

tifie

d si

te w

hich

incl

uded

:

Br

itish

Geo

logi

cal S

urve

y So

lid a

nd D

rift G

eolo

gy M

ap 1

:50,

000

Shee

t 15E

, geo

logi

cal m

appi

ng, b

edro

ck,

supe

rfici

al a

nd li

near

geo

logy

;

Br

itish

Geo

logi

cal S

urve

y G

eoIn

dex

onlin

e da

taba

se, 2

017;

Br

itish

Geo

logi

cal S

urve

y D

igita

l Hyd

roge

olog

ical

Map

of S

cotla

nd, 1

:625

,000

sca

le; a

nd

So

il Su

rvey

of S

cotla

nd 1

:250

,000

She

et 7

, map

ping

of s

oil t

ypes

and

land

cap

abilit

y fo

r agr

icul

ture

.

Dur

ing

the

desk

stu

dy p

oten

tial l

ocat

ions

for

borro

w p

its w

ere

iden

tifie

d ac

ross

the

site

for

furth

er in

vest

igat

ion

durin

g th

e en

gine

erin

g w

alko

ver s

urve

y. T

he lo

catio

ns h

ave

been

out

lined

in T

able

1 b

elow

.

Tabl

e 1.

Pro

spec

tive

borr

ow p

it lo

catio

ns

ID

Loca

tion

Com

men

ts

East

ing

Nor

thin

g

BP0

1 28

3276

61

8002

N

o ex

pose

d be

droc

k

BP0

2 28

2568

61

6537

Pr

evio

us e

xtra

ctio

n lo

catio

n

BP0

3 28

1349

61

4841

Pr

evio

us e

xtra

ctio

n lo

catio

n

BP0

4 28

1640

61

4458

Pr

evio

us e

xtra

ctio

n lo

catio

n

BP0

5 28

1957

61

3602

Pr

evio

us e

xtra

ctio

n lo

catio

n

BPA

B1

2818

96

6134

94

Res

trict

ed b

y w

ater

cour

se.

BPF

1 28

2632

61

3217

D

isco

unte

d at

Des

k S

tudy

sta

ge –

not

pra

ctic

al g

iven

ups

lope

st

abili

ty /

pote

ntia

l ben

chin

g re

quire

men

ts. L

ands

lide

Sus

cept

ibili

ty A

sses

smen

t (R

ef: 1

0739

83-0

03-0

01)

BPI

1 28

2555

61

6242

D

isco

unte

d at

Des

k S

tudy

sta

ge –

no

expo

sed

bedr

ock

BPK

1 28

1622

61

4284

D

isco

unte

d at

Des

k S

tudy

sta

ge –

no

expo

sed

bedr

ock

BPM

1 28

4159

61

5714

U

nsui

tabl

e ge

olog

y

BPA

A1

2828

90

6152

76

Pos

ition

ed o

n S

outh

ern

Upl

and

Way

1

Uns

uita

ble

borr

ow p

it lo

catio

ns

The

stud

y ar

ea fo

r thi

s as

sess

men

t con

sist

ed o

f the

are

a en

clos

ed b

y th

e si

te b

ound

ary.

A si

te v

isit

was

und

erta

ken

on 1

2th a

nd 1

3th O

ctob

er 2

016

by a

Mou

chel

eng

inee

ring

geol

ogis

t. T

he s

ite v

isit

cons

iste

d of

a w

alko

ver s

urve

y in

clud

ing

a vi

sual

insp

ectio

n of

the

pote

ntia

l bor

row

pit

loca

tions

.

Page 5: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

2

3 D

esk

Stud

y 3.

1 G

eolo

gy

The

drift

and

sol

id g

eolo

gy a

cros

s th

e si

te e

xten

ts h

ave

been

ass

esse

d us

ing

geol

ogic

al m

ap fo

r the

are

a ob

tain

ed

from

the

Briti

sh G

eolo

gica

l Soc

iety

(BG

S) (2

005)

, and

pub

licly

ava

ilabl

e ge

olog

ical

info

rmat

ion

from

the

BGS

onlin

e ai

d G

eoIn

dex

(201

7).

Drif

t Geo

logy

Geo

logi

cal m

appi

ng a

vaila

ble

on G

eoin

dex

indi

cate

s th

at th

e la

rge

maj

ority

of d

rift d

epos

its a

re u

ncla

ssifi

ed a

cros

s th

e si

te.

In t

he v

alle

ys a

nd lo

wer

gro

und

acro

ss t

he s

ite g

laci

al t

ill: d

iam

icto

n de

posi

ts is

not

ed.

Typi

cally

thi

s co

mpr

ises

stif

f, un

sorte

d an

d ov

erco

nsol

idat

ed w

ith v

ario

us g

rain

siz

es fr

om c

lay

to g

rave

l and

bou

lder

.

Allu

vium

dep

osits

are

not

ed a

long

exi

stin

g w

ater

cou

rses

in th

e va

lley

floor

s. T

hese

are

like

ly to

com

pris

e gr

avel

an

d co

bble

s, w

ith s

ome

sand

and

silt

form

ed o

n flo

od p

lain

s.

Gen

eral

ly s

hallo

w p

eat i

s re

cord

ed u

pon

the

high

er g

roun

d, in

par

ticul

ar in

the

north

ern

and

north

-wes

t fac

ing

slop

es. P

eat p

robi

ng u

nder

take

n to

dat

e by

Mou

chel

indi

cate

s av

erag

e de

pths

of 0

.44m

acr

oss

the

Dev

elop

men

t Ar

ea.

Avai

labl

e ge

olog

ical

map

ping

indi

cate

s th

at th

e la

rge

maj

ority

of s

uper

ficia

l dep

osits

are

unc

lass

ified

acr

oss

the

site

.

Bed

rock

Geo

logy

The

bedr

ock/

solid

geo

logy

of t

he s

ite h

as b

een

sum

mar

ised

in F

igur

e 4.

1.1

and

Tabl

e 2

belo

w a

long

with

the

resp

ectiv

e lo

catio

ns w

here

this

is e

xpec

ted

on th

e si

te.

Tabl

e 2.

Geo

logi

cal s

ite s

umm

ary

Geo

logi

cal G

roup

Ag

e G

eolo

gica

l Des

crip

tion

1 R

egio

n of

Si

te

Cla

ckm

anna

n G

roup

C

arbo

nife

rous

Sa

ndst

one,

silt

ston

e, m

udst

one

and

coal

; pe

bbly

bas

e W

est

Nor

th B

ritai

n Si

luro

-Dev

onia

n C

alc-

Alka

line

Dyk

e Su

ite

Silu

rian

- D

evon

ian

Fels

ite

Sout

heas

t

Mof

fat S

hale

Gro

up

Ord

ovic

ian

- Si

luria

n M

udst

one,

bla

ck a

nd d

ark

grey

silt

y, lo

cally

w

ith th

in c

hert

beds

. So

uth

Scau

r Gro

up

(Por

tpat

rick

Form

atio

n)

Ord

ovic

ian

Gre

ywac

ke s

ands

tone

, med

ium

- to

thic

k-be

dded

, cha

ract

eris

ed b

y fin

e-gr

aine

d an

desi

tic li

thoc

last

s.

Sout

h an

d Ea

st

Bar

rhill

Gro

up

(Kirc

olm

For

mat

ion

& S

poth

fore

m

embe

r) O

rdov

icia

n

Gre

ywac

ke s

ands

tone

, med

ium

- to

thin

-be

dded

, qua

rtzos

e w

ith s

ome

thic

k si

ltsto

ne in

terc

alat

ions

; che

rt be

ds a

nd

brec

cio

–con

glom

erat

e

Nor

th a

nd

Wes

t

Cra

wfo

rd G

roup

O

rdov

icia

n C

hert,

red

and

grey

ish,

bed

ded

with

red

brow

n m

udst

one,

loca

lly c

herty

; rar

e in

terb

edde

d ba

salti

c pi

llow

lava

s.

East

1 D

escr

iptio

n as

not

ed o

n B

GS

Sol

id a

nd D

rift G

eolo

gy m

ap (2

005)

.

Stru

ctur

al G

eolo

gy

The

site

is in

the

regi

on o

f the

Sou

ther

n U

plan

d Fa

ult,

whi

ch s

epar

ates

the

Mid

land

Val

ley

from

the

Sout

hern

U

plan

d te

rrane

s. T

he fa

ults

ass

ocia

ted

with

the

Sout

hern

Upl

and

Terra

nes

are

reco

rded

as

an im

bric

ated

faul

t st

ack

(Flo

yd, 2

003)

, in

the

area

of t

he s

ite th

ese

com

pris

e (fr

om n

orth

to s

outh

) the

Sou

ther

n U

plan

d Fa

ult,

Car

cow

fa

ult a

nd L

eadh

ills fa

ult.

Ther

e ar

e m

ultip

le f

ault

zone

s as

soci

ated

with

eac

h of

the

se f

aults

, ho

wev

er t

he f

ault

trace

s w

ith e

ach

trend

ap

prox

imat

ely

sout

hwes

t to

north

east

. The

Sou

ther

n U

plan

d fa

ult a

nd C

arco

w fa

ult c

ut th

roug

h th

e no

rth o

f the

si

te, w

ith th

e Le

adhi

lls fa

ult c

uttin

g th

roug

h th

e so

uth

east

of t

he s

ite. T

he S

outh

ern

Upl

and

faul

t is

note

d as

hav

ing

had

strik

e-sl

ip, n

orm

al a

nd re

vers

e m

ovem

ent a

ssoc

iate

d w

ith it

(Flo

yd, 2

003)

. The

Car

cow

faul

t is

note

d as

hav

ing

a no

rmal

sen

se o

f mov

emen

t, an

d th

e Le

adhi

lls is

not

ed a

s a

reve

rse

faul

t.

Min

eral

Dep

osits

and

wor

king

s

A sp

ecifi

c M

inin

g D

esk

Stud

y (R

ef: 1

0739

83/G

EO/R

00)

was

car

ried

out d

ated

Aug

ust 2

016.

Ref

er to

this

for

a de

taile

d ou

tline

of t

he m

iner

al d

epos

its a

ffect

ing

the

site

. The

repo

rt no

tes

that

the

unde

rgro

und

and

surfa

ce m

ine

wor

king

s ar

e co

nfin

ed to

are

as w

here

min

eral

lode

s ar

e pr

esen

t im

med

iate

ly w

est o

f Wan

lock

head

and

in th

e W

anlo

ck W

ater

Val

ley.

As

such

, the

se a

re n

ot e

xpec

ted

to im

pact

upo

n th

e pr

opos

ed b

orro

w p

it lo

catio

ns.

