= _Introduction_
== title_level2
In this report, we will explore the
various factors that influence fluid
dynamics in glaciers and how they
contribute to the formation and
behaviour of these natural structures.
+ list1
  - sublist1
  - sublist2
+ list2
  - Glaciers as the one shown in @glaciers will cease to exist if we don't take action soon!
#figure(
  image("test.png", width: 70%),
  caption: [
    _Glaciers_ form an important part
    of the earth's climate system.
  ],
)<glaciers>

= Methods
We follow the MER models
established in @van2019capsulenet.

#bibliography("test.bib")

The equation $Q = rho A v + C$ defines the glacier flow rate.

The flow rate of a glacier is
defined by the following equation:

$ Q = rho A v + C $

The flow rate of a glacier is given
by the following equation:

$ Q = rho A v + "time offset" $

Total displaced soil by glacial flow:

$ 7.32 beta +
  sum_(i=0)^nabla Q_i / 2 $

Total displaced soil by glacial flow:

$ 7.32 beta +
  sum_(i=0)^nabla
    (Q_i (a_i - epsilon)) / 2 $


$ v := vec(x_1, x_2, x_3) $

$ a arrow.squiggly b $