3.2

Hyd

roge

olog

y

Hyd

roge

olog

ical

info

rmat

ion

is s

umm

aris

ed fr

om B

GS

(198

8, 2

017)

, and

fiel

d ob

serv

atio

ns.

As re

cord

ed in

Sec

tion

3.1.

2, m

uch

of th

e si

te is

und

erla

in b

y th

e gr

eyw

acke

. Thi

s is

reco

rded

as

a lo

w p

rodu

ctiv

ity

aqui

fer.

Gro

undw

ater

is re

cord

ed a

s be

ing

conf

ined

to n

ear s

urfa

ce c

rack

s an

d jo

ins.

The

glac

ial t

ill an

d al

luvi

um d

epos

its p

rese

nt o

n th

e lo

wer

slo

pes

are

likel

y to

be

high

ly v

aria

ble

in c

ompo

sitio

n an

d m

ay c

onta

in l

ense

s of

san

d an

d gr

avel

whi

ch c

an s

uppo

rt pe

rche

d w

ater

tab

les.

The

se a

re l

ikel

y to

be

disc

ontin

uous

and

lim

ited

in e

xten

t and

will

limit

grou

ndw

ater

pot

entia

l. Th

e va

riabl

e co

mpo

sitio

n of

the

supe

rfici

al

depo

sits

indi

cate

s th

at it

may

act

as

a co

nfin

ing

laye

r to

the

unde

rlyin

g be

droc

k ge

olog

y in

som

e ar

eas.

Whe

re p

eat d

epos

its o

ccur

they

are

gen

eral

ly s

atur

ated

with

wat

er, r

esul

ting

in a

sha

llow

wat

er ta

ble

clos

e to

or

at g

roun

d su

rface

. Whe

re p

eat

is u

nder

lain

by

low

per

mea

bilit

y be

droc

k an

d su

perfi

cial

dep

osits

gro

undw

ater

in

filtra

tion

is li

kely

to b

e po

or w

ith ra

infa

ll lik

ely

to tr

ansl

ate

into

rapi

d su

rface

runo

ff. L

ater

al s

eepa

ge o

f wat

er in

th

ese

peat

dep

osits

may

influ

ence

loca

l wat

erco

urse

s.

3.3

Peat

Sta

bilit

y an

d La

ndsl

ide

Susc

eptib

ility

A Pe

at S

tabi

lity

Asse

ssm

ent h

as b

een

prep

ared

for t

his

proj

ect,

asse

ssin

g pe

at d

epth

s an

d pe

at s

tabi

lity

issu

es in

in

frast

ruct

ure

area

s ac

ross

the

Dev

elop

men

t Are

a, p

rovi

ded

as A

ppen

dix

7.2

of th

e En

viro

nmen

tal S

tate

men

t.

3.4

Suita

bilit

y of

Bed

rock

as

Aggr

egat

e

The

maj

ority

of t

he s

ite c

ompr

ises

gre

ywac

ke. T

his

is a

n in

here

ntly

var

iabl

e ro

ck, a

s it

repr

esen

ts a

seq

uenc

e of

ge

olog

y ra

ngin

g fro

m m

udst

one

to s

ands

tone

.

A re

quire

men

t whe

n us

ing

grey

wac

kes

as a

ggre

gate

is th

at th

ey h

ave

high

stre

ngth

, low

por

osity

and

whe

re u

sed

for

pave

men

t wea

ring

cour

se, s

houl

d be

res

ista

nt to

pol

ishi

ng (

Smith

et a

l., 2

001)

. Whe

re m

udst

one

/ silt

ston

e ba

nds

are

enco

unte

red,

thes

e w

ould

requ

ire fu

rther

ass

essm

ent –

the

suita

bilit

y w

ill de

pend

on

the

thic

knes

s an

d fre

quen

cy o

f th

e m

udst

one

and

the

degr

ee o

f w

eath

erin

g. W

here

mud

ston

e be

ds a

re t

hick

and

wea

ther

ed,

sele

ctiv

e w

orki

ng m

ay b

e po

ssib

le to

sep

arat

e ou

t the

uns

uita

ble

mat

eria

ls, b

ut th

is m

ay n

ot b

e pr

actic

able

whe

re

the

beds

are

thin

. A s

mal

l am

ount

of f

resh

mud

ston

e in

the

exca

vate

d m

ater

ial w

ill no

t be

a hu

ge p

robl

em fo

r use

as

cap

ping

but

may

cau

se is

sues

with

mee

ting

Los

Ange

les

Coe

ffici

ent r

equi

rem

ents

for T

ype

1 su

bbas

e. T

hin

beds

of w

eath

ered

mat

eria

l may

cau

se is

sues

with

fine

s co

nten

t in

the

exca

vate

d m

ater

ial.

Page 6: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

3

4 En

gine

erin

g G

eolo

gy W

alko

ver S

urve

y A

wal

kove

r su

rvey

of t

he s

ite w

as c

ondu

cted

on

12th a

nd 1

3th O

ctob

er 2

016

by a

Mou

chel

con

sulta

nt d

urin

g a

perio

d of

dry

wea

ther

. Vi

sual

insp

ectio

ns, p

hoto

grap

hs a

nd d

etai

led

field

not

es w

ere

take

n re

porti

ng th

e ge

olog

ical

as

pect

s of

eac

h of

the

iden

tifie

d lo

catio

ns.

A ha

nd-h

eld

GPS

was

use

d to

obt

ain

OS

grid

coo

rdin

ates

for l

ocat

ions

to

whi

ch p

rovi

de <

30m

acc

urac

y.

Elev

en p

oten

tial b

orro

w p

it se

arch

are

as w

ere

cons

ider

ed a

s ou

tline

d in

Sec

tion

2. T

hey

are

all l

ocat

ed w

ithin

the

the

wes

t and

nor

th o

f the

site

.

4.1

BP0

1

Borro

w p

it BP

01 is

loca

ted

with

in th

e no

rth e

ast o

f the

site

, cen

tred

at O

S co

ordi

nate

s 28

3276

618

002.

Thi

s lo

catio

n is

a g

entle

hills

ide

with

no

bedr

ock

expo

sed.

The

loca

tion

is w

ithin

a d

efor

este

d ar

ea a

djac

ent t

o an

exi

stin

g fo

rest

trac

k. T

he m

ain

axis

wou

ld b

e no

rth to

sou

th.

Due

to li

mite

d si

te o

bser

vatio

ns a

s no

bed

rock

is e

xpos

ed, t

he d

epth

of s

urfa

ce c

over

and

the

desc

riptio

n of

rock

w

ere

not p

ossi

ble

to b

e de

term

ined

at t

his

loca

tion.

Geo

logi

cal m

appi

ng a

vaila

ble

on B

GS

Geo

Inde

x in

dica

tes

that

th

e ar

ea is

und

erla

in b

y gr

eyw

acke

bel

ongi

ng to

Kirk

colm

For

mat

ion.

A fa

ult i

s no

ted

to ru

n al

ong

the

base

of t

he

valle

y tre

ndin

g so

uthw

est t

o no

rthea

st. T

he p

ropo

sed

borro

w p

it su

rface

ele

vatio

n is

bet

wee

n 29

5 m

and

310

m

AOD

and

cur

rent

slo

pe a

ngle

is a

ppro

xim

atel

y 11

º.

Phot

ogra

ph 1

sho

ws

hills

ide

look

ing

north

east

with

the

prop

osed

bor

row

pit

loca

tion.

BP01

is c

onsi

dere

d as

the

pref

erre

d lo

catio

n fo

r a s

ourc

e of

agg

rega

te to

con

stru

ct n

orth

ernm

ost a

cces

s tra

ck a

nd

is a

ccom

pani

ed b

y an

indi

cativ

e de

sign

pre

sent

ed in

Fig

ure

4.1.

2a.

Pho

togr

aph

1.

Pho

togr

aph

look

ing

north

wes

t sho

win

g po

tent

ial b

orro

w p

it lo

catio

n (B

P01

)

Pho

togr

aph

2.

Pho

togr

aph

show

ing

tops

oil w

ith s

uban

gula

r gra

vel (

BP

01)

Page 7: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

4

4.2

BP0

2

The

borro

w p

it (B

P) s

ite B

P02

is lo

cate

d w

ithin

the

north

of t

he s

ite, c

entre

d at

OS

coor

dina

tes

2825

68 6

1653

7.

This

loca

tion

mak

es u

se o

f an

exis

ting

wor

ked

BP a

ssum

ed to

be

used

loca

lly fo

r the

fore

st ro

ads,

whi

ch a

ppea

r to

be

cons

truct

ed o

f the

sam

e m

ater

ial.

The

loca

tion

is w

ithin

a d

efor

este

d ar

ea a

ppro

xim

atel

y 10

m n

orth

of a

n ex

istin

g fo

rest

trac

k. T

he m

ain

axis

wou

ld

be s

outh

-wes

t to

north

-eas

t.

The

expo

sed

geol

ogy

has

been

des

crib

ed in

acc

orda

nce

with

BS5

930

(201

5).

The

bedr

ock

at t

he l

ocat

ion

was

obs

erve

d as

stro

ng a

nd v

ery

stro

ng g

reen

ish

grey

thi

nly

to t

hick

ly b

edde

d G

REY

WAC

KE w

ith 0

.3m

to 1

.5m

inte

rbed

s of

wea

k an

d m

ediu

m s

trong

fiss

ile m

udst

one

/ silt

ston

e. P

redo

min

antly

w

eath

ered

, an

d de

stru

ctur

ed in

pla

ces

with

in t

he m

udst

one

/ si

ltsto

ne in

terb

eds.

Fra

ctur

es a

re p

redo

min

antly

be

ddin

g re

late

d, s

ubho

rizon

tal a

nd s

ubve

rtica

l, cl

ose

to m

ediu

m s

pace

d, p

lana

r and

ste

pped

, sm

ooth

and

roug

h.

Join

t fra

ctur

es p

rese

nt a

s su

bhor

izon

tal a

nd s

ubve

rtica

l, ve

ry c

lose

to

med

ium

spa

ced,

pla

nar,

undu

lose

and

st

eppe

d, s

moo

th a

nd ro

ugh.

Site

obs

erva

tions

indi

cate

that

- w

here

exp

osed

- th

ere

is m

inim

al s

uper

ficia

l cov

er w

ith a

max

imum

obs

erve

d de

pth

of 0

.5m

. Pea

t pro

bing

und

erta

ken

enco

unte

red

soft

supe

rfici

al d

epos

its to

a m

axim

um d

epth

of 0

.4m

bgl

in

the

area

of t

he b

orro

w p

it.

The

borro

w p

it su

rface

ele

vatio

n is

bet

wee

n 31

0 m

and

325

m A

OD

and

cur

rent

slo

pe a

ngle

is a

ppro

xim

atel

y 12

º.

The

exca

vata

bilit

y of

the

rock

mas

s ca

n be

ass

esse

d fro

m th

e G

eolo

gica

l Stre

ngth

Inde

x (T

siam

baos

, Sar

oglo

u,

2010

). Th

e G

eolo

gica

l Stre

ngth

Inde

x (G

SI)

is e

stim

ated

from

site

obs

erva

tions

indi

catin

g th

at th

e ro

ck m

ass

in

BP01

is m

ostly

stro

ng /

very

stro

ng w

ith G

SI 3

5-60

. At s

elec

ted

area

s th

e ro

ck m

ass

can

be d

escr

ibed

as

very

w

eak

/ med

ium

stro

ng w

ith G

SI 2

0-40

.

Phot

ogra

ph 3

sho

ws

the

sout

h-w

este

rn e

xpos

ed fa

ce o

f the

pot

entia

l BP.

As th

e bo

rrow

pit

is a

wor

ked

loca

tion,

bed

rock

was

loca

lly w

ell e

xpos

ed, w

ith e

xpos

ure

in th

e no

rth a

nd n

orth

wes

t ex

tent

s of

the

pit.

A be

nch

and

ram

p ap

pear

s to

hav

e be

en c

reat

ed w

ith w

orke

d ag

greg

ate

of g

rave

l and

cob

ble

size

in th

e so

uthw

est c

orne

r of t

he s

ite (P

hoto

grap

h 3)

.

It is

ass

umed

that

this

BP

was

pre

viou

sly

used

loca

lly fo

r the

fore

st ro

ads,

whi

ch a

ppea

r to

be c

onst

ruct

ed o

f the

sa

me

mat

eria

l. At

the

time

of th

e w

alko

ver,

the

track

s ap

pear

ed to

be

in g

ood

cond

ition

.

Whe

re th

e gr

eyw

acke

is e

ncou

nter

ed a

s st

rong

and

ver

y st

rong

san

dsto

ne, t

his

wou

ld p

rove

sui

tabl

e fo

r ext

ract

ion

and

use

as a

ggre

gate

. It i

s cr

itica

l, ho

wev

er, t

hat t

estin

g an

d in

trusi

ve in

vest

igat

ion

is u

nder

take

n to

con

firm

rock

qu

ality

prio

r to

cons

truct

ion.

BP02

is c

onsi

dere

d as

the

pref

erre

d lo

catio

n fo

r a s

ourc

e of

agg

rega

te to

con

stru

ct a

cen

tral a

cces

s tra

ck a

nd is

ac

com

pani

ed b

y an

indi

cativ

e de

sign

pre

sent

ed in

Fig

ure

4.1.

1b.

Pho

togr

aph

3.

Pho

togr

aph

look

ing

north

wes

t sho

win

g co

mpe

tent

bed

rock

are

a an

d ra

mp

of w

orke

d m

ater

ial p

ossi

bly

suita

ble

for u

se (B

P02

)

Pho

togr

aph

4.

Pho

togr

aph

indi

catin

g co

nditi

on w

here

stro

ng a

nd v

ery

stro

ng g

reyw

acke

is e

ncou

nter

ed (B

P02

)

Page 8: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

5

4.3

BP0

3

Borro

w p

it BP

03 is

loca

ted

with

in th

e w

est o

f the

site

, cen

tred

at O

S co

ordi

nate

s 28

1349

614

841.

Thi

s lo

catio

n m

akes

use

of a

n ex

istin

g w

orke

d BP

app

roxi

mat

ely

30m

in le

ngth

ass

umed

to h

ave

loca

lly s

uppl

ied

aggr

egat

e fo

r th

e fo

rest

road

s, w

hich

app

ear t

o be

con

stru

cted

of t

he s

ame

mat

eria

l.

The

loca

tion

is w

ithin

a d

efor

este

d ar

ea a

djac

ent t

o an

exi

stin

g fo

rest

trac

k. T

he m

ain

axis

wou

ld b

e no

rth-w

est

and

sout

h-ea

st.

The

expo

sed

geol

ogy

has

been

des

crib

ed in

acc

orda

nce

with

BS5

930

(201

5).

Whe

re th

e ro

ck is

exp

osed

in th

e no

rth a

nd c

entra

l are

a of

the

borro

w p

it, it

has

bee

n no

ted

as th

e fo

llow

ing:

The

bedr

ock

at t

he l

ocat

ion

was

obs

erve

d as

stro

ng a

nd v

ery

stro

ng g

reen

ish

grey

thi

nly

to t

hick

ly b

edde

d G

REY

WAC

KE w

ith m

any

inte

rbed

s of

ver

y w

eak

to m

ediu

m s

trong

fiss

ile m

udst

one

/ silt

ston

e. P

redo

min

antly

pa

rtial

ly w

eath

ered

with

sur

face

dis

colo

urat

ion,

and

des

truct

ured

in

plac

es w

ithin

the

mud

ston

e /

silts

tone

in

terb

eds.

Fra

ctur

es a

re p

redo

min

antly

bed

ding

rela

ted,

sub

horiz

onta

l and

sub

verti

cal,

clos

e oc

casi

onal

ly m

ediu

m

spac

ed, p

lana

r, sm

ooth

. Joi

nt fr

actu

res

pres

ent a

s su

bhor

izon

tal a

nd s

ubve

rtica

l, ve

ry c

lose

to m

ediu

m s

pace

d,

plan

ar, u

ndul

ose

and

step

ped,

sm

ooth

and

roug

h.

Site

obs

erva

tions

indi

cate

that

- w

here

exp

osed

- th

ere

is m

inim

al s

uper

ficia

l cov

er w

ith a

max

imum

obs

erve

d de

pth

of <

0.1m

. Pea

t pro

bing

und

erta

ken

enco

unte

red

soft

supe

rfici

al d

epos

its to

a m

axim

um d

epth

of 0

.4m

bgl

(b

ut m

ore

typi

cally

0.1

to 0

.2m

bgl

in th

e ar

ea o

f the

bor

row

pit.

The

prop

osed

bor

row

pit

surfa

ce e

leva

tion

is b

etw

een

290

m a

nd 3

00 m

AO

D a

nd c

urre

nt s

lope

ang

le i

s ap

prox

imat

ely

10º.

The

Geo

logi

cal S

treng

th I

ndex

(G

SI)

estim

ated

fro

m s

ite o

bser

vatio

ns in

dica

te t

hat

the

rock

mas

s in

BP0

2 is

pr

edom

inan

tly s

trong

/ ve

ry s

trong

with

GSI

40-

65. H

owev

er, o

ccas

iona

lly th

e ro

ck m

ass

can

be d

escr

ibed

as

very

w

eak

/ med

ium

stro

ng w

ith G

SI 1

5-45

.

Phot

ogra

ph 5

sho

ws

the

sout

h-w

este

rn e

xpos

ed fa

ce o

f the

pot

entia

l BP.

Whe

re th

e gr

eyw

acke

is e

ncou

nter

ed a

s st

rong

and

ver

y st

rong

san

dsto

ne, t

his

wou

ld p

rove

sui

tabl

e fo

r ext

ract

ion

and

use

as a

ggre

gate

. It i

s cr

itica

l, ho

wev

er, t

hat t

estin

g an

d in

trusi

ve in

vest

igat

ion

is u

nder

take

n to

con

firm

rock

qu

ality

prio

r to

cons

truct

ion.

BP03

is c

onsi

dere

d as

the

loca

tion

for

a so

urce

of

aggr

egat

e to

con

stru

ct s

outh

ernm

ost

acce

ss t

rack

and

is

acco

mpa

nied

by

an in

dica

tive

desi

gn p

rese

nted

in F

igur

e 4.

1.2c

.

Pho

togr

aph

5.

Pho

togr

aph

look

ing

wes

t sho

win

g co

mpe

tent

bed

rock

are

a (B

P03

).

Pho

togr

aph

6.

Pho

togr

aph

indi

catin

g de

taile

d vi

ew a

nd th

e si

ze o

f gre

ywac

ke ru

bble

(BP

03).

Page 9: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

6

4.4

BP0

4

Borro

w p

it BP

04 is

loca

ted

with

in th

e w

est o

f the

site

, cen

tred

at O

S co

ordi

nate

s 28

1640

614

458.

At t

he lo

catio

n th

ere

is a

bed

rock

out

crop

.

The

loca

tion

is w

ithin

a d

efor

este

d ar

ea a

djac

ent t

o an

exi

stin

g fo

rest

trac

k. T

he m

ain

axis

wou

ld b

e no

rth to

sou

th.

The

expo

sed

geol

ogy

has

been

des

crib

ed in

acc

orda

nce

with

BS5

930

(201

5).

The

expo

sed

rock

at h

as b

een

note

d as

the

follo

win

g:

The

bedr

ock

at th

e lo

catio

n w

as o

bser

ved

as m

ediu

m s

trong

and

stro

ng g

rey

GR

EYW

ACKE

with

occ

asio

nal b

ands

of

ver

y w

eak

thin

ly l

amin

ated

mud

ston

e /

silts

tone

. Pa

rtial

ly w

eath

ered

with

sur

face

dis

colo

urat

ion,

and

de

stru

ctur

ed in

pla

ces

with

in t

he m

udst

one

/ si

ltsto

ne in

terb

eds.

Fra

ctur

es a

re p

redo

min

antly

bed

ding

rel

ated

, su

bhor

izon

tal a

nd s

ubve

rtica

l, cl

ose

and

med

ium

spa

ced,

pla

nar,

smoo

th. J

oint

frac

ture

s pr

esen

t as

subh

oriz

onta

l an

d su

bver

tical

, ver

y cl

ose

to m

ediu

m s

pace

d, p

lana

r, un

dulo

se a

nd s

tepp

ed, s

moo

th a

nd ro

ugh.

Site

obs

erva

tions

indi

cate

that

- w

here

exp

osed

- th

ere

is m

inim

al s

uper

ficia

l cov

er w

ith a

max

imum

obs

erve

d de

pth

of <

0.6m

. Pea

t pro

bing

und

erta

ken

enco

unte

red

soft

supe

rfici

al d

epos

its to

a m

axim

um d

epth

of 0

.3m

bgl

in

the

area

of t

he b

orro

w p

it.

The

prop

osed

bor

row

pit

surfa

ce e

leva

tion

is b

etw

een

262

m a

nd 2

80 m

AO

D a

nd c

urre

nt s

lope

ang

le i

s ap

prox

imat

ely

22º.

The

Geo

logi

cal S

treng

th In

dex

(GSI

) es

timat

ed b

y si

te o

bser

vatio

ns in

dica

te t

hat t

he r

ock

mas

s in

BP0

3 is

the

stro

ng /

very

stro

ng w

ith G

SI 4

0-60

and

ver

y w

eak

/ med

ium

stro

ng w

ith G

SI 1

0-30

.

Phot

ogra

ph 7

sho

ws

the

east

ern

expo

sed

face

of t

he p

oten

tial B

P.

Whe

re th

e gr

eyw

acke

is e

ncou

nter

ed a

s st

rong

and

ver

y st

rong

san

dsto

ne, t

his

wou

ld p

rove

sui

tabl

e fo

r ext

ract

ion

and

use

as a

ggre

gate

. It i

s cr

itica

l, ho

wev

er, t

hat t

estin

g an

d in

vest

igat

ion

is u

nder

take

n to

con

firm

rock

qua

lity

prio

r to

cons

truct

ion.

BP04

is c

onsi

dere

d as

the

loca

tion

for

a so

urce

of

aggr

egat

e to

con

stru

ct s

outh

ernm

ost

acce

ss t

rack

and

is

acco

mpa

nied

by

an in

dica

tive

desi

gn p

rese

nted

in F

igur

e 4.

1.2d

.

Pho

togr

aph

7.

Pho

togr

aph

look

ing

wes

t sho

win

g ex

pose

d be

droc

k (B

P04

).

Pho

togr

aph

8.

Pho

togr

aph

show

ing

back

s sc

arp

and

deta

iled

view

of g

reyw

acke

(BP

04).

Page 10: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

7

4.5

BP0

5

Borro

w p

it BP

05 is

loca

ted

with

in th

e w

est o

f the

site

, cen

tred

at O

S co

ordi

nate

s 28

1956

613

602.

At t

he lo

catio

n th

ere

is a

pro

min

ent b

edro

ck o

utcr

op.

The

loca

tion

is w

ithin

a d

efor

este

d ar

ea a

djac

ent t

o an

exi

stin

g fo

rest

trac

k. T

he m

ain

axis

wou

ld b

e no

rth-e

ast

and

sout

h-w

est.

The

expo

sed

geol

ogy

has

been

des

crib

ed in

acc

orda

nce

with

BS5

930

(201

5).

The

expo

sed

rock

has

bee

n no

ted

as th

e fo

llow

ing:

The

bedr

ock

at t

he l

ocat

ion

was

obs

erve

d as

med

ium

stro

ng a

nd s

trong

gre

enis

h gr

ey G

RE

YWAC

KE w

ith

occa

sion

al b

ands

of v

ery

wea

k th

inly

lam

inat

ed m

udst

one

/ silt

ston

e 0.

1m to

0.6

m th

ick.

Par

tially

wea

ther

ed w

ith

surfa

ce d

isco

lour

atio

n, a

nd d

estru

ctur

ed i

n pl

aces

with

in t

he m

udst

one

/ si

ltsto

ne i

nter

beds

. Fr

actu

res

are

pred

omin

antly

bed

ding

rel

ated

, sub

horiz

onta

l and

sub

verti

cal,

clos

ely

and

very

clo

sely

spa

ced,

pla

nar,

smoo

th.

Join

t fra

ctur

es p

rese

nt a

s su

bhor

izon

tal a

nd s

ubve

rtica

l, ve

ry c

lose

to

med

ium

spa

ced,

pla

nar,

undu

lose

and

st

eppe

d, s

moo

th a

nd ro

ugh.

Site

obs

erva

tions

indi

cate

that

- w

here

exp

osed

- th

ere

is m

inim

al s

uper

ficia

l cov

er w

ith a

max

imum

obs

erve

d de

pth

of <

0.2m

. Pea

t pro

bing

und

erta

ken

enco

unte

red

soft

supe

rfici

al d

epos

its to

a m

axim

um d

epth

of 0

.4m

bgl

in

the

area

of t

he b

orro

w p

it.

The

prop

osed

bor

row

pit

surfa

ce e

leva

tion

is b

etw

een

360

m a

nd 3

76 m

AO

D a

nd c

urre

nt s

lope

ang

le i

s ap

prox

imat

ely

18º.

The

Geo

logi

cal S

treng

th In

dex

(GSI

) est

imat

ed b

y si

te o

bser

vatio

ns in

dica

te th

at th

e ro

ck m

ass

in B

P03

is m

ainl

y m

ediu

m s

trong

/ ve

ry s

trong

with

GSI

30-

75. H

owev

er, w

here

wea

k / m

ediu

m s

trong

the

rock

mas

s ha

s be

en

assi

gned

a G

SI o

f 20-

40.

Phot

ogra

ph 9

sho

ws

the

sout

h-ea

ster

n ex

pose

d fa

ce o

f the

pot

entia

l BP.

Whe

re th

e gr

eyw

acke

is e

ncou

nter

ed a

s st

rong

and

ver

y st

rong

san

dsto

ne, t

his

wou

ld p

rove

sui

tabl

e fo

r ext

ract

ion

and

use

as a

ggre

gate

. It i

s cr

itica

l, ho

wev

er, t

hat t

estin

g an

d in

trusi

ve in

vest

igat

ion

is u

nder

take

n to

con

firm

rock

qu

ality

prio

r to

cons

truct

ion.

BP05

is c

onsi

dere

d as

the

pref

erre

d lo

catio

n fo

r sou

rce

of a

ggre

gate

to c

onst

ruct

sou

ther

nmos

t acc

ess

track

and

is

acc

ompa

nied

by

an in

dica

tive

desi

gn p

rese

nted

in F

igur

e 4.

1.2e

.

Pho

togr

aph

9.

Pho

togr

aph

look

ing

north

wes

t sho

win

g ex

pose

d be

droc

k (B

P05)

.

Pho

togr

aph

10.

Phot

ogra

ph s

how

ing

deta

iled

view

of g

reyw

acke

(BP

05).

Page 11: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

8

5 As

sess

men

t of P

oten

tial B

orro

w P

it Lo

catio

ns

5.1

Intr

oduc

tion

The

aggr

egat

e re

quire

men

ts o

f the

win

dfar

m in

frast

ruct

ure

is in

tend

ed to

be

fulfi

lled

utilis

ing

the

five

prop

osed

bo

rrow

pit

site

s as

out

lined

in S

ectio

n 4.

An

asse

ssm

ent o

f the

qua

ntiti

es is

pro

vide

d in

Sec

tion

5 fo

r eac

h of

the

pros

pect

ive

borro

w p

its lo

catio

ns, s

epar

ated

into

the

two

sepa

rate

acc

esse

s fo

r the

site

.

An e

stim

ated

sui

tabl

e vo

lum

e ha

s be

en p

rovi

ded

diffe

ring

to th

e ap

prox

imat

e vo

lum

e of

the

borro

w p

it. F

or e

ach

pit t

his

is b

ased

on

the

expo

sed

geol

ogy

and

varia

tions

in th

e su

itabi

lity

of th

e be

droc

k as

out

lined

in S

ectio

n 3.

4.

The

actu

al a

mou

nt o

f sui

tabl

e m

ater

ial w

ill va

ry fr

om th

is d

epen

ding

upo

n th

e co

nditi

on o

f the

mat

eria

l in

the

rest

of

the

bor

row

pit

but

may

als

o de

pend

on

non-

geol

ogic

al c

onst

rain

ts s

uch

as f

or e

nviro

nmen

tal r

easo

ns.

Any

exce

ssiv

ely

wea

ther

ed b

edro

ck c

ould

be

dug

out u

sing

sta

ndar

d m

etho

ds o

f exc

avat

ion.

The

volu

mes

giv

en h

ave

been

cal

cula

ted

from

eac

h bo

rrow

pit

cros

s-se

ctio

n, ta

king

into

acc

ount

geo

mor

phol

ogy

and

grad

ient

s of

the

extra

ctio

n fa

ce a

nd th

e bo

rrow

pit

foot

prin

t dim

ensi

ons.

It s

houl

d be

not

ed th

at th

e pr

ovid

ed

borro

w p

it di

men

sion

s an

d vo

lum

e ar

e es

timat

es a

nd w

here

exc

avat

ed a

t the

loca

tions

of a

n ex

istin

g bo

rrow

pit

not i

ndic

ated

by

the

Dig

ital T

erra

in M

odel

(DTM

dat

a), e

xcav

atio

n vo

lum

es a

re li

kely

to v

ary.

Each

tec

hnic

al d

raw

ing

pres

ente

d in

clud

es a

loca

tion

map

for

the

bor

row

pit

with

in t

he D

evel

opm

ent

Area

, a

phot

ogra

ph o

f th

e po

tent

ial b

orro

w p

it ar

ea,

a lo

catio

n pl

an s

how

ing

the

prop

osed

bor

row

pit

foot

prin

t an

d a

sche

mat

ic c

ross

-sec

tion.

It

shou

ld b

e no

ted

that

the

bor

row

pit

foot

prin

t an

d cr

oss-

sect

ion

show

n ha

s be

en

prod

uced

usi

ng a

vaila

ble

DTM

dat

a an

d co

nseq

uent

ly is

not

a d

etai

led

desi

gn a

nd s

houl

d be

con

side

red

as

indi

cativ

e on

ly.

Whe

re ro

ck w

as e

xpos

ed th

e pr

obab

le e

xtra

ctio

n m

etho

ds h

ave

been

est

imat

ed b

y em

piric

al m

etho

d us

ing

GSI

va

lues

(Ts

iam

baos

, Sar

oglo

u, 2

010)

. The

pro

babl

e ex

tract

ion

met

hod

will

be b

est a

sses

sed

follo

win

g de

taile

d gr

ound

inve

stig

atio

ns a

nd g

eote

chni

cal t

estin

g, th

is in

form

atio

n w

ill al

so b

e re

quire

d to

info

rm d

etai

led

desi

gn o

f th

e bo

rrow

pits

. It i

s an

ticip

ated

that

, upo

n co

mpl

etio

n, e

ach

borro

w p

it w

ill be

at l

east

par

tially

rein

stat

ed.

This

will

invo

lve

the

rew

orki

ng o

f its

fac

e fo

r sl

ope

stab

ility,

par

tial

infil

ling

with

exc

avat

ed m

ater

ial

not

need

ed f

or

cons

truct

ion

or o

f uns

uita

ble

grad

e, a

nd la

ndsc

apin

g.

At th

is s

ite th

ere

may

be

the

pote

ntia

l for

env

ironm

enta

l en

hanc

emen

t pos

t use

.

5.2

Acce

ss A

Asse

ssm

ent o

f BP0

1

The

mai

n pa

rt of

the

borro

w p

it as

sess

men

t is

in th

e fo

rm o

f an

indi

cativ

e te

chni

cal d

raw

ing;

Fig

ure

4.1.

2a.

As th

ere

is n

o be

droc

k ex

pose

d, n

o si

te o

bser

vatio

ns w

ere

reco

rded

. It i

s th

eref

ore

not p

ossi

ble

to a

sses

s th

e po

tent

ial

of g

ood

qual

ity a

ggre

gate

and

the

sup

erfic

ial

over

burd

en w

ithin

thi

s ar

ea.

The

perc

enta

ge s

uita

ble

mat

eria

l has

bee

n as

sum

ed a

s 70

%, h

owev

er n

o ob

serv

atio

ns c

onfir

m th

e co

nditi

on o

f the

bed

rock

at t

he s

ite

loca

tion.

Tabl

e 3

illust

rate

s th

e pr

opos

ed b

orro

w p

it di

men

sion

s.

Tabl

e 3.

Indi

cativ

e B

P01

Dim

ensi

ons

and

Extra

ctio

n V

olum

es

ID

Loca

tion

Appr

ox.

foot

prin

t ar

ea

(m2 )

Max

. de

pth

(m)

Appr

ox.

Tota

l Ex

trac

tion

Volu

me

(m3 )

Estim

ated

su

itabl

e ag

greg

ate

(%)

Prob

able

ext

ract

ion

met

hod

BP0

1 28

3276

, 618

002

10,1

40

12.8

40

,746

80

R

ippi

ng /

Ham

mer

/ Bl

astin

g1

Tota

l Est

imat

ed A

ggre

gate

Vol

ume

(m3 )

32,5

97

1 N

o be

droc

k en

coun

tere

d bu

t bas

ed o

n ot

her o

utcr

ops

the

maj

ority

of t

he ro

ck m

ater

ial w

ill re

quire

dril

l and

bl

ast t

o ge

t suf

ficie

nt fr

agm

enta

tion

(and

impr

oved

pro

duct

ion

rate

s) a

lthou

gh it

is p

ossi

ble

that

som

e of

the

mor

e fra

ctur

ed m

ater

ial w

ill b

e rip

pabl

e.

Asse

ssm

ent o

f BP0

2

The

mai

n pa

rt of

the

borro

w p

it as

sess

men

t is

in th

e fo

rm o

f an

indi

cativ

e te

chni

cal d

raw

ing;

Fig

ure

4.1.

2b.

This

loca

tion

has

the

pote

ntia

l to

yiel

d go

od q

ualit

y ag

greg

ate.

Th

e su

perfi

cial

ove

rbur

den

with

in t

his

area

is

shal

low

, with

an

aver

age

dept

h of

<0.

5 m

.

Tabl

e 4

illust

rate

s th

e pr

opos

ed b

orro

w p

it di

men

sion

s.

Tabl

e 4.

Indi

cativ

e B

P02

Dim

ensi

ons

and

Extra

ctio

n V

olum

es

ID

Loca

tion

Appr

ox.

foot

prin

t ar

ea

(m2 )

Max

. de

pth

(m)

Appr

ox.

Tota

l Ex

trac

tion

Volu

me

(m3 )

Estim

ated

su

itabl

e ag

greg

ate

(%)

Prob

able

ext

ract

ion

met

hod

BP0

2 28

2568

, 616

537

16,2

90

19

152,

621

80

Rip

ping

/ H

amm

er /

Blas

ting1

Tota

l Est

imat

ed A

ggre

gate

Vol

ume

(m3 )

122,

097

1 Th

e m

ajor

ity o

f the

roc

k m

ater

ial w

ill r

equi

re d

rill a

nd b

last

to g

et s

uffic

ient

frag

men

tatio

n (a

nd im

prov

ed

prod

uctio

n ra

tes)

alth

ough

it is

pos

sibl

e th

at s

ome

of th

e m

ore

fract

ured

mat

eria

l will

be ri

ppab

le.

Page 12: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

9

5.3

Acce

ss B

Asse

ssm

ent o

f BP0

3

The

mai

n pa

rt of

the

borro

w p

it as

sess

men

t is

in th

e fo

rm o

f an

indi

cativ

e te

chni

cal d

raw

ing;

Fig

ure

4.1.

2c.

This

loca

tion

has

the

pote

ntia

l to

yiel

d go

od q

ualit

y ag

greg

ate.

The

sup

erfic

ial o

verb

urde

n w

ithin

this

are

a is

ver

y sh

allo

w, w

ith a

n av

erag

e de

pth

of <

0.1

m.

Tabl

e 5

illust

rate

s th

e pr

opos

ed b

orro

w p

it di

men

sion

s.

Tabl

e 5.

Indi

cativ

e B

P03

Dim

ensi

ons

and

Extra

ctio

n V

olum

es

ID

Loca

tion

Appr

ox.

foot

prin

t ar

ea

(m2 )

Max

. de

pth

(m)

Appr

ox.

Tota

l Ex

trac

tion

Volu

me

(m3 )

Estim

ated

su

itabl

e ag

greg

ate

(%)

Prob

able

ext

ract

ion

met

hod

BP0

3 28

1349

, 614

841

10,0

83

10.5

38

,034

80

R

ippi

ng /

Ham

mer

/ Bl

astin

g1

Tota

l Est

imat

ed A

ggre

gate

Vol

ume

(m3 )

30,4

27

1 Th

e m

ajor

ity o

f the

roc

k m

ater

ial w

ill r

equi

re d

rill a

nd b

last

to g

et s

uffic

ient

frag

men

tatio

n (a

nd im

prov

ed

prod

uctio

n ra

tes)

alth

ough

it is

pos

sibl

e th

at s

ome

of th

e m

ore

fract

ured

mat

eria

l will

be ri

ppab

le.

Asse

ssm

ent o

f BP0

4

The

mai

n pa

rt of

the

borro

w p

it as

sess

men

t is

in th

e fo

rm o

f an

indi

cativ

e te

chni

cal d

raw

ing;

Fig

ure

4.1.

2d.

This

loca

tion

has

the

pote

ntia

l to

yiel

d go

od q

ualit

y ag

greg

ate.

Th

e su

perfi

cial

ove

rbur

den

with

in t

his

area

is

shal

low

, with

an

aver

age

dept

h of

<0.

6 m

.

Tabl

e 6

illust

rate

s th

e pr

opos

ed b

orro

w p

it di

men

sion

s.

Tabl

e 6.

Indi

cativ

e B

P04

Dim

ensi

ons

and

Extra

ctio

n V

olum

es

ID

Loca

tion

Appr

ox.

foot

prin

t ar

ea

(m2 )

Max

. de

pth

(m)

Appr

ox.

Tota

l Ex

trac

tion

Volu

me

(m3 )

Estim

ated

su

itabl

e ag

greg

ate

(%)

Prob

able

ext

ract

ion

met

hod

BP0

4 28

1640

, 614

458

4,74

5 16

.9

40,5

30

70

Rip

ping

/ H

amm

er /

Blas

ting1

Tota

l Est

imat

ed A

ggre

gate

Vol

ume

(m3 )

28,3

71

1 Th

e m

ajor

ity o

f the

roc

k m

ater

ial w

ill r

equi

re d

rill a

nd b

last

to g

et s

uffic

ient

frag

men

tatio

n (a

nd im

prov

ed

prod

uctio

n ra

tes)

alth

ough

it is

pos

sibl

e th

at s

ome

of th

e m

ore

fract

ured

mat

eria

l will

be ri

ppab

le.

Asse

ssm

ent o

f BP0

5

The

mai

n pa

rt of

the

borro

w p

it as

sess

men

t is

in th

e fo

rm o

f an

indi

cativ

e te

chni

cal d

raw

ing;

Fig

ure

4.1.

2e.

This

loca

tion

has

the

pote

ntia

l to

yiel

d go

od q

ualit

y ag

greg

ate.

The

sup

erfic

ial o

verb

urde

n w

ithin

this

are

a is

ver

y sh

allo

w, w

ith a

n av

erag

e de

pth

of <

0.2

m.

Tabl

e 7

illust

rate

s th

e pr

opos

ed b

orro

w p

it di

men

sion

s.

Tabl

e 7.

Indi

cativ

e B

P05

Dim

ensi

ons

and

Extra

ctio

n V

olum

es

ID

Loca

tion

Appr

ox.

foot

prin

t ar

ea

(m2 )

Max

. de

pth

(m)

Appr

ox.

Tota

l Ex

trac

tion

Volu

me

(m3 )

Estim

ated

su

itabl

e ag

greg

ate

(%)

Prob

able

ext

ract

ion

met

hod

BP0

5 28

1956

, 613

602

5,60

3 11

.7

34,1

61

85

Rip

ping

/ H

amm

er /

Blas

ting1

Tota

l Est

imat

ed A

ggre

gate

Vol

ume

(m3 )

29,0

37

1 Th

e m

ajor

ity o

f the

roc

k m

ater

ial w

ill r

equi

re d

rill a

nd b

last

to g

et s

uffic

ient

frag

men

tatio

n (a

nd im

prov

ed

prod

uctio

n ra

tes)

alth

ough

it is

pos

sibl

e th

at s

ome

of th

e m

ore

fract

ured

mat

eria

l will

be ri

ppab

le.

Page 13: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

10

6 C

oncl

usio

ns a

nd R

ecom

men

datio

ns

An e

ngin

eerin

g ge

olog

y w

alko

ver

and

supp

ortin

g de

sk s

tudy

has

bee

n ca

rried

out

in

orde

r to

pro

vide

the

op

portu

nity

for a

ggre

gate

mat

eria

l to

be s

ourc

ed o

n si

te.

Usi

ng t

he i

nfor

mat

ion

gath

ered

and

tak

ing

acco

unt

of g

eolo

gica

l ch

arac

teris

tics

and

cons

train

ts,

borro

w p

it in

dica

tive

desi

gns

have

bee

n pr

epar

ed fo

r the

5 p

refe

rred

loca

tions

and

is p

rovi

ded

in A

ppen

dix

A. E

ach

desi

gn

incl

udes

app

roxi

mat

e di

men

sion

s an

d ag

greg

ate

volu

me

plus

pro

babl

e ex

tract

ion

met

hods

. Th

e ov

erbu

rden

at

thes

e lo

catio

ns is

gen

eral

ly v

ery

shal

low

and

obs

erve

d de

pths

are

<0.

6 m

. Th

e ro

ck v

olum

es w

hich

cou

ld b

e ex

tract

ed fr

om th

e in

dica

tive

desi

gn o

f the

iden

tifie

d si

tes

are:

BP

01 -

40,7

46m

3 of t

otal

mat

eria

l ext

ract

ed, p

rovi

ding

32,

597m

3 of s

uita

ble

aggr

egat

e m

ater

ial;

BP

02 -

152,

621m

3 of t

otal

mat

eria

l ext

ract

ed, p

rovi

ding

122

,097

m3 o

f sui

tabl

e ag

greg

ate

mat

eria

l;

BP

03 -

38,0

34m

3 of t

otal

mat

eria

l ext

ract

ed, p

rovi

ding

30,

427m

3 of s

uita

ble

aggr

egat

e m

ater

ial;

BP

04 -

40,5

30m

3 of t

otal

mat

eria

l ext

ract

ed, p

rovi

ding

28,

371m

3 of s

uita

ble

aggr

egat

e m

ater

ial;

and

BP

05 -

34,1

61m

3 of t

otal

mat

eria

l ext

ract

ed, p

rovi

ding

29,

037m

3 of s

uita

ble

aggr

egat

e m

ater

ial.

Com

bine

d, th

ese

five

borro

w p

it lo

catio

ns a

re a

ntic

ipat

ed to

pro

vide

a to

tal o

f 242

,529

m3

of s

uita

ble

aggr

egat

e,

prov

idin

g th

e m

ajor

ity o

f the

agg

rega

te re

quire

men

t for

the

Dev

elop

men

t.

Giv

en t

he i

nher

ent

varia

bilit

y of

gre

ywac

ke,

sele

ctiv

e w

orki

ng m

ay b

e un

derta

ken

to l

imit

the

amou

nt o

f fin

es/w

eath

ered

mat

eria

l gen

erat

ed. T

his

was

tage

is ta

ken

into

acc

ount

with

in th

e vo

lum

es p

rese

nted

in S

ectio

n 5

(“es

timat

ed s

uita

ble

aggr

egat

e”).

Ther

e is

add

ition

ally

the

pote

ntia

l for

add

ing

anot

her

low

er b

ench

bel

ow th

e de

sign

ed p

it flo

or if

mor

e ‘g

ood’

rock

is re

quire

d al

thou

gh s

uch

a be

nch

wou

ld n

eed

pum

ping

to d

eal w

ith s

urfa

ce

wat

er.

Det

aile

d gr

ound

inve

stig

atio

ns, s

lope

sta

bilit

y as

sess

men

ts a

nd g

eote

chni

cal t

estin

g w

ill be

requ

ired

in o

rder

to

conf

irm th

e su

itabi

lity

of e

ach

of th

e bo

rrow

pit

loca

tions

.

Geo

tech

nica

l roc

k te

stin

g sh

ould

be

unde

rtake

n ac

ross

the

full

exte

nts

of e

ach

prop

osed

bor

row

pit

loca

tion

in

orde

r to

ass

ess

the

suita

bilit

y of

the

aggr

egat

e fo

r co

nstru

ctio

n. T

he te

stin

g sh

ould

be

for

but n

ot li

mite

d to

the

follo

win

g:

U

ncon

fined

Com

pres

sive

Stre

ngth

;

Po

int L

oad;

Sl

akes

Dur

abilit

y In

dex;

Lo

s An

gele

s C

oeffi

cien

t; an

d

Se

ism

ic p

rofil

ing.

With

the

info

rmat

ion

retri

eved

, a d

etai

led

desi

gn e

xerc

ise

will

be re

quire

d fo

r ea

ch b

orro

w p

it. D

urin

g an

d up

on

com

plet

ion

of fo

rmin

g ea

ch b

orro

w p

it, th

e st

abilit

y of

the

quar

ried

face

s sh

ould

be

asse

ssed

by

a su

itabl

y qu

alifi

ed

engi

neer

ing

geol

ogis

t.

Any

chan

ges

to th

e w

indf

arm

des

ign

may

requ

ire a

revi

ew o

f the

bor

row

pit

requ

irem

ents

.

Page 14: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

11

7 G

eote

chni

cal R

isk

Reg

iste

r A

revi

ew o

f the

geo

tech

nica

l ris

ks a

ssoc

iate

d w

ith th

e sc

hem

e ha

s be

en u

nder

take

n an

d is

pre

sent

ed in

Tab

le

8 in

acc

orda

nce

with

the

guid

elin

es s

et o

ut in

HD

22/0

8. T

he ri

sk re

gist

er li

sts

the

antic

ipat

ed g

eote

chni

cal r

isks

as

soci

ated

with

the

borro

w p

it de

sign

for t

he D

evel

opm

ent,

cove

ring

all b

orro

w p

its. T

he ri

sk b

efor

e co

ntro

l of

the

haza

rd h

as b

een

asse

ssed

qua

ntita

tivel

y an

d fo

llow

ing

the

spec

ific

resp

onse

to

each

ris

k. T

he v

alue

s as

sign

ed to

impa

ct fo

r the

se h

azar

ds s

houl

d be

con

side

red

as q

uant

itativ

e as

det

aile

d in

Tab

le 8

.

Tabl

e 8.

Geo

tech

nica

l Ris

k E

valu

atio

n M

atric

es

PR

OB

ABIL

ITY

(P)

IM

PAC

T (I)

Probability

Im

pact

TI

ME

COST

5 4

3 2

1 Ve

ry

High

Ve

ry li

kely

>7

5%

5

Very

Hig

h

5 >5

0%

>20%

5 25

20

15

10

5

High

Pr

obab

le

40-7

5%

4

High

4

25-5

0%

10-2

0%

4

20

16

12

8 4

Med

ium

Po

ssib

le

10-4

0%

3 X

Med

ium

3

10-2

5%

5-10

%

= 3

15

12

9 6

3

Low

U

nlik

ely

2-10

%

2

Low

2

2-10

%

1-5%

2 10

8

6 4

2

Very

Lo

w

Neg

ligib

le

<2%

1

Ve

ry L

ow

1 <2

%

<1%

1 5

4 3

2 1

Ris

k Ra

tings

1

to 4

Low

Ris

k

5

to 1

0

Med

ium

Ris

k

12

to 1

6 H

igh

Ris

k

20

+ C

ritic

al R

isk

So

urce

s:

Prob

abilit

y an

d im

pact

nom

encl

atur

e an

d sc

orin

gs a

re b

ased

on

a nu

mbe

r of s

ourc

es in

clud

ing

-

H

D22

/02

Man

agin

g G

eote

chni

cal R

isk

Des

crib

ing

prob

abilit

y: T

he li

mita

tions

of n

atur

al la

ngua

ge (H

illson

)

Prob

abilit

y fre

quen

cies

and

the

% in

crea

se o

f cos

ts a

re M

ouch

el d

eriv

ed v

alue

s

Page 15: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

12

No

Haz

ard

Ris

k

Ris

k M

anag

emen

t M

easu

res

unde

rtak

en to

da

te

Ris

k ra

ting

follo

win

g ris

k m

anag

emen

t mea

sure

s un

dert

aken

to d

ate

Pr

opos

ed R

isk

Man

agem

ent

Mea

sure

s An

ticip

ated

risk

ratin

g fo

llow

ing

prop

osed

risk

man

agem

ent

Com

men

ts o

r fur

ther

in

form

atio

n P

I R

P

I R

1.

Dep

ths

of s

uper

ficia

l dep

osits

m

ay v

ary

from

the

dept

hs

asse

ssed

by

prob

ing

of s

oft

depo

sits

.

Inap

prop

riate

bor

row

pit

desi

gn

and

pote

ntia

l ins

tabi

lity

in

supe

rfici

al d

epos

its.

Addi

tiona

l cos

t and

del

ays

to

prog

ram

me.

Peat

pro

bing

3

4 12

C

arry

out

det

aile

d de

sign

Gro

und

Inve

stig

atio

n to

det

erm

ine

the

dept

h of

sup

erfic

ial d

epos

its.

1 4

4

2.

Roc

k m

ass

prop

ertie

s an

d ge

olog

ical

bac

kgro

und

(pre

senc

e of

faul

ts w

hich

may

ca

use

chan

ges

in li

thol

ogy)

ba

sed

on s

ite o

bser

vatio

ns

may

be

diffe

rent

than

in re

ality

.

Inap

prop

riate

bor

row

pit

desi

gn

and

unsu

itabl

e ag

greg

ate

mat

eria

l. Ad

ditio

nal c

ost a

nd

dela

ys to

pro

gram

me.

Site

obs

erva

tion

4 4

16

Car

ry o

ut d

etai

led

desi

gn G

roun

d In

vest

igat

ion

to d

eter

min

e th

e ro

ck

mas

s pr

oper

ties,

geo

logi

cal

back

grou

nd a

nd a

ggre

gate

sui

tabi

lity.

1 4

4

3.

Borro

w p

it yi

eld

diffe

rs to

that

es

timat

ed.

Addi

tiona

l fill

requ

irem

ents

ove

r an

d ab

ove

the

borro

w p

its

curre

ntly

pro

pose

d.

Site

obs

erva

tion

whe

re

rock

is e

xpos

ed.

4 4

16

Car

ry o

ut d

etai

led

desi

gn G

roun

d In

vest

igat

ion

to d

eter

min

e th

e qu

antit

y of

mat

eria

l tha

t can

be

yiel

ded

at e

ach

loca

tion

incl

udin

g ag

greg

ate

suita

bilit

y as

dis

cuss

ed in

R

isk

no. 2

.

1 4

4

4.

Exca

vata

bilit

y of

rock

mas

s es

timat

ed b

y em

piric

al m

etho

d m

ay d

iffer

from

the

real

ity.

Del

ays

in c

onst

ruct

ion

wor

ks.

Hav

ing

to re

vise

des

ign

prop

osal

s (if

nee

ded

volu

me

of

the

rock

mas

s is

not

pos

sibl

e to

ex

cava

te).

Non

e 4

4 16

C

arry

out

det

aile

d de

sign

Gro

und

Inve

stig

atio

n to

det

erm

ine

the

rock

pr

oper

ties.

1

4 4

5.

Gro

undw

ater

con

ditio

ns n

ot

know

n.

Inap

prop

riate

bor

row

pit

desi

gn.

Addi

tiona

l cos

t and

de

lays

to p

rogr

amm

e.

Non

e 4

4 16

Car

ry o

ut d

etai

led

desi

gn G

roun

d In

vest

igat

ion

to d

eter

min

e th

e gr

ound

wat

er c

ondi

tions

. BP

base

m

ay n

eed

to b

e in

clin

ed w

hen

pote

ntia

l of g

roun

dwat

er s

eepa

ge is

fo

und.

Dra

inag

e m

easu

res

impl

emen

ted

abov

e ro

ck fa

ce.

1 4

4

6.

Roc

k sl

ope

stab

ility

prop

ertie

s no

t kno

wn.

Inap

prop

riate

bor

row

pit

desi

gn.

Uns

uita

ble

benc

h w

idth

. Ad

ditio

nal c

ost a

nd

dela

ys to

pro

gram

me.

3.0m

ben

ches

and

max

fa

ce h

eigh

t 7.5

m c

urre

ntly

im

plem

ente

d in

bor

row

pit

desi

gn h

owev

er b

edro

ck

prop

ertie

s no

t kno

wn.

4 4

16

Car

ry o

ut d

etai

led

desi

gn G

roun

d In

vest

igat

ion

to d

eter

min

e th

e ro

ck

slop

e st

abilit

y pr

oper

ties.

1

4 4

7.

Cha

nge

in w

indf

arm

layo

ut

nece

ssita

ting

addi

tiona

l m

ater

ial r

equi

red.

Estim

ated

bor

row

pit

quan

titie

s no

t suf

ficie

nt fo

r qua

ntity

of

aggr

egat

e re

quire

d.

Non

e 2

4 8

It m

ay b

e ne

cess

ary

to e

xpan

d th

e cu

rrent

ly p

ropo

sed

borro

w p

its, o

r lo

ok in

to a

dditi

onal

loca

tions

. 2

4 8

Page 16: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

13

8 R

efer

ence

s Br

itish

Geo

logi

cal S

urve

y. (1

988)

. Hyd

roge

olog

ical

map

of S

cotla

nd, 1

:625

,000

. Not

tingh

am, U

K.

Briti

sh G

eolo

gica

l Sur

vey.

(200

5). L

eadh

ills. S

cotla

nd S

heet

15E

. Sol

id a

nd D

rift G

eolo

gy 1

:50,

000.

Not

tingh

am,

UK.

Briti

sh G

eolo

gica

l Sur

vey.

(201

7). G

eoIn

dex.

Ret

rieve

d in

Mar

ch 2

017

from

http

://w

ww

.bgs

.ac.

uk/G

eoIn

dex/

The

Briti

sh S

tand

ards

Age

ncy.

(201

5). C

ode

of p

ract

ice

for g

roun

d in

vest

igat

ions

(BS

5930

:201

5). L

ondo

n, U

K.

Floy

d, J

D. (

2003

). G

eolo

gy o

f the

Lea

dhill

s di

stric

t – a

brie

f exp

lana

tion

of th

e ge

olog

ical

map

. She

et E

xpla

natio

n of

the

Briti

sh G

eolo

gica

l Sur

vey.

1:5

0,00

0 Sh

eet 1

5E L

eadh

ills (S

cotla

nd).

Not

tingh

am, U

K.

The

Hig

hway

s Ag

ency

(200

2). D

esig

n M

anua

l for

Roa

ds a

nd B

ridge

s –

Volu

me

4 G

eote

chni

cs a

nd D

rain

age

– Se

ctio

n 1

Earth

wor

ks –

Par

t 2 M

anag

ing

geot

echn

ical

risk

(HD

22/0

8). L

ondo

n, U

K.

The

Hig

hway

s Ag

ency

(200

8). D

esig

n M

anua

l for

Roa

ds a

nd B

ridge

s –

Volu

me

4 G

eote

chni

cs a

nd D

rain

age

– Se

ctio

n 1

Earth

wor

ks –

Par

t 2 M

anag

ing

geot

echn

ical

risk

(HD

22/0

8). L

ondo

n, U

K.

Land

Use

Con

sulta

nts

(LU

C)

(201

7).

Cha

pter

4:

Sche

me

Des

crip

tion

of N

orth

Low

ther

Ene

rgy

Initi

ativ

e En

viro

nmen

tal S

tate

men

t.

Smith

, M.R

., &

Col

lis, L

. (20

01).

Agg

rega

tes:

San

d, g

rave

l and

cru

shed

rock

agg

rega

tes

for c

onst

ruct

ion

purp

oses

, 3rd

Edi

tion.

Geo

logi

cal S

ocie

ty, L

ondo

n, E

ngin

eerin

g G

eolo

gy S

peci

al P

ublic

atio

ns, 1

7.

Tsia

mba

os G

., Sa

rogl

ou H

. (20

10).

Exc

avat

abilit

y as

sess

men

t of r

ock

mas

ses

usin

g th

e G

eolo

gica

l Stre

ngth

Inde

x (G

SI).

Bul

l Eng

Geo

l Env

iron

69: 1

3-27

.

Ord

nanc

e Su

rvey

. 1:5

0,00

0 sc

ale

Land

rang

er M

ap: 7

1 La

nark

& U

pper

Nith

side

.

Page 17: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

Nort

h Lo

wth

er E

nerg

y In

itiat

ive

Borro

w P

it As

sess

men

t

14

Appe

ndix

A:

Figu

res

Figu

re 4

.1.1

Bo

rrow

Pit

Ove

rvie

w

Figu

re 4

.1.2

a

BP01

Indi

cativ

e Bo

rrow

Pit

Des

ign

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re 4

.1.2

b

BP02

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cativ

e Bo

rrow

Pit

Des

ign

Figu

re 4

.1.2

c

BP03

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cativ

e Bo

rrow

Pit

Des

ign

Figu

re 4

.1.2

d

BP04

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cativ

e Bo

rrow

Pit

Des

ign

Figu

re 4

.1.2

e

BP05

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cativ

e Bo

rrow

Pit

Des

ign

Page 18: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

1

2

3

4

56

7

89

10

11

12

13

14

15

16

17 1

8

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

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hts

2017

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e Sur

vey

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01

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erg

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itia

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ure

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orr

ow

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rvie

w

INSER

TSU

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ON

SU

LTAN

T LO

GO

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a

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ckm

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tone

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th B

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site

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th B

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n C

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th B

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eous

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icro

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ro

Page 19: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

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1 fo

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k ge

olog

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mer

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Page 20: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

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ure

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1 fo

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k ge

olog

y an

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catio

n ov

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rfic

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es u

se o

f an

exi

stin

g w

orke

d bo

rrow

put

ass

umed

to

be u

sed

loca

lly f

or

the

fore

st r

oads

, w

hich

app

ear

to b

eco

nstr

ucte

d of

the

sam

e m

ater

ial.

The

mai

nax

is w

ould

be

sout

h w

est

to n

orth

eas

t.

Dig

ging

/ R

ippi

ng/

Ham

mer

/ B

last

ing

The

prox

imity

of BP0

2 re

lative

to

turb

ine

31 w

ill h

ave

to b

e co

nfir

med

fo

llow

ing

grou

nd in

vest

igat

ion

and

asse

ssm

ent

of r

ock

stab

ility

.

Cro

ss S

ecti

on

*Pea

t de

pths

(m

) re

pres

ente

d by

tria

ngle

s.

E

B

B

AA

Ind

icat

ive

Pe

at R

est

ora

tio

n L

eve

l (1

m)

Page 21: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

# *

# *

# *# *

# *

# *

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# *# *

# *# *# * # *

# *# *# *

# *# *# *# * # *# *

# *# * # *

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0.1

0.2

0.2

0.3

0.2

0.2

0.1

0.1

0.1

0.1

0.2 0.

40.

4

0.2

0.2

0.3

0.2

0.3

0.3

0.3

0.50.

20.

20.

3 0.3

0.2

0.2

0.2 0.5

0.10.

2

0.2

0.5

0.3

0.2

BP0

3

© C

row

n co

pyri

ght

and

data

base

rig

hts

2017

Ord

nanc

e Sur

vey

0100

0316

73

Dra

wn

By -

AS,

Rev

iew

ed B

y -

SB,

Dat

e 10

/04/

2017

ESo

urce

: BG

S

No

rth

Lo

wth

er

En

erg

y In

itia

tive

Fig

ure

4.1

.2c

Ind

icat

ive

Bo

rro

wP

it D

esig

n -

BP

03

Furt

he

r In

form

ati

on

:

Bo

rro

w P

it I

D:

Nat

ion

al G

rid

Ref

:

BP

No

min

al F

oo

tpri

nt

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ensi

on

s:

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otp

rin

t A

rea:

Pre

do

min

an

t Li

tho

log

y

Terr

ain

:

Exca

vati

on

Req

uir

ed:

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3

NS 8

134

1484

10.0

83m

2

142m

x 6

3mB

P A

pp

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mat

e V

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3

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le @

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00

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ck

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on

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ent

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at R

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n L

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63m

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icat

ive

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it c

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n.

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le @

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0

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tio

n p

lan

. S

cale

@ A

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1:2

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00

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oto

gra

ph

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03

. Fa

cin

g w

est

at

NS

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34

9 1

48

41

.

1

2

15

16

17

18

24

25

26

27

28

29

2

BP0

5

BP0

4

BP0

3

00.

51

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Kilo

met

ers

012

525

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.5

Met

ers

Stro

ng a

nd v

ery

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ng g

reen

ish

grey

th

inly

to

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kly

bedd

ed G

reyw

acke

w

ith

man

y in

terb

eds

of v

ery

wea

k to

m

ediu

m s

tron

g fis

sile

mud

ston

e /

silts

tone

.Pr

edom

inan

tly

part

ially

wea

ther

ed w

ith

surf

ace

disc

olou

ratio

n, a

nd d

estr

uctu

red

in p

lace

s w

ithin

the

mud

ston

e /

silts

tone

in

terb

eds.

Fra

ctur

es a

re p

redo

min

antly

bedd

ing

rela

ted,

sub

hori

zont

al a

ndsu

bver

tica

l, cl

ose

occa

sion

ally

med

ium

spac

ed p

lana

r, sm

ooth

. Jo

int

frac

ture

s pr

esen

t at

sub

horizo

ntal

and

sub

vert

ical

, ve

ry c

lose

to

med

ium

spa

ced,

pla

nar,

undu

lose

and

ste

pped

, sm

ooth

and

rou

gh.

See

Figu

re 4

.1.1

for

bed

rock

geo

logy

an

d lo

cation

ove

rvie

w.

Thin

sup

erfic

ial c

over

age

with

over

burd

en

of 0

.2m

.

Loca

ted

in t

he w

est

of t

he s

ite,

withi

n a

defo

rest

ed a

rea

adja

cent

to a

n ex

isting

for

est

trac

k. T

his

loca

tion

mak

es u

se o

f an

exi

stin

g bo

rrow

pit

appr

oxim

atle

y 30

m in

leng

th a

ssum

edto

hav

e lo

cally

sup

plie

d ag

greg

ate

for

the

fore

st r

oads

, w

hich

app

ear

to b

eco

nstr

ucte

d of

the

sam

e m

ater

ial.

The

mai

n ax

is w

ould

be

nort

h-w

est

and

sout

h-ea

st.

Dig

ging

/

Rip

ping

/ H

amm

er /

Bla

stin

g

Indi

cativ

e de

sign

onl

y. D

etai

led

desi

gn w

ill

requ

ire

grou

nd in

vest

igat

ion

to d

eter

min

ero

ckhe

ad,

char

acte

rise

roc

k m

ass,

gr

ound

wat

er a

nd a

sses

s sl

ope

stab

ility

par

amet

ers

and

drai

nage

.Bor

row

Pit

base

will

be

slop

ed t

o al

low

for

free

dra

inag

e.

Cro

ss S

ecti

on

*Pea

t de

pths

(m

) re

pres

ente

d by

tria

ngle

s.

E

A

A

B

B

Gra

de 2

m f

rom

top

of

back

fac

eat

1:2

, to

be

revi

ewed

at

deta

iled

desi

gn Peri

met

er d

itch

to b

e in

stal

led

to in

terc

ept

surf

ace

run-

off

Page 22: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

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# *# *

# *

# *

# *

# *# *

# *

# *# *# * # * # *# *

0.1

0.3

0.20.

10.1

0.4

0.4

0.3

0.2

0.3

0.3

0.3

0.3 0.2

0.30.

1

BP0

4

© C

row

n co

pyri

ght

and

data

base

rig

hts

2017

Ord

nanc

e Sur

vey

0100

0316

73

Dra

wn

By -

AS,

Rev

iew

ed B

y -

SB,

Dat

e 10

/04/

2017

ESo

urce

:BG

S

No

rth

Lo

wth

er

En

erg

y In

itia

tive

Fig

ure

4.1

.2d

In

dic

ativ

e B

orro

wP

it D

esig

n -

BP

04

Furt

he

r In

form

ati

on

:

Bo

rro

w P

it I

D:

Nat

ion

al G

rid

Ref

:

BP

No

min

al F

oo

tpri

nt

Dim

ensi

on

s:

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Fo

otp

rin

t A

rea:

Pre

do

min

an

t Li

tho

log

y

Terr

ain

:

Exca

vati

on

Req

uir

ed:

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4

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164

1445

4,74

5m2

62m

x 7

7.5m

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ging

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ippi

ng /

Ham

mer

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00

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el

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on

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ent

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ewed

at

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iled

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gn Peri

met

er d

itch

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e in

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to in

terc

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ace

run-

off

Ind

icat

ive

Pe

at R

est

ora

tio

n L

eve

l (1

m)

56m

7.5m

7.5m

3m

3m

3m

3.7m

Ind

icat

ive

bo

rro

w p

it c

ross

sec

tio

n.

Sca

le @

A3

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:40

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n p

lan

. S

cale

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3:

1:2

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00

Ph

oto

gra

ph

of

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04

. Fa

cin

g w

est

at

NS

81

63

9 1

44

56

.

1

2

3

15

16

17

182

5

26

2728

4

2

BP0

5

BP0

4

BP0

3

00.

51

0.25

Kilo

met

ers

012

525

062

.5

Met

ers

Stro

ng g

rey

Gre

ywac

ke w

ith o

ccas

iona

lba

nds

of v

ery

wea

k th

inly

lam

inat

ed

mud

ston

e /

silts

tone

. Pa

rtia

lly w

eath

ered

with

surf

ace

disc

olou

ration

, an

d de

stru

ctur

ed in

pla

ces

withi

n th

e m

udst

one/

siltst

one

inte

rbed

s. F

ract

ures

are

pr

edom

inan

tly b

eddi

ng r

elat

ed,

subh

oriz

onta

l and

sub

vert

ical

, cl

ose

and

med

ium

spa

ced,

pla

nar,

smoo

th.

Join

tfr

actu

res

pres

ent

as s

ubho

rizo

ntal

and

subv

ertica

l, ve

ry c

lose

to

med

ium

spa

ced,

pl

anar

, un

dulo

se a

nd s

tepp

ed,

smoo

th a

ndro

ugh.

See

Figu

re 4

.1.1

for

bed

rock

geo

logy

an

d lo

cation

ove

rvie

w.

Thin

sup

erfic

ial c

over

age

with

over

burd

en

of 0

.17m

.

Loca

ted

in t

he w

est

of t

he s

ite,

withi

n a

defo

rest

ed a

rea

adja

cent

to a

n ex

isting

for

est

trac

k. T

he m

ain

axis

wou

ld b

e no

rth

to s

outh

.

E

Indi

cativ

e de

sign

onl

y. D

etai

led

desi

gn w

ill

requ

ire

grou

nd in

vest

igat

ion

to d

eter

min

ero

ckhe

ad,

char

acte

rise

roc

k m

ass,

gr

ound

wat

er a

nd a

sses

s sl

ope

stab

ility

par

amet

ers

and

drai

nage

.

Bor

row

Pit

base

will

be

slop

ed t

o al

low

for

free

dra

inag

e.

*Pea

t de

pths

(m

) re

pres

ente

d by

tria

ngle

s.

Cro

ss S

ecti

on

A

A

B

B

Gra

de 2

m f

rom

top

of

back

fac

eat

1:2

, to

be

revi

ewed

at

deta

iled

desi

gn

Page 23: North Lowther Energy Initiative: Appendix 4.1 Borrow Pit … · 2019. 9. 18. · North Lowther Energy Initiative Borrow Pit Assessment 2 3 Desk Study 3.1 Geology The drift and solid

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# *

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# *

# *

# *

# *

# *

# *

# *# *

# *

# *

# *

# *

# *

# * # *

# *

# *

# *

# *

# *

# *

# *

# *

# *

# *

# * # *# *

# *

# * # * # *

# *

# *# *

# *# *

# *

# *

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# *

0.4

0.3

0.2

0.2 0.

1

0.3

0.1

0.4

0.3

0.1

0.010.

1

0.2

0.3

0.5

0.5

0.2

0.4

0.1

0.2

0.3

0.4

0.4

0.1

0.20.2

0.3

0.3

0.5

0.5

0.2

0.3

0.3

0.4 0.3

0.3

0.2

0.7

0.3

0.10.

2

0.6

0.6

0.1

0.4

0.3

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2

BP0

5

© C

row

n co

pyri

ght

and

data

base

rig

hts

2017

Ord

nanc

e Sur

vey

0100

0316

73

Dra

wn

By -

AS,

Rev

iew

ed B

y -

SB,

Dat

e 10

/04/

2017

ESo

urce

: BG

S

No

rth

Lo

wth

er

En

erg

y In

itia

tive

Fig

ure

4.1

.2e

Ind

icat

ive

Bo

rro

wP

it D

esig

n -

BP

05

Furt

he

r In

form

ati

on

:

Bo

rro

w P

it I

D:

Nat

ion

al G

rid

Ref

:

BP

No

min

al F

oo

tpri

nt

Dim

ensi

on

s:

BP

Fo

otp

rin

t A

rea:

Pre

do

min

an

t Li

tho

log

y

Terr

ain

:

Exca

vati

on

Req

uir

ed:

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5

NS 8

195

1360

5,60

3m2

61.5

m x

107

m

Dig

ging

/ R

ippi

ng /

Ham

mer

/ B

last

ing

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Ap

pro

xim

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00

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el

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on

Ext

ent

Ind

icat

ive

Pe

at R

est

ora

tio

n L

eve

l (1

m)

55.5

m

7.5m

3m

4.8m

3m

61.5

m

Ind

icat

ive

bo

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w p

it c

ross

sec

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n.

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le @

A3

: 1

:35

0

Loca

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n p

lan

. S

cale

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3:

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00

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oto

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05

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g s

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th w

est

at N

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19

73

13

67

8.

1

2

3

4

56

15

16

17

18

19

25

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4

2

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5

BP0

4

BP0

3

00.

51

0.25

Kilo

met

ers

012

525

062

.5

Met

ers

Med

ium

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ong

and

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ng g

reen

ish

grey

Gre

ywac

ke w

ith o

ccas

iona

lba

nds

of v

ery

wea

k th

inly

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inat

edm

udst

one

/ si

ltsto

ne 0

.1m

to

0.6m

thic

k. P

artial

ly w

eath

ered

with

surf

ace

disc

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ratio

n an

dde

stru

ctur

ed in

pla

ces

withi

n th

e m

udst

one

/ si

ltsto

ne in

terb

eds.

Fr

actu

res

are

pred

omin

antly

bedd

ing

rela

ted,

sub

hori

zont

al a

ndsu

bver

tica

l, cl

osel

y an

d ve

ry c

lose

lysp

aced

, pl

anar

, un

dulo

se a

nd s

tepp

edsm

ooth

and

rou

gh.

See

Figu

re 4

.1.1

for

bed

rock

geo

logy

an

d lo

cation

ove

rvie

w.

Supe

rfic

ial c

over

gae

with

ove

rbur

den

of 0

.25m

.

Loca

ted

in t

he w

est

of t

he s

ite,

withi

n a

defo

rest

ed a

rea

adja

cent

to

an

exis

ting

for

est

trac

k. T

he m

ain

axis

wou

ld b

e no

rth

east

and

sou

th w

est.

Indi

cativ

e de

sign

onl

y. D

etai

led

desi

gn w

ill

requ

ire

grou

nd in

vest

igat

ion

to d

eter

min

ero

ckhe

ad,

char

acte

rise

roc

k m

ass,

gr

ound

wat

er a

nd a

sses

s sl

ope

stab

ility

par

amet

ers

and

drai

nage

.

Bor

row

Pit

base

will

be

slop

ed t

o al

low

for

free

dra

inag

e.

*Pea

t de

pths

(m

) re

pres

ente

d by

tria

ngle

s.

E

Cro

ss S

ecti

on

A

A

BB

Gra

de 2

m f

rom

top

of

back

fac

eat

1:2

, to

be

revi

ewed

at

deta

iled

desi

gn Peri

met

er d

itch

to b

e in

stal

led

to in

terc

ept

surf

ace

run-

off